{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1361137044036739456.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2011jc007626"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011JC007626"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011JC007626"}}],"dc:title":[{"@value":"Typhoon‐induced phytoplankton blooms and primary productivity increase in the western North Pacific subtropical ocean"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Using multiple satellite observations and series of numerical experiments, this work systematically studied phytoplankton blooms induced by tropical cyclones in the western North Pacific subtropical ocean (WNPSO) because WNPSO is among the world oceans where most number of intense tropical cyclones are found. All eleven typhoon cases passing the study domain in 2003 were examined in detail. It was observed that only two typhoons (18%) were able to induce phytoplankton blooms (chlorophyll‐a concentration increased from ≦0.1 mg m<jats:sup>−3</jats:sup> to 0.4–0.8 mg m<jats:sup>−3</jats:sup>) and strong sea surface temperature cooling of −2.5 to −6°C. The other nine typhoons, including the most intense tropical cyclone on Earth in 2003 (i.e., supertyphoon Maemi), were not able to induce phytoplankton blooms and the associated sea surface temperature cooling was weak (0 to −1.5°C). Using series of numerical experiments, it was found that the presence of warm ocean eddy can effectively isolate the cold, nutrient‐rich water to be entrained to the surface ocean. Under this situation, even category 5 typhoon Maemi at its peak intensity of 150 kts could not induce phytoplankton bloom in the WNPSO. The weak responses of the other eight typhoons were due to insufficient wind intensity and transit time (caused by relatively small storm size and fast translation speed) in this deep nutricline/mixed layer ocean. As a result, the total annual primary production increase induced by typhoons in the WNPSO was estimated to be ∼3.27 × 10<jats:sup>12</jats:sup> g C (0.00327 Pg), equivalent to 0.15% of the global annual anthropogenic CO<jats:sub>2</jats:sub> uptake. This suggests that though WNPSO has the highest number and intensity of tropical cyclones among the world oceans, tropical cyclones in the WNPSO have little contribution to enhance biological carbon fixation in the context of global carbon‐climate system.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380579819144530560","@type":"Researcher","foaf:name":[{"@value":"I.‐I. Lin"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2012-03","prism:volume":"117","prism:number":"C3","prism:startingPage":"3039"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2011JC007626"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2011JC007626"}],"createdAt":"2011-12-20","modifiedAt":"2023-10-30","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338209104384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Impact of cyclonic eddies and typhoons on biogeochemistry in the oligotrophic ocean based on biogeochemical/physical/meteorological time-series at station KEO"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231207005440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Changes in phytoplankton community structure during wind-induced fall bloom on the central Chukchi shelf"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285715167307008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variations in triple isotope composition of dissolved oxygen and primary production in a subtropical reservoir"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617572464768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Late Summer Peak and Scavenging-Dominant Metal Fluxes in Particulate Export Near a Seamount in the Western North Pacific Subtropical Gyre"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655105538432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical simulations of oceanic <i>p</i>CO<sub>2</sub> variations and interactions between Typhoon Choi‐wan (0914) and the ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694364643849600","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Time‐series observations of photosynthetic oxygen production in the subtropical western North Pacific by an underwater profiling buoy system"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713014213760","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"西部北太平洋亜熱帯海域における台風の影響を受けた可能性のある植物プランクトン群集組成と沈降粒子"},{"@language":"en","@value":"The effect of typhoons on phytoplankton communities and settling particle flux in the western North Pacific subtropical region"},{"@language":"ja-Kana","@value":"セイブ キタタイヘイヨウ アネッタイ カイイキ ニ オケル タイフウ ノ エイキョウ オ ウケタ カノウセイ ノ アル ショクブツ プランクトン グンシュウ ソセイ ト チンコウ リュウシ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2011jc007626"},{"@type":"CROSSREF","@value":"10.1007/s00300-018-2284-7_references_DOI_YhMQT9hEa1bMF1tfWSLFJax1P3t"},{"@type":"CROSSREF","@value":"10.3389/feart.2020.558823_references_DOI_PXglG7bBYTJvdwFMlq8g2467CGr"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.25.2_17_references_DOI_PXglG7bBYTJvdwFMlq8g2467CGr"},{"@type":"CROSSREF","@value":"10.5194/bg-13-6683-2016_references_DOI_PXglG7bBYTJvdwFMlq8g2467CGr"},{"@type":"CROSSREF","@value":"10.1002/jgrc.20203_references_DOI_PXglG7bBYTJvdwFMlq8g2467CGr"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0196-3_references_DOI_PXglG7bBYTJvdwFMlq8g2467CGr"},{"@type":"CROSSREF","@value":"10.1002/lno.11372_references_DOI_PXglG7bBYTJvdwFMlq8g2467CGr"}]}