Anker Weidick
Biographic Data
| ID | 5592259 |
|---|---|
| NAME | Anker Weidick |
| GIVEN NAMES | Anker |
| FAMILY NAME | Weidick |
| SIGNATURE | WEIDICK A |
| AFFILIATIONS | Geological Survey of Denmark and Greenland |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1974 |
| LATEST PUBLICATION YEAR | 2009 |
| H-INDEX | 0 |
Johan Dahl Land, south Greenland: The end of a 20th century glacier expansion
The Qajuuttap Sermia glacier system north of Johan Dahl Land, on the southern slope of the Greenland ice sheet (the inland ice), has shown continuous advancing behaviour from approximately 1940 until approximately 2000. This contrasts with neighbouring sectors of the inland ice to the west and southeast, where the ice sheet has shown a more ‘normal’ trend of recession and thinning of the margin since about 1850–1890, and that has continued throug…
Greenland Ice Sheet History Since the Last Glaciation
The position of the Inland Ice margin during the late Wisconsin-Würm glaciation (ca. 15,000 yr BP) is probably marked by offshore banks (submarine moraines?) in the Davis Strait. The history of the Inland Ice since the late Wisconsin-Würm can be divided into four principal phases: (1) Relatively slow retreat from the offshore banks occurred at an average rate of approximately 1 km/100 yr until ca. 10,000 yr BP (Younger Dryas?) when the Taserqat m…
No prominent works on this page.
Greenland Ice Sheet History Since the Last Glaciation
The position of the Inland Ice margin during the late Wisconsin-Würm glaciation (ca. 15,000 yr BP) is probably marked by offshore banks (submarine moraines?) in the Davis Strait. The history of the Inland Ice since the late Wisconsin-Würm can be divided into four principal phases: (1) Relatively slow retreat from the offshore banks occurred at an average rate of approximately 1 km/100 yr until ca. 10,000 yr BP (Younger Dryas?) when the Taserqat m…
Johan Dahl Land, south Greenland: The end of a 20th century glacier expansion
The Qajuuttap Sermia glacier system north of Johan Dahl Land, on the southern slope of the Greenland ice sheet (the inland ice), has shown continuous advancing behaviour from approximately 1940 until approximately 2000. This contrasts with neighbouring sectors of the inland ice to the west and southeast, where the ice sheet has shown a more ‘normal’ trend of recession and thinning of the margin since about 1850–1890, and that has continued throug…
Climate change and permafrost (2 works) · Cryospheric studies and observations (2 works) · Geography (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Ice sheet (2 works) · Oceanography (2 works) · Physical geography (2 works) · Climatology (1 works) · Cryosphere (1 works)