Surface Water
The Surface Water Team monitors and conducts investigative research to improve our region's understanding of extreme hydrologic events - droughts, floods and hazards, and coastal or bay storm surge and inundation. They also facilitate measurement of precipitation, streamflow, stage and computation of flow at locations in Maryland, Delaware, and the District of Columbia.
As an integrated part of the WSC, the Surface Water Team monitors and conducts investigative research to describe and improve our region's understanding of extreme hydrologic events - droughts, floods and flood hazards, and coastal or bay storm surge and inundation. They also facilitate measurement stream stages, streamflow, and computes daily streamflow at locations in Maryland, Delaware, and the District of Columbia. Surface Water also conducts surface water-quality monitoring for our Hydrologic Networks to help meet many cooperator needs.
Related Content
Storms and floods of July 30, 2016, and May 27, 2018, in Ellicott City, Howard County, Maryland
IntroductionOn July 30, 2016, and May 27, 2018, the downtown area of Ellicott City, Maryland (fig. 1), was severely flooded by intense, short-duration rainfall that resulted in loss of life; significant damage to buildings, roads, infrastructure; and hundreds of vehicles washed away. Precipitation from the 2016 event totaled 6.60 inches in 3 hours (National Oceanic and Atmospheric Administration,
Authors
Edward J. Doheny, Christopher W. Nealen
Evaluating low flow patterns, drivers and trends in the Delaware River Basin
In the humid, temperate Delaware River Basin (DRB) where water availability is generally reliable, summer low flows can cause competition between various human and ecological water uses. As temperatures continue to rise, population increases and development expands, it is critical to understand historical low flow variability to anticipate and plan for future flows. Using a sample of 325 U.S. Geol
Authors
John C. Hammond, Brandon J. Fleming
Precipitation, peak streamflow, and inundation in the Bynum Run and Winters Run watersheds in Harford County, Maryland
The Harford County Department of Public Works and the U.S. Geological Survey have been working cooperatively to monitor continuous streamflow at several streamgages in Harford County, Maryland, including Bynum Run and Winters Run. A perceived recent uptick in the number of flooding events in the Bynum Run and Winters Run watersheds have led to questions about the relative frequency and magnitude o
Authors
Christopher W. Nealen, Edward J. Doheny
Zero or not? Causes and consequences of zero-flow stream gage readings
Streamflow observations can be used to understand, predict, and contextualize hydrologic, ecological, and biogeochemical processes and conditions in streams. Stream gages are point measurements along rivers where streamflow is measured, and are often used to infer upstream watershed‐scale processes. When stream gages read zero, this may indicate that the stream has dried at this location; however,
Authors
Margaret Zimmer, Kendra E. Kaiser, Joanna Blaszczak, Samuel Zipper, John C. Hammond, Ken M. Fritz, Katie H. Costigan, Jacob D. Hosen, Sarah E Godsey, George Allen, Stephanie K. Kampf, Ryan Burrow, Corey Krabbenhoft, Walter Dodds, Rebecca Hale, Julian D. Olden, Margaret Shanafield, Amanda DelVecchia, Adam S Ward, Meryl C. Mims, Thibault Datry, Michael A. Bogan, Kate Boersma, Michelle Busch, Nathan M. Jones, Amy Burgin, Daniel Allen
Sub-annual streamflow responses to rainfall and snowmelt inputs in snow-dominated watersheds of the western U.S.
Streamflow generation in mountain watersheds is strongly influenced by snow accumulation and melt, and multiple studies have found that snow loss leads to earlier snowmelt timing and declines in annual streamflow. However, hydrologic responses to snow loss are heterogeneous, and not all areas experience streamflow declines. This research examines whether streamflow generation is different for rain
Authors
John C. Hammond, Stephanie K. Kampf
Runoff sensitivity to snow depletion curve representation within a continental scale hydrologic model
The spatial variability of snow water equivalent (SWE) can exert a strong influence on the timing and magnitude of snowmelt delivery to a watershed. Therefore, the representation of subgrid or subwatershed snow variability in hydrologic models is important for accurately simulating snowmelt dynamics and runoff response. The U.S. Geological Survey National Hydrologic Model infrastructure with the P
Authors
Graham A. Sexstone, Jessica M. Driscoll, Lauren Hay, John C. Hammond, Theodore B. Barnhart
Applying the Watershed Approach to Urban Ecosystems in Baltimore
No abstract available.
