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A review of global ocean temperature observations: Implications for ocean heat content estimates and climate change

Identifieur interne : 001106 ( Istex/Corpus ); précédent : 001105; suivant : 001107

A review of global ocean temperature observations: Implications for ocean heat content estimates and climate change

Auteurs : J. P. Abraham ; M. Baringer ; N. L. Bindoff ; T. Boyer ; L. J. Cheng ; J. A. Church ; J. L. Conroy ; C. M. Domingues ; J. T. Fasullo ; J. Gilson ; G. Goni ; S. A. Good ; J. M. Gorman ; V. Gouretski ; M. Ishii ; G. C. Johnson ; S. Kizu ; J. M. Lyman ; A. M. Macdonald ; W. J. Minkowycz ; S. E. Moffitt ; M. D. Palmer ; A. R. Piola ; F. Reseghetti ; K. Schuckmann ; K. E. Trenberth ; I. Velicogna ; J. K. Willis

Source :

RBID : ISTEX:5A22EC856060E54D88C5F8B0308932272224986B

English descriptors

Abstract

The evolution of ocean temperature measurement systems is presented with a focus on the development and accuracy of two critical devices in use today (expendable bathythermographs and conductivity‐temperature‐depth instruments used on Argo floats). A detailed discussion of the accuracy of these devices and a projection of the future of ocean temperature measurements are provided. The accuracy of ocean temperature measurements is discussed in detail in the context of ocean heat content, Earth's energy imbalance, and thermosteric sea level rise. Up‐to‐date estimates are provided for these three important quantities. The total energy imbalance at the top of atmosphere is best assessed by taking an inventory of changes in energy storage. The main storage is in the ocean, the latest values of which are presented. Furthermore, despite differences in measurement methods and analysis techniques, multiple studies show that there has been a multidecadal increase in the heat content of both the upper and deep ocean regions, which reflects the impact of anthropogenic warming. With respect to sea level rise, mutually reinforcing information from tide gauges and radar altimetry shows that presently, sea level is rising at approximately 3 mm yr−1 with contributions from both thermal expansion and mass accumulation from ice melt. The latest data for thermal expansion sea level rise are included here and analyzed.

