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 P>
collect time | 1982/01/01 - 2000/12/31 |
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collect place | Tianshan Glaciological Station, No.1 Glacier in the Source of the Urumqi River |
altitude | 3700.0m - 4200.0m |
data size | 30.6 KiB |
data format | csv |
Coordinate system | WGS84 |
Observation, experiment, determination
Labor
Raw data
# | title | file size |
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1 | T_DA_JTBH.csv | 30.6 KiB |
1982 1983 1984 1985 1986 1987 1988 1989 1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000
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