This review examines the role of the atmospheric evaporative demand (AED) in drought.
AED is a complex concept and here we discuss possible AED definitions, the subsequent …

Caption: Table A. 11. 2. Synthesis table summarising assessments presented in Tables 11.4-
11.21 for hot extremes (HOT EXT.), heavy precipitation (HEAVY PRECIP.), agriculture and …

Evapotranspiration (ET) is a parameter of major importance participating in both
hydrological cycle and surface energy balance. Trends of ET are discussed along with the …

Potential evapotranspiration (ET 0) is a key component of the water cycle and a main factor
to water resources assessment. Analysis of variation in ET 0 is significant in understanding …

Evaporation from open water surfaces is often estimated based on the pan evaporation (E
pan), which is an essential measure for estimating atmospheric evaporative demand. Within …

Reasonable estimation of reference evapotranspiration (ET o) requires some climatic inputs
which might be missing in areas with sparse data recording. This study aimed to assess …

Pan evaporation (E pan), which we examine in this study to better understand atmospheric
evaporation demand, represents a pivotal indicator of the terrestrial ecosystem and …

Pan evaporation (E pan) analysis in the Qinghai‐Tibet Plateau (QTP) is important for
improving the understanding of the climatic and environmental changes in the QTP and …

This study investigates the uncertainty in hydroclimatic modelling chain components on
future changes in potential evapotranspiration, specially on low flows, at the watershed …

Pan evaporation (E pan) was regarded as a critical indicator of climate change, especially in
the Qinghai-Tibet Plateau (QTP). By using the measured daily E pan data of 274 stations in …