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monsoon

monsoon

monsoon Sentence Examples

  • It is to be noted that the climate of the islands of the Pacific becomes more and more healthy the farther they are from the monsoon region.

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  • There are two seasons of rainfall over the province: the monsoon season, when supplies of moisture are brought up by the ocean winds from the Arabian Sea and the Bay of Bengal; and the winter season, when storms advancing eastwards from Persia and the Caspian districts occasion winds, widespread rain and snowfall.

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  • The wet season, lasting during the prevalence of the south-west monsoon, from April to December, is clearly defined on the Pacific slope.

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  • Tibet is affected by the south-west monsoon, just as the Pamirs are affected, but in varying degrees according to geographical position.

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  • Tibet is affected by the south-west monsoon, just as the Pamirs are affected, but in varying degrees according to geographical position.

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  • The wet season - May to October - corresponds with the prevalence of the south-west monsoon in the Bay of Bengal.

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  • The south-west monsoon does not generally extend, in its character of a south-west wind, over the land.

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  • The south-west monsoon does not generally extend, in its character of a south-west wind, over the land.

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  • In the two years 1899 and 1900 the monsoon was very weak, the result being a severe famine which caused great mortality among the Bhil population.

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  • At this period an exact knowledge of the depths of the ocean off after the beginning of the south-west monsoon to a minimum assumed an unlooked-for practical importance from the daring in August, the total range being 92 in.

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  • The northwest monsoon, beginning in October and lasting till March, brings the principal rainy season in the archipelago.

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  • The cool season begins with the commencement of the north-east monsoon in the China Sea in November.

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  • This appears to be about the northern limit reached by the south-west monsoon, which from June to September brings a fairly abundant rainfall to the Yemen highlands, though the Tehama remains almost entirely rainless.

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  • On the Swahili coast the south-east monsoon begins in April and the northeast monsoon in November.

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  • The slopes of the plateau which face the rain-bringing monsoon are in some places covered with primeval forest, in which timber is plentiful.

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  • and in May at the end of the north-east monsoon, and a rapid falling io S.

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  • per annum, and that of the east coast, where the north-east monsoon breaks with all its fury, is usually about 1 55 in.

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  • The characteristic feature of the south-western Pacific is therefore the relatively low pressure and the existence of a true monsoon region in the middle of the tradewind belt.

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  • The surface currents of the Pacific have not been studied in the same detail as those of the Atlantic, and their seasonal variations Circulation are little known except in the monsoon regions.

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  • Dobbo, on a small western island, is the chief place; its resident population is reinforced annually, at the time of the west monsoon, by traders from that quarter, who deal in the tripang, pearl shell, tortoise-shell, and other produce of the islands.

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  • The south-westerly winds which prevail north of the equator during the hot half of the year, to which navigators have given the name of the south-west monsoon (the latter word being a corruption of the Indian name for season), arise from the great diminution of atmospheric pressure over Asia, which begins to be strongly marked with the great rise of temperature in April and May, and the simultaneous relatively higher pressure over the equator and the regions south of it.

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  • In the monsoon regions the half-yearly change from on-shore to off-shore winds produces noticeable differences in XIX.

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  • In Annam the rainy season begins during September and lasts for three or four months, corresponding with the northeast monsoon and also with a period of typhoons.

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  • The diurnal mountain winds are very strongly marked on the Himalaya, where they probably are the most active agents in determining the precipitation of rain along the chain - the monsoon currents, as before stated, not penetrating among the mountains.

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  • along the parallel of 33° N., and arrests the monsoon currents), is subject to much the same climatic influences as the eastern Himalaya.

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  • Within the southern monsoon region there is a gradual transition to the northwest monsoon of New Guinea in low latitudes, and in higher latitudes to the north-east wind of the Queensland coast.

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  • The southwest monsoon which brings rain in Cochin-China coincides with the dry season in Annam, the reason probably being that the mountains and lofty plateaus separating the two countries retain the precipitation.

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  • The southwest monsoon which brings rain in Cochin-China coincides with the dry season in Annam, the reason probably being that the mountains and lofty plateaus separating the two countries retain the precipitation.

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  • The influence of the monsoon is greatly moderated before it reaches this region, and the rains sometimes fail altogether.

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  • Its mountains are insufficient in elevation and extent to attract their full share of the monsoon rains, which fall so abundantly on the Abyssinian highlands on the other side of the Red Sea; for this reason Arabia has neither lakes nor forests to control the water-supply and prevent its too rapid dissipation, and the rivers are mere torrent beds sweeping down occasionally in heavy floods, but otherwise dry.

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  • Sea-snakes occasionally make their way to Japan, being cairied thither by the Black Current (Kuro Shiwo) and the monsoon, but they must be regarded as merely fortuitous visitors.

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  • The Equatorial CounterCurrent flowing eastwards is largely assisted during the latter half of the year by the south-west monsoon, and from July to October the south-west winds prevailing east of 150° E.

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  • The most striking general fact as regards climate in the archipelago is that wherever that part of the south-east monsoon which has passed over Australia strikes, the climate is comparatively dry, and the vegetation is less luxuriant.

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  • The most striking general fact as regards climate in the archipelago is that wherever that part of the south-east monsoon which has passed over Australia strikes, the climate is comparatively dry, and the vegetation is less luxuriant.

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  • Owing to its tropical situation and its almost entire dependence upon the monsoon rains, India is more liable than any other country in the world to crop failures, which upon occasion deepen into famine.

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  • Owing to its tropical situation and its almost entire dependence upon the monsoon rains, India is more liable than any other country in the world to crop failures, which upon occasion deepen into famine.

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  • During the southwest monsoon, from the middle of April to the middle of October, rain falls daily and the temperature varies between 85° and 95°.

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  • During the south-west monsoon this last branch is reversed, and the surface waters of the China Sea probably unite with the Kuro Siwo.

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  • This diminution of pressure, which continues as the heat increases till it reaches its maximum in July soon after the solstice, is followed by the corresponding development of the south-west monsoon; and as the barometric pressure is gradually restored, and becomes equalized within the tropics soon after the equinox in October, with the general fall of temperature north of the equator, the south-west winds fall off, and are succeeded by a north-east monsoon, which is developed during the winter months by the relatively greater atmospheric pressure which then occurs over Asia, as compared with the equatorial region.

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  • The people depend so entirely upon agriculture, and the harvest is so entirely destroyed by a single monsoon failure, that wherever a total failure occurs the landless labourer is immediately thrown out of work and remains out of work for the whole year.

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  • In the South Pacific the northwest monsoon of Australia affects a belt running east of New Guinea to the Solomon Islands.

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  • A great part of the land-forces had been already sent off under Craterus in the earlier summer to return west by Kandahar and Seistan; the fleet was to sail under the Greek Nearchus from the Indus mouth with the winter monsoon; Alexander himself with the rest of the land-forces set out in October to go by the 2 Beside V.

