Abstract

Segura, Catalina 1 ; Pitlick, John 21 University of Colorado2 University of ColoradoThe spatial variability of sediment transport intensity at the reach scale is controlled both by the available shear stress, τ, and the

Pitlick, John 1 ; , GEOG 5100 students 2 ; Nelson, Jonathan 31 University of Colorado2 University of Colorado3 US Geological SurveyThe bed roughness in headwater streams is generally large in

Nielson, Ashley 1 ; Williams, Mark 2 ; Caine, Nel 31 INSTAAR,Niwot Ridge LTER,Department of Geography2 INSTAAR,Niwot Ridge LTER,Department of Geography3 INSTAAR,Niwot Ridge LTER,Department of

Nanus, Leora 1 ; Williams, Mark W 2 ; Campbell, Donald H 3 ; Kendall, Carol 4; Elliott, Emily M 51 University of Colorado Boulder, US Geological Survey2 University of Colorado

Mueller, Erich R 1 ; Pitlick, John 21 Department of Geography, University of Colorado2 Department of Geography, University of ColoradoChannel morphology in streams and rivers is a product of the watershed scale flux of

Miller, Matthew 1 ; McKnight, Diane 2 ; Borgnis, Evyan 31 INSTAAR, University of Colorado2 INSTAAR, University of Colorado3 University of San FranciscoThe pulse of dissolved organic matter (DOM) that

McCutchan, Jr., James H 1 ; Lewis, Jr., William M 2 ; Blankenship, Ariann L 3 ; Oppold, Mary 41 University of Colorado2 University of Colorado3 University of Colorado4 University

McCleskey, R. Blaine 1 ; Nordstrom, D. Kirk 2 ; Ball, James W. 31 U.S. Geological Survey / University of Colorado2 U.S. Geological Survey3 U.S. Geological SurveyThe Gibbon R. flows by Norris Geyser

Mallikamas, Wasin 1 ; Rajaram, Harihar 21 University of Colorado Boulder2 University of Colorado BoulderNatural rock fractures are characterized by highly irregular rough walls, which are best modeled as spatially

Hill, Kenneth 1 ; Williams, Mark 2 ; Caine, Nel 3 ; Janke, Jason 4 ; Hartman, Melannie 51 Univeristy of Colorado, INSTAAR2 University of Colorado, INSTAAR3 University of