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CO 2 uptake in the Pacific from 1985 to 2018: a comparative assessment of observation-and model-based estimates
  • +10
  • Masao Ishii,
  • Brendan R Carter,
  • Katsuya Toyama,
  • Keith B Rodgers,
  • Richard A Feely,
  • Thi-Tuyet-Trang Chau,
  • Frédéric Chevallier,
  • Flora Desmet,
  • Luke Gregor,
  • Yosuke Iida,
  • Yoshiteru Kitamura,
  • Jens Daniel Müller,
  • Hiroyuki Tsujino
Masao Ishii
Climate and Geochemistry Research Department, Meteorological Research Institute, Japan Meteorological Agency

Corresponding Author:[email protected]

Author Profile
Brendan R Carter
Cooperative Institute for Climate, Ocean, and Ecosystem Studies, University of Washington, NOAA Pacific Marine Environmental Laboratory
Katsuya Toyama
Climate and Geochemistry Research Department, Meteorological Research Institute, Japan Meteorological Agency
Keith B Rodgers
WPI-Advanced Institute for Marine Ecosystem Change, Tohoku University
Richard A Feely
NOAA Pacific Marine Environmental Laboratory
Thi-Tuyet-Trang Chau
Laboratoire des Sciences du Climat et de l'Environnement, IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay
Frédéric Chevallier
Laboratoire des Sciences du Climat et de l'Environnement, IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay
Flora Desmet
Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich
Luke Gregor
Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich
Yosuke Iida
Atmosphere and Ocean Department, Japan Meteorological Agency
Yoshiteru Kitamura
Climate and Geochemistry Research Department, Meteorological Research Institute, Japan Meteorological Agency
Jens Daniel Müller
Environmental Physics, Institute of Biogeochemistry and Pollutant Dynamics, ETH Zürich
Hiroyuki Tsujino
Climate and Geochemistry Research Department, Meteorological Research Institute, Japan Meteorological Agency

Abstract

 Net and anthropogenic CO 2 exchange in the Pacific represents a major contribution to the global CO 2 sink.  The Pacific is thought to have turned to a net sink of CO 2 that is growing primarily due to the increasing uptake of anthropogenic CO 2.  The equatorial region is key in determining net and anthropogenic CO 2 uptakes and their trends and variability in the Pacific.
08 Nov 2024Submitted to ESS Open Archive
09 Nov 2024Published in ESS Open Archive