Clear zonation can be seen with the north eastern area receiving the highest rainfall. This area of southern Brazil is classes as tropics and moist tropical air is the common feature as the river travels southwards it enters the subtropics and a more temperate climate prevails. The western reaches of the basin receives the least rain fall mainly due to the influence of the mountain range of the Andes.
The terrain in the upper basin is steep which promotes runoff while the mid and lower sections are very flat and are subject to extensive flooding
- Global rainfall for 1985
- Global rainfall for 1986
- Global rainfall for 1987
- Global rainfall for 1988
- Global rainfall for 1989
- Global rainfall for 1990
- Global rainfall for 1991
- Global rainfall for 1992
- Global rainfall for 1993
- Global rainfall for 1994
- Global rainfall for 1995
- Global rainfall for 1996
- Global rainfall for 1997
- Global rainfall for 1998
- Global rainfall for 1999























