气象卫星资料同化研究进展
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资料同化研究进展: 1 Overview
2 Approaches to assimilation
Infrared radiances (15.5–3.7 μm):
()cld L f 云量,云顶高度
1、单一层假设
2、简化的云参数,来自观测的估计,而在实际大气中,它们是不均匀和非线性的。
3、按线性组合来解释云辐射
NWP centre Model Global
Regional In the study
Infrared
Microwave
ECMWF
IFS
HIRS/AIRS/I ASI (4D-Var)
SSMI(S)/AMSR-E/TMI (4D-Var)
“all-sky system ”AMSU-A ch 3、4
ground-based radar
precipitation in the global 4D-Var system
JMA GSM MSM
AMSR-E/TMI (4D-Var in MSM)
Ground-based radar precipitation in MSM (4D-Var (2002) MF
(France)
ARPEGE AROME
AIRS/IASI
Ground radar network
(1D+3D-Var) (April 2010)
UKMO UK NAE AIRS/IASI (1D-Var/4D-V ar) AMSU-A ch 1 、2 (4D-Var) (‘Total ’ RH ) Radar rain rate(LHN) SEVIRI(1D+4D-Var) radar rain data in NAE 4D-Var NCEP
GFS NAM WRF
TMI-retrieved surface rainrate/ AMSU-A radiance data affected by clouds over ocean in GDAS
(Normalized RH and cloud water mixing ratio )
,+()cld cld cld o cld L L L p εε
=(1-N )N
τε
N(1-)=N
几何因子N ≠模式(物理)云量
εN ≠物理发射率
cld p ≠物理云顶
MMR (the Multi-variate Minimum Residual )
MMR Cloud detection :
3
k N
1
n
cld
k
k
k R N R N R ν
νν
==+∑
2
k N
ECMWF’s IFS
NCAR’s WRF 1
k N
NCEP’s GSI
Pixel
Cloud-top pressure(hPa) derived from Aqua MODIS
Cloud-top pressure(hPa)derived from AIRS using the NCAR MMR method
Mean temperature analysis impact (K) of cloud-affected infrared sounder radiance data assimilation experiments :
700hpa 850hpa
ECMWF:(September–November 2009)
M´et´eo-France:(September 2010)
Environment Canada:(September 2010)
Relative change in RMS forecast errors for selected parameters between clear + cloud-affected and clear-sky only infrared radiance data assimilation experiments:
Met Office(December 2008):
M´et´eo-France(December2008):
Microwave radiances:
Quality Control in WRF-Var :
•AIRS: Multivariate Minimum Residual (MMR) scheme for cloud detection
•AMSU, MHS, SSMIS: Scatter Index(SI)and Background CLWP for precipitation check
云检测:
对AMSU-A:散射因子、降水概率和小雨检测
对AMSU-B:通道2亮温模拟观测误差、Bennartz散射因子
UKMO:
AMSU-A channels 1 and 2
ECMWF:
“all-sky system”:AMSU-A ch 3、4,区域主要是中纬度洋面。
AMSU-A channels 5 and 6: 700hpa,400hpa,对流性云水汽凝结现象
Mean first-guess departure difference (K) of Metop AMSU-A channel 4 radiances in the radiative transfer calculations(1–8 February 2010)
(a) cloud effects are ignored VS (b) cloud effects are included