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Updated: July 1, 2003
See definitions.
Maryland And Delaware. – Streamflow increased throughout the entire bi-state area. In Western Maryland and on the upper Potomac River, streamflow increased, remaining in the above normal range for the fourth consecutive month; a new maximum monthly flow for June was established. In Central Maryland, flows increased, moving from the normal into the above normal range. Flows on the lower Potomac River increased, and remain in the above normal range for the fourth straight month; only flows recorded in June of 1972 (Hurricane Agnes) exceeded this months average. In northeast Maryland, flows increased, moving from the normal into the above normal range. On the Eastern Shore, streamflow increased, and remains in the above normal range for the fifth consecutive month; a new maximum monthly flow for June was established.
Contents of the Baltimore reservoir system increased slightly, and near month's end were 103 percent of capacity. End of month contents = 78,400 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 |
*10500 |
441 |
3.75 |
23.47 |
158 |
+8.57 |
19300 |
2900 (30) |
| Seneca C at |
*448 |
467 |
4.94 |
21.95 |
143 |
+6.65 |
1490 |
125 |
| Potomac R near |
*42000 |
453 |
4.05 |
22.45 |
165 |
+8.85 |
81200 |
13400 (30) |
| Deer C near |
*296 |
239 |
3.49 |
18.98 |
121 |
+3.28 |
722 |
167 |
| Choptank R near |
*508 |
718 |
5.02 |
29.86 |
191 |
+14.26 |
2220 |
140 |
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: 13,400 cubic feet per second (estimated).
Reference period: 1971 to 2000.
Total flow into the Chesapeake Bay was about 123 billion gallons per day, (BGD) 297 percent of average. June average: 41.5 BGD.
****Second highest June flow to the bay for the period of record; Highest June flow 221 BGD (1972).
The three largest rivers flowing into the Chesapeake Bay contributed about 85 percent of total inflow in June, with individual contributions of:
| River |
Percentage
of total inflow |
| |
|
| Susquehanna River |
44 |
| Potomac River |
26 |
| James River |
15 |
| |
|
| 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.