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dc.contributor.authorSemba, Masumbuko
dc.contributor.authorLumpkin, Rick
dc.contributor.authorKimirei, Ismael
dc.contributor.authorShaghude, Yohanna
dc.contributor.authorNyandwi, Ntahondi
dc.date.accessioned2021-05-24T12:49:58Z
dc.date.available2021-05-24T12:49:58Z
dc.date.issued2019-01-07
dc.identifier.urihttps://doi.org/10.1371/journal.pone.0210303
dc.identifier.urihttps://dspace.nm-aist.ac.tz/handle/20.500.12479/1187
dc.descriptionThis research article published by PLOS ONE, 2019en_US
dc.description.abstractThe surface current speeds within the Pemba channel were examined using 24 years of drifter data received from the Global Drifter Program. This study aimed to uncover varying surface current in the Pemba Channel in different seasons. The results revealed the Pemba Channel experiences relatively higher median surface current speeds during the southeast (SE) monsoon season compared to the northeast (NE) and inter-monsoon (IN) periods. The strongest current speeds were confined in waters deeper than 200 meters between ~39.4°E and 39.7°E. These results prove that surface currents from the drifters can be used to uncover the patterns of surface circulation even in areas where in-situ measurements are scarce.en_US
dc.language.isoenen_US
dc.publisherPLOS ONEen_US
dc.subjectResearch Subject Categories::NATURAL SCIENCESen_US
dc.titleSeasonal and spatial variation of surface current in the Pemba Channel, Tanzaniaen_US
dc.typeArticleen_US


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