EAST ASIAN MONSOON Anitha Denny Girish Jisung Latha Nuncio Soojin Xiaobin Xiefei.
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EAST ASIAN MONSOON Anitha Denny Girish Jisung Latha Nuncio Soojin Xiaobin Xiefei
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Transcript of EAST ASIAN MONSOON Anitha Denny Girish Jisung Latha Nuncio Soojin Xiaobin Xiefei.
EAST ASIAN MONSOON
AnithaDennyGirishJisungLathaNuncioSoojinXiaobinXiefei
Nearly a third of the worldPopulation is affected.
PRECIPITATION CLIMATOLOGY EASM REGION
mm
/day
Standard deviations of June-August precipitation
Observation
Difference of June-August precipitation from June-August climatology
NO
AA
,esm
2mN
OA
A,e
sm2g
NO
AA
,CM
3N
CC
-NO
RN
AS
A-G
ISS
MR
I-C
GC
M
MP
I-E
SM
-LM
MP
I-E
SM
-LR
Had
-GE
M-E
SH
ad-G
EM
-CC
MIR
OC
-CH
EM
MIR
OC
-ES
MM
IRO
C-5
IPS
LC
M5B
-LR
IPS
L-5
A-M
RIP
SL
-5A
-LR
INM
-CM
4C
ER
FAC
S
model diff model diff
model diff model diff
NINO3.4 SSTPrecip-JJA
SUMMARY
Variability biases in the precipitation are strong towards the south ofThe EASM region. However some models have a better representation of iteg. HadGEM, MPI and GFDL models.
SST during JJA is best captured by HadGem models. But DJF SSTs are not wellrepresented. Large uncertainty in simulating northwest Pacific SSTs by all modelspossibly because of the inadequate representation of Kuroshio dynamics.
Tele-connections of ENSO is manifested by Rossby wave trains (Wang, etal., 2001). It need to be seen how these wave trains are represented in models
