dc.contributor.author | Malnes, Eirik | |
dc.contributor.author | Karlsen, Stein Rune | |
dc.contributor.author | Johansen, Bernt | |
dc.contributor.author | Bjerke, Jarle W. | |
dc.contributor.author | Tømmervik, Hans | |
dc.coverage.spatial | the two northernmost counties in Norway, Troms and Finnmark | nb_NO |
dc.date.accessioned | 2016-11-30T09:45:56Z | |
dc.date.accessioned | 2016-12-22T09:48:50Z | |
dc.date.available | 2016-11-30T09:45:56Z | |
dc.date.available | 2016-12-22T09:48:50Z | |
dc.date.issued | 2016 | |
dc.identifier.citation | Environmental Research Letters 2016, 11 | nb_NO |
dc.identifier.issn | 1748-9326 | |
dc.identifier.uri | http://hdl.handle.net/11250/2425748 | |
dc.description.abstract | The duration and extent of snow cover is expected to change rapidly with climate change. Therefore,
there is a need for improved monitoring of snow for the benefit of forecasting, impact assessments and
the population at large. Remotely sensed techniques prove useful for remote areas where there are few
field-based monitoring stations. This paper reports on a study of snow season using snow cover area
fraction data from the two northernmost counties in Norway, Troms and Finnmark. The data are
derived from the daily 500mstandard snow product (MOD10A1) from the NASA Terra MODerate
Resolution Imaging Spectroradiometer (MODIS) sensor for the 2000–2010 period. This dataset has
been processed with multi-temporal interpolation to eliminate clouds. The resulting cloud-free daily
time series of snow cover fraction maps, have subsequently been used to derive the first and last snowfree
day for the entire study area. In spring, the correlation between the first snow-free day mapped by
MODIS data and snow data from 40 meteorological stations was highly significant (p<0.05) for 36 of
the stations, and with a of bias of less than 10 days for 34 of the stations. In autumn, 31 of the stations
show highly significant (p<0.05) correlation with MODIS data, and the bias was less than 10 days for
27 of the stations. However, in some areas and some years, the start and end of the snow season could
not be detected due to long overcast periods. In spring 2002 and 2004 the first snow-free day was early,
but arrived late in 2000, 2005 and 2008. In autumn 2009 snowfall arrived more than 7 days earlier in
50% of the study area as compared to the 2000–2010 average. MODIS-based snow season products
will be applicable for a wide range of sectors including hydrology, nature-based industries, climate
change studies and ecology. Therefore refinement and further testing of this method should be encouraged.
snow, MODIS, first snow free day, last snow free day, climate change, onset of spring | nb_NO |
dc.language.iso | eng | nb_NO |
dc.rights | Navngivelse 4.0 Internasjonal | * |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | * |
dc.subject | snow | nb_NO |
dc.subject | MODIS | nb_NO |
dc.subject | first snow free day | nb_NO |
dc.subject | last snow free day | nb_NO |
dc.subject | climate change | nb_NO |
dc.subject | onset of spring | nb_NO |
dc.title | Snow season variability in a boreal-Arctic transition area monitored by MODIS data | nb_NO |
dc.type | Journal article | nb_NO |
dc.type | Peer reviewed | nb_NO |
dc.date.updated | 2016-11-30T09:45:56Z | |
dc.source.volume | 11 | nb_NO |
dc.source.journal | Environmental Research Letters | nb_NO |
dc.identifier.doi | 10.1088/1748-9326/11/12/125005 | |
dc.identifier.cristin | 1406281 | |
dc.relation.project | Norges forskningsråd: 216434. Framsenteret SenSyF-Fram | nb_NO |