Authors
Peter Groffman, Laurence Band, Kenneth Belt, Neil Bettez, Aditi Bhaskar, Edward Doheny, Jonathan Duncan, Sujay Kaushal, Emma Rosi-Marshall, Claire Welty
Related Content
Storms and floods of July 30, 2016, and May 27, 2018, in Ellicott City, Howard County, Maryland
IntroductionOn July 30, 2016, and May 27, 2018, the downtown area of Ellicott City, Maryland (fig. 1), was severely flooded by intense, short-duration rainfall that resulted in loss of life; significant damage to buildings, roads, infrastructure; and hundreds of vehicles washed away. Precipitation from the 2016 event totaled 6.60 inches in 3 hours (National Oceanic and Atmospheric Administration,
Authors
Edward J. Doheny, Christopher W. Nealen
Evaluating low flow patterns, drivers and trends in the Delaware River Basin
In the humid, temperate Delaware River Basin (DRB) where water availability is generally reliable, summer low flows can cause competition between various human and ecological water uses. As temperatures continue to rise, population increases and development expands, it is critical to understand historical low flow variability to anticipate and plan for future flows. Using a sample of 325 U.S. Geol
Authors
John C. Hammond, Brandon J. Fleming
Precipitation, peak streamflow, and inundation in the Bynum Run and Winters Run watersheds in Harford County, Maryland
The Harford County Department of Public Works and the U.S. Geological Survey have been working cooperatively to monitor continuous streamflow at several streamgages in Harford County, Maryland, including Bynum Run and Winters Run. A perceived recent uptick in the number of flooding events in the Bynum Run and Winters Run watersheds have led to questions about the relative frequency and magnitude o
Authors
Christopher W. Nealen, Edward J. Doheny
Zero or not? Causes and consequences of zero-flow stream gage readings
Streamflow observations can be used to understand, predict, and contextualize hydrologic, ecological, and biogeochemical processes and conditions in streams. Stream gages are point measurements along rivers where streamflow is measured, and are often used to infer upstream watershed‐scale processes. When stream gages read zero, this may indicate that the stream has dried at this location; however,
Authors
Margaret Zimmer, Kendra E. Kaiser, Joanna Blaszczak, Samuel Zipper, John C. Hammond, Ken M. Fritz, Katie H. Costigan, Jacob D. Hosen, Sarah E Godsey, George Allen, Stephanie K. Kampf, Ryan Burrow, Corey Krabbenhoft, Walter Dodds, Rebecca Hale, Julian D. Olden, Margaret Shanafield, Amanda DelVecchia, Adam S Ward, Meryl C. Mims, Thibault Datry, Michael A. Bogan, Kate Boersma, Michelle Busch, Nathan M. Jones, Amy Burgin, Daniel Allen
Sub-annual streamflow responses to rainfall and snowmelt inputs in snow-dominated watersheds of the western U.S.
Streamflow generation in mountain watersheds is strongly influenced by snow accumulation and melt, and multiple studies have found that snow loss leads to earlier snowmelt timing and declines in annual streamflow. However, hydrologic responses to snow loss are heterogeneous, and not all areas experience streamflow declines. This research examines whether streamflow generation is different for rain
Authors
John C. Hammond, Stephanie K. Kampf
Runoff sensitivity to snow depletion curve representation within a continental scale hydrologic model
The spatial variability of snow water equivalent (SWE) can exert a strong influence on the timing and magnitude of snowmelt delivery to a watershed. Therefore, the representation of subgrid or subwatershed snow variability in hydrologic models is important for accurately simulating snowmelt dynamics and runoff response. The U.S. Geological Survey National Hydrologic Model infrastructure with the P
Authors
Graham A. Sexstone, Jessica M. Driscoll, Lauren Hay, John C. Hammond, Theodore B. Barnhart
Applying the Watershed Approach to Urban Ecosystems in Baltimore
No abstract available.
Authors
Peter Groffman, Laurence Band, Kenneth Belt, Neil Bettez, Aditi Bhaskar, Edward Doheny, Jonathan Duncan, Sujay Kaushal, Emma Rosi-Marshall, Claire Welty