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  • As to cost, one transatlantic cable repair cost 75,000; the repair of the Aden-Bombay cable, broken in a depth of 1900 fathoms, was effected with the expenditure of 176 miles of new cable, and after a lapse of 251 days, 103 being spent in actual work, which for the remainder of the time was interrupted by the monsoon; a repair of the Lisbon-Porthcurnow cable, broken in the Bay of Biscay in 2700 fathoms, eleven years after the cable was laid, took 215 days, with an expenditure of 300 miles of cable.

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  • Thus the south-west monsoon begins in the Arabian Sea with west and north-westerly winds,which draw round as the year advances to south-west and fall back again in the autumn by northwest to north.

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  • Thus the south-west monsoon begins in the Arabian Sea with west and north-westerly winds,which draw round as the year advances to south-west and fall back again in the autumn by northwest to north.

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  • During the monsoon the climate is very damp, and at times even cold and raw, thick clouds and mist enveloping the sky for many days together.

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  • The warmed air of summer produces an area of low pressure in the west-central United States, which interrupts the belt of high pressure that planetary conditions alone would form around the earth about latitude 30; hence there is a tendency of the summer winds to blow inward from the northern Pacific over the Cordilleras toward the continental centre, and from the trades of the torrid Atlantic up the Mississippi Valley; conversely in winter time, the cold air over the lands produces a large area of high pressure from which the winds tend to flow outward; thus repelling the westerly winds of the northern Pacific and greatly intensifying the outflow southward to the Gulf of Mexico and eastward to the Atlantic. As a result of these seasonal alternations of temperature and pressure there is something of a monsoon tendency developed in the winds of the Mississippi Valley, southerly infiowing winds prevailing in summer and northerly outfiowing winds in winter; but the general tendency to inflow and outflow is greatly modified by the relief of the lands, to which we next turn.

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  • The rainfall of the province is considerably heavier than in northern India, and the result of this is a cooler and more pleasant atmosphere during the monsoon season.

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  • Rain comes with the south-east monsoon, and on the northern part of the coast the rainy season is divided into two parts, the great and the little Masika: the former falls in the months of September, October, November; the latter in February and March.

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  • Rain comes with the south-east monsoon, and on the northern part of the coast the rainy season is divided into two parts, the great and the little Masika: the former falls in the months of September, October, November; the latter in February and March.

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  • These, like the mollusca, indicate the influence of the Kuro Shiwo and the south-west monsoon, for they have close affinity with species found in the Indian and Pacific Oceans.

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  • In the Bay of Bengal the strength of the southwest monsoon is rather from the south and south-east, being succeeded by north-east winds after October, which give place to northerly and north-westerly winds as the year advances.

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  • Except in the east of the Pacific, the south-east trade is only fully developed during the southern winter; at other seasons the regular trade-belt is cut across from north-west to south-east by a band twenty to thirty degrees wide, in which the trades alternate with winds from north-east and north, and with calms, the calms prevailing chiefly at the boundary of the monsoon region (5° N.-15° S., 160°-185° E.).

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  • On reaching the western Pacific part of this current passes southwards, east of New Zealand, and again east of Australia, as the East Australian Current, part northwards to join the Equatorial CounterCurrent, and during the north-east monsoon part makes its way through the China Sea towards the Indian Ocean.

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  • On the east coast the force of the north-east monsoon, which beats upon the shores of the China Sea annually from November to February, has kept the land for the most part free from mangroves, and the sands, broken here and there by rocky headlands thickly wooded, and fringed by casuarina trees, stretch for miles without interruption.

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  • The full force of the monsoon is, however, broken by the western frontier hills; and while the rainfall at Mergui is over 180, and at Moulmein 240 in., that of Bangkok seldom exceeds 54, and Chiengmai records an average of about 42 in.

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  • Four seasons are recognized - January - April, very dry and great heat; May - June, cooler and the " heavy " rains; July - September, the season of extreme heat and the south-west monsoon; October - December, the " light " rains.

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  • On the northern shore of Hong-Kong there is a patent slip at East or Matheson Point, which is serviceable during the north-east monsoon, when sailing vessels frequently approach Victoria through the Ly-ee-mun Pass.

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  • In winter, for example, when the northern monsoon begins to blow, numbers of denizens of the Sea of Okhotsk swim southward to the more genial waters of north Japan; and in summer the Indian Ocean and the Malayan archipelago send to her southern coasts a crowd of emigrants which turn homeward again at the approach of winter.

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  • The flora of Siberia presents very great local varieties, not only on account of the diversity of physical characteristics, but also in consequence of the intrusion of new species from the neighbouring regions, as widely different as the arctic littoral, the arid steppes of Central Asia, and the wet monsoon regions of the Pacific littoral.

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  • of Aden, the summer heat is tempered by the monsoon winds, and the seasonal variation of temperature is less marked.

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  • Abandoned since 495 - for Kasyapa was eventually slain during a battle fought in the plain beneath - it has, on the whole, well withstood the fury of tropical storms, and is now used again to gain access to the top. When rediscovered by Major Forbes in 1835 the portions of the gallery where it had been exposed for so many centuries to the south-west monsoon, had been carried away.

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  • The north-west coast, particularly the portions north of Cambridge Gulf and the shores of the Gulf of Carpentaria, are favoured with an annual visitation of the monsoon from December to March, penetrating as far as Soo m.

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  • to be the fall at Peking; while at Canton, which lies nearly on the northern tropic and the region of the south-west monsoon is entered, the quantity is increased to 78 in.

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  • During the north-east monsoon, from the middle of October to the middle of April, dry weather prevails and the thermometer averages from 77° to 80° F.

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  • Throughout the whole of the moister parts of the province the agricultural season is the wet period of the south-west monsoon, lasting from the middle of May until November.

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  • The cessation of the rains on the southern border of Baluchistan, west of Karachi, obviously arises from the projection of the south-east coast of Arabia, which limits the breadth of the south-west monsoon air current and the length of the coast-line directly exposed to it.

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  • The cessation of the rains on the southern border of Baluchistan, west of Karachi, obviously arises from the projection of the south-east coast of Arabia, which limits the breadth of the south-west monsoon air current and the length of the coast-line directly exposed to it.

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  • During the south-west (summer) monsoon great quantities (67 in.) of rain fall, especially in July and August.

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  • The heated body of air carried from the Indian Ocean over southern Asia by the south-west monsoon comes up highly charged with watery vapour, and hence in a condition to release a large body of water as rain upon the land, whenever it is brought into circumstances which reduce its temperature in a notable degree.

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  • More like a monsoon.

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  • The wet season, during which heavy rain falls almost daily, lasts from April to October, coinciding with the south-west monsoon.

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  • On the east coast the principal streams are the Petani, Telubin, Kelantan, Besut, Trengganu, Dungun, Kmamun, Kuantan, Pahang, Rompin, Endau and Sedeli, all guarded by difficult bars at their mouths, and dangerous during the continuance of the north-east monsoon.

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  • They occur in all the hot months, from June to October, and more rarely in November, and appear to be originated by adverse currents from the north meeting those of the south-west monsoon.

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  • Practically an outlying suburb of Victoria, Kowloon or (Nine Dragons) is free from the extreme heat of the capital, being exposed to the south-west monsoon.

