Warming of the World Ocean

We quantify the interannual-to-decadal variability of the heat content (mean temperature) of the world ocean from the surface through 3000-meter depth for the period 1948 to 1998. The heat content of the world ocean increased by ∼2 × 10 23 joules between the mid-1950s and mid-1990s, representing a volume mean warming of 0.06°C. This corresponds to a warming rate of 0.3 watt per meter squared (per unit area of Earth9s surface). Substantial changes in heat content occurred in the 300- to 1000-meter layers of each ocean and in depths greater than 1000 meters of the North Atlantic. The global volume mean temperature increase for the 0- to 300-meter layer was 0.31°C, corresponding to an increase in heat content for this layer of ∼10 23 joules between the mid-1950s and mid-1990s. The Atlantic and Pacific Oceans have undergone a net warming since the 1950s and the Indian Ocean has warmed since the mid-1960s, although the warming is not monotonic.

[1]  V. Ramanathan,et al.  Aerosols, Climate, and the Hydrological Cycle , 2001, Science.

[2]  Glenn E. Shaw,et al.  Indian Ocean Experiment: An integrated analysis of the climate forcing and effects of the great Indo-Asian haze , 2001 .

[3]  A. Cazenave,et al.  Sea Level Rise During Past 40 Years Determined from Satellite and in Situ Observations , 2001, Science.

[4]  Keith W. Dixon,et al.  Anthropogenic Warming of Earth's Climate System , 2001, Science.

[5]  Gary T. Mitchum,et al.  Variations in global mean sea level associated with the 1997–1998 ENSO event: Implications for measuring long term sea level change , 1999 .

[6]  Donald J. Cavalieri,et al.  Arctic sea ice extents, areas, and trends, 1978-1996 , 1999 .

[7]  G. Schmidt,et al.  Simulation of recent northern winter climate trends by greenhouse-gas forcing , 1999, Nature.

[8]  J. Wallace,et al.  The Arctic oscillation signature in the wintertime geopotential height and temperature fields , 1998 .

[9]  Patrick Minnis,et al.  Forcings and chaos in interannual to decadal climate change , 1997 .

[10]  William K. de la Mare,et al.  Abrupt mid-twentieth-century decline in Antarctic sea-ice extent from whaling records , 1997, Nature.

[11]  S. Levitus,et al.  Climatological and interannual variability of temperature, heat storage, and rate of heat storage in the upper ocean , 1997 .

[12]  A. Kitoh,et al.  Interannual variability in the stratospheric‐tropospheric circulation in a Coupled Ocean‐Atmosphere GCM , 1996 .

[13]  Robert R. Dickson,et al.  Long-term coordinated changes in the convective activity of the North Atlantic , 1996 .

[14]  Observational evidence of interannual to decadal-scale variability of the subsurface temperature-salinity structure of the world ocean , 1995 .

[15]  S. Levitus,et al.  World Ocean Atlas 1994. Volume 5. Interannual variability of upper ocean thermal structure , 1994 .

[16]  X. Cheng,et al.  Observed correlations between winter-mean tropospheric and stratospheric circulation anomalies , 1994 .

[17]  S. Levitus Interpentadal variability of temperature and salinity in the deep North Atlantic, 1970–1974 versus 1955–1959 , 1989 .

[18]  S. Levitus Interpentadal variability of temperature and salinity at intermediate depths of the North-Atlantic O , 1989 .

[19]  T. Nitta,et al.  Recent Warming of Tropical Sea Surface Temperature and Its Relationship to the Northern Hemisphere Circulation , 1989 .

[20]  Inez Y. Fung,et al.  Global climate changes as forecast by Goddard Institute for Space Studies three‐dimensional model , 1988 .