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Author: York University (Toronto, Ont.)
Publisher:
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Category :
Languages : en
Pages :
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Author: York University (Toronto, Ont.)
Publisher:
ISBN:
Category :
Languages : en
Pages :
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Author: W. C. Mahaney
Publisher:
ISBN:
Category : Climatic changes
Languages : en
Pages : 99
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Author: Fernando López-Vera
Publisher:
ISBN:
Category : Climatic changes
Languages : en
Pages : 670
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Author: Johannes Oerlemans
Publisher: Springer Science & Business Media
ISBN: 9401578230
Category : Science
Languages : en
Pages : 414
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Proceedings of the Symposium on Glacier Fluctuations and Climatic Change, held in Amsterdam, June 1-5, 1987
Author:
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Category : Climatic changes
Languages : en
Pages : 563
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Author: J T Andrews
Publisher: Taylor & Francis
ISBN: 1040087361
Category : Science
Languages : en
Pages : 803
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First published in 1985, Quaternary Environments represents the culmination of Quaternary research in the region of Baffin Island, Baffin Bay and West Greenland over a period of twenty years and it will serve as a timely and complementary balance to the paleo- oceanographic studies in the NE North Atlantic. The region of Baffin Island, Baffin Bay and West Greenland is probably the best place in the world to examine the interactions between ice, land and oceans on timescales of a few hundred to many thousands of years. Two introductory chapters outline the history of research and the physical background. In Part II the evidence for glacial erosion and deposition over the eastern Canadian Arctic is examined and the history of the Baffin Island continental shelf is described. Part III deals with the paleo- oceanography of Baffin Bay and the Labrador Sea through an examination of deep-sea cores dated by several different methods. In Part IV there is a comprehensive account of the stratigraphy of Baffin Island, Bylot Island, and West Greenland, from the Pliocene to the late Wisconsin. Part V examines the climatic effects of the past 10,000 years, considering evidence from pollen analysis, glacier fluctuations, changes of sea level and the response of early (Eskimo) man. This important volume will interest all quaternary scientists, especially those in glaciology, glacial geology, marine geology, and geomorphology.
Author: Nobuyuki Yonekura
Publisher:
ISBN:
Category :
Languages : en
Pages : 160
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Author: YORK UNIVERSITY. Symposium on quaternary research
Publisher:
ISBN:
Category :
Languages : en
Pages : 318
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Author: International Association for Quaternary Research
Publisher:
ISBN:
Category : Climatology
Languages : en
Pages : 159
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Author: N.-A. Mörner
Publisher: Springer Science & Business Media
ISBN: 9401576920
Category : Science
Languages : en
Pages : 651
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Nils-Axel Marner &Wibjarn Karlen Organizers of the Stockholm Symposium in 1983 Stockholm University, Sweden This book is the Proceedings of the SECOND NORDIC SYMPOSIUM ON CLIMATIC CHANGES AND RELATED PROBLEMS held in Stockholm, Sweden, May 16-20, 1983 (Frydendahl et al., 1983; Marner, 1983). This was "an international interdisciplinary symposium with special refe rence to Nordic records and their relation to global climatic changes". The first NORDIC SYMPOSIUM ON CLIMATIC CHANGES AND RELATED PROBLEMS was held in Copenhagen in 1978 ( Frydendahl, 1978) and had a very broad scientific program. The SECOND NORDIC SYMPOSIUM was specifically directed to certain problems, time ranges and sources of information, as discussed below. Scandinavia is a classical area for the study of climatic fluctuations during the last 20,000 years . A major part of the basic data for the international theories and synthesis originate from Scandinavian data. This applies, for example, to: (1) The drastic climatic fluctuations in connection with the re cession of the land-ice giving rise to the alternation of inter stadials (warm periods with rapid ice recession) and stadials (cold periods with readvances or retardations in the ice recession). (2) The climatic changes during the Holocene with its well-known sub-division according to the Blytt-Sernander system (nowadays being used far outside the boreal region for which it was origi nally defined). (3) The Holocene climatic optimum and the subsequent climatic de terioration at around 2500 BP (well-established already at the beginning of this century).