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  • It is remarkable that the dry season (October to April) is coincident with the period of the west monsoon.

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  • For this reason the up-welling coastal water is coldest close to the shore, and hence it only appears on the Somali coast during the south-west monsoon.

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  • Though he had no port in which to refit and no ally save Hyder Ali, he kept the sea and did not even return to the French islands during the north-easterly monsoon.

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  • All the western region is but slightly affected by the monsoon.

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  • The north-east monsoon, which lasts from October till April, is exceedingly violent for three months after its commencement.

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  • In the distribution of the rainfall, as dependent on the direction of the winds, the following parts of Sumatra must be distinguished: (r) south-east Sumatra, on which, as on Banka and Billiton, the heaviest rainfall occurs during the north-west monsoon, the annual volume of rainfall increasing from 98.4 in.

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  • by the south-east monsoon.

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  • Here, too, the prevailing rainfall is brought by the north-west monsoon, but in this belt its prevalence is not so pronounced, Padang getting 94 in.

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  • of rain during the north-west monsoon, against 90 in.

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  • Desert conditions also arise from local causes, as in the case of the Indian desert situated in a region inaccessible to either of the two main branches of the south-west monsoon.

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  • could approach no nearer than two miles to the shore, where typhoons of the southwest monsoon not infrequently obliged them to lie several days before they could be unloaded.

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  • In the monsoon the Cochin backwaters are broad navigable channels and lakes; in the hot weather they contract into shallows in many places not 2 ft.

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  • He holds the opinion that the tea-plant is indigenous, not to Assam only, but to the whole monsoon region of eastern Asia, where he found it growing wild as far north as the islands of southern Japan.

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  • In the deltas of southern India irrigation is only practised during the monsoon season.

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  • The Godaveri, Kistna and Kaveri all take their rise on the Western Ghats, a region where the rainfall is never known to fail in the monsoon season.

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  • For this monsoon irrigation there is always abundance of water, and so long as the canals and sluices are kept in repair, there is little trouble in distributing it over the fields.

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  • But to keep sugar-cane, or indigo, or cotton alive in summer before the monsoon sets in in India or the Nile rises in Egypt the field should be watered every ten days or fortnight, while rice requires a constant supply of water passing over it.

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  • In addition to these great perennial canals, much has been done since 1878 in enlarging and extending what are known as the " inundation canals " of the Punjab, which utilize the flood waters in the rivers during the monsoon season and are dry at other times.

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  • monsoon, which is marked at Muscat, is scarcely noticeable in the Persian Gulf proper, though recent upperair investigations conducted at Bagdad give some reason to think that the effects of the monsoon can be observed even there.

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  • On this side of the island there are but one or two possible anchoring grounds, and these only during the north-east monsoon.

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  • During this season the rivers, which are roaring torrents throughout the monsoon, are almost all lost in the dry, absorbent plains.

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  • monsoon in India, beating along the southern slopes of the Himalaya, travel up the Kabul valley as far as Laghman, though they are more clearly felt in Bajour and Panjkora, under the high spurs of the Hindu Kush, and in the eastern branches of Safed Koh.

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  • South of this the Suliman mountains may be taken as the western limit of the monsoon's action.

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  • In the absence of monsoon influences there are steadier weather indications than in India.

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  • On its eastern margin, however, in the neighbourhood of the Aravalli hills, and again in the northern Punjab, rain is more frequent, occurring both in the south-west monsoon and also at the opposite season in the cold weather.

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  • Up or down this plain, at opposite seasons, sweep the monsoon winds, in a direction at right angles to that of their nominal course; and thus vapour which has been brought by winds from the Bay of Bengal is discharged as snow and rain on the peaks and hillsides of the Western Himalayas.

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  • Together with the two parallel valleys of the Nerbudda and Tapti, which drain the flanks of its western half, it gives, at opposite seasons of the year, a decided easterly and westerly direction to the winds of this part of India, and condenses a tolerably copious rainfall during the south-west monsoon.

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  • At Ajmer, an old meteorological station at the eastern foot of the range, the wind is predominantly south-west, and there and at Mount Abu the south-west monsoon rains are a regularly recurrent phenomenon, - which can hardly be said of the region of scanty and uncertain rainfall that extends from the western foot of the range and merges in the Bikaner desert.

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  • This plateau is swept by the south-west monsoon, but not until it has surmounted the western barrier of the Ghats; and hence the rainfall is, as a rule, light at Poona and places similarly situated under the lee of the range, and but moderate over the more easterly parts of the plateau.

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  • The country to the east of the gap receives the rainfall of the south-west monsoon; and during the north-east monsoon ships passing Beypur meet with a stronger wind from the land than is felt elsewhere on the Malabar coast.

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  • In Lower Burma the western face of the Arakan Yoma hills, like that of the Western Ghats in India, is exposed to the full force of the south-western monsoon, and receives a very heavy rainfall.

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  • The continental type of weather prevails over almost the whole of India from December to May, and the oceanic type from June to November, thus giving rise to the two great divisions of the year, the dry season or north-east monsoon, and the rainy season or south-west monsoon.

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  • India thus becomes the type of a tropical monsoon climate.

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  • For the origin of the monsoon currents and their distribution see Monsoon.

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  • The two monsoon periods are divided by the change of temperature, due to solar action' upon the earth's surface, into two separate seasons; and thus the Indian year may be divided into four seasons: the cold season, including the months of January and February; the hot season, comprising the months of March, April and May; the south-west monsoon period, including the months of June, July, August, September and October; and the retreating monsoon period, including the months of November and December.

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  • The south-west monsoon currents usually set in during the first fortnight of June on the Bombay and Bengal coasts, and give more The or less general rain in every part of India during the next three months.

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  • The Bombay monsoon, after surmounting the Ghats, blows across the peninsula as a west and sometimes in places a north-west wind; but it leaves with very little rain a strip 100 to 200 m.

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  • Similarly the Bengal monsoon passes by the Coromandel coast and the Carnatic with an occasional shower, taking a larger volume to Masulipatam and Orissa, and abundant rain to Bengal, Assam and Cachar.

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  • In September the force of the monsoon begins rapidly to decline, and after about the middle of the month it ceases to carry rain to the greater part of north-western India.

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  • In its rear springs up a gentle steady north-east wind, which gradually extends over the Bay of Bengal, and is known as the north-east monsoon.

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  • The months of November and December form a transition period between the monsoon and the cold season.

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  • This excessive dependence upon a single industry, which is in its turn dependent upon the accident of the seasons, upon a favourable or unfavourable monsoon, has been held to be one of the main causes of the frequent famines which ravage India.

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  • In 5900 this district suffered severely from famine owing to the complete failure of the monsoon, and the cultivated area decreased by 50 or 60 70; but, on the whole, trade has improved of late years owing to the new railways, which have stimulated commerce and created fresh centres of industry.

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  • This zone falls within the regime of the summer monsoon rains, while those districts adjoining the coast zone enjoy also winter rains.

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  • Slight rain falls in the spring and abundant monsoon rains from June to September.

