1996
DOI: 10.1080/02626669609491546
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Rainfall and runoff in Yemen

Abstract: This paper makes use of a water balance study of a mountainous area with a wide range of average annual rainfall in an arid and semiarid region to illustrate the development of both a statistical model of daily rainfall and a rainfall-runoff model. The models are appropriate for these conditions and may be relevant to similar areas. Comparisons of mean rainfall and runoff at the arid end of the scale suggest that runoff coefficients do not conform to common assumptions. Précipitation et écoulement au YemenRésu… Show more

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Cited by 31 publications
(9 citation statements)
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“…Rainfall ranges from of 400 to 800 mm in the southern, central, and western highlands and decreases steadily to below 300 mm in northern and eastern highlands. Average temperatures are dominantly controlled by altitude . Climate data for the collection sites in this work are summarized in Table .…”
Section: Resultsmentioning
confidence: 99%
“…Rainfall ranges from of 400 to 800 mm in the southern, central, and western highlands and decreases steadily to below 300 mm in northern and eastern highlands. Average temperatures are dominantly controlled by altitude . Climate data for the collection sites in this work are summarized in Table .…”
Section: Resultsmentioning
confidence: 99%
“…Although these coastal lowlands might also have offered resources for the Pleistocene populations (Bailey, 2009), the significantly more arid climate of the Tihama coastal plain presented conditions less favorable to long-term settlement than those of the interior foothills where the sites are located. Current mean annual rainfall is between 300 and 400 mm and drops to less than 100 mm along the coast (Farquharson et al, 1996). Prevailing arid conditions during the occupation of SD1 are signaled by the presence of fauna (particularly Equus sp.…”
Section: An Inland Occupation During Mis 3 Arid Conditionsmentioning
confidence: 98%
“…The current average annual rainfall increases gradually with altitude, up to 1000 mm, and depends on two systems: the Red Sea Convergence Zone and the monsoonal Intertropical Convergence Zone (ITCZ), which are active in spring, summer, and autumn to a lesser extent (Farquharson et al, 1996). Wadi Surdud, as well as the six other major Wadi systems in the western highlands, drain west into the Red Sea, and have permanently flowing water in their upper reaches, while they retain water throughout the year in deep pools along their middle and lower reaches but their waters do not reach the Red Sea, except during rare periods of heavy rainfall (Scholte, 1992).…”
Section: Wadi Surdud Regional Settingmentioning
confidence: 99%
“…The climate along the Red Sea is hot. The average annual rainfall falls below 100 mm, and precipitation events are limited to sparse and high intensity storm rainfalls (Farquharson et al, 1996), with 80% of the annual rainfall received during the winter months. The coastal landscape is composed of high energy sandy or gravelly beaches backed by sand dunes and low cliffs.…”
Section: Wadi Surdud Regional Settingmentioning
confidence: 99%