Interannual/seasonal variability of the contribution of the moisture sources to the precipitation on the CCR


The uptake of moisture from the evaporative sources changes in intensity over time.

The method allows us to calculate the budget of (E-P)1-10 and (E-P)n over the limits defined for the moisture sources for each year.


Approach: Backward tracking from the target region

Temporal scale: Annual and Annual Seasonal

Patterns: (E-P)1-10 and (E-P)n budget over the limits defined for the sources