翻訳と辞書
Words near each other
・ Convention card
・ Convallaria
・ Convallarin
・ Convallatoxin
・ ConvaTec
・ Convectant drying
・ Convection
・ Convection cell
・ Convection heater
・ Convection microwave
・ Convection oven
・ Convection zone
・ Convection–diffusion equation
・ Convective available potential energy
・ Convective Boundary Layer
Convective condensation level
・ Convective heat transfer
・ Convective inhibition
・ Convective instability
・ Convective mixing
・ Convective momentum transport
・ Convective overshoot
・ Convective overturn
・ Convective storm detection
・ Convective temperature
・ Convector
・ Convenanter Church
・ Convencion de Juegos de Mesa y Comics
・ Convención
・ Convene


Dictionary Lists
翻訳と辞書 辞書検索 [ 開発暫定版 ]
スポンサード リンク

Convective condensation level : ウィキペディア英語版
Convective condensation level
The convective condensation level (CCL) represents the height (or pressure) where an air parcel becomes saturated when heated from below and lifted adiabatically due to buoyancy.
In the atmosphere, assuming a constant water vapor mixing ratio, the dew point temperature (the temperature where the
relative humidity is 100%) decreases with increasing height because the pressure of the atmosphere decreases with height. The CCL is determined by plotting the dew point (100%RH) verses altitude and locating the intersection with the actual measured temperature sounding. It marks where the cloud base begins when air is heated from below to the convective temperature, without mechanical lift.
Once the CCL is determined, the surface temperature necessary to raise a mass of air to that height can be found by using the Dry Adiabatic Lapse Rate (DALR) to determine the potential temperature. In the early morning, this temperature is typically larger than the surface temperature, in the mid-afternoon, it may be the same.
Compare this to the Lifting Condensation Level (LCL) where the air is lifted and cooled without first increasing the surface temperature. The LCL is less than or equal to the CCL depending on the temperature profile.
Both condensation levels indicate the altitude (or pressure) where relative humidity reaches 100%. However, since the actual condensation level depends on the availability of condensation nuclei, clouds typically do not form until the relative humidity is somewhat above 100%.
== See also ==

* Atmospheric convection
* Atmospheric thermodynamics
* Lifting condensation level and level of free convection

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Convective condensation level」の詳細全文を読む



スポンサード リンク
翻訳と辞書 : 翻訳のためのインターネットリソース

Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.