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Caldwell, Jason 1 ; Rajagopalan, Balaji 21 CIRES/University of Colorado, 91¸£ÀûÉç, CO 80309 USA2 Department of Civil Environmental and Architectural Engineering, University of Colorado, 91¸£ÀûÉç, CO 80309 USAWater

Blom, Tevis 11 University Colorado 91¸£ÀûÉçApril 1st Snow Water Equivalent (SWE) is a useful indicator of potential water resources along Colorado’s Front Range. This is especially so at altitude where snowpack serves as a seasonal storage

Ball, Lyndsay 1 ; Ge, Shemin 2 ; Caine, Jonathan Saul 3 ; Revil, André 4 ;Jardani, Abderrahim 51 Univ. of Colorado/USGS2 Univ. of Colorado3 USGS4 Colorado School of

Alexander, Katie 1 ; Turner, Jane 2 ; Pugh, Evan 3 ; Cullis, James 4 ;McKnight, Diane 51 91¸£ÀûÉç - ENVS2 91¸£ÀûÉç - CVEN3 91¸£ÀûÉç - GEOL4 91¸£ÀûÉç - CVEN5

Aigler, Brent V. 1 ; Ge, Shemin 2 ; McCaffree, Charles A. 31 Environmental Studies & INSTAAR, CU-91¸£ÀûÉç2 Geological Sciences & INSTAAR, CU-91¸£ÀûÉç3 University of Colorado at

Abel, Kali M 1 ; Anderson, Robert S 2 ; Stock, Greg 31 University of Colorado and INSTAAR2 University of Colorado and INSTAAR3 National Park ServiceThe two largest glaciers in Yosemite National Park

Weingarten, Matthew 1 ; Hsieh, Paul 21 University of Colorado at 91¸£ÀûÉç, 91¸£ÀûÉç, CO, USA2 U.S. Geological Survey, Menlo Park, CA, USASolute transport through fractured porous rocks can be described by advective-

Underhill, Vivian R 11 University of ColoradoWith rising global temperatures, a major concern is that fresh water from melting glaciers and the Greenland ice sheet will slow down global oceanic circulation patterns, in particular the North

Rengers, Francis Kevin 1 ; Moody, John 2 ; Ebel, Brian 31 University of Colorado2 USGS3 USGSRecently new work has begun to try to model the sediment deposition and erosion patterns that occurred in

Perrot, Danielle O. 1 ; Molotch, Noah P. 2 ; Musselman, Keith N. 3 ; Pugh, Evan T. 41 University of Colorado at 91¸£ÀûÉç2 University of Colorado at 91¸£ÀûÉç3 University of California,