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dc.contributor.authorNicu, Ionut Cristi
dc.contributor.authorRubensdotter, Brita Lena Eleonor Fredin
dc.contributor.authorTanyas, Hakan
dc.contributor.authorLombardo, Luigi
dc.date.accessioned2024-08-30T09:01:59Z
dc.date.available2024-08-30T09:01:59Z
dc.date.created2024-08-26T11:13:51Z
dc.date.issued2024
dc.identifier.issn2052-4463
dc.identifier.urihttps://hdl.handle.net/11250/3149264
dc.description.abstractCryospheric hazards - in this case, thaw slumps (TS) and thermo-erosion gullies (TEG) - are phenomena typical of permafrost-dominated landscapes. Open datasets informing about their spatial, temporal and size distributions in the Arctic are still uncommon, as opposed to the systematic availability of this information for geomorphic processes in mid- to low- latitudes. To date, only the most populated region of Svalbard was covered with TS and TEG inventories. Here, we extend the respective information to most of the Archipelago, totalling 8491 polygons, out of which 3679 are TSs and 4812 are TEGs. These have been manually mapped from aerial photographs throughout Svalbard across the 14 largest ice-free regions. The SvalCryo inventory is highly relevant as the Arctic environment undergoes alarming changes in response to global warming. The idea behind the two inventories is to support the geoscientific community in the quest to evaluate the environmental response to climate change, by creating a baseline for change monitoring, and ultimately to serve as basis for susceptibility, hazard and risk assessment models.en_US
dc.language.isoengen_US
dc.titleNear Pan-Svalbard permafrost cryospheric hazards inventory (SvalCryo)en_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.volume11en_US
dc.source.journalScientific Dataen_US
dc.identifier.doi10.1038/s41597-024-03754-7
dc.identifier.cristin2289355
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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