Matches in SemOpenAlex for { <https://semopenalex.org/work/W2003306812> ?p ?o ?g. }
Showing items 1 to 100 of
100
with 100 items per page.
- W2003306812 endingPage "44" @default.
- W2003306812 startingPage "37" @default.
- W2003306812 abstract "The snow cover model SNOWPACK simulates snow cover formation and evolution based on meteorological data. In the past, these data were measured by automated weather stations. Recently, SNOWPACK was also forced with data from numerical weather prediction models (NWP). In this study we assess the capability of such a model chain to simulate two types of critical layers, i.e. surface hoar and melt–freeze crusts, for virtual north and south-facing slopes as well as a flat study plot. Meteorological key parameters for snow cover formation and evolution, e.g. precipitation, radiation, air temperature and relative humidity, were measured and compared to the forecasted data to evaluate the performance of the NWP model. Systematic errors of the NWP model were corrected and the adjusted data were used to force SNOWPACK. The formation of 80 critical layers – 35 surface hoar layers and 45 melt–freeze crusts – from seven winters between 2005 and 2012 observed in the Columbia Mountains of British Columbia, Canada were investigated. To assess the performance of SNOWPACK at simulating the presence and absence of critical layers on different aspects, monthly manual snow profiles systematically observed on north, south and flat terrains between January and March during the winter of 2010–2011 were compared to the corresponding snow cover simulations. The overall accuracy to predict the formation of melt–freeze crusts was found to be between 65% and 77% depending on the aspect. Surface hoar layers were modeled with accuracy between 89% and 100%. The presence and absence of critical layers within the snow cover – surface hoar and melt–freeze crusts – were investigated during the winter of 2010–2011. Ten out of eleven observed critical layers within the snow cover were simulated, resulting in an accuracy of 91%. However, some surface hoar layers and melt–freeze crusts were simulated but not observed resulting in a low accuracy for the absence of critical layers. The simulated snow height tended to be under-estimated during the early winter season and over-estimated during the late winter season for both slopes and the flat site, especially in March on the south-facing aspect. Nevertheless, the model chain is promising considering the source of the input data. This study showed that such a model chain could become a useful tool for avalanche warning services in the future, especially for data sparse areas." @default.
- W2003306812 created "2016-06-24" @default.
- W2003306812 creator A5016299993 @default.
- W2003306812 creator A5033562873 @default.
- W2003306812 date "2013-10-01" @default.
- W2003306812 modified "2023-10-15" @default.
- W2003306812 title "Forecasting the formation of critical snow layers using a coupled snow cover and weather model" @default.
- W2003306812 cites W1249345106 @default.
- W2003306812 cites W132837105 @default.
- W2003306812 cites W1421216920 @default.
- W2003306812 cites W1484996118 @default.
- W2003306812 cites W1499472888 @default.
- W2003306812 cites W1504592712 @default.
- W2003306812 cites W1991834604 @default.
- W2003306812 cites W1993906971 @default.
- W2003306812 cites W1995871016 @default.
- W2003306812 cites W2000177823 @default.
- W2003306812 cites W2001462444 @default.
- W2003306812 cites W2061764800 @default.
- W2003306812 cites W2075948780 @default.
- W2003306812 cites W2084347101 @default.
- W2003306812 cites W2096303850 @default.
- W2003306812 cites W2102051700 @default.
- W2003306812 cites W2155762958 @default.
- W2003306812 cites W2163717774 @default.
- W2003306812 doi "https://doi.org/10.1016/j.coldregions.2013.06.007" @default.
- W2003306812 hasPublicationYear "2013" @default.
- W2003306812 type Work @default.
- W2003306812 sameAs 2003306812 @default.
- W2003306812 citedByCount "36" @default.
- W2003306812 countsByYear W20033068122013 @default.
- W2003306812 countsByYear W20033068122014 @default.
- W2003306812 countsByYear W20033068122015 @default.
