Improvement in the dissolved oxygen concentration and water exchange in Ofunato Bay, Japan, after the collapse of the bay‐mouth breakwater by the 2011 Tohoku Earthquake and tsunami. (28th November 2016)

• Record Type: Journal Article
• Authors: Kakehi, Shigeho; Kamiyama, Takashi; Kaga, Yoshimasa; Naiki, Kimiaki; Kaga, Shinnosuke
• Other Names: Kishi Michio J. guestEditor.; Oozeki Yoshioki guestEditor.; Nakata Kaoru guestEditor.
• Is Part Of: Fisheries oceanography. Volume 26:Number 2(2017)
• Page Start: 114
• Page End: 127
• Publication Date: 2016-11-28
• Subjects: 2011 Tohoku Earthquake -- bay‐mouth breakwater -- box model -- dissolved oxygen concentration -- Ofunato Bay -- water exchange; Fishery oceanography -- Periodicals; 639.2
• DOI: 10.1111/fog.12184
• Languages: English
• ISSNs: 1054-6006

Abstract

Abstract: Oyster and scallop aquaculture has flourished in Ofunato Bay, on the Sanriku Coast of Japan. Between 1967 and 2011, this bay was a highly enclosed area by a bay‐mouth breakwater, and while the breakwater provided calm conditions suitable for aquaculture, there was concern about water quality deterioration. The Tohoku Earthquake off the Pacific coast and the subsequent major tsunami on 11 March 2011 caused extensive damage to the Sanriku Coast, resulting in the collapse of the breakwater of Ofunato Bay. We analyzed the monthly hydrographic observational data that were collected between 1996 and 2015, supplemented with hydrographic observations and direct current measurements that were carried out after the earthquake. The historical hydrographic observational data showed the lowest dissolved oxygen (DO) concentrations were observed near the bottom in the bay. The average and standard deviation of the lowest DO concentrations of each monthly observation during the period before and after the earthquake were 5.81 ± 3.72 and 7.22 ± 1.49 mg L −1, respectively, and are significantly different. The oceanic water inflow and water exchange rate estimated by a box model based on the salt budget under the steady‐state estuarine circulation were also significantly different before and after the earthquake. An increase in the inflow of oceanic water and the more rapid water exchange in the bay after the earthquake induced marked improvements in the bottom DO concentration. These changes are considered to be attributable to the improved circulation of oceanic water in the bay that resulted from the collapse of the bay‐mouth breakwater.