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Passive Microwave Rainfall Retrieval Algorithm in the oceans of East Asia Eun-Kyoung Seo 1 , Geun-Hyeok Ryu 2 and Svetla Hristova-Veleva 3 1 Kongju National University(Korea), 2 KMA National Meteorological Satellite Center(Korea), and 3 JIFRESSE(UCLA) Features of the KGPM Algorithm The KGPM rainfall retrieval algorithm is to employ the following features: (1) rain detection algorithm (Hristova - Veleva 2018) (2) rain - type classification algorithm (Hristova - Veleva 2018) (3) the difference vector, between observed TBs and background (or clear - sky) TBs, which is inverted into rainfall rate (4) the 1dVAR - EOF optimized cloud - radiation database for East Asia (Seo et al. 2016) (5) the variable error covariance TB matrix for Bayesian inversion Acknowledgement This study has been supported by the National Meteorological Satellite Center (NMSC) of the Korea Meteorological Administration (KMA) According to the CFADs of radar reflectivity for 5 - year summer ( JJA) seasons, the region near the Korean Peninsula produces stronger, deeper convective clouds and more intense rain than the tropical and subtropical oceans in the East Asia, although the other regions are located in warmer environments (Seo 2011 ) . Also, shallow convective clouds producing very strong rain intensity and highly variable radar reflectivity at lower rain layers are frequently observed by the PR instrument near the Korean Peninsula (e . g . , Seo 2011 ; Sohn et al . 2013 ) . Hence, those regional rainfall features need to be reflected by rainfall retrieval algorithms around the Korean Peninsula . We designed and developed the Korean GPM (KGPM) rainfall retrieval algorithm which is suitable for the Korean Peninsula and its surrounding region . In particular, the database consisting of raining clouds and their corresponding brightness temperatures at GMI frequencies is built for rainfall systems occurring in East Asia using 1 - d variational approach in EOF space to reconcile model simulations with radar/radiometer observations . Background and Purpose Rainfall Retrieval Hydrometeor Retrieval convective stratiform mixed rain type all rain types Comparison of rain retrieval with RAR (Radar - AWS rainrate) Comparison of rain retrieval with GPROF & DPR convective stratiform With variable error covariances as a function of SST and TPW With constant error covariance Monthly evolution of SST and TPW environments error covariance as a function of (1) Seasons (2) Rain types (3) SST (4) TPW Convective stratiform Convective stratiform

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Page 1: Passive Microwave Rainfall Retrieval Algorithm in the ... · (1) rain detection algorithm (Hristova-Veleva 2018) (2) rain-type classification algorithm (Hristova-Veleva 2018) (3)

Passive Microwave Rainfall Retrieval Algorithm in the oceans of East AsiaEun-Kyoung Seo1, Geun-Hyeok Ryu2 and Svetla Hristova-Veleva3

1 Kongju National University(Korea), 2KMA National Meteorological Satellite Center(Korea), and 3JIFRESSE(UCLA)

Features of the KGPM AlgorithmThe KGPM rainfall retrieval algorithm is to employ the following features: (1) rain detection algorithm (Hristova-Veleva 2018)(2) rain-type classification algorithm (Hristova-Veleva 2018) (3) the difference vector, between observed TBs and background (or clear-

sky) TBs, which is inverted into rainfall rate (4) the 1dVAR-EOF optimized cloud-radiation database for East Asia (Seo

et al. 2016)(5) the variable error covariance TB matrix for Bayesian inversion

Acknowledgement This study has been supported by the National Meteorological Satellite Center (NMSC) of the Korea Meteorological Administration (KMA)

According to the CFADs of radar reflectivity for 5-year summer ( JJA) seasons, theregion near the Korean Peninsula produces stronger, deeper convective clouds and moreintense rain than the tropical and subtropical oceans in the East Asia, although theother regions are located in warmer environments (Seo 2011). Also, shallow convectiveclouds producing very strong rain intensity and highly variable radar reflectivity at lowerrain layers are frequently observed by the PR instrument near the Korean Peninsula(e.g., Seo 2011; Sohn et al. 2013). Hence, those regional rainfall features need to bereflected by rainfall retrieval algorithms around the Korean Peninsula.We designed and developed the Korean GPM (KGPM) rainfall retrieval algorithmwhich is suitable for the Korean Peninsula and its surrounding region. In particular, thedatabase consisting of raining clouds and their corresponding brightness temperaturesat GMI frequencies is built for rainfall systems occurring in East Asia using 1-dvariational approach in EOF space to reconcile model simulations withradar/radiometer observations.

Background and Purpose Rainfall Retrieval Hydrometeor Retrievalconvective stratiform

mixed rain type all rain types

Comparison of rain retrieval with RAR(Radar-AWS rainrate)

Comparison of rain retrieval with GPROF & DPRconvective

stratiform

With variable error covariances as a function of SST and TPW With constant error covarianceMonthly evolution of

SST and TPW environments

error covariance as a function of(1) Seasons(2) Rain types (3) SST (4) TPW

Convective stratiform Convective stratiform