Data Collection and Processing

Stage data (gage height, in feet, referenced to the North American Vertical Datum of 1988) were collected at 15-minute intervals using various types of equipment, depending on location requirements, in accordance with USGS standards (Sauer and Turnipseed, 2010a). Discharge was routinely measured by using various types of equipment, depending on depth, velocity, and environmental conditions, in accordance with USGS standards (Sauer and Turnipseed, 2010b). Because of tidal and (or) wind effects, discharge was computed, in cubic feet per second, using the index-velocity method at most sites, in accordance with USGS techniques and methods (Levesque and Oberg, 2012). Discharge was computed using a stage-discharge relation at a few sites where tidal influence was not substantial (Rantz and others, 1982). Where applicable, discharge data were filtered by using the Godin low-pass filter to remove principal tidal frequencies from unit values (Godin, 1972). By convention, the USGS designates ebb (seaward) flow as positive flow and flood (landward) flow as negative flow. The residuals are not total freshwater flows, but instead, a combination of seaward freshwater flows from the watershed and landward saltwater flows from the marine environment, along with storm surges from hurricanes or tropical storms.

Water temperature, in degrees Celsius, and specific conductance, in microsiemens per centimeter at 25 degrees Celsius, were measured at intervals of 1 hour or less in accordance with USGS techniques and methods (Wagner and others, 2006). Water-quality meters were installed in situ at sites in freshwater environments. A pump and intake system was installed at sites in harsh saltwater environments to reduce fouling. The depth of the meter or pump intake is chosen to be representative of the channel in accordance with USGS techniques and methods (Wagner and others, 2006) but may vary between sites. This setup consisted of a meter housed inside a polyvinyl chloride chamber in a shelter. In this case, water was pumped into the chamber for 1–2 minutes before each measurement and drained from the chamber between measurements. The recording interval was reduced to one measurement per hour because of the power requirements for the pump setup. Because the chamber drains between measurements, water-quality parameters can be measured at multiple levels with one meter, if necessary. A rating table was used to convert specific conductance, in microsiemens per centimeter, to salinity, in parts per thousand (Wagner and others, 2006). Salinity was calculated for every site where water temperature and specific conductance were measured.

Missing discharge data can usually be attributed to equipment malfunction, either with the stage sensor or velocity meter (if the index-velocity method is used). For tidally filtered discharge calculation, the Godin low-pass filter requires 35 hours of continuous data before and after each data point (Godin, 1972). A data gap greater than 2 hours, therefore, results in a data gap of 3 days in the tidally filtered discharge record. For sites that include a pump setup, missing water-quality data are usually a consequence of power or pump failure, which prevents water from filling the chamber where the meter is housed. Biological fouling is a more common problem with meters installed in situ, where algal growth and crustaceans can affect the conductance measurement port or the temperature probe, both of which provide data used to calculate salinity. In either case, the affected values are not used, creating gaps in the final record.

Rainfall data for Duval, Clay, St. Johns, Putnam, and Volusia Counties in 2022 were obtained from the St. Johns River Water Management District (SJRWMD), which provides details about how average monthly rainfall data are compiled for counties in their district (SJRWMD, 2023). The period of record rainfall data to determine a long-term countywide average was compiled using National Oceanic and Atmospheric Administration (NOAA) rain gages in central and north Florida through 2009. The first 13 river miles of the St. Johns River and all monitoring sites included in this study are located within Duval County, except St. Johns River at Astor, Fla. (USGS site number 02236125, map number 12) in Volusia County, St. Johns River at Dancy Point near Spuds, Fla. (USGS site number 294213081345300, map number 10) and St. Johns River at Buffalo Bluff near Satsuma, Fla. (USGS site number 02244040, map number 11) in Putnam County, St. Johns River at Racy Point near Hastings, Fla. (USGS site number 02245290, map number 9) and St. Johns River Shands Bridge near Green Cove Springs, Fla. (USGS site number 295856081372301, map number 8) in St. Johns County, and St. Johns River above Buckman Bridge at Jacksonville, Fla. (USGS site number 301057081414800, map number 6) near the left bank in Clay County (fig. 1; table 1).

Quantile plots were created to show percentiles for annual discharge data collected at monitoring sites that have at least 10 years of record and a full contemporary year of data. The quantile plots group the annual peak discharges by water year. For this report, the 2022 water year includes data from October 1, 2021, to September 30, 2022. The resulting plots show how the 2022 water year discharge at a given site compares with that of previous water years. For discharges affected by tidal fluctuations, annual mean tidally filtered discharge was used to construct the plot.

Boxplots were created to provide a visual reference of median, interquartile range, and other useful statistics for salinity. These boxplots were constructed using all approved unit values of salinity and show salinity differences between water years.

Description of St. Johns River Main-Stem Sites

All sites on the main stem of the St. Johns River have substantive tidal influence, and therefore, the calculated discharge is tidally filtered. No changes were made to the monitoring network during this year of the study.

