Climate characteristics over southern highlands Tanzania

dc.creatorMbululo, Yassin
dc.creatorNyihirani, Fatuma
dc.date2021-04-30T09:09:00Z
dc.date2021-04-30T09:09:00Z
dc.date2012
dc.date.accessioned2022-10-25T08:53:52Z
dc.date.available2022-10-25T08:53:52Z
dc.descriptionJournal article
dc.descriptionThis study was conducted to examine the climate characteristic of southern highland Tanzania (Latitude 6°S - 12°S and Longitude 29°E - 38°E). The study findings reveal that rainfall over the region is linked with SST over the Indian Ocean, where warmer (cooler) western Indian Ocean is accompanied by high (low) amount of rainfall over Tanzania. During wet (dry) years, weaker (stronger) equatorial westerlies and anticyclone (cyclonic) anomaly over the southern tropics act to reduce (enhance) the export of equatorial moisture away from East Africa. The wettest (driest) season was found to be 1978/79 (1999/00) which can be classified as the severely wet (moderate drought). Two different modes of rainfall have been identified at time scale of 1.5 and 6 years which have been associated with the quasi biennial oscillation (QBO) and El Nino Southern Oscillation (ENSO), respectively.
dc.formatapplication/pdf
dc.identifierhttps://www.suaire.sua.ac.tz/handle/123456789/3504
dc.identifier.urihttp://hdl.handle.net/123456789/94252
dc.languageen
dc.publisherScientific Research
dc.subjectTanzania
dc.subjectClimate Characteristics
dc.subjectDominant Periodicity Mode
dc.titleClimate characteristics over southern highlands Tanzania
dc.typeArticle

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