Ross D Brown
Biographic Data
| ID | 5567975 |
|---|---|
| NAME | Ross D Brown |
| GIVEN NAMES | Ross D |
| FAMILY NAME | Brown |
| SIGNATURE | BROWN R D |
| VERIFIED | No |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 24 |
| WORKS AS AUTHOR | 6 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1992 |
| LATEST PUBLICATION YEAR | 2018 |
| H-INDEX | 2 |
Snow Cover Changes
Seasonal snow covers a large fraction of the Northern Hemisphere (NH) land area (and some Southern Hemisphere mountain regions) for periods of up to 10 months of the year and is an integral part of the landscape, climate, hydrology, ecology, and economy. A snow cover (duration, depth) and its physical properties (albedo, density, crystal structure, etc.) represent an integrated response of physical processes to a number of external climate/enviro…
Snow Cover Changes
Seasonal snow covers a large fraction of the Northern Hemisphere (NH) land area (and some Southern Hemisphere mountain regions) for periods of up to 10 months of the year and is an integral part of the landscape, climate, hydrology, ecology, and economy. A snow cover (duration, depth) and its physical properties (albedo, density, crystal structure, etc.) represent an integrated response of physical processes to a number of external climate/enviro…
Changing Arctic snow cover
Snow is a critically important and rapidly changing feature of the Arctic. However, snow-cover and snowpack conditions change through time pose challenges for measuring and prediction of snow. Plausible scenarios of how Arctic snow cover will respond to changing Arctic climate are important for impact assessments and adaptation strategies. Although much progress has been made in understanding and predicting snow-cover changes and their multiple c…
Multiple Effects of Changes in Arctic Snow Cover
The Changing Face of Arctic Snow Cover
Interannual Variability of Landfast Ice Thickness in the Canadian High Arctic, 1950-89
A physical one-dimensional heat transfer model of fast ice growth was used to investigate the interannual variability of maximum fast ice thickness at four sites in the High Arctic over the period 1950-89. The insulating role of snow cover was found to be the most important factor, explaining 30-60% of the variance in maximum ice thickness values. Other snow-related processes such as slushing and density variations were estimated to explain a fur…
Interannual Variability of Landfast Ice Thickness in the Canadian High Arctic, 1950-89
A physical one-dimensional heat transfer model of fast ice growth was used to investigate the interannual variability of maximum fast ice thickness at four sites in the High Arctic over the period 1950-89. The insulating role of snow cover was found to be the most important factor, explaining 30-60% of the variance in maximum ice thickness values. Other snow-related processes such as slushing and density variations were estimated to explain a fur…
Multiple Effects of Changes in Arctic Snow Cover
The Changing Face of Arctic Snow Cover
Changing Arctic snow cover
Snow is a critically important and rapidly changing feature of the Arctic. However, snow-cover and snowpack conditions change through time pose challenges for measuring and prediction of snow. Plausible scenarios of how Arctic snow cover will respond to changing Arctic climate are important for impact assessments and adaptation strategies. Although much progress has been made in understanding and predicting snow-cover changes and their multiple c…
Snow Cover Changes
Seasonal snow covers a large fraction of the Northern Hemisphere (NH) land area (and some Southern Hemisphere mountain regions) for periods of up to 10 months of the year and is an integral part of the landscape, climate, hydrology, ecology, and economy. A snow cover (duration, depth) and its physical properties (albedo, density, crystal structure, etc.) represent an integrated response of physical processes to a number of external climate/enviro…
Snow Cover Changes
Seasonal snow covers a large fraction of the Northern Hemisphere (NH) land area (and some Southern Hemisphere mountain regions) for periods of up to 10 months of the year and is an integral part of the landscape, climate, hydrology, ecology, and economy. A snow cover (duration, depth) and its physical properties (albedo, density, crystal structure, etc.) represent an integrated response of physical processes to a number of external climate/enviro…
Arctic (6 works) · Arctic and Antarctic ice dynamics (6 works) · Climate change and permafrost (6 works) · Cryospheric studies and observations (6 works) · Environmental Science (6 works) · Geography (6 works) · Geology (6 works) · Physical geography (6 works) · Snow (6 works) · Climate change (5 works)