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  • The curve shows two rises, one at the beginning of winter, and the other at the commencement of the monsoon, and at both these times the people are driven indoors.

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  • This excessive rainfall is caused by the fact that Cherrapunji stands on the edge of the plateau overlooking the plains of Bengal, where it catches the full force of the monsoon as it rises from the sea.

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  • The rains of the south-east monsoon reach Central India as a rule about the 12th of July, and last until the end of September.

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  • 1 He gives a very accurate account of this forlorn tract, its general aridity and the necessity of obtaining water by digging in the beds of torrents; describes the food of the inhabitants as dates and fish; and adverts to the occasional occurrence of fertile spots, the abundance of aromatic and thorny shrubs and fragrant plants, and the violence of the monsoon in the western part of Makran.

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  • the period of the monsoon rains of India) the remainder of the year being comparatively dry.

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  • The condensation of vapour from the ascending currents and their gradual exhaustion as they are precipitated on successive ranges is very obvious in the cloud effects produced during the monsoon, the southern or windward face of each range being clothed day after day with a white crest of cloud whilst the northern slopes are often left entirely free.

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  • Command of the sea could not be maintained - least of all in the monsoon months - while the Portuguese fleets were based on Lisbon, which could only be reached after a six months' voyage; and experience had proved that almost every Portuguese factory required a fortress for its defence when the fleets were absent.

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  • April, May and June are hot; and the monsoon months from June to October are distinguished by damp heat and malaria.

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  • The approach of the south-west monsoon precluded the immediate renewal of the attempt; but hostilities were resumed, and Achin fell in January 1874.

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  • There were indications that monsoon influences extended as far north at least as the Great Pamir, and a definite analogy was established between the record of barometric pressure on the Pamirs and that of the outer ranges of the Himalaya.

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  • From May to August, the period of the south-east monsoon, the climate of Banka is dry and hot; but the mean annual rainfall reaches 120 in.

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  • The wet, cool season proper is from November to February, accompanying the north-west monsoon.

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  • The bamboos are a feature of tropical forest vegetation, especially in the monsoon region.

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  • But the rainy season proper, caused by the south-west monsoon, lasts from June to mid-September, and commencing in the north moves southward.

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  • The climate of Backergunje is one of the healthiest in Eastern Bengal, owing to the strong south-west monsoon, which comes up directly from the Bay of Bengal, and keeps the atmosphere cool; but the heavy rainfall and consequent humidity of the atmosphere, combined with the use of bad water, are fruitful sources of disease.

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  • The south-east monsoon blows from May to October, which is the dry season, and the west-north-west monsoon from December to March.

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  • Being exposed to the winter monsoon, the northern parts of the island enjoy much the same sort of temperate climate as the neighbouring provinces of the mainland, but in the southern parts, protected from the monsoon by the mountain ranges, the climate is almost or entirely tropical.

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  • The coast is rock-bound and difficult of access; and though it contains several bays forming fairweather ports for vessels engaged in the coasting trade, Bombay, Karachi-in-Sind, Marmagoa and Karwar alone have harbours sufficiently land-locked to protect shipping during the prevalence of the south-west monsoon.

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  • The Konkan is hot and moist, the fall of rain during the monsoon sometimes approaching 3 00 in.

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  • The south-west monsoon generally sets in about the first week in June, and pours down volumes of rain along the coast.

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  • From June to October travelling is difficult and unpleasant, except in Sind, where the monsoon rains exert little influence.

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  • The failure of the monsoon of 1896 caused widespread distress throughout the Deccan, over an area of 46,000 sq.

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  • In 1899 the monsoon again failed in Gujarat, where famine hitherto had been almost unknown; and the winter rains failed in the Deccan, so that distress gradually spread over almost the entire presidency.

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  • South of the belt salinity falls quickly as latitude increases, while to the north of it, in the monsoon region, the surface water is very fresh off the African coast and to the north-east.

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  • Probably the northern and north-eastern region, within the monsoon area, contains relatively fresh water down to very considerable depths.

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  • At the beginning of the reign it was supposed to be impossible to build a steamer which could either cross the Atlantic, or face the monsoon in the Red Sea.

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  • It was the beginning of September, and the expedition took advantage of the easterly monsoon, which carried them to Batavia.

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  • monsoon, the Jibal must be considered the most favoured district of Arabia.

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  • The south-west monsoon sweeps up the Nerbudda valley from Bombay and crossing the tableland at Neemuch gives copious supplies to Malwa, Jhalawar and Kotah and the countries which lie in the course of the Chambal river.

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  • It is only when the monsoon is in considerable force that Merwara gets a plentiful supply from it.

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  • The north-eastern monsoon sweeps up the valley of the Ganges from the Bay of Bengal and waters the northern part of Rajputana, but hardly penetrates farther west than the longitude of Ajmere.

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  • 2 In the interior of the country about the plain of Dhofar, 3 during the south-west monsoon, frankincense and other gums are gathered by the Beni Gurrah Bedouins, and might be obtained by them in much larger quantities; their lawlessness, however, and the lack of a safe place of exchange or sale are obstacles to the development of trade.

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  • The rainfall in the northern peninsula (north of the equator) differs from that of the southern; the former has rains (not caused by the monsoon), and of smaller amount, 102 in.

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  • annually; the latter has a greater rainfall, 157 in., brought by the north-western monsoon, and of which the west coast receives a much larger share than the east.

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  • More like a monsoon.

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  • But an unexpected return of warm monsoon weather hit, causing a massive avalanche.

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  • Spilling the contents of our slops bucket on my Monsoon skirt.

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  • This enhanced monsoon circulation is associated with enhanced precipitation over India.

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  • About Us Monsoon has developed a strong brand with a highly distinctive identity.

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  • drenched by the heavy monsoon rains.

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  • A long-standing sequence of disastrous famines in India led to one of the first investigations of just how the monsoon was generated.

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  • Across Asia an exceptionally early and heavy monsoon caused flash floods, landslides, and hailstorms.

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  • You know that in July 2004 Bangladesh experienced a devastating monsoon flood, it's worst ever.

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  • It was a very wet day, monsoon was in full throttle, and dumping gallons of water from the skies.

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  • However it is also during the monsoon that Goa is probably at its most beautiful, wit h greenery sprouting all around.

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  • Monsoon clouds are often likened to Krishna, finally arriving to quench the thirst of his lovers.

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  • Bless Monsoon for providing for the stage where the casual onlooker still has to wonder for a second if you have a flabby midriff.

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  • mm in 18 hours, which is more typical of a heavy monsoon storm in the Indian Sub-Continent.

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  • Monsoon on Line monsoon on Line Monsoon information, particularly on predicting monsoons.

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  • Annual precipitation at Zirahuén is dominated by the summer monsoon.

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  • April is the onset of the southwest monsoon over southern Somalia.

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  • Most rain, however, falls during the northeast monsoon (November to March ).

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  • The southwest monsoon is a gentler affair, bringing frequent rainfall to the west coast from July to September.

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  • The best time to visit is between November and March during the northeast monsoon when it is dry with very little wind.

