FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2148006733> ?p ?o ?g. }

• W2148006733 endingPage "41" @default.
• W2148006733 startingPage "31" @default.
• W2148006733 abstract "MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 268:31-41 (2004) - doi:10.3354/meps268031 Offshore phytoplankton biomass increase and its oceanographic causes in the South China Sea DanLing Tang1,2,3,*, Hiroshi Kawamura3, Tran Van Dien4, MingAn Lee5 1LED, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 164 West Xingang Road, Guangzhou 510301, China 2Department of Environmental Science and Engeneering, Fudan University, Shanghai 200433, China 3Center for Atmospheric and Oceanic Studies, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan 4Haiphong Institute of Oceanography, 246 Da Nang Street, Haiphong City 84-31, Vietnam 5Department of Environmental Biology and Fisheries Science, National Taiwan Ocean University, 2 Pei-Ning Road, Keelung 20224, Taiwan *Email: lingzistdl@yahoo.com ABSTRACT: High phytoplankton biomass often occurs in plumes near river mouths or in eutrophic coastal waters for short time periods. However, we observed an increased phytoplankton biomass in a narrow jet-shaped protrusion into the western South China Sea (SCS) using satellite chlorophyll a (chl a) data from the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) and concurrent ship measurements in 1999. In June, regional phytoplankton biomass appeared as a large jet shape extending from the coastal waters of Vietnam eastward towards the SCS, about 200 km northeast of the mouth of the Mekong River; this feature intensified in the form of a large jet or gyre from July to September, decayed in October, and disappeared entirely in November. The gyre was about 400 km in diameter with chl a concentrations from 0.5 to 2 mg m-3. Data on sea surface temperature (SST), winds, and sea surface height anomalies indicated a strong offshore upwelling during a period of strong southwesterly winds alongshore. The upwelling coincided with the regional increase in phytoplankton biomass in terms of shape, timing, and location. We observed this phenomenon during every southwesterly monsoon season from 1997 to 2002 using chl a images from 3 satellite ocean color sensors‹SeaWiFS, Ocean Color and Temperature Scanner (OCTS), and Ocean Color Imager (OCI)‹and it appeared to be related to the cross-shelf upwelling that delivers nutrients to surface waters. The phytoplankton then flowed with a large anticyclonic gyre into the western SCS. KEY WORDS: Phytoplankton · Chl a concentration · Upwelling · Monsoon · Satellite observation · SeaWiFS · South China Sea Full text in pdf format PreviousNextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 268. Online publication date: March 09, 2004 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2004 Inter-Research." @default.
• W2148006733 created "2016-06-24" @default.
• W2148006733 creator A5010597964 @default.
• W2148006733 creator A5029440132 @default.
• W2148006733 creator A5056119445 @default.
• W2148006733 creator A5057858186 @default.
• W2148006733 date "2004-01-01" @default.
• W2148006733 modified "2023-10-07" @default.
• W2148006733 title "Offshore phytoplankton biomass increase and its oceanographic causes in the South China Sea" @default.
• W2148006733 cites W1490160883 @default.
• W2148006733 cites W1996223163 @default.
• W2148006733 cites W1997468347 @default.
• W2148006733 cites W1998885244 @default.
• W2148006733 cites W2001982030 @default.
• W2148006733 cites W2004215498 @default.
• W2148006733 cites W2006042346 @default.
• W2148006733 cites W2007101051 @default.
• W2148006733 cites W2057025105 @default.
• W2148006733 cites W2088229454 @default.
• W2148006733 cites W2089211067 @default.
• W2148006733 cites W2100717594 @default.
• W2148006733 cites W2105695459 @default.
• W2148006733 cites W2110801194 @default.
• W2148006733 cites W2124839591 @default.
• W2148006733 cites W2145370293 @default.
• W2148006733 cites W2171084253 @default.
• W2148006733 cites W2550232752 @default.
• W2148006733 doi "https://doi.org/10.3354/meps268031" @default.
• W2148006733 hasPublicationYear "2004" @default.
• W2148006733 type Work @default.
• W2148006733 sameAs 2148006733 @default.