The farthest upstream discharge monitoring site is St. Johns River at Astor, Fla. (USGS site number 02236125, map number 12) (table 1; river mile 127). Approximately 37 mi downstream, discharge is also calculated for the monitoring site St. Johns River at Buffalo Bluff, near Satsuma, Fla. (USGS site number 02244040, map number 11) (river mile 90). Tidally filtered discharge values have been computed since 1994 at both of these sites. Water temperature and specific conductance are measured at St. Johns River at Buffalo Bluff near Satsuma, Fla. (USGS site number 02244040, map number 11) (river mile 90) at an approximate depth of 6 ft below the average high-tide level. Another water-quality monitoring site is St. Johns River at Dancy Point near Spuds, Fla. (USGS site number 294213081345300, map number 10) (river mile 71), where water temperature and specific conductance are measured at an approximate depth of 11.5 ft below the average high-tide level. Stage, water temperature, and specific conductance are monitored farther downstream near the right bank of the St. Johns River at the monitoring site Racy Point near Hastings, Fla. (USGS site number 02245290, map number 9) (river mile 64). The water-quality parameters are measured at an approximate depth of 2.5 ft below the average high-tide level. Water temperature and specific conductance are collected near the channel of the St. Johns River at the monitoring site St. Johns River Shands Bridge near Green Cove Springs, Fla. (USGS site number 295856081372301, map number 8) (river mile 50). This location was historically monitored from April 1995 to September 2001 at multiple depths and from April 2008 to September 2009 at the middle depth. The meter was reinstalled in May 2018 at the middle-depth location of 10 ft below the average high-tide level. Just downstream near the right bank, stage, water temperature, and specific conductance are measured at an approximate depth of 8.5 ft below the average high-tide level at the monitoring site St. Johns River below Shands Bridge near Green Cove Springs, Fla. (USGS site number 02245340, map number 7) (river mile 49).

A monitoring site is located near the left bank of the St. Johns River just upstream from Buckman Bridge. Water temperature and specific conductance are measured at an approximate depth of 4 ft below the average high-tide level at this site, St. Johns River above Buckman Bridge at Jacksonville, Fla. (USGS site number 301057081414800, map number 6) (river mile 35). The monitoring site St. Johns River Buckman Bridge at Jacksonville, Fla. (USGS site number 301124081395901, map number 5) (river mile 34) near the main channel measures stage, water temperature, and specific conductance. The water-quality parameters are measured with separate pump setups and intakes at two different depths to measure possible stratification. One water-quality meter is used in the chamber and monitors both water properties at each depth. All water-quality parameters are monitored at approximate depths of 8 ft (top) and 16 ft (bottom) below the average high-tide level. The water-quality monitoring sites St. Johns River at Christopher Point near Jacksonville, Fla. (USGS site number 301510081383500, map number 4) (river mile 29) and St. Johns River below Marco Lake at Jacksonville, Fla. (USGS site number 301817081393600, map number 3) (river mile 25) measure water temperature and specific conductance at an approximate depth of 4 ft below the average high-tide level for each location. These sites are characterized by relatively shallow water having an average depth of less than 6 ft and represent river conditions in seagrass beds near the shore.

The St. Johns River at Jacksonville, Fla., data collection site (USGS site number 02246500, map number 2), located near downtown Jacksonville (river mile 23), is the farthest downstream gage that calculates discharge. Stage and discharge were previously monitored before the dredging study began, but water temperature and specific conductance data collection began in October 2015 at an approximate depth of 11 ft below the average high-tide level. The monitoring equipment was moved to the center of the channel in April 2018 because of fender construction, and the intake was installed at a new depth of 17 ft below the average high-tide level. Velocity and streamflow direction data collection were added in October 2017. Tidally filtered discharge values have been computed since 1996. The monitoring site St. Johns River Dames Point Bridge at Jacksonville, Fla. (USGS site number 302309081333001, map number 1) (river mile 10) measures stage, velocity, water temperature, and specific conductance; calculation of salinity began in October 2016. All water-quality data are collected at approximate depths of 15 ft (top) and 22 ft (bottom) below the average high-tide level by using one water-quality meter and pump setup with separate intakes, similar to those used at the site St. Johns River Buckman Bridge at Jacksonville, Fla. (USGS site number 301124081395901, map number 5) to measure possible stratification. At monitoring site St. Johns River Dames Point Bridge at Jacksonville, Fla. (USGS site number 302309081333001, map number 1), the collection of stage data began in October 2017, and the collection of velocity and streamflow direction data began in May 2018.

Description of Tributary Sites

No changes to the tributary monitoring network occurred during this year of the study. A monitoring site on Julington Creek at Old St. Augustine Road near Bayard, Fla. (USGS site number 02246160, map number 25) calculates discharge 6.7 mi upstream from the confluence of Julington Creek with the St. Johns River (table 1). A nearby water-quality monitoring site measures water temperature and specific conductance at an approximate depth of 3.5 ft below the average high-tide level and is located at Julington Creek at Hood Landing near Bayard, Fla. (USGS site number 300803081354500, map number 24).