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  • Therefore in August 1997, we started our first thematic web site concerned with the prediction of the Asian summer monsoon.

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  • The climate varies from tropical monsoon in the south to temperate in the north.

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  • monsoon rainfall over India.

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  • monsoon rain from March to November.

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  • monsoon season brings the feeling of fear, perhaps of flooding.

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  • monsoon circulation is associated with enhanced precipitation over India.

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  • monsoon showers, announced by the cry of the peacock, the birds begin their songs.

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  • monsoon clouds are often likened to Krishna, finally arriving to quench the thirst of his lovers.

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  • These PV values are often exceeded during the summer monsoon period.

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  • If you are considering a visit to the Himalayas post monsoon, please get in contact soon to book your place.

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  • The central coast north of Nha Trang has a similar climate with the winter monsoon bringing cool, wet weather between December and February.

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  • The northeast monsoon has the worst effect on mangrove communities.

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  • monsoon in the south to temperate in the north.

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  • For a much more interesting, moving, and'real ' look at contemporary marriage mores in India, watch Monsoon Wedding.

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  • PAKISTAN: Landslide kills 14 quake victims 25-07-2006 At least 14 earthquake survivors have been killed after monsoon rains triggered mudslides in northern Pakistan.

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  • northeast monsoon (November to March ).

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  • precursory signals is not negligible and appears to be important in the early part of the monsoon season.

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  • The monsoon ragas are defined by various characteristics, all inspired by the personality of the rain.

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  • During the period June to September there is a light monsoon rain in Salalah.

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  • The present skill of the model does not allow a quantitative forecast of the monsoon rainfall over India.

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  • The weather was very pleasant in December although slightly humid and during the second week we did have several monsoon rainstorms.

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  • However, it is prone to serious flooding during the monsoon season of June to September.

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  • To say nothing of the times we brought unseasonal sleet to midsummer Norway and the monsoon to Cheshire.

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  • southwest monsoon over southern Somalia.

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  • subtropical monsoon climate.

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  • In India, the seasonal forecast of monsoon rainfall has traditionally been issued using a number of statistical techniques (see Kumar et al.

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  • temperate in the north to tropical monsoon in the south.

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  • westerlyng Asian summer monsoon is preceded by weak upper tropospheric westerlies over south Asia and vise versa.

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  • The wet season, during which heavy rain falls almost daily, lasts from April to October, coinciding with the south-west monsoon.

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  • A great part of the land-forces had been already sent off under Craterus in the earlier summer to return west by Kandahar and Seistan; the fleet was to sail under the Greek Nearchus from the Indus mouth with the winter monsoon; Alexander himself with the rest of the land-forces set out in October to go by the 2 Beside V.

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  • The north-west coast, particularly the portions north of Cambridge Gulf and the shores of the Gulf of Carpentaria, are favoured with an annual visitation of the monsoon from December to March, penetrating as far as Soo m.

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  • On the east coast the force of the north-east monsoon, which beats upon the shores of the China Sea annually from November to February, has kept the land for the most part free from mangroves, and the sands, broken here and there by rocky headlands thickly wooded, and fringed by casuarina trees, stretch for miles without interruption.

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  • On the east coast the principal streams are the Petani, Telubin, Kelantan, Besut, Trengganu, Dungun, Kmamun, Kuantan, Pahang, Rompin, Endau and Sedeli, all guarded by difficult bars at their mouths, and dangerous during the continuance of the north-east monsoon.

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  • per annum, and that of the east coast, where the north-east monsoon breaks with all its fury, is usually about 1 55 in.

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  • As to cost, one transatlantic cable repair cost 75,000; the repair of the Aden-Bombay cable, broken in a depth of 1900 fathoms, was effected with the expenditure of 176 miles of new cable, and after a lapse of 251 days, 103 being spent in actual work, which for the remainder of the time was interrupted by the monsoon; a repair of the Lisbon-Porthcurnow cable, broken in the Bay of Biscay in 2700 fathoms, eleven years after the cable was laid, took 215 days, with an expenditure of 300 miles of cable.

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  • It is warm always, but tempered by pleasant sea-breezes; very hot when the sun is northing; irregular rainfall, but usually dry during the north-east, and very wet during the south-west monsoon.

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  • The south-westerly winds which prevail north of the equator during the hot half of the year, to which navigators have given the name of the south-west monsoon (the latter word being a corruption of the Indian name for season), arise from the great diminution of atmospheric pressure over Asia, which begins to be strongly marked with the great rise of temperature in April and May, and the simultaneous relatively higher pressure over the equator and the regions south of it.

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  • This diminution of pressure, which continues as the heat increases till it reaches its maximum in July soon after the solstice, is followed by the corresponding development of the south-west monsoon; and as the barometric pressure is gradually restored, and becomes equalized within the tropics soon after the equinox in October, with the general fall of temperature north of the equator, the south-west winds fall off, and are succeeded by a north-east monsoon, which is developed during the winter months by the relatively greater atmospheric pressure which then occurs over Asia, as compared with the equatorial region.

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  • In the Bay of Bengal the strength of the southwest monsoon is rather from the south and south-east, being succeeded by north-east winds after October, which give place to northerly and north-westerly winds as the year advances.

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  • They occur in all the hot months, from June to October, and more rarely in November, and appear to be originated by adverse currents from the north meeting those of the south-west monsoon.

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  • The heated body of air carried from the Indian Ocean over southern Asia by the south-west monsoon comes up highly charged with watery vapour, and hence in a condition to release a large body of water as rain upon the land, whenever it is brought into circumstances which reduce its temperature in a notable degree.

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  • The diurnal mountain winds are very strongly marked on the Himalaya, where they probably are the most active agents in determining the precipitation of rain along the chain - the monsoon currents, as before stated, not penetrating among the mountains.

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  • to be the fall at Peking; while at Canton, which lies nearly on the northern tropic and the region of the south-west monsoon is entered, the quantity is increased to 78 in.

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  • The rainfall of the province is considerably heavier than in northern India, and the result of this is a cooler and more pleasant atmosphere during the monsoon season.

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  • Four seasons are recognized - January - April, very dry and great heat; May - June, cooler and the " heavy " rains; July - September, the season of extreme heat and the south-west monsoon; October - December, the " light " rains.

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  • During the north-east monsoon, from the middle of October to the middle of April, dry weather prevails and the thermometer averages from 77° to 80° F.

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  • During the southwest monsoon, from the middle of April to the middle of October, rain falls daily and the temperature varies between 85° and 95°.

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  • The flora of Siberia presents very great local varieties, not only on account of the diversity of physical characteristics, but also in consequence of the intrusion of new species from the neighbouring regions, as widely different as the arctic littoral, the arid steppes of Central Asia, and the wet monsoon regions of the Pacific littoral.

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  • The influence of the monsoon is greatly moderated before it reaches this region, and the rains sometimes fail altogether.

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  • In Annam the rainy season begins during September and lasts for three or four months, corresponding with the northeast monsoon and also with a period of typhoons.

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  • Throughout the whole of the moister parts of the province the agricultural season is the wet period of the south-west monsoon, lasting from the middle of May until November.

