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isotherm

isotherm

isotherm Sentence Examples

  • The July isotherm of 80° crosses the state a little N.

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  • The January isotherm of 15° F.

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  • Both the midwinter isotherm of Montreal and the midsummer one of Washington, D.C., pass through the state.

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  • and S.; thus Odessa and Konigsberg are situated on the same winter isotherm of 28°; St Petersburg, Orel and the mouth of the Ural river on about 20°; and Mezen and Ufa on 9°.

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  • The summer isotherm of 68° F., which in Europe passes through Cracow and Kaluga, traverses Omsk, Krasnoyarsk and Irkutsk, whence it turns north to Yakutsk, and then south again to Vladivostok.

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  • of the 80° isotherm the average temperature for July is between 80° and 85°.

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  • As a result, the isotherms of July are strongly convex poleward as they cross the United States, the isotherm of 70 Sweeping up to the northern boundary in the north-west, and the heat equator leaping to the overheated deserts of the south-west, where the July mean is over 90.

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  • Russia; thus the isotherm of 39° runs from St Petersburg to Orenburg, and that of 35° from Tornea in Finland to Uralsk.

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  • The isotherm of - 22° F., which touches the north point of Novaya Zemlya, passes in Siberia through Turukhansk (at the confluence of the Lena and the Lower Tunguzka) and descends as low as 55° N.

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  • The same effect is well shown by the linguiform isotherms. In January, for example, the isotherm of 14°, after skirting the north coast of the Scandinavian peninsula, turns southward along the Keel, crossing the upper part of the district of the great northern lakes.

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  • Odessa experiences the influence of the continental climate of the neighbouring steppes; its winters are cold (the average temperature for January being 23.2° F., and the isotherm for the entire season that of Konigsberg), its summers are hot (72.8° in July), and the yearly average temperature is 48.5°.

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  • Again, the July isotherm of 75° crosses the middle section of the Caspian, nearly coinciding with the January isotherm of 25°, while that of 80° skirts the southern shore of the sea, nearly coinciding with the January curve of 40°, so that the mean annual range over the northern section of the sea is 60° and over the southern section 40°.

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  • The south-eastern corner is crossed by an annual isotherm of 60°, the north-western by one of 50°; and although in the former region sometimes not a day in the year may show an average temperature below freezing-point, at Jefferson City there are occasionally two months of freezing weather, and at Rockport three.

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  • Isotherm >>

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  • adsorption isotherm.

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  • isotherm analysis and electronic zoom function simplify the identification of potential problems.

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  • This information can often be obtained from the shape of the vapor sorption isotherm.

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  • Interfacial Kinetics, 2nd Year, Trinity Term Topics to Cover (i) The Langmuir adsorption isotherm.

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  • sorption isotherm.

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  • This information can often be obtained from the shape of the vapor sorption isotherm.

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  • vapour information can often be obtained from the shape of the vapor sorption isotherm.

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  • Russia; thus the isotherm of 39° runs from St Petersburg to Orenburg, and that of 35° from Tornea in Finland to Uralsk.

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  • and S.; thus Odessa and Konigsberg are situated on the same winter isotherm of 28°; St Petersburg, Orel and the mouth of the Ural river on about 20°; and Mezen and Ufa on 9°.

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  • The summer isotherm of 68° F., which in Europe passes through Cracow and Kaluga, traverses Omsk, Krasnoyarsk and Irkutsk, whence it turns north to Yakutsk, and then south again to Vladivostok.

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  • The isotherm of - 22° F., which touches the north point of Novaya Zemlya, passes in Siberia through Turukhansk (at the confluence of the Lena and the Lower Tunguzka) and descends as low as 55° N.

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  • Both the midwinter isotherm of Montreal and the midsummer one of Washington, D.C., pass through the state.

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  • As a result, the isotherms of July are strongly convex poleward as they cross the United States, the isotherm of 70 Sweeping up to the northern boundary in the north-west, and the heat equator leaping to the overheated deserts of the south-west, where the July mean is over 90.

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  • The July isotherm of 80° crosses the state a little N.

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  • of the 80° isotherm the average temperature for July is between 80° and 85°.

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  • The January isotherm of 15° F.

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  • Again, the July isotherm of 75° crosses the middle section of the Caspian, nearly coinciding with the January isotherm of 25°, while that of 80° skirts the southern shore of the sea, nearly coinciding with the January curve of 40°, so that the mean annual range over the northern section of the sea is 60° and over the southern section 40°.

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  • The same effect is well shown by the linguiform isotherms. In January, for example, the isotherm of 14°, after skirting the north coast of the Scandinavian peninsula, turns southward along the Keel, crossing the upper part of the district of the great northern lakes.

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    0
  • The south-eastern corner is crossed by an annual isotherm of 60°, the north-western by one of 50°; and although in the former region sometimes not a day in the year may show an average temperature below freezing-point, at Jefferson City there are occasionally two months of freezing weather, and at Rockport three.

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  • Odessa experiences the influence of the continental climate of the neighbouring steppes; its winters are cold (the average temperature for January being 23.2° F., and the isotherm for the entire season that of Konigsberg), its summers are hot (72.8° in July), and the yearly average temperature is 48.5°.

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