Diurnal variability is an important yet poorly understood aspect of the warm -
season precipitation regime over southwestern North America.
Instrumental records have shown that hydroclimatic variability across the American Southwest is mostly structured around cool -
season precipitation regimes, with a few winter storms typically contributing a disproportionately large amount of the annual precipitation across this region [15].
Not exact matches
Because the model only describes the rainy
season and does not capture the annual monsoon cycle, abrupt transitions in the bistable
regime can only be interpreted intraseasonally, e.g., a month of heavy rain followed by a month of extraordinarily weak
precipitation.