Durbin Creek near Fruit Cove, Fla. (USGS site number 022462002, map number 26) is monitored for stage, discharge, water temperature, specific conductance, and salinity 6.8 mi upstream from the confluence of Durbin Creek with the St. Johns River. The water-quality parameters are measured at an approximate depth of 3 ft below the average high-tide level. These locations are all tidally influenced, but large amounts of rainfall, resulting in increased discharge, can obscure the tidal signal.

Ortega River at Kirwin Road near Jacksonville, Fla. (USGS site number 02246318, map number 23) is monitored for stage and discharge, 11 mi upstream from the confluence of Ortega River with St. Johns River. Discharge has been computed intermittently at this location since 2002, and a stage-discharge rating was used for discharge computation during the study period, as no tidal influence is apparent in the stage data. A water-quality monitoring site, Ortega River salinity at Jacksonville, Fla. (USGS site number 301204081434900, map number 22), that measures water temperature and specific conductance at an approximate depth of 6.5 ft below the average high-tide level is located approximately 3 mi downstream from Ortega River at Kirwin Road near Jacksonville, Fla. (USGS site number 02246318, map number 23). Tidal influence is evident in the salinity data during times of low flow or increased stage in the St. Johns River.

The monitoring site at Cedar River at San Juan Avenue at Jacksonville, Fla. (USGS site number 02246459, map number 21) measures stage, water temperature, and specific conductance 1.5 mi upstream from the confluence of the Cedar and St. Johns Rivers. The water-quality parameters are monitored at an approximate depth of 6 ft below the average high-tide level. Historical tidally filtered discharge values have been computed intermittently since 2002. Wind, tide, and rainfall all substantively affect flow and salinity at Cedar River at San Juan Avenue at Jacksonville, Fla. (USGS site number 02246459, map number 21), and vertically stratified, bidirectional flow is commonly measured when strong winds occur opposite the direction of flow.

The site at Pottsburg Creek near South Jacksonville, Fla. (USGS site number 02246515, map number 20) measures stage and is 7.3 mi upstream from the confluence of Pottsburg Creek with the St. Johns River. A stage-discharge rating was used for discharge computation during the study period. The data indicate tidal influence when stage is very low in the creek and elevated in the St. Johns River, but discharge measurements confirm the validity of the stage-discharge relation. Pottsburg Creek at U.S. 90 near South Jacksonville, Fla. (USGS site number 02246518, map number 19) is monitored for stage, discharge, water temperature, specific conductance, and salinity, 5.2 mi upstream from the confluence of Pottsburg Creek with the St. Johns River. The water-quality parameters are monitored at an approximate depth of 4 ft below the average high-tide level. This location has a more pronounced tidal signal than the upstream location at Pottsburg Creek near South Jacksonville, Fla. (USGS site number 02246515, map number 20), and discharge and salinity are affected primarily by rainfall and elevated stage in the river.

The monitoring site for Trout River near Jacksonville, Fla. (USGS site number 02246621, map number 18) calculates discharge 5 mi upstream from the confluence of Trout River with the St. Johns River. Water temperature and specific conductance are measured at Trout River below U.S. 1 at Dinsmore, Fla. (USGS site number 302609081453300, map number 17) 9.3 mi upstream from the confluence of Trout River with the St. Johns River at an approximate depth of 6 ft below the average high-tide level. Broward River below Biscayne Boulevard near Jacksonville, Fla. (USGS site number 02246751, map number 16) is monitored for stage, discharge, water temperature, specific conductance, and salinity, 6.3 mi upstream from the confluence of Broward River with the St. Johns River. The water-quality parameters are monitored at an approximate depth of 4.5 ft below the average high-tide level. Discharge and salinity at these sites have a pronounced tidal signal, even when stage is elevated.

Dunn Creek at Dunn Creek Road near Eastport, Fla. (USGS site number 02246804, map number 15) is monitored for stage, discharge, water temperature, specific conductance, and salinity 5.3 mi upstream from the confluence of Dunn Creek with the St. Johns River. The monitoring sites for Clapboard Creek near Jacksonville, Fla. (USGS site number 02246825, map number 13) calculates discharge 4.5 mi upstream from the confluence of Clapboard Creek with the St. Johns River. Water temperature and specific conductance are measured at a location 0.5 mi upstream. The water-quality parameters are monitored at approximate depths of 5.5 and 6.5 ft below the average high-tide level. Discharge and salinity fluctuations at these sites are dependent on rainfall in the relatively small drainage area and on wind effects from the St. Johns River, owing to the proximity of the sites to the river and Atlantic Ocean.

Rainfall

Duval County rainfall for the 2022 water year (October 2021–September 2022) was 0.4 inch (in.) below the long-term average (SJRWMD, 2023). Monthly total rainfall ranged from 3.8 in. below average in June to 5.3 in. above average in March (fig. 3). Duval County annual rainfall ranked fifth compared to the cumulative long-term average of the five counties included in this study (SJRWMD, 2023). Annual rainfall averaged 2.5 and 2.8 in. above average for Clay and St. Johns Counties, respectively (SJRWMD, 2023). The highest monthly rainfall total for Clay County occurred in March and was 6.2 in. above average, and the highest positive monthly departure for St. Johns County, 4.8 in. above average, occurred in March. The lowest monthly rainfall totals for the two counties occurred in June and were 3.2 in. below average for Clay County and 2.8 in. below average for St. Johns County (figs. 4 and 5). Of the five counties compared for this study, Clay County ranked fourth, and St. Johns County ranked third for rainfall totals in the 2022 water year.

