USGS Real Time Data Maps
The United States Geological Survey (USGS) measures streamflow conditions all over the U.S. Data is typically recorded at 5 minute intervals and transmitted to the USGS website every 30 minutes . Please see the
USGS Real Time Data Maps website for more info.
USGS Maps, Imagery and Publications
Find a variety of maps, aerial photography, satellite images, education publications and data related to water.
Please see the
USGS Maps, Imagery and Publication website.
Stream Use-Support Index
Interactive stream map – how are the streams near your home? The Stream Use Support Index (SUSI) was developed to communicate vast amounts of water quality monitoring data that is collected in Mecklenburg County. This index or score is constructed around five categories of water quality data that represent the most important pollutants and indicators of environmental health. Please see our
interactive SUSI map.
Flooding Information and Notification System
FINS is a network of more than 50 stream gages and 70 rain gages in Charlotte and Mecklenburg County. This data-collection network is cooperatively supported by Charlotte-Mecklenburg Stormwater Services and the U.S. Geological Survey Cooperative Water Program. Please see our
Report Water Pollution
Call 311 to report pollution in storm drains, streams or lakes. See our
Report a Problem webpage.
Find information about your
property in Mecklenburg County by typing in your address. Information includes water quality buffers, soil type, floodplain, impervious surface and much more. Please see
Mecklenburg County GeoPortal.
You can also find a variety of property information on Charlotte Explorer or
Charlotte-Mecklenburg Storm Water Services
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Glossary of Terms
Definitions for some technical terms used on this website.
Conductivity measures ion concentration in water that can carry electricity dependent on temperature. The standard measurement is in siemens per meter, but fresh water monitoring measures in micro-siemens per centimeter. Local geology, natural occurrences, regulated discharges, and pollution can influence conductivity. In the streams and lakes, conductivity levels remain relatively constant and range between 150-300 µS/cm depending on
Dissolved oxygen (DO) measures oxygen gas molecules in water in milligrams per liter (mg/L). The amount of DO contributes to various biological processes in waterways and can be a limiting factor for aquatic life. On average, DO ranges from 6 mg/L to 12 mg/L and can fluctuate daily. Colder, winter water holds more dissolved oxygen than warmer, summer water. Photosynthesis also drives daily DO levels.
During the day, aquatic plants produce oxygen from photosynthesis. At night, aquatic life consumes oxygen while no longer producing it, resulting in a diurnal oxygen cycle. Algal blooms alter this diurnal cycle by using more oxygen during the day than aquatic life produces, which can cause hypoxic conditions. Dissolved oxygen levels should not be below 4 mg/L which is considered hypoxic and is the North Carolina State Standard.
pH is a measurement of hydrogen ions in an aqueous solution. Values range from 0 to 14 on a unit-less scale. Solutions with a pH value below 7 are acidic, and solutions with a pH value above 7 are basic (alkaline).
Pure water is neutral with a pH of 7. In general, pH in the streams and lakes in Mecklenburg County read around 7 but can fluctuate daily and seasonally. The North Carolina State Standard for pH ranges between 6 and 9.
Water temperature changes daily and seasonally, which affects aquatic life and water chemistry. Due to water's high specific heat property, it retains heat longer than the air but also takes longer to heat up. Besides sunlight, industry and urban runoff can increase water temperatures beyond ambient levels.
Aquatic organisms have an optimal temperature range for survival as well as other biological processes, such as reproduction.
The North Carolina State Standard for temperature is 32°C (90°F) which means that the stream should not exceed this temperature anytime during the day.
Turbidity measures water clarity dependent on the amount of suspended particles. Turbidity is measured using an optical probe that shines light into the water and measures how well that light scatters in the water. Muddy and murky streams and lakes are a visual indicator of increased turbidity.
Turbid streams and lakes can be attributed to upstream construction, pollution, rain events, and other natural occurrences. For streams, the North Carolina State Standard is 50 NTU. For lakes, the North Carolina State Standard is 20 NTU.