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The time required by rain water to reach the outlet of drainage basin, is generally called
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
The shape of recession limb of a hydrograph depends upon
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
In India, which of the following is adopted as standard recording rain-gauge?
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
The stream which does not have any base flow contribution is called
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
A hyetograph is a graphical representation of
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
Phytometer method is generally used for the measurement of
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
The run off a drainage basin is
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
. A unit hydro graph has one unit of
Rainfall excess
Rainfall intensity and time
Natural siphon type
Time of concentration
Ephemeral stream
Precipitation - ground water accretion - initial recharge
basin charecteristics
transpiration
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