WA1 2 Redmond

Information about WA1 2 Redmond

Published on October 29, 2007

Author: Nivedi

Source: authorstream.com

Content

Slide1:  Climate in Three Dimensions: Integrated Mountain Climate Observations Kelly T. Redmond Western Regional Climate Center Desert Research Institute CCSP Workshop Climate Science in Support of Decision Making 14-16 November 2005 Arlington VA Slide3:  March 10, 2004 7.5” / 170 mm 12” / 300 mm 55” / 1400 mm 70” / 1800 mm Slide5:  Western Hydrology 101 High elevations: supply region. Low elevations: demand region. Supply largely falls in winter. Demand largely occurs in summer. Usage is often separated from supply, in space and in time. (Can become out of sight, out of mind.) Climates elsewhere matter for local purposes. Water flows toward a) the gravitational center of the earth, b) money. Snow is extremely important (approx 2/3 – 3/4 of water supply). Snow is the cheapest reservoir there is. Slide6:  Western populations depend on a mountain resource base Water The most necessary and most prominent resource. Other major mountain resources are affected by water Timber production and harvest Grazing lands Minerals extraction Recreation Slide7:  Change is under way in all mountain systems: Demographic Large increases in population Wildland – urban interface encroachment Technological Internet, wireless, cable, phone connectivity Physical presence not needed for some occupations Attitudinal Getting away from it all (with everybody else !) Population less tied to urban centers No longer remote and forbidding Physical Habitat fragmentation Atmospheric contaminants Climate Slide8:  www.censusscope.org Population Growth 1990-2000 1 Nevada 66 % 2 Arizona 40 3 Colorado 31 4 Utah 30 5 Idaho 29 10 Washington 21 11 Oregon 20 12 New Mexico 20 16 Alaska 15 18 California 14 20 Montana 13 31 Hawaii 9 32 Wyoming 9 11 contiguous states 11 West 28 Slide9:  www.fs.fed.us/psw/mtnclim Slide10:  CIRMOUNT COORDINATING GROUP Constance I. Millar, Co-Chair USDA Forest Service, Pacific Southwest Research Station, Albany CA Henry F. Diaz, Co-Chair NOAA Climate Diagnostics Center, Boulder CO Daniel R. Cayan University of California, Scripps Institution of Oceanography, La Jolla CA Michael D. Dettinger USGS Water Resources Division, La Jolla CA Daniel B. Fagre USGS Biological Resources Division, West Glacier MT Lisa Graumlich Big Sky Institute, Montana State University, Bozeman MT Greg Greenwood Mountain Research Initiative, Berne, Switzerland Malcolm K. Hughes University of Arizona, Laboratory of Tree-Ring Research, Tucson AZ David L. Peterson USDA Forest Service, Pacific Northwest Research Station, Seattle WA Frank L. Powell University of California, White Mountain Research Station, San Diego CA Kelly T. Redmond Desert Research Institute, Western Regional Climate Center, Reno NV John Smiley University of California, White Mountain Research Station, San Diego CA Nathan L. Stephenson USGS Biological Resources Division, Three Rivers CA Thomas W. Swetnam University of Arizona, Laboratory of Tree-Ring Research, Tucson AZ Connie Woodhouse NOAA Paleoclimatology Program, Boulder CO Slide11:  Meetings Timberline Lodge, Mt Hood, Sept 19-22 AGU Fall 2004 2005 2006 Slide12:  Mapping New Terrain (anticipated date January 2006) Four urgent challenges facing western North America climate science and policy communities: Mountain regions are vastly under-instrumented to measure climate and long-term changes. Research on western mountain climates and ecosystems is intensive, but scattered and poorly integrated. Societal demands on western mountain ecosystems are exponentially escalating, imposing new stresses on natural resources and rural community capacities. Although mountains are particularly vulnerable to climate-change impacts, projected climate changes have generally been ignored in mountain land-use planning and natural-resource policies to the detriment of their ecosystems and natural resources. Slide13:  CIRMOUNT Work Groups Mountain Climate Network (MONET) Kelly Redmond, Mark Losleben 2. Mountain-Based Hydrologic Observatories Roger