2012 State of the Climate: Ocean Heat Content
The ocean’s ability to store and release heat over long periods of time gives it a central role in stabilizing Earth’s climate system. But when the ocean absorbs more heat than it releases, its heat content increases. Warming causes water to expand, raising global sea level. Higher water temperatures can also threaten marine ecosystems, disrupting fisheries and the people who depend upon them.
Conditions in 2012
Heat content in the upper 2,300 feet, or a little less than one-half mile, of the ocean remained near record high levels in 2012. The upper ocean held more heat than average in most of the major ocean basins visible on the map above, with the exception of the Pacific Ocean. A short-lived La Niña in early 2012 left a mark of slightly cooler upper ocean temperatures in the eastern Pacific and western Indian oceans. This was mirrored by warm temperatures in the western tropical Pacific and eastern tropical Indian Ocean.
The Pacific Ocean also experienced a cool phase of the Pacific Decadal Oscillation (PDO) pattern in 2012. The tell-tale “signal” of a negative PDO phase is a horseshoe-shaped area of cool water in the eastern North Pacific that surrounds a pocket of warm water in the central North Pacific.
Change Over Time
Increasing concentrations of greenhouse gases are preventing heat from escaping into space as freely as it used to, and most of the excess heat is being stored in the upper ocean. As a result, upper ocean heat content anomalies have continued to increase significantly over the past two decades, although at a slower rate since 2003.
G. C. Johnson, J. M. Lyman, J. K. Willis, S. Levitus, T. Boyer, J. Antonov, S. A. Good, C. M. Domingues, S. Wijffels, and N. Bindoff, 2013: [Global Oceans] Ocean Heat Content [in “State of the Climate in 2012”]. Bulletin of the American Meteorological Society (BAMS), S50-S53.