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  • Its mountains are insufficient in elevation and extent to attract their full share of the monsoon rains, which fall so abundantly on the Abyssinian highlands on the other side of the Red Sea; for this reason Arabia has neither lakes nor forests to control the water-supply and prevent its too rapid dissipation, and the rivers are mere torrent beds sweeping down occasionally in heavy floods, but otherwise dry.

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  • of Aden, the summer heat is tempered by the monsoon winds, and the seasonal variation of temperature is less marked.

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  • This appears to be about the northern limit reached by the south-west monsoon, which from June to September brings a fairly abundant rainfall to the Yemen highlands, though the Tehama remains almost entirely rainless.

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  • Dobbo, on a small western island, is the chief place; its resident population is reinforced annually, at the time of the west monsoon, by traders from that quarter, who deal in the tripang, pearl shell, tortoise-shell, and other produce of the islands.

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  • On the northern shore of Hong-Kong there is a patent slip at East or Matheson Point, which is serviceable during the north-east monsoon, when sailing vessels frequently approach Victoria through the Ly-ee-mun Pass.

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  • Practically an outlying suburb of Victoria, Kowloon or (Nine Dragons) is free from the extreme heat of the capital, being exposed to the south-west monsoon.

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  • Sea-snakes occasionally make their way to Japan, being cairied thither by the Black Current (Kuro Shiwo) and the monsoon, but they must be regarded as merely fortuitous visitors.

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  • In winter, for example, when the northern monsoon begins to blow, numbers of denizens of the Sea of Okhotsk swim southward to the more genial waters of north Japan; and in summer the Indian Ocean and the Malayan archipelago send to her southern coasts a crowd of emigrants which turn homeward again at the approach of winter.

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  • These, like the mollusca, indicate the influence of the Kuro Shiwo and the south-west monsoon, for they have close affinity with species found in the Indian and Pacific Oceans.

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  • It is remarkable that the dry season (October to April) is coincident with the period of the west monsoon.

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  • During the south-west (summer) monsoon great quantities (67 in.) of rain fall, especially in July and August.

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  • In the monsoon region, where the barometer rises o 38 in.

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  • In the monsoon regions the half-yearly change from on-shore to off-shore winds produces noticeable differences in XIX.

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  • and in May at the end of the north-east monsoon, and a rapid falling io S.

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  • At this period an exact knowledge of the depths of the ocean off after the beginning of the south-west monsoon to a minimum assumed an unlooked-for practical importance from the daring in August, the total range being 92 in.

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  • For this reason the up-welling coastal water is coldest close to the shore, and hence it only appears on the Somali coast during the south-west monsoon.

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  • During the monsoon the climate is very damp, and at times even cold and raw, thick clouds and mist enveloping the sky for many days together.

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  • On the Swahili coast the south-east monsoon begins in April and the northeast monsoon in November.

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  • The slopes of the plateau which face the rain-bringing monsoon are in some places covered with primeval forest, in which timber is plentiful.

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  • Abandoned since 495 - for Kasyapa was eventually slain during a battle fought in the plain beneath - it has, on the whole, well withstood the fury of tropical storms, and is now used again to gain access to the top. When rediscovered by Major Forbes in 1835 the portions of the gallery where it had been exposed for so many centuries to the south-west monsoon, had been carried away.

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  • Nautical improvements, and the discovery that the southwest monsoon (Hippalus) gave sure navigation at certain seasons, increased the connexion of the West with South Arabia, but also wrought such a change in the trade as involved a revolution in the state of that country.

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  • The wet season - May to October - corresponds with the prevalence of the south-west monsoon in the Bay of Bengal.

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  • The full force of the monsoon is, however, broken by the western frontier hills; and while the rainfall at Mergui is over 180, and at Moulmein 240 in., that of Bangkok seldom exceeds 54, and Chiengmai records an average of about 42 in.

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  • The cool season begins with the commencement of the north-east monsoon in the China Sea in November.

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  • The northwest monsoon, beginning in October and lasting till March, brings the principal rainy season in the archipelago.

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  • monsoon of southern Asia controls the prevailing winds, its influence extending eastwards to 145° E., near the Ladrones, and southwards to the equator.

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  • In the South Pacific the northwest monsoon of Australia affects a belt running east of New Guinea to the Solomon Islands.

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  • Except in the east of the Pacific, the south-east trade is only fully developed during the southern winter; at other seasons the regular trade-belt is cut across from north-west to south-east by a band twenty to thirty degrees wide, in which the trades alternate with winds from north-east and north, and with calms, the calms prevailing chiefly at the boundary of the monsoon region (5° N.-15° S., 160°-185° E.).

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  • Within the southern monsoon region there is a gradual transition to the northwest monsoon of New Guinea in low latitudes, and in higher latitudes to the north-east wind of the Queensland coast.

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  • The characteristic feature of the south-western Pacific is therefore the relatively low pressure and the existence of a true monsoon region in the middle of the tradewind belt.

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  • It is to be noted that the climate of the islands of the Pacific becomes more and more healthy the farther they are from the monsoon region.

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  • In the monsoon region relative humidity is high, viz.

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  • The surface currents of the Pacific have not been studied in the same detail as those of the Atlantic, and their seasonal variations Circulation are little known except in the monsoon regions.

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  • The Equatorial CounterCurrent flowing eastwards is largely assisted during the latter half of the year by the south-west monsoon, and from July to October the south-west winds prevailing east of 150° E.

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  • On reaching the western Pacific part of this current passes southwards, east of New Zealand, and again east of Australia, as the East Australian Current, part northwards to join the Equatorial CounterCurrent, and during the north-east monsoon part makes its way through the China Sea towards the Indian Ocean.

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  • During the south-west monsoon this last branch is reversed, and the surface waters of the China Sea probably unite with the Kuro Siwo.

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  • The wet season, lasting during the prevalence of the south-west monsoon, from April to December, is clearly defined on the Pacific slope.

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  • Though he had no port in which to refit and no ally save Hyder Ali, he kept the sea and did not even return to the French islands during the north-easterly monsoon.

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  • The warmed air of summer produces an area of low pressure in the west-central United States, which interrupts the belt of high pressure that planetary conditions alone would form around the earth about latitude 30; hence there is a tendency of the summer winds to blow inward from the northern Pacific over the Cordilleras toward the continental centre, and from the trades of the torrid Atlantic up the Mississippi Valley; conversely in winter time, the cold air over the lands produces a large area of high pressure from which the winds tend to flow outward; thus repelling the westerly winds of the northern Pacific and greatly intensifying the outflow southward to the Gulf of Mexico and eastward to the Atlantic. As a result of these seasonal alternations of temperature and pressure there is something of a monsoon tendency developed in the winds of the Mississippi Valley, southerly infiowing winds prevailing in summer and northerly outfiowing winds in winter; but the general tendency to inflow and outflow is greatly modified by the relief of the lands, to which we next turn.

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  • The people depend so entirely upon agriculture, and the harvest is so entirely destroyed by a single monsoon failure, that wherever a total failure occurs the landless labourer is immediately thrown out of work and remains out of work for the whole year.

