K N Musselman
Biographic Data
| ID | 6818974 |
|---|---|
| NAME | K N Musselman |
| GIVEN NAMES | K N |
| FAMILY NAME | Musselman |
| SIGNATURE | MUSSELMAN K N |
| AFFILIATIONS | Institute of Arctic and Alpine Research |
| ORCID | 0000-0001-8394-491X |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2017 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
High-resolution models better simulate historical snowpack declines in the Upper Colorado River Basin
The Colorado River supplies water to 40 million people, 4.5 million acres of irrigated land, seven US states, over two dozen federally recognized and sovereign tribes and Mexico. River discharge is strongly controlled by snowpack accumulation and melt in the headwater regions, making upper-basin snow dynamics a primary driver of water availability throughout the basin. Therefore, changes in snow water equivalent (SWE) are critical for water resou…
Increasing Alaskan river discharge during the cold season is driven by recent warming
Arctic hydrology is experiencing rapid changes including earlier snow melt, permafrost degradation, increasing active layer depth, and reduced river ice, all of which are expected to lead to changes in stream flow regimes. Recently, long-term (>60 years) climate reanalysis and river discharge observation data have become available. We utilized these data to assess long-term changes in discharge and their hydroclimatic drivers. River discharge dur…
Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
Winters in snow-covered regions have warmed, likely shifting the timing and magnitude of nutrient export, leading to unquantified changes in water quality. Intermittent, seasonal, and permanent snow covers more than half of the global land surface. Warming has reduced the cold conditions that limit winter runoff and nutrient transport, while cold season snowmelt, the amount of winter precipitation falling as rain, and rain-on-snow have increased.…
Different sensitivities of snowpacks to warming in Mediterranean climate mountain areas
López-Moreno, Juan I. et. al.- 10 páginas.- Ilustraciones.- This article is an open access article distributed under the terms of the Creative Commons Attribution 3.0 licence (https://creativecommons.org/licenses/by/3.0/)
No prominent works on this page.
Different sensitivities of snowpacks to warming in Mediterranean climate mountain areas
López-Moreno, Juan I. et. al.- 10 páginas.- Ilustraciones.- This article is an open access article distributed under the terms of the Creative Commons Attribution 3.0 licence (https://creativecommons.org/licenses/by/3.0/)
Winter runoff events pose an unquantified continental-scale risk of high wintertime nutrient export
Winters in snow-covered regions have warmed, likely shifting the timing and magnitude of nutrient export, leading to unquantified changes in water quality. Intermittent, seasonal, and permanent snow covers more than half of the global land surface. Warming has reduced the cold conditions that limit winter runoff and nutrient transport, while cold season snowmelt, the amount of winter precipitation falling as rain, and rain-on-snow have increased.…
Increasing Alaskan river discharge during the cold season is driven by recent warming
Arctic hydrology is experiencing rapid changes including earlier snow melt, permafrost degradation, increasing active layer depth, and reduced river ice, all of which are expected to lead to changes in stream flow regimes. Recently, long-term (>60 years) climate reanalysis and river discharge observation data have become available. We utilized these data to assess long-term changes in discharge and their hydroclimatic drivers. River discharge dur…
High-resolution models better simulate historical snowpack declines in the Upper Colorado River Basin
The Colorado River supplies water to 40 million people, 4.5 million acres of irrigated land, seven US states, over two dozen federally recognized and sovereign tribes and Mexico. River discharge is strongly controlled by snowpack accumulation and melt in the headwater regions, making upper-basin snow dynamics a primary driver of water availability throughout the basin. Therefore, changes in snow water equivalent (SWE) are critical for water resou…
Cryospheric studies and observations (4 works) · Snow (4 works) · Drainage basin (3 works) · Environmental Science (3 works) · Geography (3 works) · Geology (3 works) · Hydrology (agriculture (3 works) · Hydrology and Watershed Management Studies (3 works) · Meteorology (3 works) · Climate change (2 works)