Url:
DOI: 10.1002/rog.20022

Links to Exploration step

ISTEX:5A22EC856060E54D88C5F8B0308932272224986B

Le document en format XML

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<name sortKey="Gilson, J" sort="Gilson, J" uniqKey="Gilson J" first="J." last="Gilson">J. Gilson</name>
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<mods:affiliation>Scripps Institution of Oceanography, California, La Jolla, USA</mods:affiliation>
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<name sortKey="Goni, G" sort="Goni, G" uniqKey="Goni G" first="G." last="Goni">G. Goni</name>
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<name sortKey="Good, S A" sort="Good, S A" uniqKey="Good S" first="S. A." last="Good">S. A. Good</name>
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<name sortKey="Gorman, J M" sort="Gorman, J M" uniqKey="Gorman J" first="J. M." last="Gorman">J. M. Gorman</name>
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<name sortKey="Gouretski, V" sort="Gouretski, V" uniqKey="Gouretski V" first="V." last="Gouretski">V. Gouretski</name>
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<mods:affiliation>Klima Campus, Hamburg University, Hamburg, Germany</mods:affiliation>
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<name sortKey="Ishii, M" sort="Ishii, M" uniqKey="Ishii M" first="M." last="Ishii">M. Ishii</name>
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<mods:affiliation>Climate Research Department, Meteorological Research Institute, Tsukuba, Japan</mods:affiliation>
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<name sortKey="Johnson, G C" sort="Johnson, G C" uniqKey="Johnson G" first="G. C." last="Johnson">G. C. Johnson</name>
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<name sortKey="Kizu, S" sort="Kizu, S" uniqKey="Kizu S" first="S." last="Kizu">S. Kizu</name>
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<name sortKey="Lyman, J M" sort="Lyman, J M" uniqKey="Lyman J" first="J. M." last="Lyman">J. M. Lyman</name>
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<mods:affiliation>Joint Institute for Marine and Atmospheric Research, University of Hawai'i at Manoa, Hawaii, Honolulu, USA</mods:affiliation>
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<name sortKey="Macdonald, A M" sort="Macdonald, A M" uniqKey="Macdonald A" first="A. M." last="Macdonald">A. M. Macdonald</name>
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<name sortKey="Minkowycz, W J" sort="Minkowycz, W J" uniqKey="Minkowycz W" first="W. J." last="Minkowycz">W. J. Minkowycz</name>
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<mods:affiliation>Department of Mechanical and Industrial Engineering, University of Illinois at Chicago, Illinois, Chicago, USA</mods:affiliation>
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<name sortKey="Moffitt, S E" sort="Moffitt, S E" uniqKey="Moffitt S" first="S. E." last="Moffitt">S. E. Moffitt</name>
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<mods:affiliation>Bodega Marine Laboratory, Bodega, California, USA</mods:affiliation>
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<mods:affiliation>Graduate Group in Ecology, University of California, California, Davis, USA</mods:affiliation>
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<name sortKey="Palmer, M D" sort="Palmer, M D" uniqKey="Palmer M" first="M. D." last="Palmer">M. D. Palmer</name>
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<name sortKey="Piola, A R" sort="Piola, A R" uniqKey="Piola A" first="A. R." last="Piola">A. R. Piola</name>
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<name sortKey="Reseghetti, F" sort="Reseghetti, F" uniqKey="Reseghetti F" first="F." last="Reseghetti">F. Reseghetti</name>
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<name sortKey="Schuckmann, K" sort="Schuckmann, K" uniqKey="Schuckmann K" first="K." last="Schuckmann">K. Schuckmann</name>
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<mods:affiliation>Ifremer, Toulon, France</mods:affiliation>
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<name sortKey="Trenberth, K E" sort="Trenberth, K E" uniqKey="Trenberth K" first="K. E." last="Trenberth">K. E. Trenberth</name>
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<mods:affiliation>National Center for Atmospheric Research, Colorado, Boulder, USA</mods:affiliation>
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<name sortKey="Velicogna, I" sort="Velicogna, I" uniqKey="Velicogna I" first="I." last="Velicogna">I. Velicogna</name>
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<mods:affiliation>Department of Earth System Science, University of California, Irvine, California, USA</mods:affiliation>
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<affiliation>
<mods:affiliation>Jet Propulsion Laboratory, California Institute of Technology, California, Pasadena, USA</mods:affiliation>
</affiliation>
