A. predicting rainfall B.tracking air massesC.determining elevationsD.obtaining directions
there are 3 types of rainfall which are still exsisting: relief rainfall convectional rainfall Frontal rainfall
Average rainfall is 41 inches.
areal rainfall?
Rainfall in mountain areas is called: Orographic rainfall.
The peak rainfall is the highest amount of rain in a place on a hydrograph.
It shows us the time between the peak rainfall and peak discharge. Peak rainfall is the highest rain amount. Peak discharge is the highest the water level reaches in the river.
because there is
500 years ago
the time between the heaviest rainfall and the peak discharge
Landslide activity happens when the hillside has become supersaturated from the peak rainfall activity and can no longer absorb any more water. The weight of the hillside, along with not enough anchoring trees or plant life to hold it, causes the slippage of the mud.
during the design of drainage, the rainfall data provides the designer rainfall factor. the area of the site or tributary area is given. the volume of water within the tributary area is equal to rainfall depth and the tributary area also it helps to estimate time of concentration and peak runoff rate it is important to design of drainage
A. predicting rainfall B.tracking air massesC.determining elevationsD.obtaining directions
there are 3 types of rainfall which are still exsisting: relief rainfall convectional rainfall Frontal rainfall
relief rainfall convectional rainfall Frontal rainfall
Average Annual Rainfall is 43.1 inches. January Rainfall: 3.57 February Rainfall: 2.84 March Rainfall: 3.92 April Rainfall: 3.26 May Rainfall: 4.29 June Rainfall: 3.63 July Rainfall: 4.21 August Rainfall: 3.9 September Rainfall: 4.08 October Rainfall: 3.43 November Rainfall: 3.32 December Rainfall: 3.25
An attenuation pond is a pond which is designed to slow the passage of water from surface run-off to the ground/drainage system e.g. stormwater sewers. It does this by storing the run-off during times of peak flow i.e. heavy rainfall, and slowly releasing it at a controlled rate after the peak flow has passed.