2020/01/08 by Viva F. Banzon, Thomas M. Smith, Michael Steele +2 · 1 voice · 1 citation
Earth and Planetary Sciences · #Arctic and Antarctic ice dynamics #Climate change and permafrost #Oceanographic and Atmospheric Processes
paper · doi:10.1175/jtech-d-19-0177.1
openalex publication_date 2020/01/08 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/01
Abstract Arctic sea surface temperatures (SSTs) are estimated mostly from satellite sea ice concentration (SIC) estimates. In regions with sea ice the SST is the temperature of open water or of the water under the ice. A number of different proxy SST estimates based on SIC have been developed. In recent years more Arctic quality-control buoy SSTs have become available, allowing better validation of different estimates and the development of improved proxy estimates. Here proxy SSTs from different approaches are evaluated and an improved proxy SST method is shown. The improved proxy SSTs were tested in an SST analysis, and showed reduced bias and random errors compared to the Arctic buoy SSTs. Almost all reduction in errors is in the warm melt season. In the cold season the SIC is typically high and all estimates tend to have low errors. The improved method will be incorporated into an operational SST analysis.