On Sunday, July 16, 2023, sea surface temperatures around Florida “reached the highest levels on record,” with readings in some areas as high as 97ºF.
How out of the ordinary are such ocean temperatures? To find out, you’d need to look at sea surface temperature anomaly data, which show the difference between current temperatures and the long-term average. The easiest way to do this is to visit the State of the Ocean (SOTO) online tool.
Developed by NASA’s Physical Oceanography Distributed Active Archive Center (PO.DAAC) and powered by NASA Worldview, SOTO provides access to a broad range of satellite-derived, ocean-focused data products and facilitates scientific oceanographic, climate, and related research.
“SOTO is a web-based user interface that allows you to visualize various scientific data products, with a focus on oceanographic-related datasets,” said Frank Greguska, a PO.DAAC scientific applications software engineer and the SOTO development lead. “It allows users to get a quick look at the data very easily, while also enabling exploratory analysis.”
SOTO allows users to:
- Visualize physical oceanography data products for near real-time monitoring of critical ocean parameters and decision support
- Access a broad range of satellite-derived products of interest to the oceanographic community (i.e., productivity, salinity, sea surface height) in NASA’s Earth Observing System Data and Information System (EOSDIS) archive
- Discover and analyze oceanographic data products to enable scientific oceanographic, climate, and related research
SOTO’s visualizations of oceanographic satellite datasets center on three parameters: chlorophyll a, sea surface temperature, and sea surface temperature anomaly.
The Chlorophyll a data layer, sourced from a Level 2 product created with data from the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument aboard NASA’s Aqua and Terra satellites, provides the near-surface concentration of chlorophyll a in milligrams of chlorophyll pigment per cubic meter (mg/m3). Chlorophyll is a light-harvesting pigment found in most photosynthetic organisms; in the ocean, phytoplankton all contain the chlorophyll pigment, which has a greenish color. The concentration of chlorophyll a is used as an index of phytoplankton biomass, and because changes in the amount of phytoplankton indicate the change in productivity of the ocean, it is a useful measure for assessing ocean health. In addition, chlorophyll features can also be used to trace oceanographic currents, atmospheric jets, upwelling and downwelling, and river plumes.
SOTO’s Sea Surface Temperature (SST) and Sea Surface Temperature Anomaly layers are created with data from the Group for High Resolution Sea Surface Temperature (GHRSST) Multiscale Ultrahigh Resolution (MUR) Level 4 Global Foundation Sea Surface Temperature Analysis (v4.1) product. These layers are critical to oceanographic research as changes in sea surface temperature impact weather, oceanic and atmospheric current patterns, ocean ecology, and even life on land. Sea surface temperatures are normally warmer near the equator and cooler near the poles, but ocean currents move warm and cold water around Earth’s oceans. When these currents flow near the surface, they are typically visible in sea surface imagery when not obscured by clouds.