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Precipitation Characteristics in West and East Africa from Satellite and in Situ Observations

机译:西部和东非的降水特征来自卫星和原位观察

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摘要

Using in situ data, three precipitation classes are identified for rainy seasons of West and East Africa: weak convective rainfall (WCR), strong convective rainfall (SCR), and mesoscale convective systems (MCSs). Nearly 75% of the total seasonal precipitation is produced by the SCR and MCSs, even though they represent only 8% of the rain events. Rain events in East Africa tend to have a longer duration and lower intensity than in West Africa, reflecting different characteristics of the SCR and MCS events in these two regions. Surface heating seems to be the primary convection trigger for the SCR, particularly in East Africa, whereas theWCR requires a dynamical trigger such as low-level convergence. The data are used to evaluate the performance of the recently launched Integrated Multisatellite Retrievals for Global Precipitation Measurement (IMERG) project. The IMERG-based precipitation shows significant improvement over its predecessor, the Tropical Rainfall Measuring Mission (TRMM) Multisatellite Precipitation Analysis (TMPA), particularly in capturing the MCSs, due to its improved temporal resolution.
机译:利用现场数据,确定了西非和东非雨季的三类降水:弱对流降水(WCR)、强对流降水(SCR)和中尺度对流系统(MCS)。近75%的季节性总降水量是由SCR和MCSs产生的,尽管它们仅占降雨事件的8%。东非的降雨事件往往比西非的持续时间更长,强度更低,反映了这两个地区SCR和MCS事件的不同特征。表面加热似乎是SCR的主要对流触发因素,尤其是在东非,而WCR需要动态触发因素,如低层辐合。这些数据用于评估最近启动的全球降水测量综合多卫星反演(IMERG)项目的性能。基于IMERG的降水显示出比其前身热带降雨测量任务(TRMM)多卫星降水分析(TMPA)的显著改进,尤其是在捕捉MCS方面,由于其时间分辨率的提高。

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