![]() ![]() Improved estimates of upper-ocean warming and multi-decadal sea-level rise. Long-term coordinated changes in the convective activity of the North Atlantic. Church, P.L. Woodworth, T. Aarup, and W.S. ![]() 143–176 in Understanding Sea-Level Rise and Variability. Ocean temperature and salinity contributions to global and regional sea-level change. Understanding and projecting sea level change. Levitus, ed., NOAA Atlas NESDIS 66, US Government Printing Office, Washington, DC, 216 pp., DVDs.Ĭazenave, A., A. The response of the Antarctic Circumpolar Current to recent climate change. Geophysical Research Letters 30(23):2183. Recent shifts in the state of the North Pacific. Miller, eds, Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA.īond, N.A., J.E. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. In Climate Change 2007: The Physical Science Basis. Observations: Oceanic climate change and sea level. Journal of Atmospheric and Oceanic Technology. ![]() Pressure sensor drifts in Argo and their impacts. Observed temperature trends in the Indian Ocean over 1960–1999 and associated mechanisms. The article concludes with an examination of the prospects for accomplishing more global temperature and salinity observations by extending autonomous measurements into the currently poorly sampled ice-covered ocean and the half of the ocean volume below the current 2,000-dbar pressure limit of the Argo array of profiling floats.Īlory, G., S. Estimates of global sea level rise due to warming and the effects of temperature and salinity on regional sea level change patterns are discussed. After a brief introduction on the importance of the ocean in the current planetary energy imbalance and the consequences for sea level rise, this article reviews the changing mix of ocean measurements of temperature and salinity, and evolving sampling patterns since the 1950s. However, the effect on global mean sea level rise of ocean freshening by land-ice melt is overwhelmed by the effect of the addition of that melted ice to the ocean. Freshening of seawater also reduces its density, and this effect contributes to regional sea level variations. Ocean warming contributes to global mean sea level rise by reducing the density of seawater, thus increasing its volume. ![]()
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