AbstractIn situ, airborne and satellite measurements are used to characterize the structure of water v'/> Structure and Dynamical Influence of Water Vapor in the Lower Tropical Troposphere
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Structure and Dynamical Influence of Water Vapor in the Lower Tropical Troposphere

机译:水蒸气在较低热带对流层中的结构与动力学影响

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AbstractIn situ, airborne and satellite measurements are used to characterize the structure of water vapor in the lower tropical troposphere—below the height,$$z_*,$$z?,of the triple-point isotherm,$$T_*.$$T?.The measurements are evaluated in light of understanding of how lower-tropospheric water vapor influences clouds, convection and circulation, through both radiative and thermodynamic effects. Lower-tropospheric water vapor, which concentrates in the first few kilometers above the boundary layer, controls the radiative cooling profile of the boundary layer and lower troposphere. Elevated moist layers originating from a preferred level of convective detrainment induce a profile of radiative cooling that drives circulations which reinforce such features. A theory for this preferred level of cumulus termination is advanced, whereby the difference between
机译:<![cdata [ <标题>抽象 ara id =“par1”>原位,空中和卫星测量用于表征水蒸气结构在较低的热带对流层面 - 低于高度, $$ z _ *,$$ z 的三点等温线, $$ t _ *。$$ t 鉴于对低层水蒸气如何影响云,通过辐射和热力学效应对流和循环。低层水蒸气,其集中在边界层上方的前几公里,控制边界层的辐射冷却曲线和较低的对流层。始于优选的对流碎屑水平的升高湿润层诱导驱动增强这些特征的循环的辐射冷却的剖面。一个理论,用于这种优选的积分终端级别的理论是先进的,由此

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