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Air-sea disequilibrium enhances ocean carbon storage during glacial periods
Author(s) -
Samar Khatiwala,
Andreas Schmittner,
Juan Muglia
Publication year - 2019
Publication title -
science advances
Language(s) - Uncategorized
Resource type - Journals
SCImago Journal Rank - 5.928
H-Index - 146
ISSN - 2375-2548
DOI - 10.1126/sciadv.aaw4981
Subject(s) - glacial period , interglacial , iron fertilization , drawdown (hydrology) , disequilibrium , environmental science , carbon dioxide in earth's atmosphere , oceanography , biological pump , last glacial maximum , carbon dioxide , carbon cycle , geology , atmospheric sciences , climate change , ecology , ecosystem , paleontology , biology , phytoplankton , medicine , ophthalmology , geotechnical engineering , nutrient , aquifer , groundwater
Temperature and iron fertilization are more important in driving glacial-interglacial CO 2 cycles than previously thought.

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