January 2005 Water Levels Normal to Above Normal
U.S. Department of the Interior
U.S. Geological Survey
Contact:
Wendy
McPherson (wsmcpher@usgs.gov)
Maryland-Delaware-D.C.
Water Science Center
5522 Research Park Drive
Baltimore, MD 21228
Phone:(443)498-5500
FAX: (443)498-5510
Updated: February 7, 2005
Rainfall in the middle of January led to high streamflows in northern Maryland and northern Delaware, according to hydrologists at the U.S. Geological Survey (USGS). Monthly water levels, however, were normal to above normal across Maryland, Delaware, and Washington, D.C., continuing the several-month-long trend of normal to above normal water levels.
Status of Streams and Wells
The map below shows the location and status of wells and streams used by the USGS to monitor water conditions in Maryland, Delaware, and Washington, D.C. for January 2005. Water levels were generally above normal in the northern parts of Maryland and Delaware, and normal in southern Maryland and most of the Delmarva Peninsula.

Precipitation
January precipitation and temperatures were close to long-term averages in Maryland and Delaware, and Washington, D.C., according to preliminary rainfall data from the National Weather Service (NWS). However, temperatures at the beginning of the month averaged about 10 degrees warmer than normal and New Year’s Day was the warmest on record at 67 degrees (from NWS statement). On January 13 and 14, 1 to 2 inches of rain fell on the region, resulting in high streamflow levels. The last half of January was about 10 degrees colder than normal and included several snowfalls.
Chesapeake Bay
Monthly mean streamflow into the Chesapeake Bay during January averaged 103 bgd (billion gallons per day), which is 80 percent above normal. Normal flow for January is 57.4 bgd.
Streamflow
Streamflow increased and was normal to above normal in streams in Maryland, Delaware, and Washington, D.C. in December. Streamflow was normal to above normal throughout 2004, except for the Choptank River, Nassawango Creek, and the Pocomoke River, which were below normal during the summer. The hydrograph of Piscataway Creek shows that streamflow levels did not follow the typical seasonal pattern because of abundant rainfall and groundwater levels.

Current and historical streamflow data can be monitored on the web at: http://waterdata.usgs.gov/. Five-year monthly streamflow hydrographs from the USGS stream-gaging network can be viewed on the web at: http://md.water.usgs.gov/surfacewater/streamflow/
Daily streamflow for the Potomac River near Washington, D.C. averaged 12.6 bgd in January, which is 39 percent above normal. More information on the Potomac River is available at: http://md.water.usgs.gov/monthly/poto.html
Groundwater
Near normal precipitation in January led to normal to above normal water levels in wells used by the USGS to monitor unconfined or shallow aquifer response to climatic conditions in Maryland and Delaware. Groundwater levels in southern Maryland and on the Delmarva Peninsula were at normal levels.
Recharge to the groundwater system typically occurs late fall to early spring when water levels rise because of low evapotranspiration (water that evaporates or is used by plants) rates. The highest groundwater levels are typically in March or April before the growing season begins. For 5-year hydrographs of groundwater levels for the climatic indicator wells, visit: http://md.water.usgs.gov/groundwater/.
Reservoir Storage
Storage in the Baltimore reservoir system rose 1 percent to 100 percent of capacity in January. The Baltimore reservoirs (Loch Raven, Liberty, and Prettyboy) have been nearly full since May 2003. Storage in the Triadelphia and Duckett Reservoirs on the Patuxent River, which serve Montgomery and Prince Georges Counties, rose 7 percent to 100 percent of capacity in January.
U.S. Geological Survey
Streamflow and groundwater levels are used to assess current water conditions and can be used to predict the potential for flooding and drought conditions. These USGS data have been provided to State and local water resource managers and are critical for making appropriate decisions on water regulation. For more information on streamflow and groundwater levels in Maryland, Delaware, and the Washington, D.C., visit Water Watch at: Water Watch.
The USGS, a Bureau within the Department of the Interior, has served the Nation and the world for 125 years by providing reliable scientific information to describe and understand the Earth; minimize loss of life and property from natural disasters; manage water, biological, energy, and mineral resources; and make important decisions and enhance and protect our quality of life.
** * USGS * * *
In-depth information about USGS programs may be found on the USGS home page at http://www.usgs.gov and http://chesapeake.usgs.gov/ for Chesapeake Bay activities.
