Page 25 - ภาษาอังกฤษสำหรับสายวิทยาการอุตุนิยมวิทยา
P. 25

20


               3.     Troposphere


               The troposphere is the layer of air that begins at the surface of the earth and extends upward
               to an average altitude of 7 miles. Its height varies from the equator to the poles, and from

               season to season. It is higher over the equator than over the poles, and it also has a greater

               height in the summer. The troposphere contains about three quarters (75%) of the earth's

               atmosphere by weight and almost all of the weather. The border between the troposphere
               and the stratosphere is called the tropopause. It is important because high-speed winds are

               often found near the tropopause. I




               4.     Stratosphere

               The stratosphere is the layer just above the tropopause. The stratosphere begins (base) at an

               average height of seven miles and extends upward to an average height of 22 miles (top).

               The characteristics of the layer are a slight increase of temperature with height and almost

               no humidity. Occasionally, however, a strong thunderstorm in the troposphere will cross the
               tropopause and enter into the lower stratosphere.
   20   21   22   23   24   25   26   27   28   29   30