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What  new information do What  new information do

What new information do - PowerPoint Presentation

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Uploaded On 2023-11-22

What new information do - PPT Presentation

we get from climate models with higher resolution Gustav Strandberg Paula Gonzalez Galia Guentchev and Gerard van der Schrier Swedish Meteorological and Hydrological Institute ID: 1034395

high res models precipitation res high precipitation models resolution primavera higher cmip5 compared danube extreme basin climate hydrological specific

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1. What new information do we get from climate models with higher resolution?Gustav Strandberg*, Paula Gonzalez, Galia Guentchev and Gerard van der Schrier *Swedish Meteorological and Hydrological Institute

2. Why is model resolution important?Topography in different models (meter above sea level)Primavera low res. ~100 km Primavera high res. ~50 km CORDEX high res. ~12 km

3. High resolution is expensive50 km

4. High resolution is expensive25 km50 km

5. High resolution is expensive12.5 km25 km50 kmDoubling the resolution (e.g. 50 to 25 km) means 8 times the computer power

6. Some important abbreviationsModel families:CMIP5 = Global climate models used in the last IPCC assessment PRIMAVERA = Global models used in the PRIMAVERA projectCORDEX = Regional climate models of higher resolution

7. By the looks of it …Low res.High res.MPI-ESM-1-2 CNRM-CM6-1 HadGEM3-GC31 EC-Earth3 ECMWF-IFSEOBSPrmean (mm/day)Precipitation benefits from higher resolution

8. By the looks of it …Low res.High res.MPI-ESM-1-2 CNRM-CM6-1 HadGEM3-GC31 EC-Earth3 ECMWF-IFSEOBSEspecially extreme precipitation benefits from higher resolutionrx1day (mm)

9. Individual models over a specific regionBRI = British IslesNo systematic differences between high and low res. for temperatureTemperature

10. Individual models over a specific regionBRI = British IslesNo systematic differences between high and low res. for temperatureSome tendency for more precipitation in high res. Higher maximum precip.TemperaturePrecipitation

11. PRIMAVERA in perspective of CMIP5 and CORDEXHigh res.Low res.ScandinaviaPrecip.

12. PRIMAVERA in perspective of CMIP5 and CORDEXIncreasing precipitation with higher resolution is a robust feature over different ensemblesHigh res.Low res.High res.Low res.ScandinaviaBritish IslesPrecip.Precip.

13. Precipitation intensitiesMedian99th percentileX Low res.X High res.

14. Precipitation intensitiesMedianMedian99th percentile99th percentileX Low res.X High res.X High res. – low res.Higher resolution mainly changes precipitation in the high end of the distribution (more extreme precipitation).

15. Precipitation intensitiesThe Alps

16. Precipitation intensitiesHigher resolution mainly changes precipitation in the high end of the distribution (more extreme precipitation).The AlpsMid Europe

17. Precipitation intensitiesHigher resolution mainly changes precipitation in the high end of the distribution (more extreme precipitation).The AlpsMid Europe

18. Let’s look at extra-tropical cyclones (ETCs)

19. ETC densitiesChange in storm track bias (as compared to ERA Interim) between CMIP5 and PRIMAVERA models.Mainly PRIMAVERA models are characterised by smaller biases overall compared to the CMIP5 models CMCCCNRMEC-EarthRed colours = reduction in bias for PRIMAVERAMPIMOHC

20. Frequency Anomalies of maximum Vorticity of ETCSBiases are largely reduced in the PRIMAVERA models especially regarding the underestimation of the stronger storms with higher vorticityCMIP5 vs ERAMaximum vorticityPRIMAVERA vs ERAMaximum vorticity

21. Let’s have a closer look at the upper Danube basinUpper Danube basin and its topography.

22. Hydrological impact over the upper Danube basinCMIP5CORDEXPRIMAVERANormalized overall error as compared with CRU TS3.25 at the basin scale (1950-2005)Mean temperatureTemperature variability

23. Hydrological impact over the upper Danube basinCMIP5CORDEXPRIMAVERANormalized overall error as compared with CRU TS3.25 at the basin scale (1950-2005)Mean precipitationPrecipitation variability

24. summaryThe general improvement of having higher resolution can be difficult to quantify – is it enough that it looks better?Improvements for specific processes are easier to quantify:Extreme precipitation is better reproduced by high resolution models. Extra Tropical Cyclones are better represented in the PRIMAVERA models compared to CMIP5 A study over the Danube basin shows that the PRIMAVERA models even outperform the CORDEX RCM for a selection of climate variables

25. Thanks for listening!Are there questions?