Rainfall totals for Putnam and Volusia Counties were 4.7 and 16.6 in. above their average yearly totals, respectively (SJRWMD, 2023). Rainfall for Putnam County ranged from 5.2 in. above average in March to 2.8 in. below average in June (fig. 6). Rainfall for Volusia County ranged from 13.9 in. above average in September to 2.2 in. below average in June (fig. 7). Of the five counties compared for this study, Putnam County ranked second, and Volusia County ranked first for rainfall totals in the 2022 water year. Rainfall for each of the five counties was below the average monthly total from January to February.

Main-Stem Sites

The parameters collected on the main stem of the St. Johns River are affected by many factors, including tidal influence, rainfall, and wind. Heavy rainfall typically increases discharge and decreases salinity, and the tidal influence introduces more fluctuations than a nontidal system. Strong northerly or easterly winds can increase salinity in the St. Johns River as ocean water with higher salinity is pushed upstream and can lower or even produce negative discharge for multiple days. When the wind calms or changes direction, discharge typically increases sharply as this ocean water and other tributary inflows exit the river.

St. Johns River at Astor, Florida—Daily tidally filtered discharge at St. Johns River at Astor, Fla. (USGS site number 02236125, map number 12) ranged from −3,350 to 6,020 cubic feet per second (ft³/s) during the 2022 water year (fig. 8), with an annual mean of 2,870 ft³/s (fig. 9). A comparison of historical annual mean tidally filtered flows indicated that 2022 streamflow was at the 52d percentile of the 28 years of record; the median tidally filtered annual mean flow for the period of record is 2,865 ft³/s (fig. 9).

St. Johns River at Buffalo Bluff near Satsuma, Florida—Daily tidally filtered discharge at St. Johns River at Buffalo Bluff near Satsuma, Fla. (USGS site number 02244040, map number 11) ranged from −21,700 to 13,900 ft³/s during the 2022 water year, with an annual mean of 4,730 ft³/s (figs. 10 and 11). Tidally filtered discharge was not computed for 5 days because of equipment malfunction. Salinity ranged from 0.3 to 0.6 parts per thousand (ppt) over this same period (fig. 12), with a median and mean of 0.4 ppt (fig. 13). A comparison of historical annual mean tidally filtered flows indicated that 2022 streamflow was at the 53d percentile of the 29 years of record; the median tidally filtered flow for the period of record is 4,670 ft³/s (fig. 11). The lowest tidally filtered discharge for the 2022 water year occurred in September from Hurricane Ian (fig. 10). The annual mean and median salinity only have a 0.2-ppt range (0.3–0.5 ppt) for each of the 6 years that salinity was calculated in the study (fig. 13).

St. Johns River at Dancy Point near Spuds, Florida—Salinity on the St. Johns River at Dancy Point near Spuds, Fla. (USGS site number 294213081345300, map number 10) ranged from 0.3 to 0.5 ppt during the 2022 water year, with a median and mean of 0.4 ppt (figs. 14 and 15). There were 3 days of missing salinity data in November and 3 days in March caused by equipment malfunction. The salinity data show fluctuations caused by tidal effects and rainfall. The annual mean and median salinity only have a 0.2-ppt range (0.3–0.5 ppt) for each of the 6 years salinity was calculated in the study (fig. 15).

St. Johns River at Racy Point near Hastings, Florida—Salinity on the St. Johns River at Racy Point near Hastings, Fla. (USGS site number 02245290, map number 9) ranged from 0.2 to 0.6 ppt during the 2022 water year, with a median and mean of 0.4 ppt (figs. 16 and 17). There were 5 days of missing salinity data in April and 6 days in August caused by equipment malfunction. The salinity at St. Johns River at Racy Point near Hastings, Fla. (USGS site number 02245290, map number 9) remained steady the entire year, with a small peak in March and June. The annual mean and median salinity only have a 0.2-ppt range (0.3–0.5 ppt) for the 5 years salinity was calculated in the study (fig. 17).

St. Johns River Shands Bridge near Green Cove Springs, Florida—Salinity on the St. Johns River Shands Bridge near Green Cove Springs, Fla. (USGS site number 295856081372301, map number 8) ranged from 0.3 to 8.9 ppt during the 2022 water year, with a median of 0.4 ppt and a mean of 0.6 ppt (figs. 18 and 19). Salinity peaked in late May when below-average rainfall occurred in St. Johns County (fig. 5). A boxplot of salinity data for the 5 years of data collection shows the highest maximum and mean salinity occurred in 2022 (fig. 19).

