Solomon Sea Ocean Transport from Gliders
The western boundary current of the South Pacific Tropical Gyre flows through the Solomon Sea and then to the equator. The degree to which this flow affects the equatorial zone and global climate depends on its transport of water and heat.
These transports have been measured since 2007 by underwater gliders crossing the Sea seasonally to monthly. Ocean temperature and salinity profiles and depth-average current are measured every few km to depths of 500 to 1000 m. Velocity shear can be inferred from measured density. Phenomena of interest are ENSO and flow in the Equatorial Undercurrent.
- Time Span
- Aug 2007 - MAY 2020
- Observations
- Temperature, Salinity, Currents
- Region
- Solomon Sea (Pacific)
- Principal Investigator
- Daniel Rudnick
- Funded by
- NOAA's GOMO Program
Science Quality Binned Project Data
Cleaned, post-processed and vertically binned to meet user needs
Project Dataset Processing
- Averaged to 10-m vertical bins
- Vertical binning improves ease of use
- The 10-m bins allow for easy integration of ADCP acoustic backscatter and velocity data
- Filtered using QC flags
- Only high-quality data are represented in each bin
How to Cite
When using this dataset, please cite the data as:
Davis, R. (2016). Solomon Sea Ocean Transport from Gliders [Data set]. Scripps Institution of Oceanography, Instrument Development Group. doi: 10.21238/S8SPRAY2718