The cumulative rainfall departure (CRD) method, based on the water-balance
principle, is often used for mimicking of Water level fluctuations. Because
of its simplicity and minimal requirement of spatial data, the CRD method
has been estimating either effective recharge or aquifer storativity, and c
onsequently gained a focus in South applied widely for estimating either ef
fective recharge or aquifer storativity, and consequently gained a focus in
South Africa. This paper critically reviews this method and proposes expan
ded algorithm. Validation of the method under typical South African conditi
ons is discussed based on model-generated and known cases. The study is aid
ed with a user-friendly Excel program called Recharge Estimation Model in E
xcel (REME).