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Co-Occurrence of Marine Extremes Induced by Tropical Storms and an Ocean Eddy in Summer 2016: Anomalous Hydrographic Conditions in the Pacific Shelf Waters off Southeast Hokkaido, Japan
This study proposes an analysis methodology to address how very rare marine extremes can be understood using limited data. In summer 2016, extreme weather and marine events occurred simultaneously around the Pacific shelf off southeastern Hokkaido, Japan. Six successive tropical storms brought extre...
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Published in: | Atmosphere 2021-07, Vol.12 (7), p.888 |
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description | This study proposes an analysis methodology to address how very rare marine extremes can be understood using limited data. In summer 2016, extreme weather and marine events occurred simultaneously around the Pacific shelf off southeastern Hokkaido, Japan. Six successive tropical storms brought extreme precipitation and an anticyclonic mesoscale eddy of subtropical Kuroshio water closely approached the coast, locally causing marine heat waves. We examined how these compound extremes affected oceanographic conditions on the coastal shelf by analyzing data from ship surveys in October 2016 on the Pacific shelf and outputs from a realistic ocean model. Climatologically, warm, high-salinity (33.0–33.7) subtropical water from the Okhotsk Sea (modified Soya Warm Current water) is distributed near the sea surface on the Pacific shelf in October and transported by the along-shelf boundary current. In 2016, however, a vertically well-mixed low-salinity ( |
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In summer 2016, extreme weather and marine events occurred simultaneously around the Pacific shelf off southeastern Hokkaido, Japan. Six successive tropical storms brought extreme precipitation and an anticyclonic mesoscale eddy of subtropical Kuroshio water closely approached the coast, locally causing marine heat waves. We examined how these compound extremes affected oceanographic conditions on the coastal shelf by analyzing data from ship surveys in October 2016 on the Pacific shelf and outputs from a realistic ocean model. Climatologically, warm, high-salinity (33.0–33.7) subtropical water from the Okhotsk Sea (modified Soya Warm Current water) is distributed near the sea surface on the Pacific shelf in October and transported by the along-shelf boundary current. In 2016, however, a vertically well-mixed low-salinity (<33.0) layer associated with the heavy rainfall was observed at 0–50 m depth on the shelf, salinity maxima (≥33.7) associated with Kuroshio water from the mesoscale eddy occurred at 50–150 m depth on the slope, and baroclinic jets formed along the salinity front near the shelfbreak. These observed salinity structures were reproduced by a 1/50° ocean model. Particle-tracking experiments revealed that the low-salinity water originated mainly off eastern Hokkaido, where heavy rainfall events occurred in August, and was modified by mixing with Soya Warm Current water before transport to the Pacific shelf.</description><identifier>ISSN: 2073-4433</identifier><identifier>EISSN: 2073-4433</identifier><identifier>DOI: 10.3390/atmos12070888</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>anticyclonic mesoscale eddy ; boundary current ; Boundary currents ; Climate change ; Climate models ; coastal shelf water ; Coasts ; compound extreme event ; Extreme weather ; Heat waves ; Heatwaves ; Heavy rainfall ; Mesoscale phenomena ; Ocean circulation ; Ocean models ; ocean monitoring ; Oceanographic conditions ; Oceans ; Precipitation ; Rain ; Rainfall ; Salinity ; Salinity effects ; Sea surface ; Storms ; Summer ; Surveys ; Tracking ; Tropical climate ; Tropical depressions ; tropical storm ; Tropical storms ; Velocity ; Vortices ; Water ; Water depth</subject><ispartof>Atmosphere, 2021-07, Vol.12 (7), p.888</ispartof><rights>2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). 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In summer 2016, extreme weather and marine events occurred simultaneously around the Pacific shelf off southeastern Hokkaido, Japan. Six successive tropical storms brought extreme precipitation and an anticyclonic mesoscale eddy of subtropical Kuroshio water closely approached the coast, locally causing marine heat waves. We examined how these compound extremes affected oceanographic conditions on the coastal shelf by analyzing data from ship surveys in October 2016 on the Pacific shelf and outputs from a realistic ocean model. Climatologically, warm, high-salinity (33.0–33.7) subtropical water from the Okhotsk Sea (modified Soya Warm Current water) is distributed near the sea surface on the Pacific shelf in October and transported by the along-shelf boundary current. In 2016, however, a vertically well-mixed low-salinity (<33.0) layer associated with the heavy rainfall was observed at 0–50 m depth on the shelf, salinity maxima (≥33.7) associated with Kuroshio water from the mesoscale eddy occurred at 50–150 m depth on the slope, and baroclinic jets formed along the salinity front near the shelfbreak. These observed salinity structures were reproduced by a 1/50° ocean model. Particle-tracking experiments revealed that the low-salinity water originated mainly off eastern Hokkaido, where heavy rainfall events occurred in August, and was modified by mixing with Soya Warm Current water before transport to the Pacific shelf.