Abstract
- Weingarten, Matthew 1 ; Hsieh, Paul 21 University of Colorado at Boulder, Boulder, CO, USA2 U.S. Geological Survey, Menlo Park, CA, USASolute transport through fractured porous rocks can be described by advective-
- Underhill, Vivian R 11 University of ColoradoWith rising global temperatures, a major concern is that fresh water from melting glaciers and the Greenland ice sheet will slow down global oceanic circulation patterns, in particular the North
- Underhill, Vivian R 1 ; Wood, Kevin R 2 ; Mahoney, Andy 31 University of Colorado, Environmental Sciences Department2 Joint Institute for the Study of the Atmosphere and Ocean3 University of Alaska,
- Swanner, Elizabeth D 1 ; Templeton, Alexis S 21 University of Colorado2 University of ColoradoIt is now established that microbial life inhabits pore spaces and fractures deep within the solid rock of our continents.
- SanClements, Michael D 1 ; McKnight, Diane M 2 ; Foreman, Christine M 31 INSTAAR, University of Colorado at Boulder2 INSTAAR, University of Colorado at Boulder3 Montana State UniversityWhile in
- Rudolph, James V 1 ; Friedrich, Katja 21 University of Colorado, Dept. of Atmospheric and Oceanic Sciences (ATOC)2 University of Colorado, Dept. of Atmospheric and Oceanic Sciences (ATOC)A 21st century precipitation
- Rengers, Francis Kevin 1 ; Moody, John 2 ; Ebel, Brian 31 University of Colorado2 USGS3 USGSRecently new work has begun to try to model the sediment deposition and erosion patterns that occurred in
- Racoviteanu, Adina 1 ; Artan, Guleid 2 ; Brown, Molly 3 ; Shrestha, Mandira 4; Bajracharya, Samjwal 5 ; Mool, Pradeep 6 ; Habib, Shahid 7 ; Tzortziou
- Pugh, Evan T 1 ; Small, Eric E 21 University of Colorado2 University of ColoradoIn western North America, the mountain pine beetle has killed more than 100,000 km2 of lodgepole pine (Pinus contorta) forest, causing
- Piscopo, Amy N 1 ; Mays, David C 2 ; Neupauer, Roseanna M 31 University of Colorado at Boulder2 University of Colorado Denver3 University of Colorado at BoulderThe lack of mixing in laminar flows is