Updated: September 2, 2003
See definitions.
Maryland And Delaware. – Streamflow decreased throughout the entire bi-state area, although flows remain in the above normal range. In Western Maryland and on the upper Potomac River, streamflow decreased, remaining in the above normal range for the sixth consecutive month. In Central Maryland, flows decreased, remaining in the above normal range. Flows on the lower Potomac River decreased, and remain in the above normal range for the sixth straight month. In northeast Maryland, flows decreased, although remaining in the above normal range. On the Eastern Shore, streamflow decreased, and remains in the above normal range for the seventh consecutive month.
Contents of the Baltimore reservoir system increased slightly, and near month's end were 100 percent of capacity. End of month contents = 75,960 million gallons. Contents of the Triadelphia and Duckett reservoirs, near month’s end, were 10.5 billion gallons, 99 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 |
*2170 |
207 |
0.80 |
25.26 |
159 |
+9.36 |
5360 |
1030 (26) |
Seneca C at |
*118 |
210 |
1.35 |
25.31 |
151 |
+8.51 |
315 |
78 |
Potomac R near |
*7790 |
189 |
0.77 |
24.30 |
168 |
+9.80 |
14600 |
5090 (25) |
Deer C near |
*152 |
211 |
1.85 |
23.18 |
122 |
+4.18 |
396 |
97 |
Choptank R near |
*139 |
332 |
1.49 |
33.85 |
208 |
+17.55 |
372 |
60 |
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 Groundwater information for Maryland and Delaware is available at https://md.water.usgs.gov/groundwater/.
Last day: 5,360 cubic feet per second (estimated).
Reference period: 1971 to 2000.
Total flow into the Chesapeake Bay was about 49.1 billion gallons per day, (BGD) 225 percent of average. August average: 21.8 BGD.
****Fourth highest August flow to the bay for the period of record; Highest August flow 62.0 BGD (1955).
The three largest rivers flowing into the Chesapeake Bay contributed about 85 percent of total inflow in August, with individual contributions of:
River |
Percentage of total
inflow |
|
|
Susquehanna River |
58 |
Potomac River |
14 |
James River |
13 |
|
|
Total |
85 |
Other rivers |
15 |
.
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.