</description><subject>anticyclonic mesoscale eddy</subject><subject>boundary current</subject><subject>Boundary currents</subject><subject>Climate change</subject><subject>Climate models</subject><subject>coastal shelf water</subject><subject>Coasts</subject><subject>compound extreme event</subject><subject>Extreme weather</subject><subject>Heat waves</subject><subject>Heatwaves</subject><subject>Heavy rainfall</subject><subject>Mesoscale phenomena</subject><subject>Ocean circulation</subject><subject>Ocean models</subject><subject>ocean monitoring</subject><subject>Oceanographic conditions</subject><subject>Oceans</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Salinity</subject><subject>Salinity effects</subject><subject>Sea surface</subject><subject>Storms</subject><subject>Summer</subject><subject>Surveys</subject><subject>Tracking</subject><subject>Tropical climate</subject><subject>Tropical depressions</subject><subject>tropical storm</subject><subject>Tropical storms</subject><subject>Velocity</subject><subject>Vortices</subject><subject>Water</subject><subject>Water depth</subject><issn>2073-4433</issn><issn>2073-4433</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNpVUd2LEzEQX0TB47xH3wd8dTXZJN1d345SbeWkQgs-hmk-runtJmuSBfun-d-ZWhEdmM_fzG8GpqpeU_KOsZ68xzyGRBvSkq7rnlU3JWI154w9_yd-Wd2ldCJFeM8axm-qn8tQb5WaYzReGQgWvmB03sDqR45mNAk2Xs_KaDicYR_D5BQOsMshjgnQ66KwVabYldZncB528ziaCA2hiw9w78OIQ5gTrM86hseI09EpWAavXXbBp8tEPhr4isrZguyOZrDwDbOJqVxjYRfmgmPKsA5PT-h0eAufcUL_qnphcUjm7o-_rfYfV_vlun7Yftos7x9qxTuSa8WMPSglGO8WmihOWtH3i0PLNbUl5YzwgjUdE61q0CotuBZGLESry5xlt9XmSqsDnuQU3YjxLAM6-bsQ4qPEmJ0ajKQ9ik4razkRXJWFlDKiu5Ziy1vNeOF6c-WaYvg-m5TlKczRl-tlIwTntGXNpau-dqkYUorG_t1Kibz8Wv73a_YLUtOdRA</recordid><startdate>20210708</startdate><enddate>20210708</enddate><creator>Kuroda, Hiroshi</creator><creator>Taniuchi, Yukiko</creator><creator>Kasai, Hiromi</creator><creator>Nakanowatari, Takuya</creator><creator>Setou, Takashi</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>SOI</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0002-9659-2551</orcidid></search><sort><creationdate>20210708</creationdate><title>Co-Occurrence of Marine Extremes Induced by Tropical Storms and an Ocean Eddy in Summer 2016: Anomalous Hydrographic Conditions in the Pacific Shelf Waters off Southeast Hokkaido, Japan</title><author>Kuroda, Hiroshi ; 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In summer 2016, extreme weather and marine events occurred simultaneously around the Pacific shelf off southeastern Hokkaido, Japan. Six successive tropical storms brought extreme precipitation and an anticyclonic mesoscale eddy of subtropical Kuroshio water closely approached the coast, locally causing marine heat waves. We examined how these compound extremes affected oceanographic conditions on the coastal shelf by analyzing data from ship surveys in October 2016 on the Pacific shelf and outputs from a realistic ocean model. Climatologically, warm, high-salinity (33.0–33.7) subtropical water from the Okhotsk Sea (modified Soya Warm Current water) is distributed near the sea surface on the Pacific shelf in October and transported by the along-shelf boundary current. In 2016, however, a vertically well-mixed low-salinity (<33.0) layer associated with the heavy rainfall was observed at 0–50 m depth on the shelf, salinity maxima (≥33.7) associated with Kuroshio water from the mesoscale eddy occurred at 50–150 m depth on the slope, and baroclinic jets formed along the salinity front near the shelfbreak. These observed salinity structures were reproduced by a 1/50° ocean model. Particle-tracking experiments revealed that the low-salinity water originated mainly off eastern Hokkaido, where heavy rainfall events occurred in August, and was modified by mixing with Soya Warm Current water before transport to the Pacific shelf.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/atmos12070888</doi><orcidid>https://orcid.org/0000-0002-9659-2551</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | anticyclonic mesoscale eddy boundary current Boundary currents Climate change Climate models coastal shelf water Coasts compound extreme event Extreme weather Heat waves Heatwaves Heavy rainfall Mesoscale phenomena Ocean circulation Ocean models ocean monitoring Oceanographic conditions Oceans Precipitation Rain Rainfall Salinity Salinity effects Sea surface Storms Summer Surveys Tracking Tropical climate Tropical depressions tropical storm Tropical storms Velocity Vortices Water Water depth |
title | Co-Occurrence of Marine Extremes Induced by Tropical Storms and an Ocean Eddy in Summer 2016: Anomalous Hydrographic Conditions in the Pacific Shelf Waters off Southeast Hokkaido, Japan |
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