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Updated: April 30, 2002
See definitions.
Maryland And Delaware. -- Streamflow continues to remain below normal throughout much of the bi-state area. In Western Maryland and on the upper Potomac River, streamflow increased, and moved from the below-normal into the normal range, after 6 months of below-normal flow. In Central Maryland, flows decreased, and remain in the below normal range for the sixth straight month. Flows on the lower Potomac River increased, and moved from the below-normal into the normal range, after 6 months of below-normal flow. In northeast Maryland, at the index station on Deer Creek, flows decreased, and continue to remain in the below-normal range (11 of the last 12 months below normal flows). On the Eastern Shore, streamflow increased, and remains in the below normal range for the sixth month straight. Lowest monthly April flows for the period of record at the index station on Deer Creek (also record low single day).
Contents of the Baltimore reservoir system increased, and near month's end were 62 percent of capacity. End of month contents = 47,030 million gallons. Contents of the Triadeplphia and Duckett reservoirs, near month’s end, were 6.55 billion gallons, 62 percent of capacity.
Ground-water levels increased throughout most of the bi-state area. In Western Maryland, ground-water levels rose, and remain in the above-normal range. In west-central Maryland, ground-water levels increased, although remaining in the below-normal range. In central Maryland, water levels increased slightly, and remained in the below-normal range, recording a record low reading for the fourth month in a row. On the Eastern Shore, water levels rose, but continue to remain in the below-normal range.
[% = 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 |
6820 |
136 |
2.43 |
4.59 |
37 |
-7.91 |
26000 |
1870 |
|
Seneca C at |
#78.3 |
50 |
0.86 |
4.97 |
49 |
-5.23 |
398 |
47 |
|
Potomac R near |
12800 |
77 |
1.24 |
2.93 |
26 |
-8.17 |
49100 |
4790 (14-15) |
|
Deer C near |
#46.0 |
28 |
0.54 |
3.38 |
29 |
-8.12 |
129 |
35 |
|
Choptank R near |
#93.5 |
49 |
0.93 |
2.86 |
22 |
-10.14 |
210 |
59 |
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: 30,600 cubic feet per second (estimated).
Reference period: 1971 to 2000.
Total flow into the Chesapeake Bay was about 54.0 billion gallons per day, (BGD) 57 percent of average. April average: 94.1 BGD.
The three largest rivers flowing into the Chesapeake Bay contributed about 86 percent of total inflow in April, with individual contributions of:
|
River |
Percentage of total
inflow |
|
|
|
|
Susquehanna River |
55 |
|
Potomac River |
20 |
|
James River |
11 |
|
|
|
|
Total |
86 |
|
Other rivers |
14 |
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.