Abstract
THE Suez Canal, being an artificially created body of water, is not in stable equilibrium with the surrounding seas. A continuous effort has to be made to keep the canal in working order, and hence the hydrography undergoes continuous changes that have to be periodically recorded and analysed. These analyses show that the currents and distribution of salt in the canal vary seasonally.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to the full article PDF.
USD 39.95
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
Fox, M. H., Trans. Zool. Soc., 22, Part 1, No. 1 (1926).
Wimpenny, E. S., Coastguards and Fisheries Service, Fisheries Research Section, Bull., No. 1 (Government Press, Cairo, 1930).
Wüst, G., Naturwissenschaften, 22, 446 (1934).
Faouzi, H., Hydrobiological and Fisheries Directorate, No. 23 (Government Press, Cairo, 1936).
Morcos, S. A., Kieler Meeresforsch., 16, Heft 2, 133 (1960).
Morcos, S. A., Nature, 214, 901 (1967).
El-Sabh, M. I., thesis. Univ. Cairo (1967).
Daily Weather Reports (Meteorological Department, UAR, 1966–67).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
EL-SABH, M. Effect of the Aswan High Dam on the Distribution of Salinity in the Suez Canal. Nature 218, 758–760 (1968). https://doi.org/10.1038/218758a0
Received:
Revised:
Issue date:
DOI: https://doi.org/10.1038/218758a0
This article is cited by
-
Soil salinization research in China: Advances and prospects
Journal of Geographical Sciences (2014)
-
Change in the current regime in the Suez Canal after construction of Aswan High Dam
Nature (1974)
-
Change in the Current Regime in the Suez Canal after Construction of Aswan High Dam
Nature (1973)
