Rain-Rate Characteristics over the Korean Peninsula and Improvement of the Goddard Profiling (GPROF) Database for TMI Rainfall Retrievals

被引:12
作者
Ryu, Geun-Hyeok [1 ]
Sohn, Byung-Ju [1 ]
Kummerow, Christian D. [2 ]
Seo, Eun-Kyoung [3 ]
Tripoli, Gregory J. [4 ]
机构
[1] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul 151747, South Korea
[2] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
[3] Kongju Natl Univ, Dept Earth Sci Educ, Kong Ju 314701, South Korea
[4] Univ Wisconsin, Dept Atmospher & Ocean Sci, Madison, WI USA
关键词
LATENT HEATING DISTRIBUTIONS; PASSIVE MICROWAVE RADIOMETRY; CLOUD MODEL MICROPHYSICS; PRECIPITATION RETRIEVAL; RADIATIVE-TRANSFER; TROPICAL RAINFALL; COMBINED RADAR; PART I; AMSR-E; TRMM;
D O I
10.1175/JAMC-D-11-094.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Summer rainfall characteristics over the Korean Peninsula are examined using six years of Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) measurements and surface rain measurements from the densely populated rain gauges spread across South Korea. A comparison of the TMI brightness temperature at 85 GHz with the measured surface rain rate reveals that a significant portion of rainfall over the peninsula occurs at warmer brightness temperatures than would be expected from the Goddard profiling (GPROF) database. By incorporating the locally observed rain characteristics into the GPROF algorithm, efforts are made to test whether locally appropriate hydrometeor profiles may be used to improve the retrieved rainfall. Profiles are obtained by simulating rain cases using the cloud-resolving University of Wisconsin Nonhydrostatic Modeling System (UW-NMS) model and matching the calculated radar reflectivities to TRMM precipitation radar (PR) reflectivities. Selected profiles and the corresponding simulated TMI brightness temperatures (limited in this study to values that are larger than 235 K) are added to the GPROF database to form a modified database that is considered to be more suitable for local application over the Korean Peninsula. The rainfall retrieved from the new database demonstrates that heavy-rainfall events-in particular, those associated with warmer clouds-are better captured by the new algorithm as compared with the official TRMM GPROF version-6 retrievals. The results suggest that a more locally suitable rain retrieval algorithm can be developed if locally representative rain characteristics are included in the GPROF algorithm.
引用
收藏
页码:786 / 798
页数:13
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