%0 Dataset
%T Qaidam area 100km resolution 0 ℃ height distribution dataset (1970-2018)
%J National Cryosphere Desert Data Center
%I National Cryosphere Desert Data Center(www.ncdc.ac.cn)
%U http://www.ncdc.ac.cn/portal/metadata/d00eefd2-7c51-4e60-bead-30970dc35fb2
%W NCDC
%R 10.12072/ncdc.Hydro.db2424.2022
%A zhu gaofeng
%K Qaidam Basin;0 ℃ altitude distribution;100km
%X The height of the 0 ℃ layer is an important characteristic layer of atmospheric detection, which reflects the temperature condition of the middle and lower troposphere. The rise and fall of this layer affects the mountain surface to a certain extent: the rise and fall of the 0 ℃ line, and then affects the freezing and thawing process of mountain water. Analyze the height and temperature of the specified layer of 39 high-altitude stations in Western China, calculate the height of the 0 ℃ layer in summer (June August), and perform Kriging interpolation to obtain the height distribution map of the 0 ℃ layer in Qaidam Basin in summer.