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Analysis on long term variations of seasonal sea ice extent and its climatological interpretation

Research Project

Project/Area Number 08640539
Research Category

Grant-in-Aid for Scientific Research (C)

Allocation TypeSingle-year Grants
Section一般
Research Field Meteorology/Physical oceanography/Hydrology
Research InstitutionKitami Institute of Technology

Principal Investigator

ENOMOTO Hiroyuki  北見工業大学, 土木開発工学科, 教授 (00213562)

Project Period (FY) 1996 – 1998
Project Status Completed (Fiscal Year 1998)
Budget Amount *help
¥2,100,000 (Direct Cost: ¥2,100,000)
Fiscal Year 1998: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1997: ¥300,000 (Direct Cost: ¥300,000)
Fiscal Year 1996: ¥1,300,000 (Direct Cost: ¥1,300,000)
KeywordsSea ice / Climatic change / cryosphere / satellite Remote Sensing / Sea of Okhotsk / Antarctic Arctic / sea ice / climatic change / okhotsk Sea / 北極・南極 / 雪氷園
Research Abstract

Sea ice fluctuations in the sea of Okhotsk was investigated by using the daily sea ice map. A new ice map was made to indicate thin/thick sea ice coverage. The algorithm for thin ice observations was developed by the University, of Washington, NASA and also by ourselves. Sea ice extent seems to be affected by the early winter conditions. Seasonal trends was observed in the extreme year ; cold/warm, then sea ice extent showed faster/later trend in the corresponding winter.
Daily polynya fluctuations were investigated. The accumulated advances of polynya area in winter reflect the variation of maximum sea ice area of the corresponding winter.
An isolated sea ice area was observed in the warmer winter, 1995196 and 1996/97. Its distribution and stability are similar to the Odden ice pattern in the Greenland Sea. This phenomena was observed only in the two years in the recent 10-years data.

Report

(4 results)
  • 1998 Annual Research Report   Final Research Report Summary
  • 1997 Annual Research Report
  • 1996 Annual Research Report
  • Research Products

    (17 results)

All Other

All Publications (17 results)

  • [Publications] H.Enomoto: "Interannanl variability of seaice conditions in Syowa Station sector deduced from DMSD SSM/I data" Proc.NIPR Symp. Polar meteorol Glacial. 10. 119-126 (1996)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] 榎本浩之: "オホーツク海の海氷成長と大気-海洋相互作用" 月刊 海洋. 28・9. 572-575 (1996)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] H.Enomoto: "Observation of thin seaice area in the Okhotsk Sea and Impacts for Climatological Study" 日本リモートセンシング学会誌. 16・2. 14-25 (1996)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] 滝沢隆俊 他: "コスモノート・ポリニア水域の水温構造とSSM/I画像から見たポリニアの特徴" 南極資料. 41・1. 335-346 (1997)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] Shirasaki, K., H.Enomoto, K.Tateyama, H.Warashina, A.Watanabe: "Observation of seaice conditions using visible and near-infrared channels in MOS-I/MESSR and ADEOS/AVNIR" Polar Meteorol, Glacial.12. 86-96 (1998)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] Enomoto, H.et al.: "Interannual variability of sea ice conditions in Syowa Station sector deduced from DMSP SSM/I data." Proc.NIPR Symp.polar Meteorol.Glaciol.10. 119-126 (1996)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] Enomoto, H.: "Sea ice growth in the Sea of Okhotsk and air-sea interaction, (in Japanese)" Kaiyo. 28. 572-575 (1996)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] Enomoto, H.: "Observation of thin sea ice area in the Okhotsk Sea and impact for climatological study." Jour.of the Remote Sensing Society of Japan. 16. 100-111 (1996)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] T.Takizawa et al.: "Temperature structure and SSM/I Images of the Cosmonaut Polynya Region(in Japanese)" Antarctic Record. 41. 335-347 (1997)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] Shirasaki, K.et al.: "Observation of sea ice conditions using visible and near-infrared channels in MOS-1/MESSR and ADEOS/AVNIR." Polar Meteorol.Glaciol. 12. 86-96 (1998)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1998 Final Research Report Summary
  • [Publications] Shirasaki,K.,H.Enomoto,K.Tateyama,H.Warashina,A.Watanabe: "Observation of sea ice conditions using visible and near-intrared channels in MOS-I/MESSR and ADEOS/AVNIR" Polar Meteorol,Glaciol.12. 86-96 (1998)

    • Related Report
      1998 Annual Research Report
  • [Publications] H.Enomoto: "Interannual variability of sea ice conditions in Syawa Station sector deduced from DMSP SSM/I data" Proc.NIPR Symp.Polar Meteorol.Glaciol. 10. 119-126 (1996)

    • Related Report
      1997 Annual Research Report
  • [Publications] 榎本浩之: "オホーツク海の海氷成長と大気-海洋相互作用" 月刊 海洋. 28・9. 572-575 (1996)

    • Related Report
      1997 Annual Research Report
  • [Publications] H.Enomoto: "Observation of thin sea ice area in the Okhotsk Sea and Impacts for Climatological Study" 日本リモートセンシング学会誌. 16・2. 14-25 (1996)

    • Related Report
      1997 Annual Research Report
  • [Publications] 滝沢隆俊 他: "コスモノート・ポリンア水域の水温構造とSSM/I画像から見たポリンアの特徴" 南極資料. 41・1. 335-346 (1997)

    • Related Report
      1997 Annual Research Report
  • [Publications] H.Enomoto: "Interannual variability of sea ice conditions in Syowa Station sector deduced from DMSP SSM/I data" Proc. NIPR Symp. Polar Meteorol, Glaciol.10. 119-126 (1996)

    • Related Report
      1996 Annual Research Report
  • [Publications] 榎本浩之: "オホーツク海の海氷成長と大気-海洋相互作用" 月刊海洋. 28・9. 572-575 (1996)

    • Related Report
      1996 Annual Research Report

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Published: 1996-04-01   Modified: 2016-04-21  

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