Explore general as well as scientific information about the movement, chemistry and biology of area surface and ground water environments.
The following data are summarized as seasonal average values for lake and river sampling locations located within the watershed. While these data are useful to serve as a general picture of watershed health, these data must be viewed with caution because these samples have been taken from ecologically different water resources.
Season | Total Nitrogen | Nitrate (NO3) | Total Phosphorus | Orthophosphate | Number of Sample Stations | Number of Samples |
---|---|---|---|---|---|---|
JUL-SEP 2024 | 1,827 ug/l | 1,506 ug/l | 2 | 2 | ||
APR-JUN 2024 | 3,141 ug/l | 5,405 ug/l | 2 | 2 | ||
JAN-MAR 2024 | 2,410 ug/l | 2,090 ug/l | 2 | 2 | ||
OCT-DEC 2023 | 2,147 ug/l | 942 ug/l | 5 | 5 | ||
JUL-SEP 2023 | 2,752 ug/l | 1,094 ug/l | 7 | 8 | ||
APR-JUN 2023 | 4,264 ug/l | 1,227 ug/l | 7 | 7 | ||
JAN-MAR 2023 | 2,664 ug/l | 1,933 ug/l | 7 | 9 | ||
OCT-DEC 2022 | 1,639 ug/l | 1,456 ug/l | 7 | 7 | ||
JUL-SEP 2022 | 1,514 ug/l | 1,085 ug/l | 6 | 6 | ||
APR-JUN 2022 | 2,364 ug/l | 1,888 ug/l | 5 | 5 | ||
JAN-MAR 2022 | 2,408 ug/l | 5,843 ug/l | 5 | 5 | ||
Five Year Seasonal Graph | ||||||
Five Year Graph of All Samples |
Season | Total Nitrogen | Nitrate (NO3) | Total Phosphorus | Orthophosphate | Number of Sample Stations | Number of Samples |
---|---|---|---|---|---|---|
JUL-SEP 2024 | 1,681 ug/l | 10.0 ug/l | 151 ug/l | 3 | 3 | |
APR-JUN 2024 | 1,504 ug/l | 380 ug/l | 1 | 1 | ||
JAN-MAR 2024 | 1,528 ug/l | 330 ug/l | 4 | 4 | ||
OCT-DEC 2023 | 3,059 ug/l | 636 ug/l | 19 | 19 | ||
JUL-SEP 2023 | 2,982 ug/l | 475 ug/l | 19 | 20 | ||
APR-JUN 2023 | 2,234 ug/l | 464 ug/l | 19 | 34 | ||
JAN-MAR 2023 | 2,210 ug/l | 238 ug/l | 19 | 46 | ||
OCT-DEC 2022 | 1,731 ug/l | 246 ug/l | 18 | 48 | ||
JUL-SEP 2022 | 1,632 ug/l | 218 ug/l | 22 | 44 | ||
APR-JUN 2022 | 1,900 ug/l | 243 ug/l | 22 | 41 | ||
JAN-MAR 2022 | 2,062 ug/l | 273 ug/l | 22 | 46 | ||
Five Year Seasonal Graph | ||||||
Five Year Graph of All Samples |
Southwest Florida Water Management District calculates the Aquifer Resource Indicator (ARI) for their three groundwater regions each month. The ARI was created to provide the public with a gauge of groundwater levels in their area, so they can develop an understanding of the severity and cycles of drought and recovery. The three regions include: North (Citrus, Hernando, Lake, Levy, Marion, and Sumter counties), Central (Hillsborough, Pasco, Pinellas, and Polk counties), and South (Charlotte, DeSoto, Hardee, Highlands, Manatee, and Sarasota counties). Learn More about the Aquifer Resource Indicator >>
To determine the ARI for a region, each well is compared weekly to its respective low-normal value and the difference is calculated. The weekly differences are reduced to a monthly value for all monitoring wells within a region, and the resulting ARI value represents how far water levels in the aquifer must rise or fall to reach their respective low-normal values.
Stream level and flow data for the Peace River - Lower Peace River Watershed. Learn More about Stream Flow »
River | Flows Whole River Range | Flows Data by Segment | Levels Whole River Range | Levels Data By Segment |
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Bowlegs Creek |
Average river flow is slower than it has been historically. |
Average water levels are higher than they have been historically. |
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Peace River |
Average river flow is faster than it has been historically. |
Average water levels are higher than they have been historically. |
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Peace Creek |
Average river flow is faster than it has been historically. |
Average water levels are higher than they have been historically. |
||
Saddle Creek |
Average river flow is faster than it has been historically. |
Average water levels are higher than they have been historically. |
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Whidden Creek |
NO DATA Recent river flow data is unavailable. |
|
Average water levels are higher than they have been historically. |
|
Charlie Creek |
Average river flow is slower than it has been historically. |
Average water levels are higher than they have been historically. |
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Payne Creek |
Average river flow is faster than it has been historically. |
Average water levels are higher than they have been historically. |
||
Sixmile Creek |
Average river flow is faster than it has been historically. |
Average water levels are higher than they have been historically. |
||
Little Charlie Creek |
Average river flow is faster than it has been historically. |
Average water levels are higher than they have been historically. |
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Barber Branch |
Average river flow is faster than it has been historically. |
Average water levels are higher than they have been historically. |
Source(s): Not Available
Source(s): Not Available