Bales, Mike Dettinger North American GLORIA (Global Observation Research Initiative in Alpine Environments), alpine plants and climate Connie Millar, Dan Fagre Mountain Ecosystem Responses to Climate Jeremy Littell, Jeff Hicke CIRMOUNT and International Relations, such as Mountain Research Initiative Greg Greenwood, Craig Allen Paleoclimatic Archives for Resource Management Connie Woodhouse, Franco Biondi Slide16:  Courtesy of Mike Dettinger, USGS / Scripps. Dettinger MD. 2005. From climate change spaghetti to climate-change distributions for 21st Century California. San Francisco Estuary and Watershed Science. Vol. 3, Issue 1, (March 2005), Article 4. http://repositories.cdlib.org/jmie/sfews/vol3/iss1/art4 Slide19:  Courtesy of Mike Dettinger, USGS / Scripps. Dettinger MD. 2005. From climate change spaghetti to climate-change distributions for 21st Century California. San Francisco Estuary and Watershed Science. Vol. 3, Issue 1, (March 2005), Article 4. http://repositories.cdlib.org/jmie/sfews/vol3/iss1/art4 Slide20:  A SIMPLE INDEX OF SENSITIVITY OF SNOWFED HYDROCLIMATE TO A +3ºC WARMING … Rain? or Snow? What fraction of each year’s precipitation historically fell on days with average temperatures just below freezing? Less vulnerable More vulnerable Computed from UW’s VIC model daily INPUTS (Bates et al, in rev). Courtesy Mike Dettinger. +3 Slide21:  Potential effects of warming temperatures on the Sacramento / San Joaquin watershed and the San Francisco estuary Noah Knowles and Dan Cayan, Climate Research Division, Scripps Institution of Oceanography P T 6 C Slide22:  1910 Elrod Glacier National Park Archives 1931 Hileman Glacier National Park Archives 1997 Fagre USGS / Glacier National Park Boulder Glacier, 1985-2003. North Cascades Glacier Climate Project Easton Glacier, 1985-2003. Slide23:  Grids. Reanalysis Resolution: Global Regional (slightly smaller; pixel resolution) Desired Resolution About 1 km Slide24:  Sierra Annual Jan-Dec 700 mb Temp (10,000 ft) 1 C Slide25:  Sierra Mar-May 700 mb Temp (10,000 ft) Freezing 1 C Slide26:  Sierra Summer Jun-Aug 700 mb Temp (10,000 ft) 1 C Slide27:  Last six years Sep-Aug Temperature As departure (F) from 1961-1990 1971-2000 1950-1995 1895-2000 Slide28:  August 30, 1997 Agriculture Cities Slide29:  Workshop: Urban Water Supplies and Climate Change in the West 2005 September 22-23 Las Vegas. Sponsors Southern Nevada Water Authority Natural Resources Defense Council Desert Research Institute Purpose Initiation of a dialog: urban water managers and climate scientists Approximately 15 urban water districts, 8 climate specialists. Follow-on: Urban Water Coalition meeting, 2005 October 21, Reno. Represents the major western cities Outcome: 1. Vulnerability to water supply disruption from temperature effects is of significant concern to cities and water suppliers. Climate issues are intersecting with many other stressors. Need to understand entire water budget: atmosphere, surface, groundwater as an integrated system. Keep the dialogue going. Slide30:  CalClim: Integration of networks. Coop RAWS Snotel ASOS Buoy CIMIS CDWR Research But still not enough at higher elevations ! <1640’ <3280’ <4920’ <6560’ <8200’ >8200’ www.calclim.dri.edu Cal Energy Commission Slide31:  South Central Sierra Snow Lab East Photo: Dave Simeral Slide32:  Slide Mountain Toward SSW Slide33:  2003 March 10 Slide34:  White Mountain Summit. Highest active live transmission station in North America. 14246 ft. / 4342 m. Summer 2003 www.wrcc.dri.edu/weather/wmtn.html Slide35:  White Mtn Summit Looking North Slide36:  White Mtn Summit Looking South Slide37:  Mt Warren View looking south up Deer Cr (NB: beautiful Pleistocene Rock Glacial cyn), a tributary of Lundy Cyn (note also limber pines at left foreslope (one of our sites). 7/00 Warren Bench Rd ends here Our highest pine sites here Deer Creek Canyon Lundy Canyon To Mono Lake Mt Warren (12327 ft) Toward South. July 2000. Photo: Connie Millar Slide40:  “You can observe a lot, just by watching.” -Yogi Berra Slide41:  Thank You

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