Hydrological drought occurs when river discharge falls below a critical threshold for an extended period, affecting water supply, ecosystems, and agriculture.
Statistical approaches estimate the likelihood of such lowβflow events by comparing observed or projected discharges to the longβterm mean and variability of the basinβs runoff.
Assuming runoff follows a normal distribution, the probability that discharge Q is less than a threshold Q_{thr} can be expressed with the standard normal cumulative distribution function.
What is hydrological drought?
How does the calculator estimate the probability of low-flow events?
What is Q_{thr} in the context of this calculator?
How does the standard normal cumulative distribution function (CDF) relate to this calculation?
Can this calculator be used for any river basin?
What are the implications of a high probability of hydrological drought?
How often should I update the discharge data for accurate results?
Results are for informational purposes only and do not constitute professional advice.
