Abstract. Climate extremes, such as floods and droughts, might have
severe economic and societal impacts. Given the high costs associated with
these events, developing early-warning systems is of high priority.
Evaporation, which is driven by around 50 % of solar energy absorbed at
surface of the Earth, is an important indicator of the global water budget,
monsoon precipitation, drought monitoring and the hydrological cycle. Here we
investigate the response of global evaporation to main modes of interannual
climate variability, including the Indian Ocean Dipole (IOD), the North
Atlantic Oscillation (NAO) and the El Niño–Southern Oscillation (ENSO).
These climate modes may have an influence on temperature, precipitation, soil
moisture and wind speed and are likely to have impacts on global evaporation.
We utilized data of historical simulations and RCP8.5 (representative concentration pathway) future simulations
derived from the Coupled Model Intercomparison Project Phase 5 (CMIP5). Our
results indicate that ENSO is an important driver of evaporation for many
regions, especially the tropical Pacific. The significant IOD influence on
evaporation is limited in western tropical Indian Ocean, while NAO is more
likely to have impacts on evaporation of the North Atlantic European areas.
There is high agreement between models in simulating the effects of climate
modes on evaporation of these regions. Land evaporation is found to be less
sensitive to considered climate modes compared to oceanic evaporation. The
spatial influence of major climate modes on global evaporation is slightly
more significant for NAO and the IOD and slightly less significant for
ENSO in the 1906–2000 period compared to the 2006–2100 period. This study
allows us to obtain insight about the predictability of evaporation and
hence, may improve the early-warning systems of climate extremes and water
resource management.