Estimating the spatial distribution of snow water equivalent in the world's mountains
Estimating the spatial distribution of snow water equivalent (SWE) in mountainous terrain is
currently the most important unsolved problem in snow hydrology. Several methods can …
currently the most important unsolved problem in snow hydrology. Several methods can …
Time–space continuity of daily maps of fractional snow cover and albedo from MODIS
Using reflectance values from the seven MODIS “land” bands with 250 or 500m resolution,
along with a corresponding cloud product, we estimate the fraction of each 500m pixel that …
along with a corresponding cloud product, we estimate the fraction of each 500m pixel that …
Scaling snow observations from the point to the grid element: Implications for observation network design
The spatial distribution of snow water equivalent (SWE) within 16‐, 4‐, and 1‐km2 grid
elements surrounding six snow telemetry (SNOTEL) stations in the Rio Grande headwaters …
elements surrounding six snow telemetry (SNOTEL) stations in the Rio Grande headwaters …
Using a fixed-wing UAS to map snow depth distribution: an evaluation at peak accumulation
We investigate snow depth distribution at peak accumulation over a small Alpine area (∼
0.3 km 2) using photogrammetry-based surveys with a fixed-wing unmanned aerial system …
0.3 km 2) using photogrammetry-based surveys with a fixed-wing unmanned aerial system …
Estimating the distribution of snow water equivalent using remotely sensed snow cover data and a spatially distributed snowmelt model: A multi-resolution, multi …
Time series of fractional snow covered area (SCA) estimates from Landsat Enhanced
Thematic Mapper (ETM+), Moderate Resolution Imaging Spectroradiometer (MODIS), and …
Thematic Mapper (ETM+), Moderate Resolution Imaging Spectroradiometer (MODIS), and …
Methods for measuring atmospheric nitrogen deposition inputs in arid and montane ecosystems of western North America
Measuring atmospheric deposition in arid and snow-dominated regions presents unique
challenges. Throughfall, the flux of nutrients transported in solution to the forest floor, is …
challenges. Throughfall, the flux of nutrients transported in solution to the forest floor, is …
More than just talk: Connecting science and decisionmaking
K Jacobs, G Garfin, M Lenart - Environment: Science and Policy for …, 2005 - Taylor & Francis
The movement toward integrat-ingscienceintodecisionmaking processes has its origins in
several arenas: environmental regulations initiated in the 1970s that encourage participation …
several arenas: environmental regulations initiated in the 1970s that encourage participation …
Simulating current and future river-flows in the Karakoram and Himalayan regions of Pakistan using snowmelt-runoff model and RCP scenarios
Upper Indus Basin (UIB) supplies more than 70% flow to the downstream agricultural areas
during summer due to the melting of snow and glacial ice. The estimation of the stream flow …
during summer due to the melting of snow and glacial ice. The estimation of the stream flow …
Snow water equivalent in the Sierra Nevada: Blending snow sensor observations with snowmelt model simulations
We estimate the spatial distribution of daily melt‐season snow water equivalent (SWE) over
the Sierra Nevada for March to August, 2000–2012, by two methods: reconstruction by …
the Sierra Nevada for March to August, 2000–2012, by two methods: reconstruction by …
SNOTEL representativeness in the Rio Grande headwaters on the basis of physiographics and remotely sensed snow cover persistence
In this study we identify the physiographic and snowpack conditions currently represented
by snowpack telemetry (SNOTEL) stations in the Rio Grande headwaters. Based on 8 years …
by snowpack telemetry (SNOTEL) stations in the Rio Grande headwaters. Based on 8 years …