TY  - Data
T1  - Changes in the Advance and Retreat of No.1 Glacier in the Source of the Urumqi River from 1982 to 2000
A1  - Bao Liang
A1  - Feiteng Wang
DO  - 10.12072/Tianshan.024.2017.db
PY  - 2020
DA  - 2020-12-23
PB  - National Cryosphere Desert Data Center
AB  - 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
DB  - NCDC
UR  - http://www.ncdc.ac.cn/portal/metadata/96601b3a-139a-11e6-8fcc-28d244cbcf8d
ER  -