![]()
Updated: June 2, 2003
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, remaining in the above normal range for the third consecutive month. In Central Maryland, flows increased, remaining in the normal range. Flows on the lower Potomac River increased, and remain in the above normal range for the third straight month. In northeast Maryland, flows increased slightly, and remain in the normal range. On the Eastern Shore, streamflow decreased, although remaining in the above normal range for the fourth consecutive month.
Contents of the Baltimore reservoir system increased slightly, and near month's end were 100 percent of capacity. End of month contents = 75,980 million gallons. Contents of the Triadelphia and Duckett reservoirs, near month’s end, were 11.4 billion gallons, 107 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 |
*10200 |
209 |
3.76 |
19.72 |
144 |
+6.02 |
38100 |
3270 (1) |
| Seneca C at |
204 |
153 |
2.33 |
17.01 |
122 |
+3.01 |
343 |
113 |
| Potomac R near |
*34100 |
232 |
3.40 |
18.40 |
146 |
+5.80 |
80000 |
12300 (2) |
| Deer C near |
167 |
96 |
2.05 |
15.49 |
112 |
+1.69 |
472 |
111 |
| Choptank R near |
*245 |
191 |
2.50 |
24.84 |
167 |
+9.94 |
994 |
79 |
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: 22,700 cubic feet per second (estimated).
Reference period: 1971 to 2000.
Total flow into the Chesapeake Bay was about 87.0 billion gallons per day, (BGD) 136 percent of average. May average: 64.1 BGD.
The three largest rivers flowing into the Chesapeake Bay contributed about 83 percent of total inflow in May, with individual contributions of:
| River |
Percentage
of total inflow |
| |
|
| Susquehanna River |
33 |
| Potomac River |
30 |
| James River |
20 |
| |
|
| Total |
83 |
| Other rivers |
17 |
.
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.