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Climate Change and Projection for Asia

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Presentation on theme: "Climate Change and Projection for Asia"— Presentation transcript:

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

9

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!


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