Abstract
ABSTRACT The hydrometeorology of Egypt is examined and the groundwater situation analyzed with reference to the use of environmental isotopes and the information they can provide as to pluvial and post-pluvial inputs to the Nubian aquifer system. Recharge to and discharge from this vast reservoir of partly fossil water indicate its dynamic state. The water table has declined appreciably in historic times. Lack of data makes extreme caution advisable in drawing general conclusions.
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