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Updated: July 31, 2001
See definitions.
Maryland And Delaware. -- Streamflow decreased throughout the entire bi-state area. In Western Maryland and on the upper Potomac River, streamflow decreased, and remained in the normal range. In Central Maryland, flows decreased, and moved from the above-normal into the normal range. Flows on the lower Potomac River decreased, and remain in the normal range. In northeast Maryland, flows decreased, and remain in the below-normal range for the third month straight. On the Eastern Shore, streamflow decreased from the previous month’s record high, although remaining in the above-normal range.
Contents of the Baltimore reservoir system decreased, and near month's end were 82 percent of capacity. End of month contents = 62,100 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, and remained in the below-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 |
1760 |
133 |
0.64 |
10.50 |
68 |
-4.90 |
8500 |
832 |
|
Seneca C at |
67.1 |
91 |
0.76 |
11.99 |
75 |
-3.91 |
212 |
36 |
|
Potomac R near |
4000 |
80 |
0.40 |
8.91 |
63 |
-5.29 |
7940 |
2330 |
|
Deer C near |
#48.9 |
52 |
0.60 |
11.50 |
66 |
-6.00 |
81 |
37 |
|
Choptank R near |
*103 |
224 |
1.05 |
19.37 |
121 |
+3.37 |
372 |
42 |
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 |
06-28 |
13.88 |
07-30 |
14.16 |
|
WA-Be 2 |
Fort Frederick |
06-28 |
31.61 |
07-30 |
33.07 |
|
MO-Eh 20 |
Fairland |
06-28 |
12.73 |
07-30 |
13.77 |
|
Jd 42-03 |
Camden |
06-28 |
4.84 |
07-26 |
5.59 |
|
Name |
Date measured |
Water level |
Departure from
average |
Change since
previous month |
Change since
previous year |
Last reversal |
|
|
Change |
Date |
||||||
|
Accident |
07-30 |
14.16 |
+0.78 |
-0.28 |
+1.19 |
-1.59 |
June 2001 |
|
Fort Frederick |
07-30 |
33.07 |
-1.23 |
-1.46 |
-1.27 |
-7.31 |
Apr 2001 |
|
Fairland |
07-30 |
13.77 |
-0.42 |
-1.04 |
-0.60 |
-1.69 |
June 2001 |
|
Camden |
07-26 |
5.59 |
+0.95 |
-0.75 |
+0.94 |
-0.75 |
July 2001 |
Last day: 5610 cubic feet per second (estimated).
Reference period: 1971 to 2000.
Total flow into the Chesapeake Bay was about 15.3 billion gallons per day, (BGD) 67 percent of average. July average: 23.0 BGD.
The three largest rivers flowing into the Chesapeake Bay contributed about 80 percent of total inflow in July, with individual contributions of:
|
River |
Percentage of total
inflow |
|
|
|
|
Susquehanna River |
46 |
|
Potomac River |
24 |
|
James River |
10 |
|
|
|
|
Total |
80 |
|
Other rivers |
20 |
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.