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  • There are two seasons of rainfall over the province: the monsoon season, when supplies of moisture are brought up by the ocean winds from the Arabian Sea and the Bay of Bengal; and the winter season, when storms advancing eastwards from Persia and the Caspian districts occasion winds, widespread rain and snowfall.

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  • In the two years 1899 and 1900 the monsoon was very weak, the result being a severe famine which caused great mortality among the Bhil population.

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  • All the western region is but slightly affected by the monsoon.

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  • along the parallel of 33° N., and arrests the monsoon currents), is subject to much the same climatic influences as the eastern Himalaya.

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  • The north-east monsoon, which lasts from October till April, is exceedingly violent for three months after its commencement.

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  • In the distribution of the rainfall, as dependent on the direction of the winds, the following parts of Sumatra must be distinguished: (r) south-east Sumatra, on which, as on Banka and Billiton, the heaviest rainfall occurs during the north-west monsoon, the annual volume of rainfall increasing from 98.4 in.

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  • by the south-east monsoon.

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  • Here, too, the prevailing rainfall is brought by the north-west monsoon, but in this belt its prevalence is not so pronounced, Padang getting 94 in.

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  • of rain during the north-west monsoon, against 90 in.

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  • Desert conditions also arise from local causes, as in the case of the Indian desert situated in a region inaccessible to either of the two main branches of the south-west monsoon.

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  • could approach no nearer than two miles to the shore, where typhoons of the southwest monsoon not infrequently obliged them to lie several days before they could be unloaded.

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  • In the monsoon the Cochin backwaters are broad navigable channels and lakes; in the hot weather they contract into shallows in many places not 2 ft.

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  • He holds the opinion that the tea-plant is indigenous, not to Assam only, but to the whole monsoon region of eastern Asia, where he found it growing wild as far north as the islands of southern Japan.

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  • In the deltas of southern India irrigation is only practised during the monsoon season.

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  • The Godaveri, Kistna and Kaveri all take their rise on the Western Ghats, a region where the rainfall is never known to fail in the monsoon season.

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  • For this monsoon irrigation there is always abundance of water, and so long as the canals and sluices are kept in repair, there is little trouble in distributing it over the fields.

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  • But to keep sugar-cane, or indigo, or cotton alive in summer before the monsoon sets in in India or the Nile rises in Egypt the field should be watered every ten days or fortnight, while rice requires a constant supply of water passing over it.

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  • In addition to these great perennial canals, much has been done since 1878 in enlarging and extending what are known as the " inundation canals " of the Punjab, which utilize the flood waters in the rivers during the monsoon season and are dry at other times.

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  • monsoon, which is marked at Muscat, is scarcely noticeable in the Persian Gulf proper, though recent upperair investigations conducted at Bagdad give some reason to think that the effects of the monsoon can be observed even there.

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  • On this side of the island there are but one or two possible anchoring grounds, and these only during the north-east monsoon.

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  • During this season the rivers, which are roaring torrents throughout the monsoon, are almost all lost in the dry, absorbent plains.

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  • monsoon in India, beating along the southern slopes of the Himalaya, travel up the Kabul valley as far as Laghman, though they are more clearly felt in Bajour and Panjkora, under the high spurs of the Hindu Kush, and in the eastern branches of Safed Koh.

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  • South of this the Suliman mountains may be taken as the western limit of the monsoon's action.

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  • In the absence of monsoon influences there are steadier weather indications than in India.

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  • On its eastern margin, however, in the neighbourhood of the Aravalli hills, and again in the northern Punjab, rain is more frequent, occurring both in the south-west monsoon and also at the opposite season in the cold weather.

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  • Up or down this plain, at opposite seasons, sweep the monsoon winds, in a direction at right angles to that of their nominal course; and thus vapour which has been brought by winds from the Bay of Bengal is discharged as snow and rain on the peaks and hillsides of the Western Himalayas.

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  • Together with the two parallel valleys of the Nerbudda and Tapti, which drain the flanks of its western half, it gives, at opposite seasons of the year, a decided easterly and westerly direction to the winds of this part of India, and condenses a tolerably copious rainfall during the south-west monsoon.

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  • At Ajmer, an old meteorological station at the eastern foot of the range, the wind is predominantly south-west, and there and at Mount Abu the south-west monsoon rains are a regularly recurrent phenomenon, - which can hardly be said of the region of scanty and uncertain rainfall that extends from the western foot of the range and merges in the Bikaner desert.

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  • This plateau is swept by the south-west monsoon, but not until it has surmounted the western barrier of the Ghats; and hence the rainfall is, as a rule, light at Poona and places similarly situated under the lee of the range, and but moderate over the more easterly parts of the plateau.

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  • The country to the east of the gap receives the rainfall of the south-west monsoon; and during the north-east monsoon ships passing Beypur meet with a stronger wind from the land than is felt elsewhere on the Malabar coast.

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  • In Lower Burma the western face of the Arakan Yoma hills, like that of the Western Ghats in India, is exposed to the full force of the south-western monsoon, and receives a very heavy rainfall.

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  • The continental type of weather prevails over almost the whole of India from December to May, and the oceanic type from June to November, thus giving rise to the two great divisions of the year, the dry season or north-east monsoon, and the rainy season or south-west monsoon.

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  • India thus becomes the type of a tropical monsoon climate.

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  • For the origin of the monsoon currents and their distribution see Monsoon.

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  • The two monsoon periods are divided by the change of temperature, due to solar action' upon the earth's surface, into two separate seasons; and thus the Indian year may be divided into four seasons: the cold season, including the months of January and February; the hot season, comprising the months of March, April and May; the south-west monsoon period, including the months of June, July, August, September and October; and the retreating monsoon period, including the months of November and December.

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  • The south-west monsoon currents usually set in during the first fortnight of June on the Bombay and Bengal coasts, and give more The or less general rain in every part of India during the next three months.

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  • The Bombay monsoon, after surmounting the Ghats, blows across the peninsula as a west and sometimes in places a north-west wind; but it leaves with very little rain a strip 100 to 200 m.

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  • Similarly the Bengal monsoon passes by the Coromandel coast and the Carnatic with an occasional shower, taking a larger volume to Masulipatam and Orissa, and abundant rain to Bengal, Assam and Cachar.

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  • In September the force of the monsoon begins rapidly to decline, and after about the middle of the month it ceases to carry rain to the greater part of north-western India.

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  • In its rear springs up a gentle steady north-east wind, which gradually extends over the Bay of Bengal, and is known as the north-east monsoon.

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  • The months of November and December form a transition period between the monsoon and the cold season.

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  • This excessive dependence upon a single industry, which is in its turn dependent upon the accident of the seasons, upon a favourable or unfavourable monsoon, has been held to be one of the main causes of the frequent famines which ravage India.

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  • In 5900 this district suffered severely from famine owing to the complete failure of the monsoon, and the cultivated area decreased by 50 or 60 70; but, on the whole, trade has improved of late years owing to the new railways, which have stimulated commerce and created fresh centres of industry.

