Titlebook: Arctic Hydrology, Permafrost and Ecosystems; Daqing Yang,Douglas L. Kane Book 2021 Springer Nature Switzerland AG 2021 Arctic Hydrology.Ar

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Arctic River Water Temperatures and Thermal Regimeser monitoring location, since water temperature at this site is strongly influenced by the heat storage of Great Bear Lake. Tests of three models, i.e., linear regression, logical regression (s-shape), and the physically based air2stream model, show that the air2stream model provided the best result

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Changing Biogeochemical Cycles of Organic Carbon, Nitrogen, Phosphorus, and Trace Elements in Arcticprocesses in Arctic rivers, with particular focus on the cycling of organic carbon, nitrogen and phosphorus species, and a suite of trace elements. Third, we identify uncertainties and current gaps in our knowledge of biogeochemical processes in Arctic rivers and recommend steps forward to address t

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Ground Temperature and Active Layer Regimes and Changes and InSAR application in the northern regions. It is important to emphasize that northern permafrost conditions have significantly changed and will continue to change in the future. In order to understand the past history and future of permafrost, we need to continue and expand the monitoring of th

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Towards a semantics for concurrent ,,f the cryosphere, show signals consistent with the warming of the past half century. This Arctic amplification of the warming arises from a number of processes in the climate system, including the feedbacks associated with the loss of sea ice and snow, the increase of atmospheric moisture, and the v

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The Places and Tools of Execution,arge-scale snow cover extent and snow water equivalent (SWE), then moves to the local scale for a discussion of the processes and interactions responsible for the spatial distribution and physical properties of Arctic snow cover, most notably the roles of blowing snow and vegetation interactions. Sn

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Jens Nachtwei Prof. Dr.,Sebastian Uedelhovener northern regions and watersheds. ET in northern regions tends to increase with the decrease of latitude. The largest ET typically appears in the forest ecosystem, while the grasslands and shrublands have small ET. While the seasonal variations in ET are usually high, the interannual variability i