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Title page for ETD etd-08182004-092537


Type of Document Thesis
Author Balas, Natasa
URN etd-08182004-092537
Title Climatic Variability in Central Africa and its Link to SSTs and El Nino/La Nina
Degree Master of Science
Department Meteorology, Department of
Advisory Committee
Advisor Name Title
Sharon Nicholson Committee Chair
James J. O'Brien Committee Member
T. N. Krishnamurti Committee Member
Keywords
  • La Nina
  • Climatic Variability
  • El Nino
Date of Defense 2003-12-01
Availability unrestricted
Abstract
A diagnostic study of rainfall variability in Africa in the area from 5oS to 10oN and from

10oE to 30oE was carried out using a gauge rainfall data. Emphasis was placed on

determining the time-scales of interannual variability, the characteristics of interseasonal

fluctuations, and on regionalization of the data. The latter was used in order to reduce the

number of regions utilized for studying this variability in the context of sea-surface

temperature fluctuations, El Nino/La Nina, and atmospheric circulation variables. Five

homogeneous regions were found in this manner. Generally, the most relevant aspects of

SST variability for interannual variability of rainfall appear to be: ENSO, Atlantic and

Indian Oceans SSTs, Atlantic upwelling and Atlantic dipole. The importance of these

varies seasonally and, to a lesser extent, regionally. There is no “symmetry” between the

factors associated with wet conditions and those producing dry conditions. Rainfall

response to SSTs is clearly seasonally specific. This is manifestation of the complexity of

the factors influencing rainfall over Central Africa and of the pronounced seasonality of

rainfall over this region. Overall, regions 1, 2 and 3 show strong teleconnection to factors

that control variability. For regions 4 and 5 such teleconnections were not found which

suggests the possibility that these two regions are not as homogeneous as it appeared

initially. One of the reasons for this could be that these two regions represent a transition

zone between influences of the Atlantic Ocean to the west and Indian Ocean to the east.

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