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
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- Fall '08