Download presentation
Presentation is loading. Please wait.
Published byDarren Bradford Modified over 6 years ago
1
IPCC overview: reliability of regional projections
Richard Jones Met Office Hadley Centre
2
IPCC regional predictions
Significant temperature changes are very likely and patterns of change are becoming clear Many statements are made relative to the global average warming which is still uncertain Patterns of precipitation change are becoming clear for many areas but little confidence in the magnitude of the changes Level of confidence/uncertainty is regionally dependent – key regions have high uncertainty Information on extremes and local changes is very patchy
3
IPCC AR4 summary seasonal precipitation change figure
Model consensus implies a level of reliability - but need mechanisms as well Lack of consensus implies no information – - but assessed at grid-scale thus maybe misleading No information on fine temporal or spatial scales
4
Response of All India rainfall (A1B, 2080s)
Most models give positive change Change often large thus policy relevant Support from physical insight
5
Lack of consensus from model patterns
Combination of some pattern and sign differences lead to lack of consensus How relevant is this if monsoon processes are captured in the models?
6
Winter temperature change summary
7
Summer temperature change summary
7
8
NARCCAP models in an IPCC context
9
Winter temperature change: NARCCAP models
CCCMA CCSM GFDL HadCM3
10
Summer temperature change: NARCCAP models
CCCMA CCSM GFDL HadCM3 10
11
Winter precipitation change summary
11
12
Summer precipitation change summary
12
13
Winter precipitation change: NARCCAP models
CCCMA CCSM GFDL HadCM3 13
14
Summer precipitation change: NARCCAP models
CCCMA CCSM GFDL HadCM3 14
15
Precipitation validation - CCCMA
15
16
Precipitation validation - CCSM
16
17
Precipitation validation - GFDL
17
18
Precipitation validation – HadCM3
18
19
CCM3 winter responses ( ) ( ) - ( ) 2m T Precip.
20
CCM3 summer responses ( ) ( ) - ( ) 2m T Precip.
21
CCCMA winter biases ( ) CGCM3-CRU2 2m T Precip.
22
CCCMA summer responses
( ) CGCM3 - CRU2 2m T Precip.
23
CCSM response summary: 2050s – 1980s Temperature and precipitation
24
HadCM3 temperature : model, obs, bias
25
HadCM3 precipitation: model, obs, bias
26
GFDL model response (low/high resolution) winter and summer surface air temperature
27
GFDL model response (low/high resolution) winter and summer precipitation
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.