The Northeast Water Polynya as an atmospheric CO2 sink: a seasonal rectification hypothesis

P. L. Yager, D. W.R. Wallace, K. M. Johnson, W. O. Smith, P. J. Minnett, J. W. Deming

Research output: Contribution to journalArticlepeer-review

100 Scopus citations

Abstract

During the multidisciplinary "NEW92' cruise of the Polar Sea to the recurrent Northeast Water (NEW) Polynya (77-81°N, 6-17°W; July-August 1992), total dissolved inorganic carbon and total alkalinity in the water column were measured. Biological processes depleted the total inorganic carbon of summer surface waters by up to 2 mol C m-2 or about 3%. On a regional basis this depletion correlated with depth-integrated values of chlorophyll a,particulate organic carbon, and the inorganic nitrogen deficit. These measurements and observations allowed formulation of a new hypothesis whereby sesonally ice-covered regions like the N EW Polynya promote a unique biologically and physically mediated "rectification' of the typical (ice free, low latitude) seasonal cycle of air-sea CO2 flux. -Authors

Original languageEnglish (US)
Pages (from-to)4389-4398
Number of pages10
JournalJournal of Geophysical Research
Volume100
Issue numberC3
DOIs
StatePublished - Jan 1 1995
Externally publishedYes

ASJC Scopus subject areas

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Fingerprint Dive into the research topics of 'The Northeast Water Polynya as an atmospheric CO<sub>2</sub> sink: a seasonal rectification hypothesis'. Together they form a unique fingerprint.

Cite this