Ocean Heat Content

LATEST MEASUREMENT:
LATEST ANNUAL AVERAGE ANOMALY:
December 2020
326 (± 2) zettajoules Created with Sketch.
The zettajoule is equal to one sextillion (1021) joules, or units of heat energy. The amount of heat energy the ocean has absorbed over the past 6-plus decades is more than eight times greater than the amount of energy humans used over that time period for cooking, electricity, industry, heating, etc.

The "(±X)" figure is the “uncertainty margin,” or the range from the mean (average) within which there is a high probability that the true number resides. For example, when we say that ocean heat content for a particular year is 220 +/- 2 zettajoules, the true value for that year has a high probability of being between 218 and 222 zettajoules. The uncertainty margin exists both because of ocean heat variability (ocean heat content above the first point in the time series) and the accuracy with which we measure the individual values.
since 1955

Ninety percent of global warming is occurring in the ocean, causing the water’s internal heat to increase since modern record-keeping began in 1955, as shown in the upper chart. (The shaded blue region indicates the 95% margin of uncertainty.) This chart shows annual estimates for the first 2,000 meters of ocean depth.

Each data point in the upper chart represents a five-year average. For example, the 2018 value represents the average change in ocean heat content (since 1955) for the years 2016 to and including 2020.

The lower chart tracks monthly changes in ocean heat content for the entire water column (from the top to the bottom of the ocean) from 1992 to 2019, integrating observations from satellites, in-water instruments, and computer models.

Heat stored in the ocean causes its water to expand, which is responsible for one-third to one-half of global sea level rise. Most of the added energy is stored at the surface, at a depth of zero to 700 meters. The last 10 years were the ocean's warmest decade since at least the 1800s. The year 2020 was the ocean's warmest recorded year and saw the highest global sea level.

About the NOAA Data

About the NASA ECCO Data

Instruments That Measure Ocean Heat

Argo floats

Conductivity, Temperature, Depth (CTDs)

Expendable BathyThermographs (XBTs)

OCEAN HEAT CONTENT CHANGES SINCE 1955 (NOAA)

Data source: Observations from various ocean measurement devices, including conductivity-temperature-depth instruments (CTDs), Argo profiling floats, and eXpendable BathyThermographs (XBTs). Credit: NOAA/NCEI World Ocean Database
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OCEAN HEAT CONTENT CHANGES SINCE 1992 (NASA)

Data source: Observations from satellites and various ocean measurement devices, including conductivity-temperature-depth instruments (CTDs), Argo profiling floats, eXpendable BathyThermographs (XBTs), instrumented mooring arrays, and ice-tethered profilers (ITPs). Credit: NASA ECCO
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Fire coral bleaching Coral bleaching is a consequence of a warming ocean. This image shows bleached coral off Islamorada, Florida. Credit: Kelsey Roberts/USGS

Covering more than 70% of Earth’s surface, our global ocean has a very high heat capacity. It has absorbed 90% of the warming that has occurred in recent decades due to increasing greenhouse gases, and the top few meters of the ocean store as much heat as Earth's entire atmosphere.

The effects of ocean warming include sea level rise due to thermal expansion, coral bleaching, accelerated melting of Earth’s major ice sheets, intensified hurricanes*, and changes in ocean health and biochemistry.

*Accurate ocean heat content data add valuable information about the heat below the ocean's surface that fuels hurricanes and affects their intensity. NASA provides estimates of ocean heat content derived from the sea surface height that has been measured by satellite altimetry missions since early 1990s, including the recently launched Sentinel-6 Michael Freilich mission.