Preboreal oscillation caused by a glacial Lake Agassiz flood
- 11 December 2001
- journal article
- Published by Elsevier in Quaternary Science Reviews
- Vol. 21 (8-9), 873-878
- https://doi.org/10.1016/s0277-3791(01)00148-2
Abstract
No abstract availableKeywords
This publication has 31 references indexed in Scilit:
- Changes in the Bathymetry and Volume of Glacial Lake Agassiz Between 11,000 and 9300 14C yr B.P.Quaternary Research, 2000
- Last Glacial Maximum and deglaciation of devon island, arctic canada: support for an innuitian ice sheetQuaternary Science Reviews, 1999
- Early Preboreal cooling in the Nordic seas region triggered by meltwaterGeology, 1998
- The Preboreal oscillation around the Nordic Seas: terrestrial and lacustrine responsesJournal of Quaternary Science, 1997
- Coupled ocean‐atmosphere model response to freshwater input: Comparison to Younger Dryas EventPaleoceanography and Paleoclimatology, 1997
- Temporal‐geographical meltwater influences on the North Atlantic conveyor: Implications for the Younger DryasPaleoceanography and Paleoclimatology, 1997
- High‐resolution stable isotope records from southwest Sweden: The drainage of the Baltic Ice Lake and Younger Dryas Ice Margin OscillationsPaleoceanography and Paleoclimatology, 1997
- Complexity of Holocene Climate as Reconstructed from a Greenland Ice CoreScience, 1995
- Constraints on the Late Weichselian ice sheet over the Barents Sea from observations of raised shorelinesQuaternary Science Reviews, 1995
- Glacial Lake Agassiz: The northwestern outlet and paleofloodGeology, 1993