Results 211 to 220 of about 25,716 (256)

Discrete ecological gradient in thermokarst ponds in a palsa mire in northern Norway. [PDF]

Sci Rep
Jabłońska E, Lyngstad A, Jaszczuk I, Kucharzyk J, Hassel K, Grygoruk M, Kotowski W.   +6 more
europepmc   +1 more source

Retrogressive Thaw Slumps Produce a Changing Disturbance Regime for Arctic Stream Invertebrates. [PDF]

Glob Chang Biol
Dolan M, Musetta-Lambert J, Chin KS, Kokelj SV, Tank SE, Lento J, Power M, Culp JM.   +7 more
europepmc   +1 more source

First retrogressive thaw slump (RTS) inventory for the Kanin Peninsula (NW Russia). [PDF]

Sci Data
Nicu IC, Rubensdotter L, Tanyaș H, Lombardo L.   +3 more
europepmc   +1 more source

Modeling earthquake-induced wavefields and stresses in alpine mountains with extreme topography. [PDF]

Sci Rep
Limberger F, Rümpker G, Kruse JP, Duretz T.   +3 more
europepmc   +1 more source

A comprehensive water bodies dataset of high-mountain Asia. [PDF]

Sci Data
Sui Y, Hu Z, Zhang K, Yan D, Su Y, Xu J, Wang R, Feng M.   +7 more
europepmc   +1 more source

The Active Soil Layer of Thawing Permafrost Is an Emergent Source for Organic Substances of Concern to Water Resources. [PDF]

Environ Sci Technol Lett
Han M, Jin B, Arp HPH.
europepmc   +1 more source

Wild, scenic, and toxic: Recent degradation of an iconic Arctic watershed with permafrost thaw. [PDF]

Proc Natl Acad Sci U S A
Sullivan PF, Dial RJ, Cooper DJ, Diamond C, Tino CJ, Gregory DD, Wong RE, Lyons TW.   +7 more
europepmc   +1 more source

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Effects of permafrost degradation on ecosystems

Acta Ecologica Sinica, 2010
Abstract Permafrost, covering approximately 25% of the land area in the Northern Hemisphere, is one of the key components of terrestrial ecosystem in cold regions. As a product of cold climate, permafrost is extremely sensitive to climate change. Climate warming over past decades has caused degradation in permafrost widely and quickly.
Zhao-ping Yang, Yang Hua Ou, Xing-liang Xu, Lin Zhao, Ming-hua Song, Cai-ping Zhou   +5 more
openaire   +3 more sources

Highway Embankment on Degrading Permafrost

Cold Regions Engineering 2009, 2009
The highway embankment is about 800 km (500 miles) north of Winnipeg, Manitoba, Canada in an area where permafrost is degrading rapidly. Soil sampling and installation of instrumentation (temperatures, settlements, lateral deformations and pore water pressures) was undertaken in October 2008.
H. Batenipour, D. Kurz, M. Alfaro, J. Graham, T. N. S. Ng   +4 more
openaire   +1 more source