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- INABA Hideo
- 東海大学海洋学部
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- KATSUMATA Takaaki
- 東海大学海洋学部
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- YASUDA Kuniaki
- 東海大学海洋学部
Bibliographic Information
- Other Title
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- 駿河湾300m層の流動と水温の変動
- スルガワン 300mソウ ノ リュウドウ ト スイオン ノ ヘンドウ
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Abstract
In order to investigate the temporal variations of the current and temperature at 300 m in Suruga Bay, the current and temperature data obtained from a moored ADCP observation in the sea at the eastern part of the bay mouth were analyzed. Observed maximum current speed of the inflow and outflow were 57 cm/sec and 40 cm/sec, respectively. The mean current throughout the whole observing period was less than 1 cm/sec. The maximum and minimum observed temperature were 12.7°C and 7.0°C, respectively. The range of the temperature variation was as large as 5.7°C. Comparing with those values to those off Cape Muroto-misaki, those at Suruga Bay were 2.9°C higher for maximum, 1.1°C lower for minimum and 4°C larger for the range. Therefore, the deep sea water at 300 m in the bay can not be low temperature and constant.
Journal
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- DEEP OCEAN WATER RESEARCH
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DEEP OCEAN WATER RESEARCH 2 (1), 1-8, 2001
DEEP OCEAN WATER APPLICATION SOCIETY
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Keywords
Details 詳細情報について
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- CRID
- 1390001205275929600
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- NII Article ID
- 130005450616
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- NII Book ID
- AA11858274
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- ISSN
- 1884958X
- 13458477
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- NDL BIB ID
- 5877847
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- Data Source
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- JaLC
- NDL
- CiNii Articles
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- Abstract License Flag
- Disallowed