Clausius–Clapeyron Scaling of CAPE from Analytical Solutions to RCESource: Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 009::page 3719Author:Romps, David M.
DOI: 10.1175/JAS-D-15-0327.1Publisher: American Meteorological Society
Abstract: y deriving analytical solutions to radiative?convective equilibrium (RCE), it is shown mathematically that convective available potential energy (CAPE) exhibits Clausius?Clapeyron (CC) scaling over a wide range of surface temperatures up to 310 K. Above 310 K, CAPE deviates from CC scaling and even decreases with warming at very high surface temperatures. At the surface temperature of the current tropics, the analytical solutions predict that CAPE increases at a rate of about 6%?7% per kelvin of surface warming. The analytical solutions also provide insight on how the tropopause height and stratospheric humidity change with warming. Changes in the tropopause height exhibit CC scaling, with the tropopause rising by about 400 m per kelvin of surface warming at current tropical temperatures and by about 1?2 km K?1 at surface temperatures in the range of 320?340 K. The specific humidity of the stratosphere exhibits super-CC scaling at temperatures moderately warmer than the current tropics. With a surface temperature of the current tropics, the stratospheric specific humidity increases by about 6% per kelvin of surface warming, but the rate of increase is as high as 30% K?1 at warmer surface temperatures.
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contributor author | Romps, David M. | |
date accessioned | 2017-06-09T16:59:20Z | |
date available | 2017-06-09T16:59:20Z | |
date copyright | 2016/09/01 | |
date issued | 2016 | |
identifier issn | 0022-4928 | |
identifier other | ams-77504.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4220070 | |
description abstract | y deriving analytical solutions to radiative?convective equilibrium (RCE), it is shown mathematically that convective available potential energy (CAPE) exhibits Clausius?Clapeyron (CC) scaling over a wide range of surface temperatures up to 310 K. Above 310 K, CAPE deviates from CC scaling and even decreases with warming at very high surface temperatures. At the surface temperature of the current tropics, the analytical solutions predict that CAPE increases at a rate of about 6%?7% per kelvin of surface warming. The analytical solutions also provide insight on how the tropopause height and stratospheric humidity change with warming. Changes in the tropopause height exhibit CC scaling, with the tropopause rising by about 400 m per kelvin of surface warming at current tropical temperatures and by about 1?2 km K?1 at surface temperatures in the range of 320?340 K. The specific humidity of the stratosphere exhibits super-CC scaling at temperatures moderately warmer than the current tropics. With a surface temperature of the current tropics, the stratospheric specific humidity increases by about 6% per kelvin of surface warming, but the rate of increase is as high as 30% K?1 at warmer surface temperatures. | |
publisher | American Meteorological Society | |
title | Clausius–Clapeyron Scaling of CAPE from Analytical Solutions to RCE | |
type | Journal Paper | |
journal volume | 73 | |
journal issue | 9 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/JAS-D-15-0327.1 | |
journal fristpage | 3719 | |
journal lastpage | 3737 | |
tree | Journal of the Atmospheric Sciences:;2016:;Volume( 073 ):;issue: 009 | |
contenttype | Fulltext |