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

dc.contributor.authorKyewalyanga, Margareth S.
dc.contributor.authorPeter, Nyamisi
dc.contributor.authorSemba, Masumbuko
dc.contributor.authorMahongo, Shigalla B.
dc.date.accessioned2021-05-24T10:45:41Z
dc.date.available2021-05-24T10:45:41Z
dc.date.issued2021-02-11
dc.descriptionSDG 14: Life Below Water, SDG 13: Climate Action, SDG 6: Clean Water and Sanitation.en_US
dc.description.abstractThis 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.en_US
dc.identifier.urihttps://doi.org/10.4314/wiojms.si2020.1.3
dc.identifier.urihttp://dspace.nm-aist.ac.tz/handle/20.500.12479/1186
dc.language.isoenen_US
dc.publisherAfrican Journals Onlineen_US
dc.subjectChlorophyll-aen_US
dc.subjectMonsoon seasonsen_US
dc.subjectPemba Channelen_US
dc.titleCoastal upwelling and seasonal variation in phytoplankton biomass in the Pemba Channelen_US
dc.typeArticleen_US

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