Not exact matches
Data analyses have found an
increase of
drought intensity at many locations [130]--[131] The magnitude of change depends on the
drought index employed [132], but soil moisture provides a good means to separate the effect of shifting
seasonal precipitation and confirms an overall
drought intensification [37].
In wetter regions, more intense
seasonal droughts can be managed by current water - supply systems and by adaptation; for example, demand can be reduced by using water more efficiently, or supply can be
increased by
increasing the storage capacity in reservoirs.
Seasonal drought risk is also projected to
increase in summer and fall as higher temperatures lead to greater evaporation and earlier winter and spring snowmelt.11
Data analyses have found an
increase of
drought intensity at many locations [130]--[131] The magnitude of change depends on the
drought index employed [132], but soil moisture provides a good means to separate the effect of shifting
seasonal precipitation and confirms an overall
drought intensification [37].
In particular,
seasonal and multi-year
drought frequency and intensity may have
increased, and such
increase could in part be attributable to anthropogenic forcing (e.g., Dai, 2011; Li et al., 2008).
Which is a bit strange considering a report from the European Environment Agency showing that temperatures in the Alps are
increasing a twice rate of the global average with more
droughts and greater
seasonal variability in precipitation forecast.