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A Combined Multisensor Optimal Estimation Retrieval Algorithm for Oceanic Warm Rain Clouds

机译:海洋暖雨云的组合多传感器最优估计反演算法

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The complicated interactions between cloud processes in the tropical hydrologic cycle and their responses to changes in environmental variables have been the focus of many recent investigations. Most studies that examine the response of the hydrologiccycle to temperature changes focus on deep convection and cirrus production, but recent results suggest that warm rain clouds may be more sensitive to temperature changes. These clouds are prevalent in the tropics and make considerable contributions tothe radiation budget and to total tropical rainfall, as well as serving to moisten and precondition the atmosphere for deep convection. A change in the properties of these clouds in climate-change scenarios could have significant implications for the hydrologic cycle. Existing microwave and visible retrievals of warm rain cloud liquid water path (LWP) disagree over the range of sea surface temperatures (SST) observed in the tropical western Pacific Ocean. Although both retrieval methods show similar behavior for nonraining clouds, the two methods show very different warm-rain-cloud LWP responses to SST, both in magnitude and trend. This makes changes to the relationship between precipitation and cloud properties in changing temperature regimes difficult to interpret. A combined optimal estimation retrieval algorithm that takes advantage of the strengths of the different satellite measurements available on the Tropical Rainfall Measuring Mission (TRMM) satellite has been developed. Deconvolved TRMM Microwave Imager brightness temperatures are combined with cloud fraction from the Visible and Infrared Scanner and rainwater estimates from the TRMM precipitation radar to retrieve the cloud LWP in warm rain systems. This algorithm is novel in that it takes into account the water in the rain and estimates the LWP due to only the cloud water in a raining cloud, thus allowing investigation of the effects of precipitation on cloud properties.
机译:热带水文循环中的云过程与其对环境变量变化的响应之间复杂的相互作用一直是许多近期研究的重点。大多数研究水文循环对温度变化的反应的研究都集中在深对流和卷云的产生上,但是最近的结果表明温暖的雨云可能对温度变化更敏感。这些云层在热带地区盛行,对辐射预算和热带总降水量做出了巨大贡献,并为深层对流增湿和预处理大气。在气候变化情景中,这些云的性质发生变化可能会对水文循环产生重大影响。在热带西太平洋观测到的海表温度范围内,现有的微波和可见的暖雨云液态水路径(LWP)的取回不一致。尽管两种检索方法对非降雨云都表现出相似的行为,但两种方法在幅度和趋势上都表现出非常不同的暖雨云LWP对SST的响应。这使得难以解释在不断变化的温度状态下降水与云性质之间关系的变化。已经开发出一种组合的最佳估计检索算法,该算法利用了热带降雨测量任务(TRMM)卫星上可用的不同卫星测量的优势。解卷积的TRMM微波成像仪的亮度温度与可见光和红外扫描仪中的云量以及TRMM降水雷达的雨水估算值相结合,以检索暖雨系统中的云LWP。该算法是新颖的,因为它考虑了雨中的水,并且仅由于下雨的云中的云水而估计了LWP,因此可以研究降水对云特性的影响。

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