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<name sortKey="Willis, J K" sort="Willis, J K" uniqKey="Willis J" first="J. K." last="Willis">J. K. Willis</name>
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<term>Antarctic</term>
<term>Antarctic bottom water</term>
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<term>Apparent temperature bias</term>
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<term>Argo program</term>
<term>Atmos</term>
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<term>Bias</term>
<term>Bias correction schemes</term>
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<term>Bindoff</term>
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<term>Cambridge univ</term>
<term>Clim</term>
<term>Climate change</term>
<term>Climate model simulations</term>
<term>Climate system</term>
<term>Climatological</term>
<term>Climatological reference</term>
<term>Correction</term>
<term>Corrections</term>
<term>Ctds</term>
<term>Data assembly centers</term>
<term>Data bias</term>
<term>Data center</term>
<term>Data sets</term>
<term>Database</term>
<term>Dbar</term>
<term>Decadal</term>
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<term>Deep xbts</term>
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<term>Depth corrections</term>
<term>Depth range</term>
<term>Different types</term>
<term>Domingues</term>
<term>Drop height</term>
<term>Druck</term>
<term>Dynamic model</term>
<term>Dynamic models</term>
<term>Energy imbalance</term>
<term>Enso</term>
<term>Error bars</term>
<term>Expendable</term>
<term>Expendable bathythermograph</term>
<term>Expendable bathythermographs</term>
<term>Fall rate</term>
<term>Fasullo</term>
<term>Fourth assessment report</term>
<term>Future directions</term>
<term>Geophys</term>
<term>Gilson</term>
<term>Gleckler</term>
<term>Glider</term>
<term>Global</term>
<term>Global energy</term>
<term>Global ocean</term>
<term>Global ocean heat content</term>
<term>Global temperature</term>
<term>Goni</term>
<term>Gouretski</term>
<term>Hamon</term>
<term>Hanawa</term>
<term>Heat content</term>
<term>Heat storage</term>
<term>Heat uptake</term>
<term>Hydrographic</term>
<term>Hydrographic observations</term>
<term>Imbalance</term>
<term>Instrumental biases</term>
<term>Interannual</term>
<term>Interannual variability</term>
<term>Intergovernmental panel</term>
<term>Ipcc</term>
<term>Ishii</term>
<term>Kimoto</term>
<term>Kizu</term>
<term>Lett</term>
<term>Level change</term>
<term>Level rise</term>
<term>Levitus</term>
<term>Linear trends</term>
<term>Lockheed martin sippican</term>
<term>Lyman</term>
<term>Marginal seas</term>
<term>Maximum depth</term>
<term>Mbts</term>
<term>Measure pressure</term>
<term>Mechanical bathythermograph</term>
<term>Median</term>
<term>Metadata</term>
<term>Modeling</term>
<term>Multidecadal</term>
<term>Multidecadal periods</term>
<term>Multidecadal timescales</term>
<term>Nansen</term>
<term>Nansen bottle</term>
<term>Noaa</term>
<term>Oat</term>
<term>Objective mapping</term>
<term>Observational estimates</term>
<term>Ocean</term>
<term>Ocean heat content</term>
<term>Ocean heat content estimates</term>
<term>Ocean heat uptake</term>
<term>Ocean observations</term>
<term>Ocean observations figure</term>
<term>Ocean surface</term>
<term>Ocean temperature</term>
<term>Ocean temperature measurements</term>
<term>Ocean temperatures</term>
<term>Ocean warming</term>
<term>Oceanic</term>
<term>Oceanic technol</term>
<term>Oceanogr</term>
<term>Oceanographic</term>
<term>Optimal interpolation</term>
<term>Phys</term>
<term>Physical oceanography</term>
<term>Physical science basis</term>
<term>Planetary energy imbalance</term>
<term>Planetary heat storage</term>
<term>Pressure bias</term>
<term>Pressure drift</term>
<term>Pressure sensor</term>
<term>Pressure values</term>
<term>Probe</term>
<term>Probe mass</term>
<term>Publication venice</term>
<term>Pure temperature</term>
<term>Purkey</term>
<term>Quality control</term>
<term>Reanalysis</term>
<term>Reference data</term>
<term>Reseghetti</term>
<term>Reverdin</term>
<term>Robust</term>
<term>Roemmich</term>
<term>Rossby</term>
<term>Salinity</term>
<term>Satellite altimeter</term>
<term>Satellite altimetry</term>
<term>Schuckmann</term>
<term>Sensor</term>
<term>Ship motion</term>
<term>Simple gridding</term>
<term>Solo whoi</term>
<term>Southern ocean</term>
<term>Spilhaus</term>
<term>Stammer</term>
<term>Standard errors</term>
<term>Strip chart recorders</term>
<term>Subsurface</term>
<term>Subsurface temperature</term>
<term>Surface temperature</term>
<term>Systematic errors</term>
<term>Technol</term>
<term>Technological advances</term>
<term>Temperature bias</term>
<term>Temperature drift</term>
<term>Temperature gradient</term>
<term>Temperature measurements</term>
<term>Temperature sensors</term>
<term>Thermal bias</term>
<term>Thermal energy</term>
<term>Thermal expansion</term>
<term>Thermistor</term>
<term>Thermosteric</term>
<term>Time period</term>
<term>Time series</term>
<term>Timescales</term>
<term>Tndp</term>
