1 / 19

Vimal Mishra 1 , Francina Dominguez 2 , and Dennis P. Lettenmaier 1

Precipitation Extremes in Western U.S. Urban Areas: How Reliable are Regional Climate Model Projections. Vimal Mishra 1 , Francina Dominguez 2 , and Dennis P. Lettenmaier 1 1 Civil and Environmental Engineering, University of Washington, Seattle, WA 2 University of Arizona, Tucson, AZ.

echo-hobbs
Télécharger la présentation

Vimal Mishra 1 , Francina Dominguez 2 , and Dennis P. Lettenmaier 1

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Precipitation Extremes in Western U.S. Urban Areas: How Reliable are Regional Climate Model Projections Vimal Mishra1, Francina Dominguez2, and Dennis P. Lettenmaier1 1Civil and Environmental Engineering, University of Washington, Seattle, WA 2University of Arizona, Tucson, AZ PNW Climate Science Conference,2011 vmishra@hydro.washington.edu

  2. Introduction

  3. Introduction “there is now mounting evidence to suggest that a warmer climate will be one in which the hydrological cycle will in general be more intense, leading to more heavy rain events” (IPCC, 1996) Warmer Climate Intensified Hydrologic Cycle More Precipitation Extremes

  4. Precipitation Extremes Trends in heavy and very heavy rain events Groisman et al., 2005, J. of Climate

  5. Human contribution to more-intense precipitation extremes Given that atmospheric water-holding capacity is expected to increase roughly exponentially with temperature—and that atmospheric water content is increasing in accord with this theoretical expectation—it has been suggested that human-influenced global warming may be partly responsible for increases in heavy precipitation. S-K Min et al.Nature470, 378-381 (2011) doi:10.1038/nature09763

  6. Need for the regional climate models for precipitation extremes • Spatial resolution of GCMs is too coarse to resolve the processes that control precipitation extremes • RCMs partially resolved finer scale variability related to topography and land cover • However, RCMs have been evaluated for precipitation extremes in urban areas Source: NCAR

  7. Precipitation Extremes and Urban Areas • About 80% of U.S. population lives in urban areas • Urban areas have large infrastructure and wealth and precipitation extremes may cause more damage than expected • Increasing precipitation extremes may lead to substantial changes in drainage water infrastructure

  8. Precipitation Extremes in Urban Areas August 8, 2007, 8:49 AM Flooding Cripples Subway System (New York Times) HEAVY RAIN CAUSES MORE FLOODING IN CHICAGO SUBURBS Friday, August 24, 2007

  9. Introduction • So far relatively little work has been done evaluating the ability of RCMs to simulate precipitation extremes in major urban areas in U.S. Science Question How effective are RCM-downscaled climate simulations in reconstructing observed sub-daily to daily scale precipitation extremes over the major urban areas in the western United States?

  10. Study Region • 20 major urban areas across the Western United States • Hourly precipitation data from the nearby stations

  11. Data • Observed hourly precipitation data from NCDC • RCMs simulated 3-hourly data from North American Regional Climate Change Program (NARCCAP) • GCM boundary conditions [1968-1999] • Reanalysis boundary conditions [1979-2003] • Spatial Resolution– 50 km • Models: RCM3, CRCM, HRM3, MM5I, ECPC

  12. Analysis • Data quality check- years with more than 10% missing data were removed • Extracted observed and RCMs simulated precipitation maxima at 3, 6, 12 and 24 hour durations • Used areal reduction factor to convert point precipitation measurement to their areal equivalent • Estimated annual precipitation maxima for 2 to 100 years return period using the Generalized Extreme Value (GEV) distribution • Estimated ensemble mean bias in characteristics of precipitation maxima from the RCMs

  13. Can RCMs reproduce the timing of precipitation maxima ? Summer Winter

  14. Can RCMs reproduce the timing of precipitation maxima ? Summer Winter

  15. Ensemble mean percentage bias in annual precipitation maxima • Overestimation in the Interior west • Underestimation in the southwest GCM Reanalysis

  16. Ensemble mean percentage bias in variability in annual precipitation maxima • Overestimation and underestimation of variability in annual precipitation maxima in majority of urban areas GCM Reanalysis

  17. Ensemble mean percentage bias annual precipitation maxima at 5 and 100 years return period • Overestimation in the Interior west • Underestimation in the southwest GCM Reanalysis

  18. Conclusions • Regardless of the boundary conditions (reanalysis/GCM), most of the NARCCAP RCMs are unable to reproduce the seasonality of precipitation extremes • RCMs underestimate annual precipitation maxima in urban areas located in the coastal and southwest regions, while overpredict in the interior

  19. Conclusions • RCMs overestimated (underestimated) precipitation maxima at 5 and 100 years return intervals for most of the urban areas in the interior (southwest) • The deficiencies in RCMs may be attributable to the coarse resolution and parameterization related to the processes of precipitation extremes • Further improvements are needed in RCMs before they can be considered reliable source of information for engineering design purpose.

More Related