St. Johns River below Shands Bridge near Green Cove Springs, Florida—Salinity on the St. Johns River below Shands Bridge near Green Cove Springs, Fla. (USGS site number 02245340, map number 7) ranged from 0.4 to 6.9 ppt during the 2022 water year, with a median of 0.4 ppt and a mean of 0.6 ppt (figs. 20 and 21). Like St. Johns River Shands Bridge near Green Cove Springs, Fla. (USGS site number 295856081372301, map number 8), salinity peaked in late May when below-average rainfall occurred in St. Johns County (fig. 5). The 2022 median salinity tied for second highest among those computed for the 6 years of data collection at this site, and the 2022 mean salinity was third highest (fig. 21).

St. Johns River above Buckman Bridge at Jacksonville, Florida—Salinity on the St. Johns River above Buckman Bridge at Jacksonville, Fla. (USGS site number 301057081414800, map number 6) ranged from 0.3 to 17 ppt during the 2022 water year, with a median of 0.8 ppt and mean of 2.0 ppt (figs. 22 and 23). There were 6 days of missing salinity data in October caused by equipment malfunction. Daily maximum salinity peaked above 17 ppt in May, which is the highest value computed over the 5 years of the study. The median salinity tied for second highest and the mean salinity for 2022 ranked third highest among those computed for the 5 years of data collection, although the 2018 record is incomplete because the monitoring site was installed that year (fig. 23).

St. Johns River Buckman Bridge at Jacksonville, Florida—Salinity on the St. Johns River Buckman Bridge at Jacksonville, Fla. (USGS site number 301124081395901, map number 5) ranged from 0.3 to 24 ppt for the top location during the 2022 water year, with a median of 1.0 ppt and mean of 2.3 ppt, and from 0.3 to 25 ppt for the bottom location, with a median of 1.0 ppt and mean of 2.7 ppt (figs. 24–27). The monitoring site did not record water-quality data at the top location for 2 days in June or at the bottom location for 1 day in June because of equipment malfunction. Salinity at both locations peaked in late May when below-average rainfall occurred in Duval County (fig. 3). This was the highest maximum salinity at both locations over the 6 years of data collection at this site. The 2022 median and mean salinity at both the top and bottom locations ranked fourth highest and third highest, respectively, among those computed for the 6 years of data collection (figs. 26 and 27).

St. Johns River at Christopher Point near Jacksonville, Florida—Salinity at St. Johns River at Christopher Point near Jacksonville, Fla. (USGS site number 301510081383500, map number 4) ranged from 0.3 to 24 ppt during the 2022 water year, with a median of 2.0 ppt and mean of 3.2 ppt (figs. 28 and 29). The monitoring site did not record water-quality data for 2 days in December, 2 days in January, 5 days in February, 30 days between May and June, 6 days in July, and 4 days in September because of equipment malfunction. The annual maximum salinity occurred in May when below-average rainfall occurred in Duval County (fig. 3). The 2022 maximum salinity tied for second highest among those computed for the 7 years of data collection, and the median and mean salinity both ranked fourth highest (fig. 29).

St. Johns River below Marco Lake at Jacksonville, Florida—Salinity at St. Johns River below Marco Lake at Jacksonville, Fla. (USGS site number 301817081393600, map number 3) ranged from 0.3 to 30 ppt during the 2022 water year, with a median of 4.7 ppt and mean of 5.9 ppt (figs. 30 and 31). Salinity was not computed for 6 days between May and June and 5 days in August because of equipment malfunction. The annual maximum salinity at this site occurred in September when below-average rainfall occurred in Duval County (fig. 3). This was the second highest salinity recorded so far in the 7 years of data collection. The 2022 median and mean salinity ranked fourth highest among those computed for the 7 years of the study (fig. 31).

St. Johns River at Jacksonville, Florida—Daily tidally filtered discharge at the St. Johns River at Jacksonville, Fla. (USGS site number 02246500, map number 2) site ranged from −63,900 to 34,400 ft³/s during the 2022 water year, with an annual mean of 5,390 ft³/s (figs. 32 and 33). Salinity ranged from 0.3 to 31 ppt over this same period, with a median of 6.2 ppt and mean of 7.4 ppt (figs. 34 and 35). Salinity was not computed for 1 day in October, November, February, April, and June, 15 days between July and August, and 5 days in September because of equipment malfunction. A comparison of historical annual mean tidally filtered flows indicated that the 2022 streamflow was at the 44th percentile of the 26 years of record; the median tidally filtered flow for the period of record is 5,660 ft³/s (fig. 33). Annual mean tidally filtered streamflow record was used from 1997 onward because of data collection gaps in the historical data prior to 1997. Salinity exceeded 27 ppt and the lowest tidally filtered discharge was computed in late September because of Hurricane Ian. The 2022 mean salinity ranked fourth highest and the median salinity ranked third highest among those computed for the 7 years of data collection (fig. 33).

