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Final Report Supplement - Joint Fire Science Program

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Zotero <strong>Report</strong> zotero://report/items/520446_XG98FERT-520446_89BHQIMS-520446...<br />

URL http://hol.sagepub.com/cgi/content/abstract/12/5/597<br />

Extra Keywords: fire history; dendrochronology; climate; fire scars; El Niño-Southern Oscillation; Pacific Northwest<br />

USA.<br />

Date Added Monday, August 29, 2011 5:30:07 PM<br />

Modified Monday, August 29, 2011 5:34:29 PM<br />

Anthropogenic reduction of Santa Ana winds<br />

Type Conference Paper<br />

Author Mimi Hughes<br />

Author Alex Hall<br />

Author Jinwon Kim<br />

Abstract The frequency of Santa Ana wind events is investigated within a high-resolution downscaling of the European<br />

Centre for Medium-Range Weather Forecasts ERA-40 reanalysis data to 6-kilometer resolution over Southern<br />

California. In this climate reconstruction, the number of Santa Ana days per winter season declines significantly<br />

over the 44-year reanalysis period, resulting in over 30 percent fewer events per year over the final decade of<br />

the reconstruction (1991–2001) compared to the first decade (1959–1969). This study investigates this signal<br />

further in late-twentieth and mid-twenty-first century realizations of the National Center for Atmospheric<br />

Research Community Climate System Model, version 3.0, global climate change scenario run downscaled to a<br />

12-kilometer resolution over California. The reduction in events per year in the mid-twenty-first century<br />

compared with the late-twentieth century is similar to that seen in the ERA-40 downscaling, suggesting the<br />

cause of the decrease is a change in the climate due to anthropogenic forcing. A regression model is used to<br />

reproduce the Santa Ana time series based on two previously documented forcing mechanisms: synopticallyforced<br />

strong offshore winds at the mountain tops (which transport offshore momentum to the surface), and a<br />

local desert-ocean temperature gradient causing katabatic-like winds as the cold desert air pours down the<br />

coastal topography. Both past and future climate simulations show a large reduction in the contribution of the<br />

local thermodynamic forcing. This reduction is due to the differential warming that occurs during transient<br />

climate change conditions, with more warming in the desert interior than over the ocean. Thus the mechanism<br />

responsible for the decrease in Santa Ana frequency originates from a well-known aspect of the climate<br />

response to increasing greenhouse gases, but cannot be understood or simulated without mesoscale atmospheric<br />

dynamics.<br />

Date August 2009<br />

Proceedings Title Proceedings of the American Geophysical Union 2008 Fall Meeting<br />

Conference Name American Geophysical Union Fall Meeting, San Francisco, CA, 15-19 December 2008<br />

Place Los Angeles, CA<br />

Publisher California Energy Commission, California Climate Change Center<br />

Pages 29 p.<br />

URL http://adsabs.harvard.edu/abs/2008AGUFMGC22A..05H<br />

Archive http://www.energy.ca.gov/2009publications/CEC-500-2009-015/CEC-500-2009-015-F.PDF<br />

Extra Keywords: regional climate; climate change; Santa Ana winds; fire weather; Southern California.<br />

Date Added Monday, August 29, 2011 5:30:07 PM<br />

Modified Monday, August 29, 2011 5:30:07 PM<br />

Application of economic techniques to fire management - A status review and evaluation<br />

Type <strong>Report</strong><br />

Author Julie K. Gorte<br />

Author Ross W. Gorte<br />

Abstract no abstract<br />

<strong>Report</strong> Number GTR lNT-53<br />

<strong>Report</strong> Type General Technical <strong>Report</strong><br />

Place Ogden, UT<br />

Institution U.S. Department of Agriculture, Forest Service, Intermountain Research Station<br />

50 of 626 9/1/2011 11:40 AM

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