Zobrazeno 1 - 10
of 28
pro vyhledávání: '"W. S. Broecker"'
Autor:
M. Alonso-Garcia, H. (. F. Kleiven, J. F. McManus, P. Moffa-Sanchez, W. S. Broecker, B. P. Flower
Publikováno v:
Climate of the Past, Vol 13, Iss 4, Pp 317-331 (2017)
Arctic freshwater discharges to the Labrador Sea from melting glaciers and sea ice can have a large impact on ocean circulation dynamics in the North Atlantic, modifying climate and deep water formation in this region. In this study, we present for t
Externí odkaz:
https://doaj.org/article/420b42b6b2c446a09d069e50e0edef40
Autor:
W S, Broecker, S, Hemming
Publikováno v:
Science (New York, N.Y.). 294(5550)
Autor:
W S, Broecker
Publikováno v:
Science (New York, N.Y.). 291(5508)
Autor:
M, Stute, M, Forster, H, Frischkorn, A, Serejo, J F, Clark, P, Schlosser, W S, Broecker, G, Bonani
Publikováno v:
Science (New York, N.Y.). 269(5222)
A 30,000-year paleotemperature record derived from noble gases dissolved in carbon-14-dated ground water indicates that the climate in lowland Brazil (Piaui Province, 7 degrees S, 41.5 degrees W; altitude, 400 meters) was 5.4 degrees +/- 0.6 degrees
Autor:
W. S. Broecker
Publikováno v:
Paleoceanography. 14:232-232
Comment on 'Iron deficiency limits phytoplankton growth in Antarctic waters' by John H. Martin et al
Autor:
W. S. Broecker
Publikováno v:
Global Biogeochemical Cycles. 4:3-4
Autor:
W. S. Broecker
Publikováno v:
Global Biogeochemical Cycles. 4:347-347
Autor:
W. S. Broecker
Publikováno v:
Paleoceanography. 4:213-220
The goal of this paper is to explore whether the low deep to surface radiocarbon age difference of 600 years reconstructed for the glacial Atlantic requires strong North Atlantic Deep Water production and its consequent large heat delivery to the atm
Autor:
W. S. Broecker
Publikováno v:
Paleoceanography. 4:207-212
In today's ocean the salinity of low-latitude surface waters in the Pacific is on the average 1 per mil lower than in the Atlantic. Oxygen isotope records for planktonic foraminifera suggest that an even larger salinity deficit may have existed for P
Publikováno v:
Journal of Marine Research. 41:769-792