<term>Total bias</term>
<term>Total temperature bias</term>
<term>Transects</term>
<term>Traon</term>
<term>Trenberth</term>
<term>Unknown type</term>
<term>Upper ocean</term>
<term>Upper ocean warming</term>
<term>Variability</term>
<term>Vema channel</term>
<term>Warm bias</term>
<term>Warming</term>
<term>Warming rates</term>
<term>Water column</term>
<term>Water temperature</term>
<term>Water viscosity</term>
<term>Whoi</term>
<term>Wijffels</term>
<term>Woce</term>
<term>Wong</term>
<term>Woods hole</term>
<term>World ocean</term>
<term>World ocean circulation experiment</term>
<term>World ocean database</term>
<term>Xbts</term>
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<term>Abraham</term>
<term>Abyssal</term>
<term>Accuracy requirement</term>
<term>Altimetry</term>
<term>Anomaly</term>
<term>Antarctic</term>
<term>Antarctic bottom water</term>
<term>Anthropogenic</term>
<term>Antonov</term>
<term>Apparent temperature bias</term>
<term>Argo</term>
<term>Argo array</term>
<term>Argo data</term>
<term>Argo program</term>
<term>Atmos</term>
<term>Atmospheric research</term>
<term>Autonomous</term>
<term>Bathythermograph</term>
<term>Bias</term>
<term>Bias correction schemes</term>
<term>Bias values</term>
<term>Bindoff</term>
<term>Bottom waters</term>
<term>Boundary currents</term>
<term>Bourdon tube</term>
<term>Boyer</term>
<term>Cambridge univ</term>
<term>Clim</term>
<term>Climate change</term>
<term>Climate model simulations</term>
<term>Climate system</term>
<term>Climatological</term>
<term>Climatological reference</term>
<term>Correction</term>
<term>Corrections</term>
<term>Ctds</term>
<term>Data assembly centers</term>
<term>Data bias</term>
<term>Data center</term>
<term>Data sets</term>
<term>Database</term>
<term>Dbar</term>
<term>Decadal</term>
<term>Deep argo</term>
<term>Deep ocean</term>
<term>Deep ocean heat content</term>
<term>Deep xbts</term>
<term>Deployment</term>
<term>Depth biases</term>
<term>Depth corrections</term>
<term>Depth range</term>
<term>Different types</term>
<term>Domingues</term>
<term>Drop height</term>
<term>Druck</term>
<term>Dynamic model</term>
<term>Dynamic models</term>
<term>Energy imbalance</term>
<term>Enso</term>
<term>Error bars</term>
<term>Expendable</term>
<term>Expendable bathythermograph</term>
<term>Expendable bathythermographs</term>
<term>Fall rate</term>
<term>Fasullo</term>
<term>Fourth assessment report</term>
<term>Future directions</term>
<term>Geophys</term>
<term>Gilson</term>
<term>Gleckler</term>
<term>Glider</term>
<term>Global</term>
<term>Global energy</term>
<term>Global ocean</term>
<term>Global ocean heat content</term>
<term>Global temperature</term>
<term>Goni</term>
<term>Gouretski</term>
<term>Hamon</term>
<term>Hanawa</term>
<term>Heat content</term>
<term>Heat storage</term>
<term>Heat uptake</term>
<term>Hydrographic</term>
<term>Hydrographic observations</term>
<term>Imbalance</term>
<term>Instrumental biases</term>
<term>Interannual</term>
<term>Interannual variability</term>
<term>Intergovernmental panel</term>
<term>Ipcc</term>
<term>Ishii</term>
<term>Kimoto</term>
<term>Kizu</term>
<term>Lett</term>
<term>Level change</term>
<term>Level rise</term>
<term>Levitus</term>
<term>Linear trends</term>
<term>Lockheed martin sippican</term>
<term>Lyman</term>
<term>Marginal seas</term>
<term>Maximum depth</term>
<term>Mbts</term>
<term>Measure pressure</term>
<term>Mechanical bathythermograph</term>
<term>Median</term>
<term>Metadata</term>
<term>Modeling</term>
<term>Multidecadal</term>
<term>Multidecadal periods</term>
<term>Multidecadal timescales</term>
<term>Nansen</term>
<term>Nansen bottle</term>
<term>Noaa</term>
<term>Oat</term>
<term>Objective mapping</term>
<term>Observational estimates</term>
<term>Ocean</term>
<term>Ocean heat content</term>
<term>Ocean heat content estimates</term>
<term>Ocean heat uptake</term>
<term>Ocean observations</term>
<term>Ocean observations figure</term>
<term>Ocean surface</term>
<term>Ocean temperature</term>
<term>Ocean temperature measurements</term>
<term>Ocean temperatures</term>
<term>Ocean warming</term>
<term>Oceanic</term>
<term>Oceanic technol</term>
<term>Oceanogr</term>
<term>Oceanographic</term>
<term>Optimal interpolation</term>
<term>Phys</term>
<term>Physical oceanography</term>
<term>Physical science basis</term>
<term>Planetary energy imbalance</term>
<term>Planetary heat storage</term>
<term>Pressure bias</term>
<term>Pressure drift</term>
<term>Pressure sensor</term>
<term>Pressure values</term>
<term>Probe</term>
<term>Probe mass</term>
<term>Publication venice</term>
<term>Pure temperature</term>
<term>Purkey</term>
<term>Quality control</term>
<term>Reanalysis</term>
<term>Reference data</term>
<term>Reseghetti</term>
<term>Reverdin</term>
<term>Robust</term>
<term>Roemmich</term>
<term>Rossby</term>
<term>Salinity</term>
<term>Satellite altimeter</term>
<term>Satellite altimetry</term>
<term>Schuckmann</term>
<term>Sensor</term>
<term>Ship motion</term>
