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As scientists study more about the Chesapeake Bay ecosystem, they discover more evidence that links air and water. Its now known that air pollution can contribute nitrogen and toxic chemicals to land and to water. That pollution is carried in the form of rain or snow, which eventually becomes groundwater.
Its estimated that the Bays nine largest tributaries contribute 93% of the total freshwater that enters the Bay. However, drops of rain that fall today may not make it into those tributaries or the Bay for five years or more. This natural, slow process by which water travels on land is called groundwater lag time. For example, runoff from storm events can infiltrate the ground before reaching a stream, can move with groundwater, then can eventually seep back into streams, rivers and the Bay.
Lag time can have an impact even when theres no precipitation. In the Bay watershed, several cities and towns use groundwater as a source for their public water supplies. During times of drought, a lack of precipitation eventually disrupts supplies of groundwater. Though its impossible for humans to control the climate, we can make the precipitation she gives us a little "cleaner" before it seeps into the Bays tributaries. Any actions to reduce the amount of nutrients in the air and on land will help. And, once water is in the ground, grasses, vegetation, trees and roots (buffers) next to waterways can trap sediment pollution before the water reaches streams and rivers. This is another reason to help protect and restore streamside forest buffers in the Bay region.
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