2008
- Williams, Mark WÌý11ÌýCU-91ÃÛÌÒ¸óMountains, like the polar regions, are likely to experience the effects of global warming before lowland sites. Seasonally snow-covered areas are like canaries in a coal mine; early warning systems that
- Vogel, Richard MÌý11ÌýTufts 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, CatalinaÌý1Ìý;ÌýPitlick, JohnÌý21Ìý91ÃÛÌÒ¸ó2Ìý91ÃÛÌÒ¸óThe spatial variability of sediment transport intensity at the reach scale is controlled both by the available shear stress, Ï„, and the
- Pitlick, JohnÌý1Ìý;Ìý, GEOG 5100 studentsÌý2Ìý;ÌýNelson, JonathanÌý31Ìý91ÃÛÌÒ¸ó2Ìý91ÃÛÌÒ¸ó3ÌýUS Geological SurveyThe bed roughness in headwater streams is generally large in
- Nielson, AshleyÌý1Ìý;ÌýWilliams, MarkÌý2Ìý;ÌýCaine, NelÌý31ÌýINSTAAR,Niwot Ridge LTER,Department of Geography2ÌýINSTAAR,Niwot Ridge LTER,Department of Geography3ÌýINSTAAR,Niwot Ridge LTER,Department of
- Nanus, LeoraÌý1Ìý;ÌýWilliams, Mark WÌý2Ìý;ÌýCampbell, Donald HÌý3Ìý;ÌýKendall, CarolÌý4;ÌýElliott, Emily MÌý51Ìý91ÃÛÌÒ¸ó 91ÃÛÌÒ¸ó, US Geological Survey2Ìý91ÃÛÌÒ¸ó
- Mueller, Erich RÌý1Ìý;ÌýPitlick, JohnÌý21ÌýDepartment of Geography, 91ÃÛÌÒ¸ó2ÌýDepartment of Geography, 91ÃÛÌÒ¸óChannel morphology in streams and rivers is a product of the watershed scale flux of
- Miller, MatthewÌý1Ìý;ÌýMcKnight, DianeÌý2Ìý;ÌýBorgnis, EvyanÌý31ÌýINSTAAR, 91ÃÛÌÒ¸ó2ÌýINSTAAR, 91ÃÛÌÒ¸ó3ÌýUniversity of San FranciscoThe pulse of dissolved organic matter (DOM) that
- McCutchan, Jr., James HÌý1Ìý;ÌýLewis, Jr., William MÌý2Ìý;ÌýBlankenship, Ariann LÌý3Ìý;ÌýOppold, MaryÌý41Ìý91ÃÛÌÒ¸ó2Ìý91ÃÛÌÒ¸ó3Ìý91ÃÛÌÒ¸ó4ÌýUniversity
- McCleskey, R. BlaineÌý1Ìý;ÌýNordstrom, D. KirkÌý2Ìý;ÌýBall, James W.Ìý31ÌýU.S. Geological Survey / 91ÃÛÌÒ¸ó2ÌýU.S. Geological Survey3ÌýU.S. Geological SurveyThe Gibbon R. flows by Norris Geyser