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From:Geoscientific Model Development (Vol. 15, Issue 9) Peer-ReviewedMicrotopography can be a key driver of heterogeneity in the ground thermal and hydrological regime of permafrost landscapes. In turn, this heterogeneity can influence plant communities, methane fluxes, and the initiation...
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From:Geoscientific Model Development (Vol. 15, Issue 6) Peer-ReviewedBoreal forests of Siberia play a relevant role in the global carbon cycle. However, global warming threatens the existence of summergreen larch-dominated ecosystems, likely enabling a transition to evergreen tree taxa...
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From:Earth System Science Data (Vol. 14, Issue 1) Peer-ReviewedPast efforts to synthesize and quantify the magnitude and change in carbon dioxide (CO.sub.2) fluxes in terrestrial ecosystems across the rapidly warming Arctic-boreal zone (ABZ) have provided valuable information but...
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From:Atmospheric Measurement Techniques (Vol. 14, Issue 11) Peer-ReviewedThe WPL (Webb, Pearman, and Leuning) correction is fully accepted to correct trace gas fluxes like CO.sub.2 for density fluctuations due to water vapour and temperature fluctuations for open-path gas analysers. It is...
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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:The Cryosphere (Vol. 13, Issue 2) Peer-Reviewed
Earth system models (ESMs) are our primary tool for projecting future climate change, but their ability to represent small-scale land surface processes is currently limited. This is especially true for permafrost...
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From:Biogeosciences (Vol. 17, Issue 16) Peer-ReviewedConnections between vegetation and soil thermal dynamics are critical for estimating the vulnerability of permafrost to thaw with continued climate warming and vegetation changes. The interplay of complex biophysical...
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From:Earth System Science Data (Vol. 10, Issue 1) Peer-ReviewedByline: Julia Boike, Inge Juszak, Stephan Lange, Sarah Chadburn, Eleanor Burke, Pier Paul Overduin, Kurt Roth, Olaf Ippisch, Niko Bornemann, Lielle Stern, Isabelle Gouttevin, Ernst Hauber, Sebastian Westermann To...
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From:Earth System Science Data (Vol. 11, Issue 1) Peer-Reviewed
Ground-based observations of land-atmosphere fluxes are necessary to progressively improve global climate models. Observed data can be used for model evaluation and to develop or tune process models. In arctic...
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From:The Cryosphere (Vol. 12, Issue 2) Peer-ReviewedByline: Simon Zwieback, Steven V. Kokelj, Frank Gü,nther, Julia Boike, Guido Grosse, Irena Hajnsek To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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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:The Cryosphere (Vol. 11, Issue 3) Peer-ReviewedPermafrost is a sensitive element of the cryosphere, but operational monitoring of the ground thermal conditions on large spatial scales is still lacking. Here, we demonstrate a remote-sensing-based scheme that is...
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From:The Cryosphere (Vol. 12, Issue 11) Peer-Reviewed
The shortage of information on snow properties in high latitudes places a major limitation on permafrost and more generally climate modelling. A dedicated field program was therefore carried out to investigate snow...
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From:Biogeosciences (Vol. 18, Issue 2) Peer-ReviewedBoreal forests in permafrost regions make up around one-third of the global forest cover and are an essential component of regional and global climate patterns. Further, climatic change can trigger extensive ecosystem...
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From:The Cryosphere (Vol. 15, Issue 5) Peer-ReviewedPermafrost degradation in steep rock walls and associated slope destabilization have been studied increasingly in recent years. While most studies focus on mountainous and sub-Arctic regions, the occurring...
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From:The Cryosphere (Vol. 12, Issue 1) Peer-ReviewedByline: Kristoffer Aalstad, Sebastian Westermann, Thomas Vikhamar Schuler, Julia Boike, Laurent Bertino To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 17) Peer-ReviewedIn the context of the Arctic amplification of climate change affecting the regional atmospheric hydrological cycle, it is crucial to characterize the present-day moisture sources of the Arctic. The isotopic composition...
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From:The Cryosphere (Vol. 13, Issue 4) Peer-ReviewedByline: Jan Nitzbon, Moritz Langer, Sebastian Westermann, Lé,o Martin, Kjetil Schanke Aas, Julia Boike To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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From:Biogeosciences (Vol. 18, Issue 12) Peer-ReviewedLakes in permafrost regions are dynamic landscape components and play an important role for climate change feedbacks. Lake processes such as mineralization and flocculation of dissolved organic carbon (DOC), one of the...