Loss and Damage in the mountain cryosphere [PDF]
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]
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
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]
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]
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]
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]
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]
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]
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]
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