## Abstract The process of aquifer recharge by flood events in an arid region was investigated as applied to the Hazeva Formation (the Karkom graben, the Wadi Paran watershed, Israel). The hydrological model was established as a complex system, with due regard for groundwater and transmission losse
A unique flood event in an arid zone
โ Scribed by Michael O. Walter
- Book ID
- 102264561
- Publisher
- John Wiley and Sons
- Year
- 1989
- Tongue
- English
- Weight
- 421 KB
- Volume
- 3
- Category
- Article
- ISSN
- 0885-6087
No coin nor oath required. For personal study only.
โฆ Synopsis
And regions generally lack surface water records for developing flood characteristics for hydraulic design purposes. Consequently good records of floods, particularly large ones, are a data asset to arid zone hydrology.
A large rainfall and runoff event which occurred on 23 April 1985 has been fully recorded on Wadi Ghat, a 597 km2 catchment in southwest Saudi Arabia.
Maximum point rainfall intensity was 115.4 mm hr-'. The peak discharge was 3200 m3 s-l. Point rainfall has an expected frequency of occurrence in excess of once every 200 years. The peak discharge is expected to occur on an average once in 143 years.
๐ SIMILAR VOLUMES
Hydrological process in arid zones differs substantially from that in better documented humid environments. The ponding point for infiltration is reached within 10 mins of first rain and overland flow forms the major component of basin runoff. Drainage densities are high, approaching 100 km.krn-', m