Results 231 to 240 of about 1,094,471 (304)

Retrievals and simulations of terrestrial water storage changes and runoff over the Tibetan Plateau: Challenges and opportunities. [PDF]

Fundam Res
Li X, Long D, Scanlon BR, Slater LJ.
europepmc   +1 more source

Subaqueous evidence of the last glacial maximum and its termination in southern Patagonia. [PDF]

Sci Rep
Fedotova A, Magnani MB.
europepmc   +1 more source

Tidewater cycle drives alpine glacial sediment plume geochemistry. [PDF]

Nat Commun
Forsch KO, Ruacho A, Aarons SM.
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Poleward shift of subtropical highs drives Patagonian glacier mass loss. [PDF]

Nat Commun
Noël B, Lhermitte S, Wouters B, Fettweis X.   +3 more
europepmc   +1 more source

Precipitation drives western Patagonian glacier variability and may curb future ice mass loss. [PDF]

Sci Rep
Troch M, Åkesson H, Cuzzone JK, Bertrand S.   +3 more
europepmc   +1 more source

Metabolically flexible microorganisms rapidly establish glacial foreland ecosystems. [PDF]

Nat Commun
Ricci F, Bay SK, Nauer PA, Wong WW, Ni G, Jimenez L, Jirapanjawat T, Leung PM, Bradley JA, Eate VM, Hall M, Stubbusch AKM, Fernández-Marín B, de Los Ríos A, Cook PLM, Schroth MH, Chiri E, Greening C.   +17 more
europepmc   +1 more source

The diversity and abundance of chytrids on the Greenland Ice Sheet – new quantitative data

Perini L, Zervas A, Feld L, Jacobsen CS, Benning LG, Tranter M, Anesio AM.   +6 more
europepmc   +1 more source

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Linear modelling of glacier length fluctuations

Geografiska Annaler, Series A: Physical Geography, 2012
In this contribution a linear first-order differential equation is used to model glacier length fluctuations. This equation has two parameters describing the physical characteristics of a glacier: the climate sensitivity, expressing how the equilibrium glacier length depends on the climatic state, and the response time, indicating how fast a glacier ...
Johannes Oerlemans
exaly   +2 more sources

Seasonal and Interannual Fluctuations of Glacier Mass Balance and Climate Response Processes on the Tibetan Plateau Based on GRACE/GRACE-FO

IEEE Transactions on Geoscience and Remote Sensing, 2023
Glacier mass changes in high mountainous areas are in an unbalanced status due to global climate warming. In this study, we use the Gravity Recovery and Climate Experiment as well as its Follow-on mission (GRACE/GRACE-FO) data to constrain the ...
Meilin He, Zhao Li, Weiping Jiang, Yuanjin Pan, J. Jiao, Yixin Xiao   +5 more
semanticscholar   +1 more source