Results 31 to 40 of about 38,278 (336)

Loss and Damage in the mountain cryosphere [PDF]

open access: yesRegional Environmental Change, 2018
The mountain cryosphere, which includes glaciers, permafrost, and snow, is one of the Earth’s systems most strongly affected by climate change. In recent decades, changes in the cryosphere have been well documented in many high-mountain regions. While there are some benefits from snow and ice loss, the negative impacts, including from glacier lake ...
Christian Huggel   +7 more
openaire   +4 more sources

Estimation of subsurface porosities and thermal conductivities of polygonal tundra by coupled inversion of electrical resistivity, temperature, and moisture content data [PDF]

open access: yes, 2020
Studies indicate greenhouse gas emissions following permafrost thaw will amplify current rates of atmospheric warming, a process referred to as the permafrost carbon feedback.
Atchley, AL   +7 more
core   +2 more sources

Fostering multidisciplinary research on interactions between chemistry, biology, and physics within the coupled cryosphere-atmosphere system

open access: yesElementa: Science of the Anthropocene, 2019
The cryosphere, which comprises a large portion of Earth’s surface, is rapidly changing as a consequence of global climate change. Ice, snow, and frozen ground in the polar and alpine regions of the planet are known to directly impact atmospheric ...
Jennie L. Thomas   +34 more
doaj   +1 more source

Aspect ratio affects iceberg melting [PDF]

open access: yesPhys. Rev. Fluids 6, 023802 (2021), 2020
Iceberg meltwater is a critical freshwater flux from the cryosphere to the oceans. Global climate simulations therefore require simple and accurate parameterisations of iceberg melting. Iceberg shape is an important but often neglected aspect of iceberg melting.
arxiv   +1 more source

Snow spectral albedo at Summit, Greenland: measurements and numerical simulations based on physical and chemical properties of the snowpack [PDF]

open access: yes, 2013
The broadband albedo of surface snow is determined both by the near-surface profile of the physical and chemical properties of the snowpack and by the spectral and angular characteristics of the incident solar radiation.
Arnaud, L   +10 more
core   +3 more sources

The Disappearing Cryosphere: Impacts and Ecosystem Responses to Rapid Cryosphere Loss [PDF]

open access: yesBioScience, 2012
The cryosphere—the portion of the Earth's surface where water is in solid form for at least one month of the year—has been shrinking in response to climate warming. The extents of sea ice, snow, and glaciers, for example, have been decreasing. In response, the ecosystems within the cryosphere and those that depend on the cryosphere have been changing ...
Fountain, Andrew G.   +5 more
openaire   +3 more sources

A double continuum hydrological model for glacier applications [PDF]

open access: yes, 2014
Peer reviewedPublisher ...
de Fleurian, B.   +6 more
core   +2 more sources

Suppression of the water ice and snow albedo feedback on planets orbiting red dwarf stars and the subsequent widening of the habitable zone [PDF]

open access: yesAstrobiology, vol 12, pp 3-8 (2012), 2011
M-stars comprise 80% of main-sequence stars, and so their planetary systems provide the best chance for finding habitable planets, i.e.: those with surface liquid water. We have modelled the broadband albedo or reflectivity of water ice and snow for simulated planetary surfaces orbiting two observed red dwarf stars (or M-stars) using spectrally ...
arxiv   +1 more source

Representing moisture fluxes and phase changes in glacier debris cover using a reservoir approach [PDF]

open access: yes, 2014
Due to the complexity of treating moisture in supraglacial debris, surface energy balance models to date have neglected moisture infiltration and phase changes in the debris layer.
Brock, Benjamin   +5 more
core   +1 more source

Cryodiversity: the World of Cold on the Earth and in the Solar System [PDF]

open access: yesФилософия и космология, 2018
Effects and objects associated with the cryosphere, the world of cold, are extremely diverse due to anomalous thermodynamic and electromagnetic properties of ice, intermediate strength of hydrogen bonds, broad occurrence of cryogenic systems, and ...
Vladimir Melnikov, Victor Gennadinik
doaj   +1 more source

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