The Atmosphere During the Younger Dryas-Reference-Cited by-同舟云学术

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The Atmosphere During the Younger Dryas

Published:1993-07-09 Issue:5118 Volume:261 Page:195-197
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Mayewski P. A.¹,Meeker L. D.¹,Whitlow S.¹,Twickler M. S.¹,Morrison M. C.¹,Alley R. B.²,Bloomfield P.³,Taylor K.⁴

Affiliation:

1. Glacier Research Group, Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham, NH 03824

2. Earth System Science Center and Department of Geosciences, Pennsylvania State University, University Park, PA 16802

3. Department of Statistics, North Carolina State University, Raleigh, NC 27695

4. Desert Research Institute, University of Nevada System, Reno, NV 89506

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference31 articles.

1. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event

2. BIRCHFIELD, G. E., PALEOCEANOGRAPHY 5: 835 (1990).

3. Bloomfield, P., Least Absolute Deviations: Theory, Applications, and Algorithms: 131 (1983).

4. BROCCOLI, A. J., GEOGRAPHIE PHYSIQUE ET QUATERNAIRE 41: 291 (1987).

5. BROECKER, W.S., THE ROLE OF OCEAN-ATMOSPHERE REORGANIZATIONS IN GLACIAL CYCLES, GEOCHIMICA ET COSMOCHIMICA ACTA 53: 2465 (1989).

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