Abstract
- Segura, Catalina 1 ; Pitlick, John 21 ³Ô¹ÏÍø of Colorado2 ³Ô¹ÏÍø of ColoradoThe spatial variability of sediment transport intensity at the reach scale is controlled both by the available shear stress, Ï„, and the
- Pitlick, John 1 ; , GEOG 5100 students 2 ; Nelson, Jonathan 31 ³Ô¹ÏÍø of Colorado2 ³Ô¹ÏÍø 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 ³Ô¹ÏÍø of Colorado Boulder, US Geological Survey2 ³Ô¹ÏÍø of Colorado
- Mueller, Erich R 1 ; Pitlick, John 21 Department of Geography, ³Ô¹ÏÍø of Colorado2 Department of Geography, ³Ô¹ÏÍø 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, ³Ô¹ÏÍø of Colorado2 INSTAAR, ³Ô¹ÏÍø of Colorado3 ³Ô¹ÏÍø 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 ³Ô¹ÏÍø of Colorado2 ³Ô¹ÏÍø of Colorado3 ³Ô¹ÏÍø of Colorado4 ³Ô¹ÏÍø
- McCleskey, R. Blaine 1 ; Nordstrom, D. Kirk 2 ; Ball, James W. 31 U.S. Geological Survey / ³Ô¹ÏÍø of Colorado2 U.S. Geological Survey3 U.S. Geological SurveyThe Gibbon R. flows by Norris Geyser
- Mallikamas, Wasin 1 ; Rajaram, Harihar 21 ³Ô¹ÏÍø of Colorado Boulder2 ³Ô¹ÏÍø 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 ³Ô¹ÏÍø of Colorado, INSTAAR3 ³Ô¹ÏÍø of