Elementary Physiography
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In our eReader you can find the full English version of the book. Read Elementary Physiography Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Elementary Physiography
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The high temperature (90° and alcove) in the southwestern part^ of the United States in July is accounted for partly by the fact that the region is somewhat shut in by mountains. The diyness of the soil and of the air al)()ve it also tend to raise its temperature.
Altitude affects temperature, as already explained, l)ut isother- mal charts show' no relation lietween isothennal lines and surface relief. The reason is that isothermal lines are represented on. Maps as if they w^ere at sea-level. T...his is done by making allowance for altitude at the average rate of 1° F. For about 330 feet. Thus if the temperature of a place at an altitude of 3, 300 feet is 60°, it is 248 PHYSIOGRAPHY put down on the chart as 70° (60° + 10°). Isothermal charts, therefore, are intended to show the temperature as it would he if the land irere at sea-Ievel.
Daily range of temperature. The temperature of a day when the sun shines is generally warmer than the temperature of the night. The cUfference is often as much as 40° or 50° F.
What to read after Elementary Physiography?
You can find similar books in the "Read Also" column, or choose other free books by Rollin D Salisbury to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The high temperature (90° and alcove) in the southwestern part^ of the United States in July is accounted for partly by the fact that the region is somewhat shut in by mountains. The diyness of the soil and of the air al)()ve it also tend to raise its temperature.
Altitude affects temperature, as already explained, l)ut isother- mal charts show' no relation lietween isothennal lines and surface relief. The reason is that isothermal lines are represented on. Maps as if they w^ere at sea-level. T...his is done by making allowance for altitude at the average rate of 1° F. For about 330 feet. Thus if the temperature of a place at an altitude of 3, 300 feet is 60°, it is 248 PHYSIOGRAPHY put down on the chart as 70° (60° + 10°). Isothermal charts, therefore, are intended to show the temperature as it would he if the land irere at sea-Ievel.
Daily range of temperature. The temperature of a day when the sun shines is generally warmer than the temperature of the night. The cUfference is often as much as 40° or 50° F.
What to read after Elementary Physiography?
You can find similar books in the "Read Also" column, or choose other free books by Rollin D Salisbury to read onlineMoreLess
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