Commonly-used drought indices characterize hydrological, agricultural, and meteorological conditions; however, they do not incorporate salinity, a key stressor associated with coastal drought. Salinity is a critical response variable that integrates hydrologic and coastal dynamics including sea level, tides, winds, precipitation, streamflow, and tropical storms.
In response to this need, the U.S. Geological Survey developed a Coastal Salinity Index (CSI) to characterize coastal drought, monitor changing salinity conditions, and improve our understanding of the effects of changing salinities on fresh and saltwater ecosystems, fish habitat, and freshwater availability, providing economic, human health, and environmental benefits.
What Is the Coastal Salinity index (CSI)?
The CSI is a drought index tool that uses salinity data to characterize saline (drought) and freshwater (wet) conditions in coastal surface waters.
- The CSI uses an approach similar to the Standardized Precipitation Index (SPI) to show the probability of recording a given amount of salinity.
- The CSI can be computed for multiple time intervals from 1 to 24 months to characterize short- and long-term conditions.
- The CSI does not depict hourly to daily salinity fluctuations, but the response to monthly (and longer) precipitation and streamflow conditions.
The motivation for a CSI came from the NIDIS Drought Early Warning System (DEWS) program for coastal North Carolina and South Carolina. In 2012, participants at the Coastal Carolinas DEWS Scoping Workshop recommended the development of an indicator that would be appropriate for assessing and characterizing drought conditions in coastal areas. The Coastal Salinity Index project has been supported by the National Integrated Drought Information System (NIDIS), the National Oceanic and Atmospheric Administration (NOAA), the Carolinas Integrated Sciences and Assessments program (a NOAA RISA), and the U.S. Geological Survey.