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Does the ocean–atmosphere system have more than one stable mode of operation?
scholarly article
Does the ocean-atmosphere system have more than one stable mode of operation?
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instance of
scholarly article
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title
Does the ocean–atmosphere system have more than one stable mode of operation?
(English)
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main subject
atmosphere
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author
Wallace Broecker
series ordinal
1
object named as
Wallace S. Broecker
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author name string
Dorothy M. Peteet
series ordinal
2
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David Rind
series ordinal
3
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language of work or name
English
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publication date
May 1985
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published in
Nature
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volume
315
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issue
6014
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page(s)
21-26
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exact match
https://scigraph.springernature.com/pub.10.1038/315021a0
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cites work
Polar ice evidence that atmospheric CO2 20,000 yr BP was 50% of present
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https://api.crossref.org/works/10.1038%2F315021A0
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7 January 2021
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Ice core sample measurements give atmospheric CO2 content during the past 40,000 yr
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reference URL
https://api.crossref.org/works/10.1038%2F315021A0
retrieved
7 January 2021
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Is there a tie between atmosphere CO2 content and ocean circulation
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https://api.crossref.org/works/10.1038%2F315021A0
retrieved
7 January 2021
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inferred from DOI database lookup
A new model for the role of the oceans in determining atmospheric PCO2
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https://api.crossref.org/works/10.1038%2F315021A0
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7 January 2021
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Rapid atmospheric CO2 variations and ocean circulation
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https://api.crossref.org/works/10.1038%2F315021A0
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7 January 2021
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Pleistocene Temperatures
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7 January 2021
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Insolation changes, ice volumes, and the O18record in deep-sea cores
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https://api.crossref.org/works/10.1038%2F315021A0
retrieved
7 January 2021
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Oxygen Isotope and Palaeomagnetic Stratigraphy of Equatorial Pacific Core V28-238: Oxygen Isotope Temperatures and Ice Volumes on a 105 Year and 106 Year Scale
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reference URL
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7 January 2021
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Variations in the Earth's Orbit: Pacemaker of the Ice Ages
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Modeling the climatic response to orbital variations
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A new greenland deep ice core
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Lake Sediments as Continental δ18O Records from the Glacial/Post-Glacial Transition
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One thousand centuries of climatic record from cAMP century on the greenland ice sheet
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Glacial to interglacial changes in ocean chemistry
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Ocean chemistry during glacial time
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Radiocarbon measurements on coexisting benthic and planktic foraminifera shells: potential for reconstructing ocean ventilation times over the past 20 000 years
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14C measurements on foraminifera of deep sea core V28-238 and their preliminary interpretation
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7 January 2021
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Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence
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Weyl's Theory of Glaciation Supported by Isotopic Study of Norwegian Core K 11.
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Radiocarbon dating of the last glaciation in Peru
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Oxygen Isotope Profiles through the Antarctic and Greenland Ice Sheets
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https://api.crossref.org/works/10.1038%2F315021A0
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7 January 2021
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inferred from DOI database lookup
A revised estimate for the radiocarbon age of North Atlantic deep water
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reference URL
https://api.crossref.org/works/10.1038%2F315021A0
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7 January 2021
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Hydrology and ocean circulation
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reference URL
https://api.crossref.org/works/10.1038%2F315021A0
retrieved
7 January 2021
based on heuristic
inferred from DOI database lookup
Identifiers
DOI
10.1038/315021A0
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ADS bibcode
1985Natur.315...21B
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Dimensions Publication ID
1049069712
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