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  1. National Taiwan Ocean University Research Hub
  2. 海洋科學與資源學院
  3. 海洋環境與生態研究所
Please use this identifier to cite or link to this item: http://scholars.ntou.edu.tw/handle/123456789/19114
DC FieldValueLanguage
dc.contributor.authorShih, Yung-Yenen_US
dc.contributor.authorShiah, Fuh-Kwoen_US
dc.contributor.authorLai, Chao-Chenen_US
dc.contributor.authorChou, Wen-Chenen_US
dc.contributor.authorTai, Jen-Huaen_US
dc.contributor.authorWu, Yu-Shunen_US
dc.contributor.authorLai, Cheng-Yangen_US
dc.contributor.authorKo, Chia-Yingen_US
dc.contributor.authorHung, Chin-Changen_US
dc.date.accessioned2021-12-10T00:28:16Z-
dc.date.available2021-12-10T00:28:16Z-
dc.date.issued2021-10-4-
dc.identifier.issn2296-7745-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/19114-
dc.description.abstractSatellite-based observations of primary production (PP) are broadly used to assess carbon fixation rate of phytoplankton in the global ocean with small spatiotemporal limitations. However, the remote sensing can only reach the ocean surface, the assumption of a PP vertically exponential decrease with increasing depth from the surface to the bottom of euphotic zone may cause a substantial and potential discrepancy between in situ measurements and satellite-based observations of PP. This study compared euphotic zone integrated PP derived from measurements based on ship-based in situ incubation (i.e., PPin situ) and those derived from the satellite-based vertically generalized production model (VGPM; PPVGPM) for the period 2003 similar to 2016 at the South East Asian Time-series Study (SEATS) station. PP values obtained during the NE-monsoon (NEM: Nov similar to Mar; PPin situ = 323 +/- 134; PPVGPM = 443 +/- 142 mg-C m(-2) d(-1)) were similar to 2-fold higher than those recorded during the SW-monsoon (SWM: Apr similar to Oct; PPin situ = 159 +/- 58; PPVGPM = 250 +/- 36 mg-C m(-2) d(-1)), regardless of the method used for derivation. The main reason for the higher PP values during the NEM appears to have been a greater abundance of inorganic nutrients were made available by vertical advection. Note that on average, PPin situ estimates were similar to 50% lower than PPVGPM estimates, regardless of the monsoon. These discrepancies can be mainly attributed to differences from the euphotic zone depth between satellite-based and in situ measurements. The significantly negative relationship between PP measurements obtained in situ and sea surface temperatures observed throughout this study demonstrates that both methods are effective indicators in estimating PP. Overall, our PPin situ analysis indicates that a warming climate is unfavorable for primary production in low-latitude open ocean ecosystems.en_US
dc.language.isoen_USen_US
dc.publisherFRONTIERS MEDIA SAen_US
dc.relation.ispartofFRONT MAR SCIen_US
dc.subjectPARTICULATE ORGANIC-CARBONen_US
dc.subjectPRIMARY PRODUCTION-MODELen_US
dc.subjectEXPORT PRODUCTIONen_US
dc.subjectOCEAN COLORen_US
dc.subjectPHYTOPLANKTON BLOOMSen_US
dc.subjectBACTERIAL-PRODUCTIONen_US
dc.subjectFIELD OBSERVATIONSen_US
dc.subjectSEASONAL DYNAMICSen_US
dc.subjectCONTINENTAL-SHELFen_US
dc.subjectMIXED-LAYERen_US
dc.titleComparison of Primary Production Using in situ and Satellite-Derived Values at the SEATS Station in the South China Seaen_US
dc.typejournal articleen_US
dc.identifier.doi10.3389/fmars.2021.747763-
dc.identifier.isiWOS:000717038300001-
dc.relation.journalvolume8en_US
item.fulltextno fulltext-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.grantfulltextnone-
item.openairetypejournal article-
item.cerifentitytypePublications-
item.languageiso639-1en_US-
crisitem.author.deptCollege of Ocean Science and Resource-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.deptInstitute of Marine Environment and Ecology-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Ocean Science and Resource-
Appears in Collections:海洋環境與生態研究所
13 CLIMATE ACTION
15 LIFE ON LAND
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