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From:Earth System Dynamics (Vol. 12, Issue 4) Peer-ReviewedClimate change over High Mountain Asia (HMA, including the Tibetan Plateau) is investigated over the period 1979-2014 and in future projections following the four Shared Socioeconomic Pathways: SSP1-2.6, SSP2-4.5,...
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From:The Cryosphere (Vol. 15, Issue 8) Peer-ReviewedIn this study, we use run-time bias correction to correct for the Action de Recherche Petite Echelle Grande Echelle (ARPEGE) atmospheric model systematic errors on large-scale atmospheric circulation. The bias-correction...
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From:The Cryosphere (Vol. 14, Issue 8) Peer-ReviewedCMIP5, CMIP6, and ERA5 Antarctic precipitation is evaluated against CloudSat data. At continental and regional scales, ERA5 and the median CMIP models are biased high, with insignificant improvement from CMIP5 to CMIP6....
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From:Biogeosciences (Vol. 14, Issue 22) Peer-ReviewedIt is important that climate models can accurately simulate the terrestrial carbon cycle in the Arctic due to the large and potentially labile carbon stocks found in permafrost-affected environments, which can lead to a...
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From:Biogeosciences (Vol. 14, Issue 12) Peer-ReviewedThe land surface models JULES (Joint UK Land Environment Simulator, two versions) and ORCHIDEE-MICT (Organizing Carbon and Hydrology in Dynamic Ecosystems), each with a revised representation of permafrost carbon, were...
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From:Geoscientific Model Development (Vol. 12, Issue 1) Peer-Reviewed
Future sea surface temperature and sea-ice concentration from coupled ocean-atmosphere general circulation models such as those from the CMIP5 experiment are often used as boundary forcings for the downscaling of...
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From:Geoscientific Model Development (Vol. 12, Issue 7) Peer-Reviewed
The importance of northern peatlands in the global carbon cycle has been recognized, especially for long-term changes. Yet, the complex interactions between climate and peatland hydrology, carbon storage, and area...
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From:Geoscientific Model Development (Vol. 9, Issue 8) Peer-ReviewedThe Land Surface, Snow and Soil Moisture Model Intercomparison Project (LS3MIP) is designed to provide a comprehensive assessment of land surface, snow and soil moisture feedbacks on climate variability and climate...
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From:Geoscientific Model Development (Vol. 11, Issue 12) Peer-Reviewed
This paper describes ESM-SnowMIP, an international coordinated modelling effort to evaluate current snow schemes, including snow schemes that are included in Earth system models, in a wide variety of settings against...
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From:Proceedings of the National Academy of Sciences of the United States (Vol. 114, Issue 41) Peer-ReviewedCitation Only
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From:Proceedings of the National Academy of Sciences of the United States (Vol. 115, Issue 15) Peer-ReviewedAbstract Only
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From:The Cryosphere (Vol. 10, Issue 4) Peer-ReviewedA realistic simulation of snow cover and its thermal properties are important for accurate modelling of permafrost. We analyse simulated relationships between air and near-surface (20â¯cm) soil...
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From:Geoscientific Model Development (Vol. 11, Issue 2) Peer-ReviewedByline: To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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From:Proceedings of the National Academy of Sciences of the United States (Vol. 115, Issue 38) Peer-ReviewedAbstract Only
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From:The Cryosphere (Vol. 14, Issue 9) Peer-ReviewedPermafrost is a ubiquitous phenomenon in the Arctic. Its future evolution is likely to control changes in northern high-latitude hydrology and biogeochemistry. Here we evaluate the permafrost dynamics in the global...
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From:The Cryosphere (Vol. 15, Issue 2) Peer-Reviewed
Future surface mass balance and surface melt in the Amundsen sector of the West Antarctic Ice Sheet.
We present projections of West Antarctic surface mass balance (SMB) and surface melt to 2080-2100 under the RCP8.5 scenario and based on a regional model at 10 km resolution. Our projections are built by adding a CMIP5... -
From:The Cryosphere (Vol. 13, Issue 11) Peer-ReviewedOwing to increase in snowfall, the Antarctic Ice Sheet surface mass balance is expected to increase by the end of the current century. Assuming no associated response of ice dynamics, this will be a negative contribution...
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From:The Cryosphere (Vol. 14, Issue 12) Peer-ReviewedThe 30-year simulations of seasonal snow cover in 22 physically based models driven with bias-corrected meteorological reanalyses are examined at four sites with long records of snow observations. Annual snow cover...
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From:Geoscientific Model Development (Vol. 10, Issue 12) Peer-ReviewedSimulation of vegetation-climate feedbacks in high latitudes in the ORCHIDEE land surface model was improved by the addition of three new circumpolar plant functional types (PFTs), namely non-vascular plants...
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From:Geoscientific Model Development (Vol. 11, Issue 8) Peer-Reviewed
Widely present in boreal regions, peatlands contain large carbon stocks because of their hydrologic properties and high water content, which makes primary productivity exceed decomposition rates. We have enhanced the...