Figure 4.5: Typical hydrographs in accordance with climatic settings
Source: Note: For tropical climates close to the equator (Af), perennial rivers flow all year. Towards the north and south the tropical climates have a
distinct rainy season and a dry season (Am and Aw). In dry climates (B) rivers are often ephemeral and only flow periodically after a storm.
In the temperate Cf climate, there is no distinct dry or wet season, whereas the ‘Mediterranean climate’ (Cs) has a pronounced seasonal
water deficit in the summer and a rainy winter reflected in the hydrograph. The cold climates (D) have a distinct snowmelt runoff peak and
the Df climate has an additional peak in the autumn caused by rain.
Source: Stahl and Hisdal 2004.