Our results suggest that productivity reduction in eastern and western Europe can be explained
by rainfall deficit and extreme summer heat, respectively.
Not exact matches
Natural processes changed the timing and magnitude of soil moisture, streamflow, and groundwater
deficits by up to several years, and caused the amplification of
rainfall declines in streamflow to be greater than in normal dry years.
By using an idealized heating to force a comprehensive atmospheric model, the large negative anomalous latent heating associated with the observed
deficit in central tropical Pacific
rainfall is shown to be mainly responsible for the global quasi-stationary waves in the upper troposphere.