Water-level conditions in southern Florida
All data presented on this site are considered to be PROVISIONAL DATA and subject to revision pending further review.
Site information from NWIS:
LOCATION.-- Lat 27° 25' 04", long 81° 12' 01", in NE 1/4 NE 1/4 SW 1/4, sec.23, T.35 S., R.31 E., Highlands County, Hydrologic Unit 03090101.
AQUIFER.-- Surficial aquifer of the Pleistocene Age, Geologic Unit 112NRSD.
WELL CHARACTERISTICS.-- Drilled, observation, water-table well, diameter 6 in., depth 16 ft, screened 13 to 16 ft.
INSTRUMENTATION.-- Satellite data collection platform.
DATUM.-- Measuring point: Top of recorder shelf, 51.12 ft above National Geodetic Vertical Datum of 1929. From February 2, 1956 to June 22, 1989, measuring point was top of casing, 51.02 ft above National Geodetic Vertical Datum of 1929
LAND-SURFACE DATUM.-- Land surface is approximately 49 ft above NGVD.
REMARKS.-- Operated by USGS Office in Orlando, FL.
Online map showing USGS_272504081120101 (through Google Maps - not a USGS site) at (27.4180946,-81.2000656).
Daily values tables - HTML tables
Daily values tables - raw retrieval
Most recent monitoring data received at H-11A:
(Recorded within last 60 days of site monitoring or during site visit within past 180 days.)
Data type Value Date Time
Computed water level elevation 44.90 21-NOV-2009 19:00:00
Online data inventory for H-11A: Data type Start End Number of records Computed water-level elevation 23-JUN-1987 20-NOV-2009 86975 Daily maximum water-level elevation 16-SEP-1975 19-NOV-2009 21296
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Continuously recorded water levels for the past 30 days are compared to daily (maximum) water levels from last year, the minimum and maximum daily levels for the corresponding weeks of the year for the site period of record, and daily levels for the 2001 drought year.
Data used to produce the current 30-day hydrograph at H-11A (272504081120101)
Description of information presented in the current 30-day hydrograph at H-11A (272504081120101)
The change in daily water-level elevations has not been mathematically correlated to time for the period of record based on operational considerations. Instead of a long-term trend line, the data are, therefore, compared to the zero-slope (flat, linear) regression curve for the existing period of record daily water-level elevations. This approximates, but may not equal, the period of record mean. (Description of statistical methods)
D
Continuously recorded water levels for the past 90 days are compared to daily (maximum) water levels from last year, the minimum and maximum daily levels for the corresponding weeks of the year for the site period of record, and daily levels for the 2001 drought year.
Data used to produce the current 90-day hydrograph at H-11A (272504081120101)
Description of information presented in the current 90-day hydrograph at H-11A (272504081120101)
The change in daily water-level elevations has not been mathematically correlated to time for the period of record based on operational considerations. Instead of a long-term trend line, the data are, therefore, compared to the zero-slope (flat, linear) regression curve for the existing period of record daily water-level elevations. This approximates, but may not equal, the period of record mean. (Description of statistical methods)
D
Daily maximum water levels for the year are compared to water levels from last year, the minimum and maximum daily levels for the corresponding weeks of the year for the site period of record, and daily levels for the 2001 drought year.
Data used to produce the current year-to-date hydrograph at H-11A (272504081120101)
Description of information presented in the current year-to-date hydrograph at H-11A (272504081120101)
The change in daily water-level elevations has not been mathematically correlated to time for the period of record based on operational considerations. Instead of a long-term trend line, the data are, therefore, compared to the zero-slope (flat, linear) regression curve for the existing period of record daily water-level elevations. This approximates, but may not equal, the period of record mean. (Description of statistical methods)
D
Long-term water-level elevation trends are estimated by statistical analysis, then water-level elevations for the past year are compared to the duration information, compensated for long-term trends, for the corresponding weeks of the year.
Data used to produce the one-year hydrograph at H-11A (272504081120101)
Description of information presented in the one-year hydrograph at H-11A (272504081120101)
The change in daily water-level elevations has not been mathematically correlated to time for the period of record based on operational considerations. Instead of a long-term trend line, the data are, therefore, compared to the zero-slope (flat, linear) regression curve for the existing period of record daily water-level elevations. This approximates, but may not equal, the period of record mean. (Description of statistical methods)
D
Water-level elevations from the past 35 years.
Data used to produce the period of record hydrograph - past 35 years at H-11A WELL NEAR LAKE PLACID, FL (USGS 272504081120101)
Description of information presented in the period of record hydrograph - past 35 years at H-11A WELL NEAR LAKE PLACID, FL (USGS 272504081120101)
The change in daily water-level elevations has not been mathematically correlated to time for the period of record based on operational considerations. Instead of a long-term trend line, the data are, therefore, compared to the zero-slope (flat, linear) regression curve for the existing period of record daily water-level elevations. This approximates, but may not equal, the period of record mean. (Description of statistical methods)
Funding for the USGS to design and maintain this site has been provided through a cooperative agreement with the South Florida Water Management District (SFWMD). Water-level conditions are monitored by the USGS with support from Federal, State, and local cooperators.