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dc.contributor.authorSultan, S A R-
dc.contributor.authorAhmad, F-
dc.date.accessioned2014-01-13T05:36:09Z-
dc.date.available2014-01-13T05:36:09Z-
dc.date.issued2000-09-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/25521-
dc.description201-205en_US
dc.description.abstractAnalysis of monthly means of sea level averaged over a period of three years (1991-1993) at Jeddah reveals the presence of a semi-annual component in addition to the annual one. The variance explained by the two components are 20 % and 78% respectively. Their respective amplitudes are 8.7 and 17.3 cm. The two cycles are induced by the combined effect of wind stress and evaporation rate. The cross-shore stress is the most contributing factor to the annual variation of the sea level. In contrast the long-shore stress is the dominant factor in inducing the semi-annual cycle. The evaporation contributes more to the semi-annual component of the sea level than to the annual one.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.29(3) [September 2000]en_US
dc.titleAnnual and semi-annual variations of sea level at Jeddah, central coastal station of the Red Seaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.29(3) [September 2000]

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