Journal of Water Resources and Ocean Science

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Exchanges of Methane between Lakes and the Atmosphere in Hokkaido, Subarctic Climate Region, Japan

Received: 12 December 2014    Accepted: 27 December 2014    Published: 04 January 2015
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Abstract

Dissolved methane concentrations (DM) at twelve major lakes in Hokkaido, the northernmost island in Japan were observed in the open water season during 2006 ~ 2009 to estimate diffusive flux from lake surfaces to the atmosphere. An inverse relationship between lake size and DM was obtained in lakes in Hokkaido as was found for the European boreal lakes. All lake images larger than 0.001 km2 were obtained by image processing of map data and area and number distributions were analyzed in order to calculate mass fluxes of diffusive methane. Total area of all (1,269) lakes in Hokkaido is 809 km2. Regional diffusive flux of methane from lakes to the atmosphere in Hokkaido was estimated to be 0.581 Gg CH4 yr–1. Average diffusive flux density (per lake area) was about 0.718 g CH4 m–2 yr–1. This is a similar value to that in European boreal lakes on no-permafrost inland areas. Extremely high flux was found in Lake Abashiri-ko, one of highly eutrophic, meromictic lakes.

DOI 10.11648/j.wros.20140306.14
Published in Journal of Water Resources and Ocean Science (Volume 3, Issue 6, December 2014)
Page(s) 89-94
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Methane Flux, Lakes, Eutrophication, Global Warming

References
[1] Sasaki, M., S. Imura, S. Kudoh, T. Yamanouchi, S. Morimoto and G. Hashida (2009), Methane efflux from bubbles suspended in ice-covered lakes in Syowa Oasis, East Antarctica., J. Geophys. Res., 114, D18114, doi: 10.1029/2009JD011849.
[2] Sasaki, M., N. Endoh, S. Imura, S. Kudoh, T. Yamanouchi, S. Morimoto and G. Hashida (2010), Air-lake exchange of methane during the open water season in Syowa Oasis, East Antarctica., J. Geophys. Res., 115, D16313, doi: 10.1029/2010JD013822.
[3] Liss P.S. and L. Merlivat (1986), Air-sea gas exchange rates: Introduction and synthesis, in The Role of Air-Sea Gas Exchange in Geochemical Cycling, edited by P. Buat-Menard , pp.113-127, D. Reidel, Norwell, Mass.
[4] Liss P.S. and Slater P. (1974), Flux of gases across the air-sea interface, Nature 247, pp.181-184.
[5] Nightingale P.D. and Liss P.S. (2003), Gases in seawater, in The Oceans and Marine Geochemistry, ed H. Elderfield, Vol 6 of A Treatise on Geochemistry (eds Holland and Turekian) Ch 3, 49 – 82.
[6] Cole J. J. and N. F. Caraco, 1998, Atmospheric exchange of carbon dioxide in a low-wind oligotrophic lake measured by the addition of SF6, Limnology and Oceanography, 43(4), 647-656
[7] Deacon, E.L. (1977), Gas transfer to and across an air-water interface, Tellus, 29, 363-374.
[8] Bastviken, D., J. Cole, M. Pace and L. Tranvik (2004), Methane emissions from lakes: Dependence of lake characteristics, two regional assessments, and a global estimate, Global Biogeochemical Cycles, vol. 18, GB4009, doi: 10.1029/2004GB002238.
[9] Downing, J. A., Y. T. Prairie, J. J. Cole, C. M. Duarte, L. J. Tranvik, R. G. Striegl, W. H. McDowell, P. Kortelainen, N. F. Caraco, J. M. Melack and J. J. Middelburg (2006), The global abundance and size distribution of lakes, ponds, and impoundments, Limnology and Oceanography, 51(5), 2388-2397
[10] Juutinen, S., M. Rantakari, P. Kortelainen, J. T. Huttunenn, T. Larmala, J. Alm, J. Silvola and P. J. Martikainen (2009), Methane dynamics in different boreal lake types, Biogeosciences, 6, 209-223.
Author Information
  • Department of Mechanical Engineering, Kitami Institute of Technology, Kitami, Japan

