4/15/2024 0 Comments Density of sea water![]() Journal of Atmospheric and Oceanic Technology 25:2,091–2,095. Automated Ice-Tethered Profilers for seawater observations under pack ice in all seasons. Journal of Atmospheric and Oceanic Technology 24:1,301–1,308. Pp. 99–112 in Ocean Circulation and Climate. Upper equatorial Pacific Ocean current and salinity variability during the 1996–1998 El Niño-La Niña cycle. Journal of Geophysical Research 113, C05027. Quantifying Antarctic Bottom Water and North Atlantic Deep Water volumes. Steric sea level changes estimated from historical ocean subsurface temperature and salinity analyses. Reevaluation of historical ocean heat content variations with time-varying XBT and MBT depth bias corrections. Changes in the global hydrological‐cycle inferred from ocean salinity. Robust responses of the hydrological cycle to global warming. Journal of Physical Oceanography 37:174–187. Is the world ocean warming? Upper-ocean temperature trends: 1950–2000. ![]() Earth’s energy imbalance: Confirmation and implications. Venice, Italy, September 21–25, 2009, ESA Publication WPP-306. Proceedings of OceanObs’09: Sustained Ocean Observations and Information for Society, vol. On depth and temperature biases in bathythermograph data: Development of a new correction scheme based on analysis of a global ocean database. How much is the ocean really warming? Geophysical Research Letters 34, L01610. ![]() Eos, Transactions, American Geophysical Union 85(19):185. Argo profiling floats bring new era of in situ ocean observations. Decadal-scale temperature trends in the Southern Hemisphere ocean. Warming of the Southern Ocean since the 1950s. Bottom water warming in the North Pacific Ocean. ![]() Decadal variability of the Pacific subtropical cells and their influence on the southeast Indian Ocean. Data Analysis Methods in Physical Oceanography. Fifty-year trends in global ocean salinities and their relationship to broad-scale warming. 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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