Not exact matches
The methods used
for drought prediction based on certain drought indicators can be used directly to predict other hazards related to
hydroclimatic variables, such as flood forecasting, although a difference may exist in the properties of variables of interest;
for example, low quantile is of interest
for drought prediction while high quantile is of interest
for flood prediction.
This is especially true
for smaller (seasonal and regional) scales and weather and climate extremes, and
for important
hydroclimatic variables such as precipitation and water availability.
Although important differences must be acknowledged —
for example, the causes and the amplitudes of the warming, and the probable impacts of land cover change on temperatures — the medieval droughts can provide some direct evidence of the Southwest
hydroclimatic response to warming and a plausible, but conservative, worst - case scenario to be considered in sustainable water - resource planning.