  • Department of Mechanical Engineering, Kitami Institute of Technology, Kitami, Japan

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  • APA Style

    Masafumi Sasaki, Noboru Endoh. (2015). Exchanges of Methane between Lakes and the Atmosphere in Hokkaido, Subarctic Climate Region, Japan. Journal of Water Resources and Ocean Science, 3(6), 89-94. https://doi.org/10.11648/j.wros.20140306.14

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    ACS Style

    Masafumi Sasaki; Noboru Endoh. Exchanges of Methane between Lakes and the Atmosphere in Hokkaido, Subarctic Climate Region, Japan. J. Water Resour. Ocean Sci. 2015, 3(6), 89-94. doi: 10.11648/j.wros.20140306.14

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    AMA Style

    Masafumi Sasaki, Noboru Endoh. Exchanges of Methane between Lakes and the Atmosphere in Hokkaido, Subarctic Climate Region, Japan. J Water Resour Ocean Sci. 2015;3(6):89-94. doi: 10.11648/j.wros.20140306.14

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  • @article{10.11648/j.wros.20140306.14,
      author = {Masafumi Sasaki and Noboru Endoh},
      title = {Exchanges of Methane between Lakes and the Atmosphere in Hokkaido, Subarctic Climate Region, Japan},
      journal = {Journal of Water Resources and Ocean Science},
      volume = {3},
      number = {6},
      pages = {89-94},
      doi = {10.11648/j.wros.20140306.14},
      url = {https://doi.org/10.11648/j.wros.20140306.14},
      eprint = {https://download.sciencepg.com/pdf/10.11648.j.wros.20140306.14},
      abstract = {Dissolved methane concentrations (DM) at twelve major lakes in Hokkaido, the northernmost island in Japan were observed in the open water season during 2006 ~ 2009 to estimate diffusive flux from lake surfaces to the atmosphere. An inverse relationship between lake size and DM was obtained in lakes in Hokkaido as was found for the European boreal lakes. All lake images larger than 0.001 km2 were obtained by image processing of map data and area and number distributions were analyzed in order to calculate mass fluxes of diffusive methane. Total area of all (1,269) lakes in Hokkaido is 809 km2. Regional diffusive flux of methane from lakes to the atmosphere in Hokkaido was estimated to be 0.581 Gg CH4 yr–1. Average diffusive flux density (per lake area) was about 0.718 g CH4 m–2 yr–1. This is a similar value to that in European boreal lakes on no-permafrost inland areas. Extremely high flux was found in Lake Abashiri-ko, one of highly eutrophic, meromictic lakes.},
     year = {2015}
    }
    

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  • TY  - JOUR
    T1  - Exchanges of Methane between Lakes and the Atmosphere in Hokkaido, Subarctic Climate Region, Japan
    AU  - Masafumi Sasaki
    AU  - Noboru Endoh
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    DO  - 10.11648/j.wros.20140306.14
    T2  - Journal of Water Resources and Ocean Science
    JF  - Journal of Water Resources and Ocean Science
    JO  - Journal of Water Resources and Ocean Science
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    PB  - Science Publishing Group
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    UR  - https://doi.org/10.11648/j.wros.20140306.14
    AB  - Dissolved methane concentrations (DM) at twelve major lakes in Hokkaido, the northernmost island in Japan were observed in the open water season during 2006 ~ 2009 to estimate diffusive flux from lake surfaces to the atmosphere. An inverse relationship between lake size and DM was obtained in lakes in Hokkaido as was found for the European boreal lakes. All lake images larger than 0.001 km2 were obtained by image processing of map data and area and number distributions were analyzed in order to calculate mass fluxes of diffusive methane. Total area of all (1,269) lakes in Hokkaido is 809 km2. Regional diffusive flux of methane from lakes to the atmosphere in Hokkaido was estimated to be 0.581 Gg CH4 yr–1. Average diffusive flux density (per lake area) was about 0.718 g CH4 m–2 yr–1. This is a similar value to that in European boreal lakes on no-permafrost inland areas. Extremely high flux was found in Lake Abashiri-ko, one of highly eutrophic, meromictic lakes.
    VL  - 3
    IS  - 6
    ER  - 

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