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Sensitivity of North American Monsoon Rainfall to Multisource Sea Surface Temperatures in MM5

机译:MM5中北美季风降雨对多源海表温度的敏感性

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In this article, four continually processed sea surface temperature (SST) datasets, including the Reynolds SST (RYD), the global final analysis of skin temperature at oceans (FNL), and two Moderate Resolution Imaging Spectroradiometer (MODIS) Aqua SSTs retrieved from thermal infrared imagery (TIR) and midinfrared imagery (MIR), were compared. The results show variations from each other. In comparison with the RYD SST, the FNL data have -0.5° ~ 0.5℃ perturbations, while the TIR and MIR SSTs possess larger deviations of -2° ~ 1℃, mainly due to algorithm and/or sensor differences in these SST datasets. A regional model, the fifth-generation Pennsylvania State University-National Center for Atmospheric Research (Penn State-NCAR) Mesoscale Model (MM5), was used to investigate whether model atmospheric predictions, especially those concerning precipitation during the North American monsoon season, are sensitive to these SST variations. A comparison of rainfall, atmospheric height, temperature, and wind fields produced by model results, reanalysis data, and observations indicates that, at monthly scale, the model shows changes in the simulations for three consecutive years; in particular, rainfall amounts, timing, and even patterns vary at some specific regions. Forced by the MODIS Aqua midinfrared SST (MIR), which includes large regions with SST values lower than the conventional Reynolds SST, the MM5 rain field predictions show reduced errors over land and oceans compared to when the model is forced by other SST data. Specifically, rainfall estimates are improved over the offshore of southern Mexico, the Gulf of Mexico, the coastal regions of southern and eastern Mexico, and the southwestern U.S. monsoon active region, but only slightly improved over the monsoon core and the high-elevated Great Plains. Using MIR SST data, one is also capable of improving geopotential height and temperature fields in comparison with the reanalysis data.
机译:本文中,有四个连续处理的海面温度(SST)数据集,包括雷诺(Reynolds)SST(RYD),全球对皮肤温度的全球最终分析(FNL),以及从热学获取的两个中等分辨率成像光谱仪(MODIS)Aqua SST比较了红外图像(TIR)和中红外图像(MIR)。结果显示彼此不同。与RYD SST相比,FNL数据的扰动为-0.5°〜0.5℃,而TIR和MIR SST的偏差为-2°〜1℃,这主要归因于这些SST数据集的算法和/或传感器差异。区域模型,即第五代宾夕法尼亚州立大学-国家大气研究中心(Penn State-NCAR)中尺度模型(MM5),用于调查模型的大气预测,特别是有关北美季风季节降水的预测是否对这些SST变化敏感。对模型结果,再分析数据和观测结果产生的降雨,大气高度,温度和风场的比较表明,该模型按月显示连续三年的模拟变化。特别是在某些特定地区,降雨量,时间甚至模式都有所不同。由MODIS Aqua中红外SST(MIR)推动,该区域包括SST值低于传统雷诺SST的较大区域,与其他SST数据强推该模型相比,MM5雨场预测显示出陆地和海洋的误差减少。具体而言,墨西哥南部,墨西哥湾,墨西哥南部和东部沿海地区以及美国西南季风活动区的降雨估计有所改善,但季风核心区和高海拔大平原仅略有改善。使用MIR SST数据,与重新分析数据相比,还可以改善地势高度和温度场。

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