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The Climate and Hydrology of the Upper Blue Nile River

✍ Scribed by DECLAN CONWAY


Book ID
111208881
Publisher
John Wiley and Sons
Year
2000
Tongue
English
Weight
957 KB
Volume
166
Category
Article
ISSN
0016-7398

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πŸ“œ SIMILAR VOLUMES


Models for recession flows in the upper
✍ A. Mishra; T. Hata; A. W. Abdelhadi πŸ“‚ Article πŸ“… 2004 πŸ› John Wiley and Sons 🌐 English βš– 375 KB

## Abstract Stream‐flow recessions are commonly characterized by the exponential equation or in the alternative power form equation of a single linear reservoir. The most common measure of recession is the recession constant __K__, which relates to the power function form of the recession equation

Hydrologic model calibration using disco
✍ Ungtae Kim; Jagath J. Kaluarachchi πŸ“‚ Article πŸ“… 2009 πŸ› John Wiley and Sons 🌐 English βš– 509 KB

## Abstract Hydrologic models using water balance approaches typically use continuously observed streamflow data for calibration. Many large river basins in developing countries such as the upper Blue Nile River Basin of Ethiopia have discontinuous hydrographs that contain short continuous periods.

El NiΓ±o Southern Oscillation link to the
✍ Wossenu Abtew; Assefa M. Melesse; Tibebe Dessalegne πŸ“‚ Article πŸ“… 2009 πŸ› John Wiley and Sons 🌐 English βš– 360 KB

## Abstract The objective of this study is to evaluate the relationships of El NiΓ±o Southern Oscillation (ENSO) indices and the Blue Nile River Basin hydrology using a new approach that tracks cumulative ENSO indices. The results of this study can be applied for water resources management decision

Recession flow analysis of the Blue Nile
✍ Anil Mishra; Takeshi Hata; A. W. Abdelhadi; Akio Tada; Haruya Tanakamaru πŸ“‚ Article πŸ“… 2003 πŸ› John Wiley and Sons 🌐 English βš– 152 KB

## Abstract Estimates of the amount of recession flow can be derived from streamflow records. Such estimates are critical in the assessment of low flow characteristics for the Blue Nile River, from which about two‐thirds of the irrigation requirements in Sudan are satisfied. The recession flow hydr