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Estimation of latent heat profiles of deep convective clouds using cloudsat radar

机译:利用cloudsat雷达估算深对流云的潜热剖面

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The earth's atmosphere is highly coupled between the vertical layers and the surface. Understanding the circulations in the atmosphere is important for developing models and improving weather forecast. The latent heat exchanges in the atmosphere is one of the key driving forces of these circulations. There have been numerous studies which have highlighted the latent heat being the source of many atmospheric waves and oscillations. It is therefore very important to accurately estimate the latent heat in the atmosphere, especially for the convective clouds which have proven to be one of the major sources of gravity waves. Currently, satellite based latent heat estimation is very limited due to which, any detailed global study regarding latent heat effects and relationships with atmospheric phenomena have been restricted to theoretical works. There is a need for developing more methods to increase the spatial and temporal coverage of latent heat estimates which is the objective of the current study. A method has been proposed in this study which retrieves the accumulated latent heat profiles of deep convective clouds from combined CloudSat-CALIPSO cloud profiles. A realistic database of simulated deep connective cloud events are compared with observations using the Bayesian Monte Carlo method to derive an estimate. This study would help to understand the atmospheric circulations originated by heating, in more detail.
机译:地球的大气层在垂直层和地表之间高度耦合。了解大气环流对于开发模型和改善天气预报很重要。大气中的潜热交换是这些循环的主要驱动力之一。已经有许多研究强调了潜热是许多大气波和振荡的源头。因此,准确估算大气中的潜热非常重要,尤其是对于已被证明是重力波主要来源之一的对流云而言。当前,基于卫星的潜热估计非常有限,因此,有关潜热效应以及与大气现象的关系的任何详细的全球研究都仅限于理论研究。需要开发更多的方法来增加潜热估计的时空覆盖范围,这是当前研究的目标。在这项研究中提出了一种方法,该方法可以从结合的CloudSat-CALIPSO云剖面中检索深对流云的累积潜热剖面。使用贝叶斯蒙特卡洛方法将模拟的深层结云事件的真实数据库与观测值进行比较,以得出估计值。这项研究将有助于更详细地了解由加热引起的大气环流。

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