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Late Pleistocene Climatic Record in Norwegian and Greenland Sea Deep-sea Cores

Late Pleistocene Climatic Record in Norwegian and Greenland Sea Deep-sea Cores PDF Author: Thomas Bartlett Kellogg
Publisher:
ISBN:
Category :
Languages : en
Pages : 1090

Book Description


Late Pleistocene Climatic Record in Norwegian and Greenland Sea Deep-sea Cores

Late Pleistocene Climatic Record in Norwegian and Greenland Sea Deep-sea Cores PDF Author: Thomas Bartlett Kellogg
Publisher:
ISBN:
Category :
Languages : en
Pages : 1090

Book Description


Late Pleistocene Climatic Record in Norwegian and Greenland Sea Deep-sea Cores

Late Pleistocene Climatic Record in Norwegian and Greenland Sea Deep-sea Cores PDF Author: T. B. Kellogg
Publisher:
ISBN:
Category :
Languages : en
Pages : 1090

Book Description


Late Pleistocene Climatic Record in Norwegian and Greenland Deep-sea Cores

Late Pleistocene Climatic Record in Norwegian and Greenland Deep-sea Cores PDF Author: Thomas Bartlett Kellogg
Publisher:
ISBN:
Category :
Languages : en
Pages : 1090

Book Description


Investigation of Late Quaternary Paleoceanography and Paleoclimatology

Investigation of Late Quaternary Paleoceanography and Paleoclimatology PDF Author: R. M. Cline
Publisher: Geological Society of America
ISBN: 0813711452
Category : Science
Languages : en
Pages : 636

Book Description


The Geologic Record of Climatic Change

The Geologic Record of Climatic Change PDF Author: Thomas J. Crowley
Publisher:
ISBN:
Category : Climatic changes
Languages : en
Pages : 168

Book Description


Ice Drift, Ocean Circulation and Climate Change

Ice Drift, Ocean Circulation and Climate Change PDF Author: Jens Bischof
Publisher: Springer Science & Business Media
ISBN: 9781852336486
Category : Nature
Languages : en
Pages : 254

Book Description
The issue of global warming and climate change is of continuous concern. Since the 1970s, it bas been shown that the pack-ice around the Arctic Ocean is thinning, the margin of permafrost is moving north and the vegetation in the high northern parts of the world is changing (the 'greening' of the Arctic). But are these changes the result of human activity or simply regular variations of the Earth's climate system? Over thousands of years, a continuous archive of iceberg and sea ice drift bas formed in the deep-sea sediments, revealing the place of the ice's origin and allowing a reconstruction of the surface currents and the climate of the past. However, the drift of floating ice from one place to another is not just a passive record of past ocean circulation. It actively influences and changes the surface ocean circulation, thus having a profound effect on climate change. Ice Drift, Ocean Circulation and Climate Change is the first book to focus on the interactions between ice, the ocean and the atmosphere and to describe how these three components of the climate system influence each other. It makes clear the positive contribution of paleoclimatology and paleoceanography and should be read by anyone concerned with global warming and climate change.

International Decade of Ocean Exploration

International Decade of Ocean Exploration PDF Author: United States. Environmental Data Service
Publisher:
ISBN:
Category : Marine resources
Languages : en
Pages : 444

Book Description


Start of a Glacial

Start of a Glacial PDF Author: George J. Kukla
Publisher: Springer Science & Business Media
ISBN: 3642769543
Category : Science
Languages : en
Pages : 414

Book Description
Some 115 thousand years ago the world as we know it today shifted into a much colder glacial mode which culminated with huge ice sheets reaching as far south as New York, Berlin and St. Petersburg. The numerical climate models, used to predict the next century climate, were as yet unable to explain what happened. The reader of the book gains a detailed picture of what is known on the most important episodes of the past climate history, what to expect during the transition into a glacial climate mode, and which aspects and elements of the climate system seem mostsusceptible to change. The climate modelers will realize that the long term history of natural climate variations may hold important clues to the mechanism of climate changes which should be taken in account if the near future CO2 rich climate have to be predicted with any degree ofreliability.

Late Neogene Chronostratigraphy, Biostratigraphy, Biochronology and Paleoclimatology

Late Neogene Chronostratigraphy, Biostratigraphy, Biochronology and Paleoclimatology PDF Author: William A. Berggren
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 834

Book Description
The integration of modern paleomagnetic, radiometric, and biostratigraphic studies has provided an accurate geochronological framework for the past 10 million years--the Late Neogene. Marine zones based on calcareous and siliceous planktonic organisms are recognized from the sub-Arctic region to the sub-Antarctic and their correlation to the paleomagnetic time scale is now feasible in some detail for the past 5 my. Likewise, the relationship of geochemically calibrated mammalian biochronology to the marine succession has been greatly improved. Within this framework of time it is possible to delineate the history of major features in Late Neogene paleontology, climatology, and oceanography. (Author).

The Northern North Atlantic

The Northern North Atlantic PDF Author: Priska Schäfer
Publisher: Springer Science & Business Media
ISBN: 3642568769
Category : Science
Languages : en
Pages : 520

Book Description
The northern North Atlantic is one of the regions most sensitive to past and present global changes. This book integrates the results of an interdisciplinary project studying the properties of the Greenland-Iceland-Norwegian Seas and the processes of pelagic and benthic particle formation, particle transport, and deposition in the deep-sea sediments. Ice-related and biogeochemical processes have been investigated to decipher the spatial and temporal variability of the production and fate of organic carbon in this region. Isotopic stratigraphy, microfossil assemblages and paleotemperatures are combined to reconstruct paleoceanographic conditions and to model past climatic changes in the Late Quaternary. The Greenland-Iceland-Norwegian Seas can now be considered one of the best studied subbasins of the world`s oceans.