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Shoaei, Farrokh 1 ; Crimaldi, John P. 21 University of Colorado Boulder2 University of Colorado Boulder Abstract to be uploaded later.

Famiglietti, Jay 11 NASA Jet Propulsion LaboratoryJust as the settling and development of the arid American West was fueled by harnessing its available fresh water, the growing lack of water availability may well be its undoing. California

Zhang, Qinghuan 1 ; Williams, Mark 2 ; Cowie, Rory 31 Geography & INSTAAR, University of Colorado Boulder2 Geography & INSTAAR, University of Colorado Boulder3 Geography & INSTAAR,

Yates, David 1 ; Miller, Kathleen A 2 ; Wilby, Robert L 3 ; Kaatz, Laurna 42 Presenting Author1 NCAR2 NCAR3 Loughborough University4 Denver WaterDrought episodes and climate

Wohl, Ellen 11 Colorado State UniversityChannel-spanning logjams occur on rivers throughout Rocky Mountain National Park. Each jam creates a backwater area in which finer sediment and organic matter are deposited. Jams thus slow the

Wilson, Alāna M. 1 ; Williams, Mark W. 21 Geography & INSTAAR, ���Ҵ�ý�ƽ������2 Geography & INSTAAR, ���Ҵ�ý�ƽ������New results from tritium (H3) analysis of waters from the Langtang Valley, Nepal offer insight into the

Weingarten, Matthew 1 ; Ge, Shemin 21 University of Colorado-Boulder2 University of Colorado-BoulderAn unprecedented increase in earthquakes in the central and eastern US (CEUS) began in 2009. Many of these earthquakes

Watson, Abigail 1 ; Kasprzyk, Joseph 21 CU-Boulder2 CU-BoulderIncreasingly, decision support systems seek to provide structured robust decision-making support for stakeholders and decision makers under the context of

Tomkinson, Lauren J 11 INSTAARThe Center for Water, Earth Science and Technology (CWEST) is a scientific and educational partnership between the U.S. Geological Survey (USGS) and ���Ҵ�ý�ƽ������. Housed within the Institute of Arctic and Alpine

Thompson, Sally 11 University of California, BerkeleySeasonally dry ecosystems (or SDEs) include Mediterranean, Monsoonal and Tropically Dry climates. SDEs occur worldwide and share a pronounced contrast in precipitation between a wet