The Relationship between Surface Water Masses, Oceanographic Fronts and Paleoclimatic Proxies in Surface Sediments of the Greenland, Iceland, Norwegian Seas
- 1 January 1994
- book chapter
- Published by Springer Nature
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- The role of ocean-atmosphere reorganizations in glacial cyclesPublished by Elsevier ,2003
- On the Structure and Origin of Major Glaciation Cycles 1. Linear Responses to Milankovitch ForcingPaleoceanography and Paleoclimatology, 1992
- Evidence from Southern Ocean sediments for the effect of North Atlantic deep-water flux on climateNature, 1992
- The GIN Sea—A synthesis of its physical oceanography and literature review 1972–1985Earth-Science Reviews, 1991
- Evidence for two-step deglaciation and its impact on North Atlantic deep-water circulationNature, 1990
- Reconstruction of the last deglaciation: deconvolved records of ?18O profiles, micropaleontological variations and accelerator mass spectrometric14C datingClimate Dynamics, 1987
- Surface ocean circulation in the Norwegian Sea 15,000 B.P. to presentBoreas, 1985
- Thermohaline circulation in the Arctic Mediterranean SeasJournal of Geophysical Research: Oceans, 1985
- Eddies and meanders in the Iceland-Faroe Ridge areaDeep Sea Research Part A. Oceanographic Research Papers, 1979
- The Surface of the Ice-Age EarthScience, 1976