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Ch1 (4) - ———Tfi Fall 2009 Page 4 of 4 least depth...

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Unformatted text preview: ———Tfi Fall 2009 Page 4 of 4 least depth over the c. The depth of the tro 5 here is ot the same everywhere around the . Depth varies with Ears IE; lg . . Greatest depth over the +or ; Characteristics of the Stratosphere a. Temperature ll: [K (as: 5 with height. Called an [k N: X 5]- lllCl . 5 What causes this morease in temperature with height? ‘ htfialnby CDhLCVWl/atmw oF 010m ' Mme. waswlo’: UN mamas“ b. Not much “weather’ ’(clouds/precipitation) occurs in the stratosphere. Can you think of one reason why? no WOWU/ wapor 7. The Tropopause Define: Boundary between the “O? D'E‘AOKA (N00 SWQWSPhQ—N Q, Think of the tropopause as an upper limit to the weather we have' in the troposphere. Example: tops of thunderstorms don’ t usually extend above the tropopause. Also the< Q: 'l‘ SI t( (a [I] is located near the tropopause. . The Ionosphere 3. Contains electrically charged particles called H 1 I§§ b. Important for 2 reasons: 1. RH-eérs HM mam tvcimmissmm 2. when, Burrows (mucus (Newman \tgws) 99¢qu :5 MUSQSP were 21V ‘W‘Zflh‘ksk éifl' V060 opl/Vf‘. lr’c ll - _ 1- mama; (4.. r W E.“ o 908D hCr g “m“fi’ worm Wimp a». m . l Nit (Aég Temé l ...
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