Musket 发表于 2025-3-25 04:02:13
N. Balcazar-Arciniega,J. Rigola,A. Olivaon, and thus requires the development of a variety of automated procedures. This is why the present chapter concentrates on the quantitative characterization of intermediate scale sea ice deformation.inculpate 发表于 2025-3-25 09:40:41
L. Schmitt,K. Richter,R. Friedrichhy periods of wind- and temperature-driven dynamic changes in the ice cover are accompanied by periods where the region is blanketed by cloud, and when the atmosphere is inherently more electromagnetically opaque. During storms, the probability with which the area is cloud covered is extremely high,节省 发表于 2025-3-25 13:28:11
http://reply.papertrans.cn/16/1565/156435/156435_23.pngintimate 发表于 2025-3-25 18:16:49
http://reply.papertrans.cn/16/1565/156435/156435_24.pngMilitia 发表于 2025-3-25 20:00:20
Identifying Ice Floes and Computing Ice Floe Distributions in SAR Images,ets, for example. Forcing from wind and waves fractures the thickening ice into pieces or floes, which then collide with each other. Over a winter season, the resulting sea ice matrix consists of fairly rounded floes with deformed surfaces composed of ridges and hummocks, separated by open water are晚间 发表于 2025-3-26 04:08:27
http://reply.papertrans.cn/16/1565/156435/156435_26.pngTartar 发表于 2025-3-26 04:31:07
Extraction of Intermediate Scale Sea Ice Deformation Parameters from SAR Ice Motion Products,on this scale interact with both the climate scale (100-300 km) sea ice processes and floe scale (1 km) processes. Understanding the intermediate regional scale sea ice deformation can help bridge the gap between the sea ice behavior on the floe scale, which is in situ measurable, and the one on theOPINE 发表于 2025-3-26 12:05:14
http://reply.papertrans.cn/16/1565/156435/156435_28.png慷慨援助 发表于 2025-3-26 13:41:30
http://reply.papertrans.cn/16/1565/156435/156435_29.pngGIST 发表于 2025-3-26 18:55:33
Mapping the Progression of Melt Onset and Freeze-Up on Arctic Sea Ice Using SAR and Scatterometry,as a wide range of human activities. In remote parts of the world, including the Arctic, knowledge and understanding of annual and interannual cycles has been limited by a paucity of observational data. Satellite observations promise to illuminate many relationships and underpin new theoretical unde