The term “flash drought” is currently used in an ambiguous manner in the scientific literature. We recommend that these climate features should be identified based on how rapidly they intensify.

Given the increasing use of the term “flash drought” by the media and scientific community, it is prudent to develop a consistent definition that can be used to identify these events and to understand their salient characteristics. It is generally accepted that flash droughts occur more often during the summer due to increased evaporative demand; however, two distinct approaches have been used to identify them. The first approach focuses on their rate of intensification, whereas the second approach implicitly focuses on their duration. These conflicting notions for what constitutes a flash drought (i.e., unusually fast intensification versus short duration) introduce ambiguity that affects our ability to detect their onset, monitor their development, and understand the mechanisms that control their evolution.

Here, we propose that the definition for flash drought should explicitly focus on its rate of intensification rather than its duration, with droughts that develop much more rapidly than normal identified as flash droughts. There are two primary reasons for favoring the intensification approach over the duration approach.

First, longevity and impact are fundamental characteristics of drought.

Thus, short-term events lasting only a few days and having minimal impacts are inconsistent with the general understanding of drought and therefore should not be considered flash droughts.

Second, by focusing on their rapid rate of intensification, the proposed flash drought definition highlights the unique challenges faced by vulnerable stakeholders who have less time to prepare for its adverse effects.