
The preliminary version of NOAA's daily quarter-degree sea-surface temperature grid, available one day behind; the final version follows about two weeks later and revises the last days by a few hundredths.About two weeks after the NRT product is released, a final version becomes available. This final version incorporates additional data, including more accurate satellite retrievals and in-situ measurements from ships and buoys that arrive late. It also applies improved corrections for known biases, such as those caused by volcanic aerosols or instrument drift. The final product revises the NRT temperatures by a few hundredths of a degree Celsius—a small amount, but significant for detecting long-term climate trends. The NRT version is essential for applications that need current data, such as weather forecasting and marine navigation, while the final version is used for climate research where precision is paramount.
NOAA's operational SST analysis began in the 1980s with coarse 1-degree resolution. The current quarter-degree product, known as OISST (Optimum Interpolation Sea Surface Temperature), was introduced in the early 2000s and has been continuously updated to incorporate new satellite sensors.
The SST maps are produced by blending satellite infrared and microwave measurements with in-situ observations. Infrared sensors (like VIIRS) provide high-resolution data but are blocked by clouds, while microwave sensors (like AMSR2) can see through clouds but have coarser resolution. The data assimilation system merges these sources, along with ship and buoy measurements, using optimal interpolation to fill gaps and produce a complete, smooth field. The NRT version uses only data available within a day, while the final version waits for delayed-mode data and applies additional quality control.
The NRT SST product is used to initialize weather models, track marine heatwaves, and support fisheries management, while the final version underpins climate monitoring and studies of ocean warming trends.
The difference between the NRT and final versions, though only a few hundredths of a degree, is large enough to affect the calculation of global average temperature trends, which are measured in tenths of a degree per decade.








