Recent fluctuation of snow cover on mountainous areas in Japan
نویسندگان
چکیده
منابع مشابه
Downscaling Snow Cover Fraction Data in Mountainous Regions Based on Simulated Inhomogeneous Snow Ablation
High-resolution snow distributions are essential for studying cold regions. However, the temporal and spatial resolutions of current remote sensing snow maps remain limited. Remotely sensed snow cover fraction (SCF) data only provide quantitative descriptions of snow area proportions and do not provide information on subgrid-scale snow locations. We present a downscaling method based on simulat...
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RESUME It has been established that optical and near-infrared sensors can monitor the seasonal variations of snow cover in alpine areas in cloud free conditions. However, only microwave sensors are able to acquire data independently of day light and in adverse weather conditions. The effects of dry snow on currently available C-band SAR data are rather small and difficult to detect. On the cont...
متن کاملA physiographic approach to downscaling fractional snow cover data in mountainous regions
a r t i c l e i n f o Keywords: Fractional snow covered area Snow covered extent Downscaling Topography Hillslope scale Landsat NDSI Digital elevation models Snow remote sensing Watershed hydrology Accurate characterization of snow-covered area (SCA) and snow water equivalent (SWE) in complex terrain is needed to improve estimation of streamflow timing and volume, and is important for land surf...
متن کاملMultitemporal snow cover mapping in mountainous terrain for Landsat climate data record development
a r t i c l e i n f o A multitemporal method to map snow cover in mountainous terrain is proposed to guide Landsat climate data record (CDR) development. The Landsat image archive including MSS, TM, and ETM + imagery was used to construct a prototype Landsat snow cover CDR for the interior northwestern United States. Landsat snow cover CDRs are designed to capture snow-covered area (SCA) variab...
متن کاملSnow Cover
Snow cover is a layer of snow on the earth’s surface, which is mainly results from snowfalls. The snow cover can be temporary, when a snow melts during several hours or days after its formation, and it can be stable, when it remains for the whole winter or with short interruptions. The snow cover formation on the globe is determined (conditioned) by the geographical zonality, surface relief, an...
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ژورنال
عنوان ژورنال: Annals of Glaciology
سال: 2001
ISSN: 0260-3055,1727-5644
DOI: 10.3189/172756401781818987