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Coastal upwelling and seasonal variation in phytoplankton biomass in the Pemba Channel

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dc.creator Kyewalyanga, Margareth S.
dc.creator Peter, Nyamisi
dc.creator Semba, Masumbuko
dc.creator Mahongo, Shigalla B.
dc.date 2021-05-24T10:45:41Z
dc.date 2021-05-24T10:45:41Z
dc.date 2021-02-11
dc.date.accessioned 2022-10-25T09:24:49Z
dc.date.available 2022-10-25T09:24:49Z
dc.identifier https://doi.org/10.4314/wiojms.si2020.1.3
dc.identifier http://dspace.nm-aist.ac.tz/handle/20.500.12479/1186
dc.identifier.uri http://hdl.handle.net/123456789/95804
dc.description This research article published by African Journals Online, 2021
dc.description This study was conducted in the Pemba Channel off Tanga Region in northern Tanzania to investigate physical and chemical factors that drive changes in phytoplankton biomass. Three transects off Mwaboza, Vyeru and Sahare were selected. For each transect, ten stations were sampled. Phytoplankton biomass was determined as chlorophyll-a (Chl-a) concentration. Similarly, physico-chemical variables (temperature, salinity, dissolved oxygen, pH and nutrients) were determined. It was observed that the Chl-a concentration was significantly higher during the northeast monsoon (median 1.44 mg m-3) as compared to the southeast monsoon (median 1.19 mg m-3; W = 2216, p = 0.029). The higher productivity during the northeast monsoon is attributed to the presence of high-nutrient water caused by coastal upwelling. It is concluded that indication of upwelling, observed through relatively low temperatures during the northeast monsoon season, could be responsible for bringing nutrient-rich waters to the surface, which in turn stimulated the increase in Chl-a concentration.
dc.format application/pdf
dc.language en
dc.publisher African Journals Online
dc.subject Chlorophyll-a
dc.subject Monsoon seasons
dc.subject Pemba Channel
dc.title Coastal upwelling and seasonal variation in phytoplankton biomass in the Pemba Channel
dc.type Article


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