Synoptic control on snow avalanche activity in central Spitsbergen

dc.contributor.authorHancock, Holt
dc.contributor.authorHendrikx, Jordy
dc.contributor.authorEckerstorfer, Markus
dc.contributor.authorWickström, Siiri
dc.date.accessioned2022-06-17T19:54:02Z
dc.date.available2022-06-17T19:54:02Z
dc.date.issued2021-08
dc.description.abstractAtmospheric circulation exerts an important control on a region's snow avalanche activity by broadly determining the mountain weather patterns that influence snowpack development and avalanche release. In central Spitsbergen, the largest island in the High Arctic Svalbard archipelago, avalanches are a common natural hazard throughout the winter months. Previous work has identified a unique snow climate reflecting the region's climatically dynamic environmental setting but has not specifically addressed the synoptic-scale control of atmospheric circulation on avalanche activity here. In this work, we investigate atmospheric circulation's control on snow avalanching in the Nordenskiöld Land region of central Spitsbergen by first constructing a four-season (2016/2017–2019/2020) regional avalanche activity record using observations available on a database used by the Norwegian Water Resources and Energy Directorate (NVE). We then analyze the synoptic atmospheric conditions on days with differing avalanche activity situations. Our results show atmospheric circulation conducive to elevated precipitation, wind speeds, and air temperatures near Svalbard are associated with increased avalanche activity in Nordenskiöld Land, but different synoptic signals exist for days characterized by dry, mixed, and wet avalanche activity. Differing upwind conditions help further explain differences in the frequency and nature of avalanche activity resulting from these various atmospheric circulation patterns. We further employ a daily atmospheric circulation calendar to help contextualize our results in the growing body of literature related to climate change in this location. This work helps expand our understanding of snow avalanches in Svalbard to a broader spatial scale and provides a basis for future work investigating the impacts of climate change on avalanche activity in Svalbard and other locations where avalanche regimes are impacted by changing climatic and synoptic conditions.en_US
dc.identifier.citationHancock, H., Hendrikx, J., Eckerstorfer, M., & Wickström, S. (2021). Synoptic control on snow avalanche activity in central Spitsbergen. The Cryosphere, 15(8), 3813-3837.en_US
dc.identifier.issn1994-0424
dc.identifier.urihttps://scholarworks.montana.edu/handle/1/16838
dc.language.isoenen_US
dc.publisherCopernicus GmbHen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.titleSynoptic control on snow avalanche activity in central Spitsbergenen_US
dc.typeArticleen_US
mus.citation.extentfirstpage3813en_US
mus.citation.extentlastpage3837en_US
mus.citation.issue8en_US
mus.citation.journaltitleThe Cryosphereen_US
mus.citation.volume15en_US
mus.data.thumbpage3en_US
mus.identifier.doi10.5194/tc-15-3813-2021en_US
mus.relation.collegeCollege of Nursingen_US
mus.relation.departmentEarth Sciences.en_US
mus.relation.universityMontana State University - Bozemanen_US

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