System Wide Monitoring Program
A primary focus of the NIWB NERR Research and Monitoring Program is participation in the National Estuarine Research Reserve’s System-Wide Monitoring Program (SWMP). SWMP is a national initiative among all NERRs, developed and initiated in 1995, that is designed to develop quantitative measurements of short-term variability and long-term changes in the water quality, biotic diversity, and land-use ⁄ land -cover characteristics of estuaries and estuarine ecosystems for the purposes of contributing to effective coastal zone management.
Long-term monitoring conducted within the national network of NERR sites is intended to improve our fundamental understanding of the temporal and spatial dynamics of estuarine ecological processes. It provides the baseline data necessary to evaluate changes in estuarine ecosystems in response to natural perturbations and anthropogenic disturbance. Continued operation of the long-term monitoring efforts within the NERRs network further provides valuable data for assessments and models on the cumulative effects of environmental stressors in estuarine ecosystems at the local, regional and national scales.
Current Components of SWMP
Meteorological monitoring under NERRS SWMP protocols began in 1997, although meteorological conditions in North Inlet were monitored by the Baruch Laboratory beginning in 1982. The principal objective of the Reserve’s long-term meteorological monitoring program is to quantify climatic changes or trends over time. Meteorological data is collected at an automated weather station located at the end of the Oyster Landing (OL) pier. Data collected at this location include: Wind speed and direction; air temperature; barometric pressure; relative humidity; rainfall; total short-wave solar radiation (280 - 2800 nm wavelengths); and photosynthetically active solar radiation (400-700 nm wavelengths). Sensors are all located on an aluminum tower at a height of approximately 3.5 meters. Sensors are connected to a data logger that records the meteorological conditions every 5 seconds continuously throughout the year, producing averages for 15 minute, hourly, and daily data. All 15 minute averages are transmitted on an hourly basis to the NOAA Geostationary Operational Environmental Satellites (GOES) to provide near real-time data accessibility.
The principal objective of the Reserve’s long-term water quality monitoring program is to quantify variability and trends over time in the physical parameters of water quality at four permanent sampling locations within the Reserve boundary. Parameters measured are: specific conductivity; salinity; dissolved oxygen; water temperature; pH; turbidity; and water level. These parameters all represent important indicators of habitat quality for numerous estuarine species. Data are collected every 15 minutes continuously throughout the year with a YSI 6600 V2 data sonde situated approximately 0.5 m above the sediment surface. The data from two locations (Oyster Landing and Debidue Creek) are transmitted on an hourly basis to the NOAA Geostationary Operational Environmental Satellites (GOES) to provide near real-time data accessibility.
The principal objective of the Reserve’s long-term monitoring of water chemistry and chlorophyll (a semi-quantitative index of phytoplankton biomass) is to quantify variability and trends over time in key chemical and biological indices of water quality at four permanent sampling locations within the Reserve boundary. Water chemistry and chlorophyll are sampled at exactly 20 day intervals, so as to minimize sampling bias with respect to spring – neap tidal periodicity over the annual cycle. On these 20 day intervals, both duplicate low tide grab sampling and diel sampling (13 samples collected at 2 hr and 4 min intervals over a full semidiurnal tidal cycle of 24h:48min) are conducted at each of the four locations. Diel sampling is accomplished through the deployment of ISCO model 3600 automated water samplers. In addition to chlorophyll, water chemistry parameters analyzed include: dissolved inorganic nutrients (NH4+, NO2-, NO3- and PO4-3); total nitrogen and total phosphorus in both the particulate and dissolved phases, which allow organic nitrogen and phosphorus fractions to be determined as the difference between total and inorganic fractions; total suspended solids, plus organic and inorganic suspended solids (determined by difference before and after combustion at 450 °C); and dissolved organic carbon. These parameters collectively provide critical information on nutrient enrichment and eutrophication in estuarine waters.
Monitoring Stations
The NIWB NERR has four long-term monitoring sites established as part of SWMP:
The Oyster Landing meteorological and water quality monitoring site is located near the western, upland edge of the North Inlet basin, at the confluence of two 1st order tidal creeks: the upper reaches of Crabhaul Creek and a much smaller un-named creek that directly drains pine forested uplands and wetlands. The sampling site is approximately 2.8 km from the terminus of Crabhaul Creek. The vegetation of the Crabhaul Creek sub-basin is dominated by Spartina alterniflora that transitions into salt pan, Juncus roemerianus and mixed vegetation communities along its upland edge. At the monitoring site the creek has an average depth of ≈ 2m at MHW and an average width of ≈ 150m at MHW. The average tidal range is ≈ 1.4 m. Salinity has ranged from 0-40, with a long-term average of 32.0. The creek bottom is comprised mostly of oyster shell hash with some fine sediment and detritus. The site is considered to represent relatively pristine conditions due to the absence of significant disturbance in its drainage area. Water quality, nutrient and chlorophyll monitoring was initiated at this site in 1993. Oyster Landing is also the site of a NOAA NOS tide gauge, established in 2001.
The Debidue Creek monitoring site is located in an ocean-dominated Spartina alterniflora marsh that forms the northern most drainage of the North Inlet basin. The monitoring site is approximately 1 km south of the DeBordieu Colony. The Colony is a large residential development, the only developed land presently in the watershed of North Inlet, which is built around wetlands, stormwater retention ponds and constructed canals that directly drain into the northern portion of Debidue Creek. The average tidal range is ≈ 2 m. Salinity has ranged from 0.8 to 38.9, with a long-term average of 32.3. The approximate depth and width of the creek at the monitoring location at MHW is 2.2 m and 70 m, respectively. The bottom is mostly comprised of oyster shell hash with some fine sediment and detritus. The site is considered impacted due to the presence of the development upstream. Water quality, nutrient and chlorophyll monitoring was initiated at this site in 1998.
The Clambank Creek monitoring site is located roughly in the center of the reserve boundary. This site is surrounded by a Spartina alterniflora marsh and does not drain a defined sub-basin of the North Inlet estuary (as is the case for Crabhaul and Debidue Creeks). It is predominantly influenced by oceanic waters due to its close proximity to North Inlet, but is occasionally influenced by water entering from Winyah Bay at the creek’s southern end. Salinity has ranged from 5.1 to 39.1, with a long-term average of 33.3. The bottom is mostly comprised of oyster shell hash and some fine sediment. Water quality, nutrient and chlorophyll monitoring was initiated at this site in 2001.
The Thousand Acre monitoring site is located ≈ 15 m from the mouth of creek that drains a tidal brackish marsh emptying into the northeastern side of the mid portion of Winyah Bay. The marsh, which is now dominated by brackish plants such as Spartina cynosuroides was formerly impounded for rice cultivation. Rice cultivation was abandoned prior to the Civil War. The upland drainage consists of undeveloped pine forest and forested wetlands. At the monitoring site, the creek depth is ≈ 2 m at MHW and creek width is ≈ 10 m. The average tidal range is ≈ 1 m. Salinity has ranged from 0 to 33.4, with a long-term average of 8.5. The bottom is mostly composed of fine sediments and detritus. The city of Georgetown, 5 km upstream from the Thousand Acre site and on the southern side of Winyah Bay, is the home to a number of heavy industries including a steel plant, paper mill, chemical plant, and a coal fired power plant. A public sewage treatment plant, which discharges into the bay, is also located in Georgetown. Water quality, nutrient and chlorophyll monitoring was initiated at this site in 1993.