Although hydrological drought events vary greatly in spatial and temporal scale and can be driven by exogenous socioeconomic factors, can negative anomalies in inundated areas (e.g. wetlands, reservoirs, aqueducts) precede drought conditions? Maybe there is a trigger level that indicates a higher probability of a future drought? Have any studies been conducted that analyze the relationship between negative anomalies of inundation and initial and lagged drought conditions across spatial domains? Any discussion, thoughts, papers regarding this topic would be useful.
Many thanks!
Andrew