Benchmark climate models for Indo-‐Pacific variability
Impact of extreme El Niño events
2 |
January 1998, Peru
3 |
1994, Gash River flooding in Kassala, Eastern Sudan, 300,000 displaced
4 |
Characteris?cs of extreme El Ninos
5 |
Green 5 mm per day
6 |
Extreme events
Warm pool (purple) extends to east Pacific
ITCZ moves to eastern equatorial Pacific
Zonal SPCZ
7 |
Box 1 SST – Box 2 SST < 0
ITCZ moves to the equator
Rainfall skewness 2.7
CMIP3 good models
8 |
(1) Skewness + (2) 5 mm per day
9 |
10 |
CMIP5 good models
11 |
12 |
CMIP3+5 good model ensemble
13 |
There is a doubling of extreme El Nino events
Mechanism
14 |
15 |
16 |
17 |
1997 1995
18 |
Observed IODE skewness is -1
(1) Skewness + (2) Nonlinearity
19 |
20 |
21 |
22 |
23 |
24 |