This is an open-access article.
At the heart of modern hydrology lies the concept of the hydrological cycle: a water circulation paradigm first proposed by European naturalists in the XVII century based on what was becoming “Western” Science. The water cycle describes the balance and regularity of evaporation, precipitation, infiltration and runoff dynamics, focusing on cyclicity and constancy in water flows. This epistemological view, having historically situated roots has informed both theoretical and practical hydrological applications worldwide. As a result, a kind of stigmatization of non-temperate, non-European water patterns developed within the scientific community, which could be termed “hydrological orientalism”. This ideological attitude sees especially drylands (and the people who inhabit them) as flawed by chronic scarcity of water in the form of surface flow or accumulation. This view fails to recognize that water dynamics function according to the specific characteristics and ecologies of each place, and peoples’ relationship with water depends on adapting to local hydrological dynamics, not disconnected ideas of what water availability “should” be. This imposed view legitimates the need of engineering interventions that “fix” the local riotous hydrology (and civilize the technical-social context) (Linton, 2008).