%0 Dataset
%T Changes in the Advance and Retreat of No.1 Glacier in the Source of the Urumqi River from 1982 to 2000
%J National Cryosphere Desert Data Center
%I National Cryosphere Desert Data Center(www.ncdc.ac.cn)
%U http://www.ncdc.ac.cn/portal/metadata/96601b3a-139a-11e6-8fcc-28d244cbcf8d
%W NCDC
%R 10.12072/Tianshan.024.2017.db
%A Bao Liang
%A Feiteng Wang
%K Glaciers advance and retreat;glaciers change;melt
%X The types of glacier advance and retreat changes include: ① seasonal advance and retreat. Glaciers tend to melt less in winter, resulting in advancing at the end or steepening ice cliffs. In summer, glaciers tend to melt more, retreating at the end or slowing down ice cliffs Years of advancement and retreat. Glaciers continuously move forward or retreat over a long period of time, reflecting changes in climate conditions. This dataset is the data on glacier advance and retreat changes of No.1 Glacier in the source of the Urumqi River from 1982 to 2000