USGS - science for a changing world

South Atlantic Water Science Center - Georgia

 South Atlantic WSC  Georgia office  Information/data  Projects  Publications  RiverCam  Drought  Flood  About  Contact
Picture of flooding on Northside Drive at Peachtree Creek, Atlanta.



Peachtree Creek home page. Peachtree Creek home


USGS Water Science Centers are located in each state.

There is a USGS Water Science Center office in each State. Washington Oregon California Idaho Nevada Montana Wyoming Utah Colorado Arizona New Mexico North Dakota South Dakota Nebraska Kansas Oklahoma Texas Minnesota Iowa Missouri Arkansas Louisiana Wisconsin Illinois Mississippi Michigan Indiana Ohio Kentucky Tennessee Alabama Pennsylvania West Virginia Georgia Florida Caribbean Alaska Hawaii New York Vermont New Hampshire Maine Massachusetts South Carolina North Carolina Rhode Island Virginia Connecticut New Jersey Maryland-Delaware-D.C.

How much water flows during a storm?
Peachtree Creek WaterWatch

Much of the total streamflow occurs in a short period of time

As is typical of small urban streams, Peachtree Creek rises quickly and exhibits a large increase in streamflow when a major rainstorm hits the watershed. Thus, during a storm, many times more water can flow in a few hours as flows in a few days of base flow (generally periods of minimal/near minimal streamflow when no precipitation has fallen for a while). The pie charts below show that a large amount of the total streamflow occuring during a year can occur in just a few days. In 2001, for example, the 10 highest days of daily mean streamflow accounted for 36 percent of the total streamflow for the year.

Pie charts below show that a large amount of the total streamflow occuring during a year can occur in just a few days

[D] - Descriptive link of data for this chart.

If you have ever wondered how many gallons of water falls during a storm, use our interactive rainfall calculator to find out!

Case study: The storm of December 24, 2002

On Dec. 24, 2002, about two inches of rainfall fell in the Peachtree Creek watershed. This provides a good example to describe streamflow characteristics during a storm since the rain fell for only a few hours on that day and Peachtree Creek was at base-flow conditions before the rain started.

The chart below shows rainfall, in inches, during each 15-minute increment on Dec. 24th and the continuous measure of streamflow, in cubic feet per second (ft3/s).

Chart showing rainfall every 15 minutes and continuous streamflow during December 24, 2002.

A lot more water flows during a storm than during base-flow conditions

If you have ever seen pictures of Peachtree Creek during a flood, you can see that much more water is flowing than during baseflow conditions. You might be surprised at just how much more water is flowing. As the table of streamflows during the storm of Dec. 24, 2002 shows (data are rounded), streamflow during a flood can be well over 100 times more than during base flow.

Comparison of streamflow before and during the flood of Dec. 24, 2002
 Instantaneous streamflow 
TimeStream stage, in feetCubic feet per secondGallons per secondStreamflow, in gallons, during 15-minute interval

The instantaneous streamflow at 10:00 was about 154 times greater than it was at midnight. Almost 50,000 gallons of water per second was flowing during the peak streamflow period.

The instantaneous streamflow at 10:00 was about 154 times greater than it was at midnight. Almost 50,000 gallons of water per second was flowing during the peak streamflow period.

It is possible to estimate the total amount of water that flowed during Dec. 24, 2002, and compare it to a day when the streamflows are at baseflow conditions. Using the rating curve for Dec. 24th, on a day when stream stage stays at 2.81 feet, an estimated 27,800,000 gallons of water will flow by the Peachtree Creek gaging station. Using mean streamflows for each 15-minute period during the storm of Dec. 24, an estimated 4,290,000,000 gallons flowed by. That would be about 154 times more water than during a day of base flow.

Peachtree Creek is typical of urban streams

The chart of the Dec. 24th storm illustrates a number of typical patterns significant to how small urban streams react to heavy rainfall.

  • Peachtree Creek rises quickly when a heavy storm hits
    The watersheds of urban streams often have a lot of impervious areas, such as roads, parking lots, and development. In natural watersheds, more precipitation seeps into the ground, but impervious surfaces prevent this. Water falling on impervious surfaces runs off into storm sewers that empty into streams. Thus, a lot of runoff enters Peachtree Creek within minutes of a storm.
  • Streamflow quickly returns to baseflow conditions
    As the chart shows, Peachtree Creek streamflow had fallen back to near-baseflow conditions within hours of the end of the storm. In natural conditions, precipitation that seeped into the ground would be gradually released into the streambank at a much slower rate.
  • Streamflow rises faster than it falls
    The storm on Dec. 24th brought a lot of rainfall in a short period of time. The intensity and amount of rainfall caused a lot of runoff to drain into Peachtree Creek very quickly.
  • Streamflow continues to rise after rain stops
    The Peachtree Creek at Northside Drive measurement site is at a location that is a collection point for the runoff in the 86.8 square miles of watershed upstream in the Peachtree Creek watershed. It can take time for runoff miles upstream to make its way past the site.
  • The rainfall/streamflow pattern may be different for different storms
    Since the streamflow at Peachtree Creek reflects precipitation patterns in the complete Peachtree Creek watershed, rainfall that occurs only miles upstream can affect streamflow at the site. Streamflow can rise at the gaging site without any rainfall occuring at the site.
  • Base flows are lower than they used to be
    Water seeping into the stream beds from the surrounding ground is responsible for the water flowing in streams when no rainfall has occured in a while (base flow). As the amount of impervious surfaces increase in a watershed, the amount of water that infiltrates into the ground when it rains decreases, thus, there is less water in the surrounding ground to supply water for base flow.

USGS Home Water Climate Change Core Science Ecosystems Energy and Minerals Env. Health Hazards

Accessibility FOIA Privacy Policies and Notices logo U.S. Department of the Interior | U.S. Geological Survey
Page Contact Information:
Page Last Modified: Friday, 03-Oct-2014 07:24:01 EDT