The effect of sea-ice growth on air–sea CO2 flux in a tank experiment

Nomura, Daiki; Yoshikawa-Inoue, Hisayuki; Toyota, Takenobu

doi:10.1111/j.1600-0889.2006.00204.x


Hokkaido University \| Library \| HUSCAP	Advanced Search		言語

	Home
	About HUSCAP
	Open Access Policy

	Browse by Author

Browse
	Communities & Collections

	Scholarly Journals
	Theses
	Doctoral Dissertations Listed by Graduate Schools
	Conference Procs.
	Events

	HUSCAP Senior (in Japanese)

	Societies

	Downloads (country)

For university staff
	How to post your papers to HUSCAP
	Publication of theses
	Helpline about theses publication

Open Archives Compliant

You can search our collection also at:
	Google
	Google Scholar
	CiNii
	IRDB
	OAIster
	NDLTD

Hokkaido University Collection of Scholarly and Academic Papers >
Graduate School of Fisheries Sciences / Faculty of Fisheries Sciences >
Peer-reviewed Journal Articles, etc >

The effect of sea-ice growth on air–sea CO2 flux in a tank experiment

This item is licensed under:Creative Commons Attribution 4.0 International

Files in This Item:

Tellus(2006)_58B_418-426.pdf

504.57 kB

PDF

View/Open

Please use this identifier to cite or link to this item:http://hdl.handle.net/2115/70575

Title:	The effect of sea-ice growth on air–sea CO2 flux in a tank experiment
Authors:	Nomura, Daiki Browse this author →KAKEN DB
	Yoshikawa-Inoue, Hisayuki Browse this author →KAKEN DB
	Toyota, Takenobu Browse this author →KAKEN DB
Issue Date:	2006
Publisher:	Taylor & Francis
Journal Title:	Tellus B : Chemical and Physical Meteorology
Volume:	58
Issue:	5
Start Page:	418
End Page:	426
Publisher DOI:	10.1111/j.1600-0889.2006.00204.x
Abstract:	In order to clarify the CO2 exchange between the seawater and the overlying air during the sea-ice formation, we have carried out tank experiments in a low-temperature room. CO2 concentration above the sea-ice began to increase since the beginning of the sea-ice formation, and increased at larger rates with time and the decrease in air temperature. This increase of CO2 concentration in air was mainly caused by the increase in dissolved inorganic carbon concentration in the brine of the upper part of sea-ice, changes in CO2 solubility and dissociation constants of carbonic acid. The CO2 flux increased logarithmically with time, and reached a level of 2 × 10-4 to 5 × 10-4 g-C m-2 hr-1 at 50 mm ice thickness. We found that the CO2 flux was correlated well with the salinity and negatively with the volume of the brine in the upper part of the sea-ice. These suggested the larger role of the difference in partial pressure of CO2 between brine and air as compared to that of competitive change in the brine volume. Present results suggest the necessity to examine the CO2 exchange between the seawater and air in seasonal sea-ice areas.
Rights:	https://creativecommons.org/licenses/by/4.0/
Type:	article
URI:	http://hdl.handle.net/2115/70575
Appears in Collections:	水産科学院・水産科学研究院 (Graduate School of Fisheries Sciences / Faculty of Fisheries Sciences) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

Submitter: 野村大樹

OAI-PMH ( junii2 , jpcoar_1.0 )

- Hokkaido University