LESSON 3.5 Flashcards

1
Q

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.

A

Point rainfall

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2
Q

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:

A

Arithmetic average method
Thiessen polygon method
The isohyetal method

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3
Q

It is obtained by simply averaging arithmetically the amounts of rainfall at
the individual rain-gauge stations in the area

A

Arithmetic Average Method

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4
Q

method attempts to allow for non-uniform distribution of gauges by
providing a weighting factor for each gauge.

A

Thiessen Polygon Method

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5
Q

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

A

Isohyetal Method

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