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Updated: March 3, 2003
See definitions.
Maryland And Delaware. – Streamflow remained in the normal to above normal range throughout the bi-state area. In Western Maryland and on the upper Potomac River, streamflow decreased, and remains in the normal range. In Central Maryland, flows increased, and remains in the above normal range. Flows on the lower Potomac River decreased, and remain in the normal range. In northeast Maryland, flows increased, and remain in the normal range. On the Eastern Shore, streamflow increased, and moved from normal into the above normal range.
Contents of the Baltimore reservoir system increased, and near month's end were 77 percent of capacity. End of month contents = 58,620 million gallons. Contents of the Triadelphia and Duckett reservoirs, near month’s end, were 11.1 billion gallons, 105 percent of capacity.
[% = percent; ft³/s =
cubic feet per second; in. = inches; Date = day of month;
1 = Includes diversions for water supply; * = Above normal range; #
= Below normal range]
|
Station name |
Discharge |
Runoff |
Cumulative runoff |
Maximum |
Minimum |
|||
|
Mean |
Percent of |
Total |
Percent of |
Departure |
||||
|
Potomac R at |
4730 |
91 |
1.57 |
7.85 |
110 |
+0.75 |
23800 |
1250 (16) |
|
Seneca C at |
*245 |
181 |
2.52 |
8.85 |
134 |
+2.25 |
1660 |
53 |
|
Potomac R near |
17600 |
109 |
1.58 |
7.49 |
105 |
+0.39 |
96900 |
2800 (18) |
|
Deer C near |
205 |
138 |
2.26 |
7.87 |
106 |
+0.47 |
1000 |
78 |
|
Choptank R near |
*426 |
196 |
3.93 |
14.04 |
2.10 |
+7.34 |
2900 |
86 |
Normal is defined as the median (50th percentile) of long-term monthly-mean discharge or monthly total runoff. The normal range is defined as discharge or runoff falling between the 75th and 25th percentiles of long-term records.
Detailed ground-water information for Maryland and Delaware is available at http://md.water.usgs.gov/groundwater/.
Last day: 33,600 cubic feet per second (estimated).
Reference period: 1971 to 2000.
Total flow into the Chesapeake Bay was about 60.9 billion gallons per day, (BGD) 89 percent of average. February average: 68.5 BGD.
The three largest rivers flowing into the Chesapeake Bay contributed about 79 percent of total inflow in february, with individual contributions of:
|
River |
Percentage of total
inflow |
|
|
|
|
Susquehanna River |
30 |
|
Potomac River |
23 |
|
James River |
26 |
|
|
|
|
Total |
79 |
|
Other rivers |
21 |
.
Period of record: 1937 to Present.
Monthly Water Conditions in the Chesapeake Bay Region
Northeast Regional Climate Center (from Cornell University)
For additional information, contact:
info@md.water.usgs.gov or call 410-238-4200.