Influence of monsoonal winds on chlorophyll-α distribution in the Beibu Gulf

The influence of seasonal, monsoonal winds on the temporal and spatial variability of chlorophyll-a (chl-a) in the Beibu Gulf is studied based on long-term satellite data of sea surface winds, chl-a concentration and sea surface temperature (SST) and in-situ observations for the years from 2002 to 2...

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Veröffentlicht in:PloS one 2018-01, Vol.13 (1), p.e0191051-e0191051
Hauptverfasser: Shen, Chunyan, Yan, Yunrong, Zhao, Hui, Pan, Jiayi, T Devlin, Adam
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Yan, Yunrong
Zhao, Hui
Pan, Jiayi
T Devlin, Adam
description The influence of seasonal, monsoonal winds on the temporal and spatial variability of chlorophyll-a (chl-a) in the Beibu Gulf is studied based on long-term satellite data of sea surface winds, chl-a concentration and sea surface temperature (SST) and in-situ observations for the years from 2002 to 2014. The analysis results indicated that under northeasterly monsoonal winds, chl-a concentrations were substantially elevated in most area of the Beibu Gulf, with a high chl-a concentration (>2 mg m-3) patch extending southwestward from the coastal water of the northeastern Gulf, consistent with the winter wind pattern. Meanwhile, the spatial distribution of high chl-a concentration is correlated with low SST in the northeastern Gulf. In the southern Gulf, there was generally low chl-a, except in the coastal waters southwest of Hainan Island. Here, the upwelling cold water prevails outside the mouth of the Beibu Gulf, driven by the southwesterly monsoonal winds and the runoff from the Changhua River, as implied by low observed SST. Correlation analysis indicated the chl-a concentration was strongly modulated by wind speed (r = 0.63, p0.7, p
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The analysis results indicated that under northeasterly monsoonal winds, chl-a concentrations were substantially elevated in most area of the Beibu Gulf, with a high chl-a concentration (&gt;2 mg m-3) patch extending southwestward from the coastal water of the northeastern Gulf, consistent with the winter wind pattern. Meanwhile, the spatial distribution of high chl-a concentration is correlated with low SST in the northeastern Gulf. In the southern Gulf, there was generally low chl-a, except in the coastal waters southwest of Hainan Island. Here, the upwelling cold water prevails outside the mouth of the Beibu Gulf, driven by the southwesterly monsoonal winds and the runoff from the Changhua River, as implied by low observed SST. Correlation analysis indicated the chl-a concentration was strongly modulated by wind speed (r = 0.63, p&lt;0.001), particularly in the middle of the northern Gulf and southern Hainan Island (r&gt;0.7, p&lt;0.001). Integrated analysis also showed that stratification is weak and mixing is strong in winter as affected by the high wind speed, which suggests that the wind-induced mixing is a dominant mechanism for entrainment of nutrients and the spatial distribution of chl-a in winter.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0191051</identifier><identifier>PMID: 29329314</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Chlorophyll ; Coastal waters ; Cold water ; Correlation analysis ; Earth Sciences ; Ecology and Environmental Sciences ; Entrainment ; Fisheries ; Fluid mechanics ; Funding ; Information science ; Monsoons ; Nutrients ; Remote sensing systems ; Rivers ; Runoff ; Salinity ; Satellite data ; Sea surface temperature ; Software ; Spatial distribution ; Spatial variability ; Studies ; Surface temperature ; Surface wind ; Upwelling ; Wind ; Wind effects ; Wind patterns ; Wind speed ; Winter</subject><ispartof>PloS one, 2018-01, Vol.13 (1), p.e0191051-e0191051</ispartof><rights>2018 Shen et al. 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The analysis results indicated that under northeasterly monsoonal winds, chl-a concentrations were substantially elevated in most area of the Beibu Gulf, with a high chl-a concentration (&gt;2 mg m-3) patch extending southwestward from the coastal water of the northeastern Gulf, consistent with the winter wind pattern. Meanwhile, the spatial distribution of high chl-a concentration is correlated with low SST in the northeastern Gulf. In the southern Gulf, there was generally low chl-a, except in the coastal waters southwest of Hainan Island. Here, the upwelling cold water prevails outside the mouth of the Beibu Gulf, driven by the southwesterly monsoonal winds and the runoff from the Changhua River, as implied by low observed SST. Correlation analysis indicated the chl-a concentration was strongly modulated by wind speed (r = 0.63, p&lt;0.001), particularly in the middle of the northern Gulf and southern Hainan Island (r&gt;0.7, p&lt;0.001). Integrated analysis also showed that stratification is weak and mixing is strong in winter as affected by the high wind speed, which suggests that the wind-induced mixing is a dominant mechanism for entrainment of nutrients and the spatial distribution of chl-a in winter.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>29329314</pmid><doi>10.1371/journal.pone.0191051</doi><orcidid>https://orcid.org/0000-0002-7481-4061</orcidid><oa>free_for_read</oa></addata></record>
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subjects Chlorophyll
Coastal waters
Cold water
Correlation analysis
Earth Sciences
Ecology and Environmental Sciences
Entrainment
Fisheries
Fluid mechanics
Funding
Information science
Monsoons
Nutrients
Remote sensing systems
Rivers
Runoff
Salinity
Satellite data
Sea surface temperature
Software
Spatial distribution
Spatial variability
Studies
Surface temperature
Surface wind
Upwelling
Wind
Wind effects
Wind patterns
Wind speed
Winter
title Influence of monsoonal winds on chlorophyll-α distribution in the Beibu Gulf
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