Assimilation of the FY-4A AGRI Clear-Sky Radiance Data in a Regional Numerical Model and Its Impact on the Forecast of the "21•7" Henan Extremely Persistent Heavy Rainfall

被引:31
作者
Xu, Lan [1 ,2 ]
Cheng, Wei [3 ]
Deng, Zhongren [4 ]
Liu, Juanjuan [1 ,2 ]
Wang, Bin [1 ,2 ]
Lu, Bin [5 ]
Wang, Shudong [6 ]
Dong, Li [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
[3] Beijing Inst Appl Meteorol, Beijing 100029, Peoples R China
[4] Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster Minist Educ KLME, Joint Int Res Lab Climate & Environm Change ILCEC, Nanjing 210044, Peoples R China
[5] China Meteorol Adm, Inst Urban Meteorol, Beijing 100089, Peoples R China
[6] China Meteorol Adm, Publ Meteorol Serv Ctr, Beijing 100081, Peoples R China
基金
国家重点研发计划;
关键词
FY-4A; AGRI; clear-sky radiance; satellite data assimilation; 21; 7" Henan extremely persistent heavy rainfall; INFRARED BRIGHTNESS TEMPERATURES; RADIATIVE-TRANSFER MODEL; BIAS CORRECTION SCHEME; ALL-SKY; WEATHER PREDICTION; SATELLITE DATA; SEVERE STORM; PART I; HIMAWARI-8; WATER;
D O I
10.1007/s00376-022-1380-3
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Assimilation of the Advanced Geostationary Radiance Imager (AGRI) clear-sky radiance in a regional model is performed. The forecasting effectiveness of the assimilation of two water vapor (WV) channels with conventional observations for the "21 center dot 7" Henan extremely heavy rainfall is analyzed and compared with a baseline test that assimilates only conventional observations in this study. The results show that the 24-h cumulative precipitation forecast by the assimilation experiment with the addition of the AGRI exceeds 500 mm, compared to a maximum value of 532.6 mm measured by the national meteorological stations, and that the location of the maximum precipitation is consistent with the observations. The results for the short periods of intense precipitation processes are that the simulation of the location and intensity of the 3-h cumulative precipitation is also relatively accurate. The analysis increment shows that the main difference between the two sets of assimilation experiments is over the ocean due to the additional ocean observations provided by FY-4A, which compensates for the lack of ocean observations. The assimilation of satellite data adjusts the vertical and horizontal wind fields over the ocean by adjusting the atmospheric temperature and humidity, which ultimately results in a narrower and stronger WV transport path to the center of heavy precipitation in Zhengzhou in the lower troposphere. Conversely, the WV convergence and upward motion in the control experiment are more dispersed; therefore, the precipitation centers are also correspondingly more dispersed.
引用
收藏
页码:920 / 936
页数:17
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