LESSON 3.5 Flashcards
It is the rainfall at a single station. For small areas less than 50 km2, point rainfall may be taken as
the average depth over the area.
Point rainfall
As the rainfall over a
large area is not uniform, the average depth of rainfall over the area is determined by one of the following three
methods:
Arithmetic average method
Thiessen polygon method
The isohyetal method
It is obtained by simply averaging arithmetically the amounts of rainfall at
the individual rain-gauge stations in the area
Arithmetic Average Method
method attempts to allow for non-uniform distribution of gauges by
providing a weighting factor for each gauge.
Thiessen Polygon Method
the point rainfalls are plotted on a suitable base map and the
lines of equal rainfall (isohyets) are drawn giving consideration to orographic effects and storm
morphology
Isohyetal Method