On the carbonate system of the East-Siberian sea waters

I. I. Pipko, I. P. Semiletov, S. P. Pugach

Arctic Seas Carbon Research Internatonal Lab

Research output: Contribution to journal › Article › peer-review

Abstract

East-Siberian Sea waters were estimated as potential source and/or drainage reservoir for excessive atmospheric CO₂. For the studied region carbon dioxide fluxes in ocean-atmosphere system were calculated using cubic parametrization connecting CO₂ fluxes with wind velocity taken with diurnal averaging. It is shown that the considered water area generally was carbon dioxide source to the atmosphere.

Original language	English
Pages (from-to)	398-401
Number of pages	4
Journal	Doklady Akademii Nauk
Volume	402
Issue number	3
Publication status	Published - 2005

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title = "On the carbonate system of the East-Siberian sea waters",

abstract = "East-Siberian Sea waters were estimated as potential source and/or drainage reservoir for excessive atmospheric CO2. For the studied region carbon dioxide fluxes in ocean-atmosphere system were calculated using cubic parametrization connecting CO2 fluxes with wind velocity taken with diurnal averaging. It is shown that the considered water area generally was carbon dioxide source to the atmosphere.",

author = "Pipko, {I. I.} and Semiletov, {I. P.} and Pugach, {S. P.}",

year = "2005",

language = "English",

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AU - Semiletov, I. P.

AU - Pugach, S. P.

PY - 2005

Y1 - 2005

N2 - East-Siberian Sea waters were estimated as potential source and/or drainage reservoir for excessive atmospheric CO2. For the studied region carbon dioxide fluxes in ocean-atmosphere system were calculated using cubic parametrization connecting CO2 fluxes with wind velocity taken with diurnal averaging. It is shown that the considered water area generally was carbon dioxide source to the atmosphere.

AB - East-Siberian Sea waters were estimated as potential source and/or drainage reservoir for excessive atmospheric CO2. For the studied region carbon dioxide fluxes in ocean-atmosphere system were calculated using cubic parametrization connecting CO2 fluxes with wind velocity taken with diurnal averaging. It is shown that the considered water area generally was carbon dioxide source to the atmosphere.

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JO - Doklady Akademii Nauk

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