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New Horizons in Paleoclimatology Toby Ault 5.6.2008
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Overview: Proxy-model integration Experiment design Results Future work
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Overview: Proxy-model integration Experiment design Results Future work
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Overview: Proxy-model integration Experiment design Results Future work
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Overview: Proxy-model integration Experiment design Results Future work
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Overview: Proxy-model integration Experiment design Results Future work
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Proxy-Model Integration
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10’s of km GCM Data: Proxy Data: 100’s of km Image from: http://ipcc-wg1.ucar.edu/wg1/Report/AR4WG1_Print_Ch11.pdfhttp://ipcc-wg1.ucar.edu/wg1/Report/AR4WG1_Print_Ch11.pdf
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1°x1° (~111 km)
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Case example: the Monsoon
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August, 2006 PRISM mean precip. (mm/day) http://www.prism.oregonstate.edu/products/viewer.phtml?file=/pub/prism/us/graphics/ppt/2000-2009/us_ppt_2006.08.png&year=2006&vartype=ppt&month=08&status=final&zoom=yes
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Observational Monsoon 0.5˚x 0.5˚ JJA mean precip. (mm/day) *Mitchell, T. D., and P. D. Jones (2005), An improved method of constructing a database of monthly climate observations and associated high-resolution grids, International Journal of Climatology, 25(6), 693-712.
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CCSM3’s Monsoon JAS mean precip. (mm/day)
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CCSM3’s Monsoon JAS mean precip. (mm/day) What about the future?
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*Joellen Russell, Pers. comm. GFDL - Weaker CCSM - No change UKMO - Stronger
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*Joellen Russell, Pers. comm. GFDL - Weaker CCSM - No change UKMO - Stronger No good consensus… Absent in other models… Turn to proxies!
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Mid-Holocene climate http://geochange.er.usgs.gov/sw/impacts/biology/pastclim/
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Proxies in N. America
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http://www.swaebr.org/images/Packrat.jpg
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Wetter summers… OR …drier winters!
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Playa Lakes: Occasionally filled during Mid-Holocene Likely monsoon related… http://en.wikipedia.org/wiki/Playa
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Speleothems: Stronger Monsoon Connection to North Atlantic ITCZ shifted northward?
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Modeling 6ka climates
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PMIP (Paleoclimate Model Intercomparison Project) Mean JJA precipitation for CCSM 6ka simulation http://www.ncdc.noaa.gov/paleo/modelvis.html
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Harrison et al., 2003 CCSM3-JJA: 6ka-0ka (mm/day)
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Harrison et al., 2003 CCSM3-JJA: 6ka-0ka (mm/day) No Change?
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10’s of km GCM Data: Proxy Data: 100’s of km Image from: http://ipcc-wg1.ucar.edu/wg1/Report/AR4WG1_Print_Ch11.pdfhttp://ipcc-wg1.ucar.edu/wg1/Report/AR4WG1_Print_Ch11.pdf
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10’s of km GCM Data: Proxy Data: 100’s of km Can regional downscaling bridge this gap?
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Experiment Design
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Model: WRF Nesting: None Physics: Defaults X-domain: 119˚W to 110˚W Y-domain: 20˚N to 34˚N Resolution: ~30km Time: Aug. 2-25, 2006 T: 3hrs
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Boundary Conditions: NCEP/NCAR Reanalysis 2.5˚x 2.5˚ resolution
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Results
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Means Precipitation (mm/day) NNRPWRF
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Variance Precipitation variance (mm/day) 2 NNRPWRF
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August 2006 - NNRP Link to animation
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August 2006 - WRF Link to animation
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Smaller scale Better representation of mechanisms
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Future Work
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1. Comparison with observations 2. Better analysis of dynamics 3. Cumulus parameterization scheme 4. Downscaling modern CCSM3 runs 5. Paleoclimate downscaling
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1. Comparison with observations 2. Better analysis of dynamics 3. Cumulus parameterization scheme 4. Downscaling modern CCSM3 runs 5. Paleoclimate downscaling
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1. Comparison with observations 2. Better analysis of dynamics 3. Cumulus parameterization scheme 4. Downscaling modern CCSM3 runs 5. Paleoclimate downscaling
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1. Comparison with observations 2. Better analysis of dynamics 3. Cumulus parameterization scheme 4. Downscaling modern CCSM3 runs 5. Paleoclimate downscaling
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1. Comparison with observations 2. Better analysis of dynamics 3. Cumulus parameterization scheme 4. Downscaling modern CCSM3 runs 5. Paleoclimate downscaling
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1. Comparison with observations 2. Better analysis of dynamics 3. Cumulus parameterization scheme 4. Downscaling modern CCSM3 runs 5. Paleoclimate downscaling
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Acknowledgements: Jason Criscio, Andy Penny, and CCIT - THANKS!
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