St. Johns River Dames Point Bridge at Jacksonville, Florida—Salinity on the St. Johns River Dames Point Bridge at Jacksonville, Fla. (USGS site number 302309081333001, map number 1) ranged from 11 to 36 ppt for the top location during the 2022 water year, with a median and mean of 23 ppt, and from 12 to 34 ppt for the bottom location, with a median of 24 ppt and mean of 23 ppt (figs. 36–39). Salinity was not computed for 4 days during November and 7 days during September because of equipment malfunction. Salinity during the year was generally lower at the top location relative to the bottom and fluctuated weekly at both locations because of upstream conditions. The 2022 mean and median salinity at the top location were the highest and tied for the highest, respectively, among those calculated for the 6 years of data collection (figs. 38 and 39). The 2022 mean and median salinity at the bottom location tied for second highest and tied for the highest, respectively, among those calculated for the 6 years of data collection (figs. 38 and 39).

Tributary Sites

The parameters measured on the tributaries of the St. Johns River are mainly affected by rainfall and at most sites by tidal fluctuations. Heavy rainfall typically increases discharge and decreases salinity, and the tidal influence introduces more daily fluctuation at tidal sites than at nontidal sites. Like the main stem, tributaries of the St. Johns River are also affected by strong easterly winds. Because of their distance from the ocean, tributary sites and main-stem sites farther upstream require prolonged or extremely strong winds, such as those from a hurricane, to experience increased salinity.

Julington Creek at Old St. Augustine Road near Bayard, Florida—Daily tidally filtered discharge at Julington Creek at Old St. Augustine Road near Bayard, Fla. (USGS site number 02246160, map number 25) ranged from −47.8 to 358 ft³/s during the 2022 water year, with an annual mean flow of 31.5 ft³/s (fig. 40). The lowest daily tidally filtered discharge in 2022 occurred in September just before Hurricane Ian. This was the lowest discharge on record at this site. Daily tidally filtered discharge was not calculated for 4 days in February because of equipment malfunction.

Julington Creek at Hood Landing near Bayard, Florida—Salinity at Julington Creek at Hood Landing near Bayard, Fla. (USGS site number 300803081354500, map number 24) ranged from 0.1 to 4.8 ppt during the 2022 water year, with a median of 0.2 ppt and mean of 0.6 ppt (figs. 41 and 42). The salinity peaked in mid-May during low flows (fig. 40) after below-average rainfall in April in Duval County (fig. 3). The 2022 median and mean salinity tied for second highest among those computed for the 7 years of data collection (fig. 42).

Durbin Creek near Fruit Cove, Florida—Daily tidally filtered discharge at Durbin Creek near Fruit Cove, Fla. (USGS site number 022462002, map number 26) ranged from −52.2 to 336 ft³/s during the 2022 water year, with an annual mean of 35.8 ft³/s (fig. 43). The lowest daily tidally filtered discharge in 2022 was the lowest on record at this site and occurred in May as a result of below-average rainfall in St. Johns County (fig. 5). Salinity ranged from 0.1 to 2.7 ppt, with a median of 0.1 ppt and mean of 0.2 ppt (figs. 44 and 45). The boxplot for Durbin Creek near Fruit Cove, Fla. (USGS site number 022462002, map number 26) salinity data in 2022 shows the same median for all 7 years of the study; the maximum salinity ranked highest among those computed for the 7 years of data collection (fig. 45). The boxplot includes no whiskers because of the low and steady salinities of freshwater flows through the creek. Salinity is missing for 7 days in October because of equipment malfunction.

Ortega River at Kirwin Road near Jacksonville, Florida—Daily discharge for Ortega River at Kirwin Road near Jacksonville, Fla. (USGS site number 02246318, map number 23) ranged from 5.88 to 726 ft³/s during the 2022 water year, with an annual mean of 54.1 ft³/s (figs. 46 and 47). The largest discharge peak at Ortega River at Kirwin Road near Jacksonville, Fla. (USGS site number 02246318, map number 23) in the 2022 water year occurred in September because of above-average rainfall in Duval County (fig. 3). The peak streamflow for the period of record ranked in the 76th percentile of the 15 years of record (fig. 47). The peak streamflow record does not include 2016, which has an incomplete record because the monitoring site was installed that year.

Ortega River salinity at Jacksonville, Florida—Salinity at the Ortega River salinity at Jacksonville, Fla. site (USGS site number 301204081434900, map number 22) ranged from 0.0 to 11 ppt during the 2022 water year, with a median of 0.1 ppt and mean of 0.4 ppt (figs. 48 and 49). Salinity was not calculated for 21 days in December because of equipment malfunction. Peak maximum daily salinity values were calculated in mid-May when below-average rainfall occurred in Duval County (fig. 3), and the St. Johns River at Jacksonville, Fla. (USGS site number 02246500, map number 2) site computed negative tidally filtered discharge (fig. 32). The 2022 maximum salinity ranked third highest among those calculated for the 7 years of data collection, and the mean salinity ranked fourth highest (fig. 49).

Cedar River at San Juan Avenue at Jacksonville, Florida—Daily tidally filtered discharge at Cedar River at San Juan Avenue at Jacksonville, Fla. (USGS site number 02246459, map number 21) ranged from −8.49 to 578 ft³/s during the 2022 water year, with an annual mean of 62.1 ft³/s (fig. 50). Salinity ranged from 0.0 to 19 ppt, with a median of 0.7 ppt and mean of 2.1 ppt (figs. 51 and 52). Salinity was not calculated for 1 day in October, 1 day in June, and 2 days in August. The peak discharge at Cedar River at San Juan Avenue at Jacksonville, Fla. (USGS site number 02246459, map number 21) for the 2022 water year occurred in March because of above-average rainfall in Duval County (fig. 3). The 2022 mean and median salinity ranked fourth highest among those computed for the 7 years of data collection (fig. 52).