• W2148006733 citedByCount "139" @default.
• W2148006733 countsByYear W21480067332012 @default.
• W2148006733 countsByYear W21480067332013 @default.
• W2148006733 countsByYear W21480067332014 @default.
• W2148006733 countsByYear W21480067332015 @default.
• W2148006733 countsByYear W21480067332016 @default.
• W2148006733 countsByYear W21480067332017 @default.
• W2148006733 countsByYear W21480067332018 @default.
• W2148006733 countsByYear W21480067332019 @default.
• W2148006733 countsByYear W21480067332020 @default.
• W2148006733 countsByYear W21480067332021 @default.
• W2148006733 countsByYear W21480067332022 @default.
• W2148006733 countsByYear W21480067332023 @default.
• W2148006733 crossrefType "journal-article" @default.
• W2148006733 hasAuthorship W2148006733A5010597964 @default.
• W2148006733 hasAuthorship W2148006733A5029440132 @default.
• W2148006733 hasAuthorship W2148006733A5056119445 @default.
• W2148006733 hasAuthorship W2148006733A5057858186 @default.
• W2148006733 hasBestOaLocation W21480067331 @default.
• W2148006733 hasConcept C111368507 @default.
• W2148006733 hasConcept C115540264 @default.
• W2148006733 hasConcept C117082904 @default.
• W2148006733 hasConcept C117467278 @default.
• W2148006733 hasConcept C127313418 @default.
• W2148006733 hasConcept C135895429 @default.
• W2148006733 hasConcept C14168384 @default.
• W2148006733 hasConcept C142796444 @default.
• W2148006733 hasConcept C162284963 @default.
• W2148006733 hasConcept C166957645 @default.
• W2148006733 hasConcept C18903297 @default.
• W2148006733 hasConcept C191935318 @default.
• W2148006733 hasConcept C202041845 @default.
• W2148006733 hasConcept C205649164 @default.
• W2148006733 hasConcept C2780892065 @default.
• W2148006733 hasConcept C30380174 @default.
• W2148006733 hasConcept C39432304 @default.
• W2148006733 hasConcept C505870484 @default.
• W2148006733 hasConcept C514101110 @default.
• W2148006733 hasConcept C86803240 @default.
• W2148006733 hasConceptScore W2148006733C111368507 @default.
• W2148006733 hasConceptScore W2148006733C115540264 @default.
• W2148006733 hasConceptScore W2148006733C117082904 @default.
• W2148006733 hasConceptScore W2148006733C117467278 @default.
• W2148006733 hasConceptScore W2148006733C127313418 @default.
• W2148006733 hasConceptScore W2148006733C135895429 @default.
• W2148006733 hasConceptScore W2148006733C14168384 @default.
• W2148006733 hasConceptScore W2148006733C142796444 @default.
• W2148006733 hasConceptScore W2148006733C162284963 @default.
• W2148006733 hasConceptScore W2148006733C166957645 @default.
• W2148006733 hasConceptScore W2148006733C18903297 @default.
• W2148006733 hasConceptScore W2148006733C191935318 @default.
• W2148006733 hasConceptScore W2148006733C202041845 @default.
• W2148006733 hasConceptScore W2148006733C205649164 @default.
• W2148006733 hasConceptScore W2148006733C2780892065 @default.
• W2148006733 hasConceptScore W2148006733C30380174 @default.
• W2148006733 hasConceptScore W2148006733C39432304 @default.
• W2148006733 hasConceptScore W2148006733C505870484 @default.
• W2148006733 hasConceptScore W2148006733C514101110 @default.
• W2148006733 hasConceptScore W2148006733C86803240 @default.
• W2148006733 hasLocation W21480067331 @default.
• W2148006733 hasOpenAccess W2148006733 @default.
• W2148006733 hasPrimaryLocation W21480067331 @default.
• W2148006733 hasRelatedWork W1972126846 @default.
• W2148006733 hasRelatedWork W1975327107 @default.
• W2148006733 hasRelatedWork W2093912591 @default.
• W2148006733 hasRelatedWork W2097544817 @default.
• W2148006733 hasRelatedWork W2116065726 @default.

• next