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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク equivalent potential temperature ： ウィキペディア英語版 equivalent potential temperature Equivalent potential temperature, commonly referred to as theta-e $\backslash left(\; \backslash theta\_e\; \backslash right)$, is a quantity related to the stability of a column of air in the atmosphere. $\backslash theta\_e$ is the temperature a parcel of air would reach if all the water vapor in the parcel were to condense, releasing its latent heat, and the parcel was brought adiabatically to a standard reference pressure, usually 1000 hPa (1000 mbar) which is roughly equal to atmospheric pressure at sea level. In stable conditions, $\backslash theta\_e$ increases with altitude. If $\backslash theta\_e$ decreases with height, convection can occur. The comparison of the equivalent potential temperature of parcels of air at different pressures thus provides a measure of the instability of the column of air.〔(www.theweatherprediction.com )〕 ==Explanation== 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「equivalent potential temperature」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.