Maps for each month use a 15 year average (1985-1999) to show what average annual evaporation is like.
The rate at which evaporation takes place is influenced by temperature, sunshine, wind and the humidity of the air – with temperature and sunshine being the most important. Consequently season and climate zones mean different areas of the globe are experiencing different evaporation rates over the period of a year.
During the summer months (June/July/August in N. Hemisphere and Dec./Jan./Feb. in S. Hemisphere) the high energy input from solar radiation mean that higher evaporation rates than in the winter months are recorded.
Some areas of the globe experience low evaporation rates year round because of low water content in the soil. For example, the Sahara desert has low evaporation because of dry conditions, despite the high solar radiation. However, it is interesting to observe the Nile River up to the Aswan dam with its constant available water shows higher evaporation than the surrounding desert area.
- Average evaporation for Jan
- Average evaporation for Feb
- Average evaporation for Mar
- Average evaporation for Apr
- Average evaporation for May
- Average evaporation for Jun
- Average evaporation for Jul
- Average evaporation for Aug
- Average evaporation for Sep
- Average evaporation for Oct
- Average evaporation for Nov
- Average evaporation for Dec
- Average evaporation for Jan
- Average evaporation for Feb
- Average evaporation for Mar
- Average evaporation for Apr
- Average evaporation for May
- Average evaporation for Jun
- Average evaporation for Jul
- Average evaporation for Aug
- Average evaporation for Sep
- Average evaporation for Oct
- Average evaporation for Nov
- Average evaporation for Dec

















