Permafrost temperature and active-layer thickness of Yakutia with 0.5-degree spatial resolution for model evaluation

被引:20
作者
Beer, C. [1 ,2 ,3 ]
Fedorov, A. N. [4 ,5 ]
Torgovkin, Y. [4 ]
机构
[1] Max Planck Inst Biogeochem, D-07745 Jena, Germany
[2] Stockholm Univ, Dept Appl Environm Sci ITM, S-10691 Stockholm, Sweden
[3] Stockholm Univ, Bert Bolin Ctr Climate Res, S-10691 Stockholm, Sweden
[4] Melnikov Permafrost Inst SB RAS, Yakutsk, Russia
[5] North Eastern Fed Univ, Int Ctr BEST, Yakutsk 677000, Russia
关键词
THERMAL STATE;
D O I
10.5194/essd-5-305-2013
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Based on the map of landscapes and permafrost conditions in Yakutia (Merzlotno-landshaftnaya karta Yakutskoi0 ASSR, Gosgeodeziya SSSR, 1991), rasterized maps of permafrost temperature and active-layer thickness of Yakutia, East Siberia were derived. The mean and standard deviation at 0.5-degree grid cell size are estimated by assigning a probability density function at 0.001-degree spatial resolution. The gridded datasets can be accessed at the PANGAEA repository (doi: 10.1594/PANGAEA.808240). Spatial pattern of both variables are dominated by a climatic gradient from north to south, and by mountains and the soil type distribution. Uncertainties are highest in mountains and in the sporadic permafrost zone in the south. The maps are best suited as a benchmark for land surface models which include a permafrost module.
引用
收藏
页码:305 / 310
页数:6
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