Archived News Releases 2000-Present
2006
- 01-06-2006 Water Resources Plentiful at End of December 2005; Chesapeake Bay Flow Normal in 2005
2005
- 07-06-2005 Water Levels Fall as Summer Arrives
- 04-06-2005 March 2005 Water Levels Near Normal
- 03-04-2005 Flow Below Normal in Potomac River and Chesapeake Bay
- 02-07-2005 January 2005 Water Levels Normal to Above Normal
- 01-07-2005 2004 Ends with Normal to Above Normal Water Levels
2004
- 12-04-2004 Water Levels Remain Generally Above Normal
- 11-04-2004 Dry October Causes Water Levels to Drop
- 10-06-2004 Highest September Flow to the Chesapeake Bay Since 1937
- 09-03-2004 August Hurricanes Raise Water Levels in Southern Maryland
- 08-06-2004 Localized Flooding in Northeastern Maryland and Delaware in July
- 07-07-2004 Water Levels Normal to Above Normal in June
- 06-04-2004 Streams Return to Normal Levels in Maryland and Delaware during May 2004
- 05-06-2004 Streams Rise to Above Normal Levels in Maryland
- 04-07-2004 Streamflow and Groundwater Levels Fell in March 2004
- 03-04-2004 Streamflow and Groundwater Levels Normal to Above Normal in February 2004
- 02-04-2004 Cold, Dry January Leads to Drop in Water Levels
- 01-06-2004 Wettest Year Leads to Record-High Water Levels Including Third Highest Flow to Chesapeake Bay in December and 2003
2003
- 12-04-2003 More Record-High Water Levels in November 2003
- 11-04-2003 Record High Groundwater Levels in October 2003
- 10-03-2003 Flow to Chesapeake Bay in Water Year 2003 Second Highest Since 1937
- 09-05-2003 Third Consecutive Month of High Flow into the Chesapeake Bay
- 08-06-2003 Flow into Chesapeake Bay near Record High Levels
- 07-07-2003 Record Breaking High Water Levels in Maryland and Delaware
- 06-06-2003 Streamflow and Groundwater Levels High in May
- 05-07-2003 April Water Levels Normal
- 04-05-2003 Water Levels High in March - Water Restrictions Lifted
- 03-05-2003 Exceptionally Wet February Leads to High Water Levels
- 02-06-2003 Maryland and Delaware Streamflow and Groundwater Levels Remain Normal in January 2003
- 01-07-2003 2002: A Record-Setting Year for Low Groundwater Levels - Water Levels Recover to Normal in December 2002
2002
- 12-01-2002 Hydrologic Drought Wanes as Water Levels Rise
- 11-01-2002
Water Levels Rise Across
Maryland and Delaware,
But Drought Persists in Some Areas - 10-03-2002 Water Levels Remain at Record-Setting Lows
- 09-05-2002 Groundwater in Parts of Maryland Reaches Lowest Levels Since 1962, Despite Late August Rains
- 08-06-2002 Drought Conditions Lead to 10 Record Low Monthly Groundwater Levels in July
- 07-03-2002 Record Low Water Levels Show the Effects of Long-Term Hydrologic Drought
- 06-04-2002 Groundwater Levels Reflect Long-Term Effects of Drought
- 05-02-2002 April Showers Not Enough to Raise Groundwater Levels
- 04-05-2002 The Drought in Full Bloom: Low Water Levels Result in Water Restrictions
2001
- 12-03-2001 Record Low Water Levels Set in November
- 11-02-2001 Dry October Leads to Low Water Levels
- 10-05-2001 Water Levels Low in Northern Maryland
- 09-07-2001 Water Levels Stable in August
- 08-06-2001 High and Low Water Levels in July
- 07-06-2001 Water Levels Continued to Improve in June
- 06-06-2001 Needed Rain Helps Avert a Drought in May
- 05-08-2001 Water Levels Still Normal in April, but More Rain is Needed
- 04-05-2001 Spring Rains Help Water Levels
- 03-06-2001 Water Levels Improve, But Are Still Below Normal
- 02-06-2001 Streamflow Still Low in Maryland in January
- 01-05-2001 Streamflow to Chesapeake Bay in 2000 Reflects Dry Autumn
2000
- 12-05-2000 Streamflow in Maryland Beginning to Show the Effects of Lack of Rain
- 11-07-2000 Despite Lack of Rain October Water Conditions near Normal
- 10-06-2000 September Water Conditions Above Normal in Maryland, Delaware, and D.C.
- 09-08-2000 August Water Conditions Above Normal in Maryland, Delaware, and D.C.
- 08-07-2000 July Water Conditions Continue Normal in Maryland, Delaware, and D.C.
- 07-07-2000 June Water Conditions Normal in Maryland, Delaware, and D.C.
- 06-06-2000 Water conditions begin to decline in Maryland, Delaware, and D.C.
- 05-05-2000 Water Conditions Continue to Improve in Maryland, Delaware, and D.C.
- 04-07-2000 Water Conditions Continue to Improve in Maryland, Delaware, and D.C.
- 03-07-2000 Water Conditions Improving in Maryland, Delaware, and D.C.
- 02-08-2000 January Streamflow and Groundwater Levels Still Low
- 01-06-2000 1999 Flow Into Chesapeake Bay Lowest Since 1960s Drought


