Results 21 to 30 of about 406,760 (210)

Impacts of landscape and climatic factors on snow cover in the Altai Mountains, China

open access: yesAdvances in Climate Change Research, 2021
Snow properties and their changes are crucial to better understanding of hydrological processes, soil thermal regimes, and surface energy balances. Reliable data and information on snow depth and snow water equivalent (SWE) are also crucial for water ...
Xin-Yue Zhong   +10 more
doaj   +1 more source

Spatio-temporal influence of tundra snow properties on Ku-band (17.2 GHz) backscatter [PDF]

open access: yes, 2015
During the 2010/11 boreal winter, a distributed set of backscatter measurements was collected using a ground-based Ku-band (17.2 GHz) scatterometer system at 26 open tundra sites.
Derksen, Chris   +7 more
core   +1 more source

Spatiotemporal Variation of Snow Depth in the Northern Hemisphere from 1992 to 2016

open access: yesRemote Sensing, 2020
A comprehensive and hemispheric-scale snow cover and snow depth analysis is a prerequisite for all related processes and interactions investigation on regional and global surface energy and water balance, weather and climate, hydrological processes, and ...
Xiongxin Xiao   +3 more
doaj   +1 more source

Trends in wintertime climate in the northeastern United States: 1965–2005 [PDF]

open access: yes, 2008
Humans experience climate variability and climate change primarily through changes in weather at local and regional scales. One of the most effective means to track these changes is through detailed analysis of meteorological data.
Braswell, Rob   +3 more
core   +2 more sources

Comparison of passive microwave remote-sensing snow-depth products on Arctic sea ice

open access: yesPolar Research, 2019
Changes in snow cover on the surface of Arctic sea ice affect the energy balance between the atmosphere and the ocean and play a vital role in the global climate system.
Chenlei Zhang   +4 more
doaj   +1 more source

Spatially distributed water-balance and meteorological data from the Wolverton catchment, Sequoia National Park, California [PDF]

open access: yes, 2018
Accurate water-balance measurements in the seasonal, snow-dominated Sierra Nevada are important for forest and downstream water management. However, few sites in the southern Sierra offer detailed records of the spatial and temporal patterns of snowpack ...
E. M. Stacy   +6 more
core   +4 more sources

Snow Depth and Snow Density at Resolute, Northwest Territories [PDF]

open access: yesJournal of Glaciology, 1960
AbstractObservations of the snow depth at 21 sites at Resolute were made twice weekly during the winter of 1957–58. As a result of these observations, and of other observations on snow made for the National Research Council, it is shown that the snow depth and the water content of the snow did not continue to increase during the winter as the snow fell.
openaire   +2 more sources

Satellite Remote Sensing of Snow Depth on Antarctic Sea Ice: An Inter-Comparison of Two Empirical Approaches

open access: yesRemote Sensing, 2016
Snow on Antarctic sea ice plays a key role for sea ice physical processes and complicates retrieval of sea ice thickness using altimetry. Current methods of snow depth retrieval are based on satellite microwave radiometry, which perform best for dry ...
Stefan Kern, Burcu Ozsoy-Çiçek
doaj   +1 more source

Snow depth on Arctic sea ice from historical in situ data [PDF]

open access: yesThe Cryosphere, 2018
The snow data from the Soviet airborne expeditions Sever in the Arctic collected over several decades in March, April and May have been analyzed in this study.
E. V. Shalina, E. V. Shalina, S. Sandven
doaj   +1 more source

Tree canopy and snow depth relationships at fine scales with terrestrial laser scanning [PDF]

open access: yesThe Cryosphere, 2021
Understanding the impact of tree structure on snow depth and extent is important in order to make predictions of snow amounts and how changes in forest cover may affect future water resources.
A. Hojatimalekshah   +10 more
doaj   +1 more source

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