ugh biogeophysical and biogeochemical processes that modify both surface-atmosphere exchanges of momentum, energy and greenhouse gases and surface roughness.
The feedback mechanisms between the land surface and the atmosphere have been increasingly investigated during last decade due to the increasing computational power. Therefore, in order to study the potential impacts of LCC on local climate, the simulations performed by General Circulation Models (GCMs) have been complemented by the use of Regional Climate Models (RCMs): in fact, the coarse resolution of the GCMs limits their capability to capture mesoscale features that play a pivotal role in regional dynamics.
Figure. Differences of deforestated and control simulations of horizontal wind vectors (arrows, m/s) and temperature (shaded area, K) at 960 hPa over the summer season (JJA). The contour lines indicate where these differences are statistically significant (t test for 90% confidence level).
River discharge data analysis
River discharge is one of the five components of the Mediterranean Sea water budget, together with the net inflow of Atlantic water through the Strait of Gibraltar that from the Black Sea at the Dardanelles Strait, evaporation, and precipitation. In terms of absolute values, river discharge (R) represents the smallest contributionto this budget. In fact, climatological annual mean discharge is less than 20% of the atmospheric water budget evaporation minus precipitation (E - P), and the amplitude of its seasonal cycle is almost negligible with respect to the seasonal cycle of E-P. Nevertheless, discharge together with precipitation is the only freshwater input into the basin, and during spring the two basin-integrated components E -P and R are fairly comparable.
We collected historical river discharge monthly series from different hydrological database in order to assess the river discharge contribution to the Mediterranean fresh water input. We identified 68 rivers discharging into the Mediterranean and we estimated the climatological