Determination and Impacts of Surface Radiative Fluxes for TOGA COARE

为了支持TOGA/COARE的目标，该项目是一个 西太平洋地面辐射过程的研究 暖池区 该计划的目标是提供 分析：海面“表皮”温度，可降水量， 云的特性，以及地面长波和 短波辐射通量，空间分辨率为30公里， 整个TOGA COARE初级的时间分辨率为3小时 域 分析数据将主要从 利用ISCCP数据集， 算法发挥了重要作用。 可用表面和 飞机数据将用于验证遥感 算法，也将与卫星检索混合， 最终分析产品。 飞机子程序是 专门用来研究云的辐射特性， 并验证卫星反演的地表通量。 拟议的研究将分三个阶段完成： 一）遥感试点研究，以开发和比较卫星 算法; ii）使用 TOGA COARE IOP水面和飞机观测和准备 IOP的高分辨率分析;以及iii）诊断和 研究利用分析字段的建模研究。 天气和中尺度大气聚焦的诊断通量 将进行。 海洋的时间反应 层到表面辐射通量的波动将是 使用海洋混合层模型进行检查。 海洋混合层 模式将耦合到一个大气辐射对流 评估辐射和云反馈发生的模式 大气层和海洋边界层之间。 这项研究很重要，因为它是一个 TOGA/COARE对负责以下过程的主要研究： 世界上最敏感的地区，西太平洋， TOGA/COARE的现场。

In support of the TOGA/COARE objectives, this project is a study of the surface radiative processes in the western Pacific warm pool region. The objective of the program is to provide analyses of: sea-surface "skin" temperature, precipitable water, cloud properties, and components of the surface longwave and shortwave radiative fluxes, with spatial resolution of 30 km and temporal resolution of 3 hours for the entire TOGA COARE primary domain. The data for the analyses will be obtained principally by satellite remote sensing, with the ISCCP data set and algorithms playing a substantial role. Available surface and aircraft data will be utilized to validate the remote sensing algorithms and will also be blended with the satellite retrievals for the final analysis products. An aircraft sub-program is proposed specifically to investigate cloud-radiative properties, and to validate the satellite-derived surface fluxes. The proposed research will be accomplished in three stages: i) remote sensing pilot study to develop and compare satellite algorithms; ii) validation of remote sensing algorithms using TOGA COARE IOP surface and aircraft observations and preparation of high-resolution analyses for the IOP; and iii) diagnostic and studies modeling studies utilizing the analyzed fields. Diagnostic fluxes by synoptic and mesoscale atmospheric focing will be conducted. The temporal response of the ocean mixed layer to fluctuations in the surface radiative fluxes will be examined using an ocean mixed-layer model. The ocean mixed-layer model will be coupled to an atmospheric radiative-convective model to assess the radiative and cloud feedbacks occurring between the atmospheric and oceanic boundary layers. This research is important because it serves as one of the principal TOGA/COARE studies of the processes responsible for sensitive region of the world, the western Pacific Ocean, the field site of TOGA/COARE.