TY - JOUR
T1 - Vertical Structures of Typical Meiyu Precipitation Events Retrieved From GPM-DPR
AU - Sun, Yuting
AU - Dong, Xiquan
AU - Cui, Wenjun
AU - Zhou, Zhimin
AU - Fu, Zhikang
AU - Zhou, Lingli
AU - Deng, Yi
AU - Cui, Chunguang
N1 - Funding Information:
This study was jointly supported by the National Natural Science Foundation of China (under grant 41620104009) and the National Key Research and Development Program of China (under grant 2018YFC1507200). This study was also funded by the Hubei Meteorological Bureau Project (under grants 2018Z05 and 2019Q02). The authors are grateful for the CNSMC of CMA, the Japan Aerospace Exploration Agency (JAXA), and National Aeronautics and Space Administration (NASA) for providing the FY‐2G, FY‐2E, and GPM observation data sets. FY‐2G data and FY‐2E data are available at http://satellite.nsmc.org.cn ; GPM version 06A 2ADPR data are available at the Precipitation Processing System, NASA Goddard Space Flight Center ( https://storm.pps.eosdis.nasa.gov/storm/data/Service.jsp?serviceName=Order ). The surface disdrometer measurements used in this study will be available at http://doi.org/10.5281/zenodo.3579584 .
Funding Information:
This study was jointly supported by the National Natural Science Foundation of China (under grant 41620104009) and the National Key Research and Development Program of China (under grant 2018YFC1507200). This study was also funded by the Hubei Meteorological Bureau Project (under grants 2018Z05 and 2019Q02). The authors are grateful for the CNSMC of CMA, the Japan Aerospace Exploration Agency (JAXA), and National Aeronautics and Space Administration (NASA) for providing the FY-2G, FY-2E, and GPM observation data sets. FY-2G data and FY-2E data are available at http://satellite.nsmc.org.cn; GPM version 06A 2ADPR data are available at the Precipitation Processing System, NASA Goddard Space Flight Center (https://storm.pps.eosdis.nasa.gov/storm/data/Service.jsp?serviceName=Order). The surface disdrometer measurements used in this study will be available at http://doi.org/10.5281/zenodo.3579584.
Publisher Copyright:
©2019. American Geophysical Union. All Rights Reserved.
PY - 2020/1/16
Y1 - 2020/1/16
N2 - This work for the first time analyzed the vertical structures of the different stages of Meiyu precipitation systems over the Yangtze-Huai River Valley in central China using measurements and retrievals from the Global Precipitation Measurement Mission Dual-Frequency Precipitation Radar (GPM-DPR) and Feng Yun satellites. GPM-DPR-retrieved near-surface rain and drop size distributions were first validated against the surface disdrometer measurements and showed good agreement. Then we analyzed three cases from the Integrative Monsoon Frontal Rainfall Experiment to demonstrate the different characteristics of convective precipitation and stratiform precipitation (SP) in the developing, mature, and dissipating stages of the Meiyu precipitation systems, respectively. For statistical analysis, all Meiyu cases during the period 2016–2018 detected by GPM-DPR were collected and classified into different types and stages. In the stratiform regions of Meiyu precipitation systems, coalescence slightly overwhelms breakup and/or evaporation processes, but it was dominant in the convective regions when raindrops fall. There were large numbers of large ice particles during the developing stage due to strong updrafts and abundant moisture, whereas there were both large ice and liquid particles in the mature stage. The vertical structures of the SP examined in this study were similar to those over the ocean regions due to high relative humidity but different to the mountainous west regions of the USA. The findings of the stage-dependent SP vertical structures provide better understanding of the evolution of monsoon frontal precipitation, as well as the associated microphysical properties, and provide insights to improve microphysical parameterization in future models.
AB - This work for the first time analyzed the vertical structures of the different stages of Meiyu precipitation systems over the Yangtze-Huai River Valley in central China using measurements and retrievals from the Global Precipitation Measurement Mission Dual-Frequency Precipitation Radar (GPM-DPR) and Feng Yun satellites. GPM-DPR-retrieved near-surface rain and drop size distributions were first validated against the surface disdrometer measurements and showed good agreement. Then we analyzed three cases from the Integrative Monsoon Frontal Rainfall Experiment to demonstrate the different characteristics of convective precipitation and stratiform precipitation (SP) in the developing, mature, and dissipating stages of the Meiyu precipitation systems, respectively. For statistical analysis, all Meiyu cases during the period 2016–2018 detected by GPM-DPR were collected and classified into different types and stages. In the stratiform regions of Meiyu precipitation systems, coalescence slightly overwhelms breakup and/or evaporation processes, but it was dominant in the convective regions when raindrops fall. There were large numbers of large ice particles during the developing stage due to strong updrafts and abundant moisture, whereas there were both large ice and liquid particles in the mature stage. The vertical structures of the SP examined in this study were similar to those over the ocean regions due to high relative humidity but different to the mountainous west regions of the USA. The findings of the stage-dependent SP vertical structures provide better understanding of the evolution of monsoon frontal precipitation, as well as the associated microphysical properties, and provide insights to improve microphysical parameterization in future models.
KW - Drop Size Distribution
KW - GPM-DPR
KW - Meiyu Precipitation
KW - Microphysical Process
KW - Vertical Structures
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U2 - 10.1029/2019JD031466
DO - 10.1029/2019JD031466
M3 - Article
AN - SCOPUS:85078243231
SN - 2169-897X
VL - 125
JO - Journal of Geophysical Research Atmospheres
JF - Journal of Geophysical Research Atmospheres
IS - 1
M1 - e2019JD031466
ER -