Large-basin hydrological response to climate model outputs: uncertainty caused by the internal atmospheric variability

Temperature and precipitation from 16 climate models each using two emissions sce- narios (lower B1 and mid-high A2) were used to characterize the range of potential climate changes

The impacts from climate change (RCP 8.5 scenario) in the Lavrinha watershed runoff were analyzed based on the “Distributed Hydrology Soil Vegetation Model” (DHSVM), forced with

After a brief description of the area of study (Sect. 2), the five large-scale times se- ries derived from the reanalyses regions and LMDZ boxes are presented (Sect. 4, the

We examine the response of the deep cell in the eastern basin to two types of modifi- cation of the atmospheric forcing, both amounting to a decrease in buoyancy loss: (i) a

Considering the relative simplicity of the routing channel, the model provides a good estimation of the surface water dynamics: the spatio-temporal variability of the flooded areas,

A main result of our analysis is that the connectivity of the forced variabi- lity network is heavily affected by “El Niño”: removing the NINO3.4 index yields a general loss

Using four different climate models, we investi- gate sea level pressure variability in the extratropical North Atlantic in the preindustrial climate (1750 AD) and at the Last

] between soil moisture and latent heat flux for the control simulation (top-row) and change due to deforestation (bottom-row) for NDJFM, AMJ and JASO... Atmospheric leg of