![]() |
|
|
|
|
How
floods are predicted A TECHNICAL REPORT ABOUT HOW THE SYSTEM PERFORMED DURING THE JANUARY 1996 FLOOD (PDF) Knowledge of topography, geology, and hydrology is important. The following are two distinct ways that the basin's topography and geology contribute to flooding. The first situation occurs when a section of river is very wide, but then is suddenly squeezed into a steep, narrow gorge. During heavy rainfall events or when the winter ice begins to break up, the increased flow of water or ice backs up in the narrow gorge, causing the river to overflow its banks. Also, when the ice jam breaks, a sudden surge of water can cause downstream flooding. The second situation occurs when a river flows through an area with very little slope, and shallow banks. In this topography, which is fairly common in the basin, the river levels out and flows slowly. During heavy rainfall events, the river quickly swells and overflows its banks. When winter ice breaks up, the slow-moving flow causes the ice to jam easily, creating obstacles and backing up the water.
The flood
warning system requires a cooperative effort The U.S. Geological Survey provides data to the National Weather Service on precipitation, river stages and water flow from a network of stream gages. The Baltimore District of the U.S. Army Corps of Engineers also provides reservoir and gaging information.
|
|||
![]() |
||||
|
|
||||
|
|
Return to SRBC home page.