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  • This zone falls within the regime of the summer monsoon rains, while those districts adjoining the coast zone enjoy also winter rains.

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  • Slight rain falls in the spring and abundant monsoon rains from June to September.

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  • The curve shows two rises, one at the beginning of winter, and the other at the commencement of the monsoon, and at both these times the people are driven indoors.

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  • This excessive rainfall is caused by the fact that Cherrapunji stands on the edge of the plateau overlooking the plains of Bengal, where it catches the full force of the monsoon as it rises from the sea.

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  • The rains of the south-east monsoon reach Central India as a rule about the 12th of July, and last until the end of September.

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  • 1 He gives a very accurate account of this forlorn tract, its general aridity and the necessity of obtaining water by digging in the beds of torrents; describes the food of the inhabitants as dates and fish; and adverts to the occasional occurrence of fertile spots, the abundance of aromatic and thorny shrubs and fragrant plants, and the violence of the monsoon in the western part of Makran.

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  • the period of the monsoon rains of India) the remainder of the year being comparatively dry.

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  • The condensation of vapour from the ascending currents and their gradual exhaustion as they are precipitated on successive ranges is very obvious in the cloud effects produced during the monsoon, the southern or windward face of each range being clothed day after day with a white crest of cloud whilst the northern slopes are often left entirely free.

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  • Command of the sea could not be maintained - least of all in the monsoon months - while the Portuguese fleets were based on Lisbon, which could only be reached after a six months' voyage; and experience had proved that almost every Portuguese factory required a fortress for its defence when the fleets were absent.

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  • April, May and June are hot; and the monsoon months from June to October are distinguished by damp heat and malaria.

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  • The approach of the south-west monsoon precluded the immediate renewal of the attempt; but hostilities were resumed, and Achin fell in January 1874.

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  • There were indications that monsoon influences extended as far north at least as the Great Pamir, and a definite analogy was established between the record of barometric pressure on the Pamirs and that of the outer ranges of the Himalaya.

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  • From May to August, the period of the south-east monsoon, the climate of Banka is dry and hot; but the mean annual rainfall reaches 120 in.

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  • The wet, cool season proper is from November to February, accompanying the north-west monsoon.

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  • The bamboos are a feature of tropical forest vegetation, especially in the monsoon region.

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  • But the rainy season proper, caused by the south-west monsoon, lasts from June to mid-September, and commencing in the north moves southward.

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  • The climate of Backergunje is one of the healthiest in Eastern Bengal, owing to the strong south-west monsoon, which comes up directly from the Bay of Bengal, and keeps the atmosphere cool; but the heavy rainfall and consequent humidity of the atmosphere, combined with the use of bad water, are fruitful sources of disease.

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  • The south-east monsoon blows from May to October, which is the dry season, and the west-north-west monsoon from December to March.

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  • Being exposed to the winter monsoon, the northern parts of the island enjoy much the same sort of temperate climate as the neighbouring provinces of the mainland, but in the southern parts, protected from the monsoon by the mountain ranges, the climate is almost or entirely tropical.

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  • The coast is rock-bound and difficult of access; and though it contains several bays forming fairweather ports for vessels engaged in the coasting trade, Bombay, Karachi-in-Sind, Marmagoa and Karwar alone have harbours sufficiently land-locked to protect shipping during the prevalence of the south-west monsoon.

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  • The Konkan is hot and moist, the fall of rain during the monsoon sometimes approaching 3 00 in.

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  • The south-west monsoon generally sets in about the first week in June, and pours down volumes of rain along the coast.

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  • From June to October travelling is difficult and unpleasant, except in Sind, where the monsoon rains exert little influence.

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  • The failure of the monsoon of 1896 caused widespread distress throughout the Deccan, over an area of 46,000 sq.

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  • In 1899 the monsoon again failed in Gujarat, where famine hitherto had been almost unknown; and the winter rains failed in the Deccan, so that distress gradually spread over almost the entire presidency.

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  • South of the belt salinity falls quickly as latitude increases, while to the north of it, in the monsoon region, the surface water is very fresh off the African coast and to the north-east.

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  • Probably the northern and north-eastern region, within the monsoon area, contains relatively fresh water down to very considerable depths.

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  • During the northern summer the south-west monsoon, which is sufficiently strong to bring navigation practically to a standstill except for powerful steamers, sets up a strong north-easterly drift in the Arabian Sea, and the water removed from the east African coast is replaced by the upwelling of cold water from below; this is one of the best illustrations of this action extant.

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  • At the beginning of the reign it was supposed to be impossible to build a steamer which could either cross the Atlantic, or face the monsoon in the Red Sea.

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  • It was the beginning of September, and the expedition took advantage of the easterly monsoon, which carried them to Batavia.

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  • monsoon, the Jibal must be considered the most favoured district of Arabia.

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  • The south-west monsoon sweeps up the Nerbudda valley from Bombay and crossing the tableland at Neemuch gives copious supplies to Malwa, Jhalawar and Kotah and the countries which lie in the course of the Chambal river.

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  • It is only when the monsoon is in considerable force that Merwara gets a plentiful supply from it.

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  • The north-eastern monsoon sweeps up the valley of the Ganges from the Bay of Bengal and waters the northern part of Rajputana, but hardly penetrates farther west than the longitude of Ajmere.

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  • 2 In the interior of the country about the plain of Dhofar, 3 during the south-west monsoon, frankincense and other gums are gathered by the Beni Gurrah Bedouins, and might be obtained by them in much larger quantities; their lawlessness, however, and the lack of a safe place of exchange or sale are obstacles to the development of trade.

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  • The rainfall in the northern peninsula (north of the equator) differs from that of the southern; the former has rains (not caused by the monsoon), and of smaller amount, 102 in.

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  • annually; the latter has a greater rainfall, 157 in., brought by the north-western monsoon, and of which the west coast receives a much larger share than the east.

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  • The monsoon ragas are defined by various characteristics, all inspired by the personality of the rain.

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  • During the period June to September there is a light monsoon rain in Salalah.

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  • The weather was very pleasant in December although slightly humid and during the second week we did have several monsoon rainstorms.

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  • However, it is prone to serious flooding during the monsoon season of June to September.

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  • To say nothing of the times we brought unseasonal sleet to midsummer Norway and the monsoon to Cheshire.

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  • Climate: Taiwan has an oceanic, subtropical monsoon climate.

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  • In India, the seasonal forecast of monsoon rainfall has traditionally been issued using a number of statistical techniques (see Kumar et al.

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  • The climate varies from temperate in the north to tropical monsoon in the south.

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  • The OMZ is created by the monsoon upwelling nutrient-rich water from greater depths which drives plankton growth, increasing productivity in the surface waters.

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  • A strong Asian summer monsoon is preceded by weak upper tropospheric westerlies over south Asia and vise versa.

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  • JM: I can not compete with the high streets wedding offerings at the likes of Debenhams, Monsoon etc but I compete quite well with the Bridal Boutique.

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  • Monsoon Lagoon: An amazing wave pool ideal for inner tubing, body surfing, and swimming.

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