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Showing posts with label isothrope. Show all posts
Showing posts with label isothrope. Show all posts

Tuesday, July 21, 2015

Adiabatic Lapse Rates

What do you know about the Wet Adiabatic Lapse rate?
-       Less than dry adiabatic lapse rate

The more it slants = greater lapse rate
 
Lapse rate = Rate of cooling


What’s the difference between the Dry and Wet Adiabatic Lapse Rate?
-   Unsaturated à reaches LCL à Saturated
-   Latent “Hidden” heat - The heat either released or absorbed as a result of a change of state.

-   When a cloud forms….
o   The water vapor reaches the LCL à Temperature decreases à It’s doing work à slows the rate of cooling
-   Water vapor condenses à latent heat is released
Mixing ratio (w) - A measurement of the amount of water vapor in the air of a given sized quantity of dry air. Grams of vapor per kilogram of dry air.

W = Water vapor in the box
-   Dewpoint Lapse Rate = As it goes up it decreases = 2 deg C / km


-   Dew point (Td) - The temperature to which air must cool at constant pressure in order for air to reach saturation (commonly dew to form); indicates moisture content.