Pottsburg Creek near South Jacksonville, Florida—Daily discharge for Pottsburg Creek near South Jacksonville, Fla. (USGS site number 02246515, map number 20) ranged from 0.85 to 188 ft³/s during the 2022 water year, with an annual mean flow of 17.8 ft³/s (figs. 53 and 54). Similar to Cedar River at San Juan Avenue at Jacksonville, Fla. (USGS site number 02246459, map number 21), the highest discharge during the 2022 water year was in March when Duval County had above-average rainfall (fig. 3). The peak streamflow for the period of record ranked in the 21st percentile of the 12 years of record (fig. 54).

Pottsburg Creek at U.S. 90 near South Jacksonville, Florida—Daily tidally filtered discharge at Pottsburg Creek at U.S. 90 near South Jacksonville, Fla. (USGS site number 02246518, map number 19) ranged from −0.62 to 221 ft³/s during the 2022 water year, with an annual mean flow of 35.7 ft³/s (fig. 55). The daily discharge peaked twice over 200 ft³/s in March when above-average rainfall occurred in Duval County (fig. 3). Salinity ranged from 0.1 to 14 ppt, with a median of 0.5 ppt and mean of 1.4 ppt (figs. 56 and 57). Peak salinity occurred in mid-May during periods of below-average rainfall in Duval County (fig. 3) and reverse flow in the St. Johns River at Jacksonville, Fla. (USGS site number 02246500, map number 2) (fig. 32). The 2022 median salinity tied with 2016 for the highest and the mean ranked second highest (fig. 57).

Trout River near Jacksonville, Florida—Daily tidally filtered discharge at Trout River near Jacksonville, Fla. (USGS site number 02246621, map number 18) ranged from −228 to 913 ft³/s during the 2022 water year, with an annual mean flow of 61.9 ft³/s (fig. 58). The daily discharge exceeded 600 ft³/s twice in March when above-average rainfall occurred in Duval County (fig. 3).

Trout River below U.S. 1 at Dinsmore, Florida—Salinity at Trout River below U.S. 1 at Dinsmore, Fla. (USGS site number 302609081453300, map number 17) ranged from 0.0 to 14 ppt during the 2022 water year, with a median of 0.9 ppt and mean of 2.3 ppt (figs. 59 and 60). Daily maximum salinity values peaked above 8 ppt from mid-May to the beginning of July (fig. 59). The 2022 mean salinity tied with 2020 for fourth highest among those calculated for the 7 years of data collection, and the median tied with 2017 for third highest (fig. 60).

Broward River below Biscayne Blvd. near Jacksonville, Florida—Daily tidally filtered discharge at Broward River below Biscayne Boulevard near Jacksonville, Fla. (USGS site number 02246751, map number 16) ranged from −58.1 to 261 ft³/s during the 2022 water year, with an annual mean flow of 9.13 ft³/s (fig. 61). Daily tidally filtered discharge was not calculated for 21 days from June to July because of equipment malfunction. Discharge was relatively consistent during the period, with four peaks of daily tidally filtered discharge exceeding 200 ft³/s. Salinity ranged from 0.0 to 19 ppt, with a median of 0.8 ppt and mean of 1.7 ppt (figs. 62 and 63). Peak salinity occurred in mid-May during periods of below-average rainfall in Duval County (fig. 3). This was the highest salinity recorded over the 7 years of data collection. The 2022 median salinity ranked second highest among those calculated for the 7 years of data collection, and the mean tied with 2020 for third highest (fig. 63).

Dunn Creek at Dunn Creek Road near Eastport, Florida—Daily tidally filtered discharge at Dunn Creek at Dunn Creek Road near Eastport, Fla. (USGS site number 02246804, map number 15) ranged from −6.23 to 200 ft³/s during the 2022 water year, with an annual mean of 26.8 ft³/s (fig. 64). Daily tidally filtered discharge was not calculated for 5 days in February because of equipment malfunction. The peak daily tidally filtered discharge in August was the fourth highest peak on record. Salinity during the 2022 water year ranged from 0.0 to 17 ppt, with a median of 2.4 ppt and mean of 3.2 ppt (figs. 65 and 66). The 2022 mean salinity ranked second highest among those calculated for the 7 years of data collection, and the median salinity tied with 2016 for second highest (fig. 66).

Clapboard Creek near Jacksonville, Florida—Daily tidally filtered discharge at Clapboard Creek near Jacksonville, Fla. (USGS site number 02246825, map number 13) ranged from −183 to 184 ft³/s during the 2022 water year, with an annual mean flow of 75.8 ft³/s (fig. 67). Daily tidally filtered discharge was not calculated for 14 days in July, 2 days in August, and 3 days in September because of equipment malfunctions. The lowest daily tidally filtered discharge of 2022 occurred in late September just before Hurricane Ian and was the second lowest on record. Sustained wind speeds above 30 miles per hour from the north and northeast were recorded at NOAA weather site Jacksonville Naval Air Station for 3 days before the storm, contributing to the low flow (NOAA, 2022).

