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An increase in precipitation.

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Gerda O'Conner

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3y ago

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Related Questions

What is the factor that could account for a rise in the water table is?

An increase in precipitation.


One factor that could account for a drop in the water table?

pumping water from aquifers


One factor that could account for the rise in the water table is what?

An increase in precipitation.


One factor could account for a drop in the water table is?

less rain and snow


What is One factor that could account for a drop in the water table is?

One factor that could account for a drop in the water table is temperature. If temperatures are too warm the water may be evaporating.


One factor that could account for a rise in the water table is what?

An increase in precipitation or a decrease in water usage can lead to a rise in the water table. This allows more water to percolate down into the ground, causing the water table to increase.


One factor that could account for a drop in the water table is?

Water extraction by people or industry or less rain. pumping water from aquifers. less rain and snow


What factor is lowered when more water is removed from groundwater than is returned to it?

The water table.


Which factor have lead to the reduction of the water table in India?

use of chemical fertilisers.


Use water table in a sentence?

Example sentences:The water table was so high that everyone had water in their basements.The water table was so high that the town could not handle anymore rain.


How many ways can you empty a glass of water which is on a table without touching either the table or the glass?

You could blow on the water, causing it to spill out of the glass. Alternatively, you could tilt the table slightly to pour out the water without physically touching the glass or the table.


What is the slope of the water table is called?

The slope of the water table is called the hydraulic gradient. This gradient represents the rate of change in water table elevation over a specific distance. It is an important factor in determining the direction and velocity of groundwater flow.