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[B−7.2 Partial pressure of carbon dioxide and quantitative evaluations of ocean parameters.]


[Contact person]

      Shoichi Taguchi
      Scientist
      Inter-spheric Environmental Section
      Environmental Assessment Department
      National Institute for Resources and Environment
      National Institute of Advanced Industrial Science and Technology
      Ministry of Economy and Industrial Technology
      Onogawa 16-3, Tsukuba, Ibaraki, 305-8569 Japan
      Tel: +81-298-61-8384 Fax: +81-298-61-8358
      E-mail: s.taguchi@aist.go.jp


[Total Budget for FY1996-2000]

 52,033,000 Yen
 (FY 2000; 9,043,000 Yen)

[Abstract]

 Flux of carbon dioxide from the atmosphere to the ocean over north Pacific Ocean, 15瀘-60瀘 was estimated to be 0.35 PgC/yr based on the gradient of partial pressure of carbon dioxide and gas transfer velocity derived from surface winds. The same flux was estimated to be 0.3 PgC/yr based on the concentrations of carbon dioxide in the atmosphere using atmospheric inverse method. These estimates are smaller than the previous estimate of 0.45 PgC/yr. Filling gaps among these estimate requires accurate observations of the gradient of partial pressure at middle of the north Pacific, Sea of Japan and Sea of Okhotsk in winter to spring.


[Key Words]

 Carbon dioxide, material transport between atmosphere and ocean, inverse method, IPCC