Clapboard Creek above Buckhorn Bluff near Jacksonville, Florida—Salinity at Clapboard Creek above Buckhorn Bluff near Jacksonville, Fla. (USGS site number 302657081312400, map number 14) ranged from 2.6 to 31 ppt during the 2022 water year, with a median and mean of 21 ppt (figs. 68 and 69). Salinity was missing for 3 days in June because of equipment malfunction. The minimum salinity occurred in March when rainfall in Duval County was the highest monthly departure from average (fig. 3). The 2022 median salinity tied with 2017, 2019, and 2020 for second highest among those calculated for the 6 years of the study, and the mean salinity tied with 2017 and 2019 for second highest as well (fig. 69).

Discharge and Salinity Site Comparison

Analysis of the annual mean tidally filtered discharge for the 2022 water year along the main stem of the St. Johns River indicates that streamflow increased with distance downstream, as expected (fig. 70). Relative to the 2021 water year, annual mean discharge for the 2022 water year was lower at all main-stem sites. Over the 7 years considered for this study, the annual mean discharge for the 2022 water year at St. Johns River at Astor, Fla. (USGS site number 02236125, map number 12) ranked fourth highest for that site, and mean annual discharge in 2022 at St. Johns River at Buffalo Bluff near Satsuma, Fla. (USGS site number 02244040, map number 11) and Jacksonville (Acosta Bridge) both ranked fifth highest for those sites. Among the tributaries compared to one another, annual mean discharge in 2022 was highest at Clapboard Creek near Jacksonville, Fla. (USGS site number 02246825, map number 13), followed by Cedar River at San Juan Avenue at Jacksonville, Fla. (USGS site number 02246459, map number 21), Trout River near Jacksonville, Fla. (USGS site number 02246621, map number 18), Ortega River at Kirwin Road near Jacksonville, Fla. (USGS site number 02246318, map number 23), Durbin Creek near Fruit Cove, Fla. (USGS site number 022462002, map number 26), Pottsburg Creek at U.S. 90 near South Jacksonville, Fla. (USGS site number 02246518, map number 19), Julington Creek at Old St. Augustine Road near Bayard, Fla. (USGS site number 02246160, map number 25), Dunn Creek at Dunn Creek Road near Eastport, Fla. (USGS site number 02246804, map number 15), Pottsburg Creek near South Jacksonville, Fla. (USGS site number 02246515, map number 20), and Broward River below Biscayne Boulevard near Jacksonville, Fla. (USGS site number 02246751, map number 16), whose annual mean was lowest (fig. 71). Annual mean discharge at 8 of the 10 tributary monitoring sites was lower for the 2022 water year than for the 2021 water year. Furthermore, the computed annual mean flow at Broward River below Biscayne Boulevard near Jacksonville, Fla. (USGS site number 02246751, map number 16) was the lowest recorded over the 7 years of data collection (fig. 71). The countywide annual rainfall for the 2022 water year was above the average yearly rainfall in four of the five counties. It was also higher in two of the five counties for the 2022 water year relative to the 2021 water year (fig. 72).

Annual mean salinity for the main-stem sites decreased with distance upstream, which was expected (fig. 73). Of all sites in 2022, St. Johns River Dames Point Bridge at Jacksonville, Fla. (USGS site number 302309081333001, map number 1) had the highest annual mean salinities, which were 22 ppt near the surface and 23 ppt near the bottom of the water column. The 2022 annual mean salinity was higher than that of 2021 at all main-stem sites, except for St. Johns River at Buffalo Bluff near Satsuma, Fla. (USGS site number 02244040, map number 11) and St. Johns River at Dancy Point near Spuds, Fla. (USGS site number 294213081345300, map number 10), which were the same (fig. 73). The 2022 annual mean salinity at the remainder of the main-stem sites were all near the average of the 7 years of the study.

Clapboard Creek above Buckhorn Bluff near Jacksonville, Fla. (USGS site number 302657081312400, map number 14) had the highest annual mean salinity (21 ppt) of all tributaries in 2022 because of its proximity to the Atlantic Ocean. Durbin Creek near Fruit Cove, Fla. (USGS site number 022462002, map number 26) salinity (0.2 ppt) was the lowest of all monitoring locations and was slightly lower than those of Julington Creek at Hood Landing near Bayard, Fla. (USGS site number 300803081354500, map number 24) (0.6 ppt) and Ortega River salinity at Jacksonville, Fla. (USGS site number 301204081434900, map number 22) (0.4 ppt) (fig. 74). A visual comparison of annual mean salinity at tributary sites between the 2021 and 2022 water years indicates salinity was higher in 2022 at all locations (fig. 74). As with the main-stem sites, the 2022 annual mean salinity at the remainder of the tributary sites were all near the average of the 7 years of the study.