- W2003306812 countsByYear W20033068122016 @default.
- W2003306812 countsByYear W20033068122017 @default.
- W2003306812 countsByYear W20033068122018 @default.
- W2003306812 countsByYear W20033068122019 @default.
- W2003306812 countsByYear W20033068122020 @default.
- W2003306812 countsByYear W20033068122021 @default.
- W2003306812 countsByYear W20033068122022 @default.
- W2003306812 countsByYear W20033068122023 @default.
- W2003306812 crossrefType "journal-article" @default.
- W2003306812 hasAuthorship W2003306812A5016299993 @default.
- W2003306812 hasAuthorship W2003306812A5033562873 @default.
- W2003306812 hasBestOaLocation W20033068121 @default.
- W2003306812 hasConcept C107054158 @default.
- W2003306812 hasConcept C127313418 @default.
- W2003306812 hasConcept C147947694 @default.
- W2003306812 hasConcept C153294291 @default.
- W2003306812 hasConcept C158960510 @default.
- W2003306812 hasConcept C161840515 @default.
- W2003306812 hasConcept C197046000 @default.
- W2003306812 hasConcept C205649164 @default.
- W2003306812 hasConcept C2778877292 @default.
- W2003306812 hasConcept C2779395273 @default.
- W2003306812 hasConcept C2983043445 @default.
- W2003306812 hasConcept C3018601724 @default.
- W2003306812 hasConcept C39432304 @default.
- W2003306812 hasConcept C49204034 @default.
- W2003306812 hasConcept C58640448 @default.
- W2003306812 hasConcept C64649846 @default.
- W2003306812 hasConcept C91586092 @default.
- W2003306812 hasConceptScore W2003306812C107054158 @default.
- W2003306812 hasConceptScore W2003306812C127313418 @default.
- W2003306812 hasConceptScore W2003306812C147947694 @default.
- W2003306812 hasConceptScore W2003306812C153294291 @default.
- W2003306812 hasConceptScore W2003306812C158960510 @default.
- W2003306812 hasConceptScore W2003306812C161840515 @default.
- W2003306812 hasConceptScore W2003306812C197046000 @default.
- W2003306812 hasConceptScore W2003306812C205649164 @default.
- W2003306812 hasConceptScore W2003306812C2778877292 @default.
- W2003306812 hasConceptScore W2003306812C2779395273 @default.
- W2003306812 hasConceptScore W2003306812C2983043445 @default.
- W2003306812 hasConceptScore W2003306812C3018601724 @default.
- W2003306812 hasConceptScore W2003306812C39432304 @default.
- W2003306812 hasConceptScore W2003306812C49204034 @default.
- W2003306812 hasConceptScore W2003306812C58640448 @default.
- W2003306812 hasConceptScore W2003306812C64649846 @default.
- W2003306812 hasConceptScore W2003306812C91586092 @default.
- W2003306812 hasFunder F4320315156 @default.
- W2003306812 hasLocation W20033068121 @default.
- W2003306812 hasOpenAccess W2003306812 @default.
- W2003306812 hasPrimaryLocation W20033068121 @default.
- W2003306812 hasRelatedWork W1990066466 @default.
- W2003306812 hasRelatedWork W2012918299 @default.
- W2003306812 hasRelatedWork W2042231989 @default.
- W2003306812 hasRelatedWork W2096152360 @default.
- W2003306812 hasRelatedWork W2134984707 @default.
- W2003306812 hasRelatedWork W2150907087 @default.
- W2003306812 hasRelatedWork W3098101688 @default.
- W2003306812 hasRelatedWork W4221025217 @default.
- W2003306812 hasRelatedWork W4244899108 @default.
- W2003306812 hasRelatedWork W2481866728 @default.
- W2003306812 hasVolume "94" @default.
- W2003306812 isParatext "false" @default.
- W2003306812 isRetracted "false" @default.
- W2003306812 magId "2003306812" @default.
- W2003306812 workType "article" @default.