²ÊÃñ±¦µä

Vogel, Richard M 11 Tufts University, Department of Civil and Environmental EngineeringA general introduction to the new field of ‘hydromorphology’ will be given. Hydromorphology is to hydrology, as geomorphology is to geology.

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, Ï„, 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

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

Mallikamas, Wasin 1 ; Rajaram, Harihar 21 ²ÊÃñ±¦µä2 ²ÊÃñ±¦µäNatural 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

Frederick, Zanden A 1 ; Anderson, Suzanne P 2 ; Striegl, Rob G 31 University of Colorado, Boulder Department of Geography & INSTAAR2 University of Colorado, Boulder Department of Geography &

Dombroski, Daniel E 1 ; Crimaldi, John P 21 University of Colorado at Boulder2 University of Colorado at BoulderFine-scale aspects of stirring and mixing are examined in turbulent boundary layer flow using a three-

Dillin, Matthew 1 ; Neupauer, Roseanna 21 University of Colorado2 University of ColoradoWavelet analysis involves an integral transform of, for example, a permeability data set, using wavelet as the kernel of the