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Updated: August 31, 2001
See definitions.
Maryland And Delaware. -- Streamflow increased throughout most of the bi-state area. In Western Maryland and on the upper Potomac River, streamflow increased, and moved from the normal to above normal range. In Central Maryland, flows increased, and moved from the normal to above-normal range. Flows on the lower Potomac River increased, and remain in the normal range. In northeast Maryland, flows increased, and moved from the below-normal into the normal range, after three months of below normal flow. On the Eastern Shore, streamflow decreased, and moved from the above-normal into the normal range.
Contents of the Baltimore reservoir system increased, and near month's end were 87 percent of capacity. End of month contents = 66,320 million gallons.
Ground-water levels decreased throughout most of the bi-state area. In western Maryland, ground-water levels fell, and remained in the above-normal range. In west-central Maryland, ground-water levels decreased, although moving from the below to the above-normal range. In central Maryland, water levels decreased, and remained in the below-normal range. On the Eastern Shore, water levels fell, and remained in the above-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 |
*1870 |
178 |
0.69 |
11.19 |
70 |
-4.71 |
4570 |
826 |
|
Seneca C at |
*117 |
208 |
1.34 |
13.33 |
79 |
-3.47 |
887 |
31 |
|
Potomac R near |
5860 |
142 |
0.59 |
9.50 |
66 |
-5.00 |
12800 |
2830 |
|
Deer C near |
51.2 |
71 |
0.62 |
12.12 |
64 |
-6.88 |
131 |
34 |
|
Choptank R near |
39.1 |
93 |
0.40 |
19.77 |
121 |
+3.47 |
96 |
23 |
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.
|
Well number |
Well name |
Previous month |
Reporting month |
||
|
Date measured |
Level |
Date measured |
Level |
||
|
GA-Bc 1 |
Accident |
07-30 |
14.16 |
08-30 |
14.25 |
|
WA-Be 2 |
Fort Frederick |
07-30 |
33.07 |
08-30 |
33.14 |
|
MO-Eh 20 |
Fairland |
07-30 |
13.77 |
08-30 |
14.27 |
|
Jd 42-03 |
Camden |
07-26 |
5.59 |
08-29 |
6.38 |
|
Name |
Date measured |
Water level |
Departure from
average |
Change since
previous month |
Change since
previous year |
Last reversal |
|
|
Change |
Date |
||||||
|
Accident |
08-30 |
14.25 |
+0.24 |
-0.09 |
+0.49 |
-1.68 |
June 2001 |
|
Fort Frederick |
08-30 |
33.14 |
+0.21 |
-0.07 |
-1.18 |
-7.38 |
Apr 2001 |
|
Fairland |
08-30 |
14.27 |
-0.51 |
-0.50 |
-0.53 |
-2.19 |
June 2001 |
|
Camden |
08-29 |
6.38 |
+0.46 |
-0.79 |
-0.38 |
-1.54 |
July 2001 |
Last day: 2920 cubic feet per second (estimated).
Reference period: 1971 to 2000.
Total flow into the Chesapeake Bay was about 15.4 billion gallons per day, (BGD) 78 percent of average. August average: 19.8 BGD.
The three largest rivers flowing into the Chesapeake Bay contributed about 80 percent of total inflow in August, with individual contributions of:
|
River |
Percentage of total
inflow |
|
|
|
|
Susquehanna River |
23 |
|
Potomac River |
33 |
|
James River |
20 |
|
|
|
|
Total |
76 |
|
Other rivers |
24 |
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.