Flash Drought Response to Precipitation and Atmospheric Evaporative Demand in Spain

Flash drought is the result of strong precipitation deficits and/or anomalous increases in atmospheric evaporative demand (AED), which triggers a rapid decline in soil moisture and stresses vegetation over short periods of time. However, little is known about the role of precipitation and AED in the...

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Bibliographic Details

Published in:	Atmosphere
Main Authors:	Iván Noguera, Fernando Domínguez-Castro, Sergio M. Vicente-Serrano
Format:	Article
Language:	English
Published:	MDPI AG 2021-01-01
Subjects:	flash drought sensitivity atmospheric evaporative demand precipitation standardized drought indices SPEI
Online Access:	https://www.mdpi.com/2073-4433/12/2/165