Download presentation
Presentation is loading. Please wait.
1
Climate Change and Projection for Asia
Data and Uncertainty\
2
Modeling the climate processes AND Model Outputs for Climate Change Analysis
Climate model is reduced complexity numerical system, which simulates one possible time evolution in which the major features have a response to primary forcing similar to the real world. GCM skill lies at spatial and temporal aggregated scales, hence: Consider the spatial pattern response Consider time averages GCMs have different internal structures, hence positioning of climate boundaries varies between models – this will lead to disagreement between GCMs in transitional climate locations The first step is to validate the model: can it represent the primary processes of relevance for your region?
3
SNU RCM Downscaled Climate Change for East Asia Region
4
SNU RCM Downscaled Climate Change for East Asia Region
5
Dispersion and Inconsistency in downscaling
Seasonal Cycles by RMIP models
6
Dispersion and Inconsistency in climate projections
7
Dispersion and Inconsistency in climate projection
ΔP(mm/day) South China Center China RMIP downscaled Precipitation changes
8
Sources of Uncertainty
Structure of unpredictability of a system, which can arise from a set of sources
10
Interannual variability for future climate by multi-RCMs
Asia Land Ocean Annual T Trends for (c/10yr)
11
Ensembles in RMIP
12
Ensembles in RMIP
13
Ensembles in RMIP Smaller std.?
14
Ensembles in RMIP
15
Ensembles in RMIP Ensemble averages work well for mean climate; Explorer the best methods for evaluating changes and extremes; Use ensemble spread to inform uncertainty;
16
Model outputs and Observation
For surface climate: Daily average MSLP, maximal/minimal temperature, surface wind speed (optional) 3-hourly: 2m temperature, RH, convective precipitation, large scale precipitation, evaporation, 10m wind (U,V) (optional, depending on individual model) For upper level atmosphere Daily average: U, V, T, H at 200, 500, 850 hPa Observation CRU surface temperature, OISST SST APHRODITE and GPCP Precipitation
17
RMIP data http://rmip.nju.edu.cn, available soon,
Contact
18
Thank you!
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.