91ÃÛÌÒ¸ó

Segura, Catalina 1 ; Pitlick, John 21 91ÃÛÌÒ¸ó2 91ÃÛÌÒ¸óThe 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 91ÃÛÌÒ¸ó2 91ÃÛÌÒ¸ó3 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, 91ÃÛÌÒ¸ó2 Department of Geography, 91ÃÛÌÒ¸óChannel morphology in streams and rivers is a product of the watershed scale flux of

Mallikamas, Wasin 1 ; Rajaram, Harihar 21 91ÃÛÌÒ¸ó 91ÃÛÌÒ¸ó2 91ÃÛÌÒ¸ó 91ÃÛÌÒ¸óNatural 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 91ÃÛÌÒ¸ó, INSTAAR3 University of

Frederick, Zanden A 1 ; Anderson, Suzanne P 2 ; Striegl, Rob G 31 91ÃÛÌÒ¸ó, 91ÃÛÌÒ¸ó Department of Geography & INSTAAR2 91ÃÛÌÒ¸ó, 91ÃÛÌÒ¸ó Department of Geography &

Dombroski, Daniel E 1 ; Crimaldi, John P 21 91ÃÛÌÒ¸ó at 91ÃÛÌÒ¸ó2 91ÃÛÌÒ¸ó at 91ÃÛÌÒ¸óFine-scale aspects of stirring and mixing are examined in turbulent boundary layer flow using a three-

Dillin, Matthew 1 ; Neupauer, Roseanna 21 91ÃÛÌÒ¸ó2 91ÃÛÌÒ¸óWavelet analysis involves an integral transform of, for example, a permeability data set, using wavelet as the kernel of the

Cawley, Kaelin M 1 ; McKnight, Diane M 21 91ÃÛÌÒ¸ó at 91ÃÛÌÒ¸ó2 91ÃÛÌÒ¸ó at 91ÃÛÌÒ¸óHarmful algal blooms (HABs) are a global concern in freshwater and coastal ecosystems because they can lead