<term>Simple gridding</term>
<term>Solo whoi</term>
<term>Southern ocean</term>
<term>Spilhaus</term>
<term>Stammer</term>
<term>Standard errors</term>
<term>Strip chart recorders</term>
<term>Subsurface</term>
<term>Subsurface temperature</term>
<term>Surface temperature</term>
<term>Systematic errors</term>
<term>Technol</term>
<term>Technological advances</term>
<term>Temperature bias</term>
<term>Temperature drift</term>
<term>Temperature gradient</term>
<term>Temperature measurements</term>
<term>Temperature sensors</term>
<term>Thermal bias</term>
<term>Thermal energy</term>
<term>Thermal expansion</term>
<term>Thermistor</term>
<term>Thermosteric</term>
<term>Time period</term>
<term>Time series</term>
<term>Timescales</term>
<term>Tndp</term>
<term>Total bias</term>
<term>Total temperature bias</term>
<term>Transects</term>
<term>Traon</term>
<term>Trenberth</term>
<term>Unknown type</term>
<term>Upper ocean</term>
<term>Upper ocean warming</term>
<term>Variability</term>
<term>Vema channel</term>
<term>Warm bias</term>
<term>Warming</term>
<term>Warming rates</term>
<term>Water column</term>
<term>Water temperature</term>
<term>Water viscosity</term>
<term>Whoi</term>
<term>Wijffels</term>
<term>Woce</term>
<term>Wong</term>
<term>Woods hole</term>
<term>World ocean</term>
<term>World ocean circulation experiment</term>
<term>World ocean database</term>
<term>Xbts</term>
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<front>
<div type="abstract">The evolution of ocean temperature measurement systems is presented with a focus on the development and accuracy of two critical devices in use today (expendable bathythermographs and conductivity‐temperature‐depth instruments used on Argo floats). A detailed discussion of the accuracy of these devices and a projection of the future of ocean temperature measurements are provided. The accuracy of ocean temperature measurements is discussed in detail in the context of ocean heat content, Earth's energy imbalance, and thermosteric sea level rise. Up‐to‐date estimates are provided for these three important quantities. The total energy imbalance at the top of atmosphere is best assessed by taking an inventory of changes in energy storage. The main storage is in the ocean, the latest values of which are presented. Furthermore, despite differences in measurement methods and analysis techniques, multiple studies show that there has been a multidecadal increase in the heat content of both the upper and deep ocean regions, which reflects the impact of anthropogenic warming. With respect to sea level rise, mutually reinforcing information from tide gauges and radar altimetry shows that presently, sea level is rising at approximately 3 mm yr−1 with contributions from both thermal expansion and mass accumulation from ice melt. The latest data for thermal expansion sea level rise are included here and analyzed.</div>
</front>
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<json:string>climate variability</json:string>
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<json:string>monsoon analysis</json:string>
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<json:string>indian ocean</json:string>
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<json:string>recent discovery</json:string>
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<json:string>external bladder</json:string>
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<json:string>unsampled grid boxes</json:string>
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<json:string>total ocean volume</json:string>
<json:string>predictability project</json:string>
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<json:string>estimation approaches</json:string>
<json:string>french cruises</json:string>
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<json:string>temperature dependence</json:string>
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<json:string>least squares</json:string>
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<json:string>climatological references</json:string>
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<json:string>spatial coverage</json:string>
<json:string>year period</json:string>
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<json:string>large contribution</json:string>
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<json:string>oceanographic temperature measurements</json:string>
<json:string>oceanographic community</json:string>
<json:string>common types</json:string>
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<json:string>deep water</json:string>
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<json:string>deep ocean heat content changes</json:string>
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<author>
<json:item>
<name>J. P. Abraham</name>
<affiliations>
<json:string>School of Engineering, University of St. Thomas, Minneapolis, St. Paul, USA</json:string>
<json:string>E-mail: jpabraham@stthomas.edu</json:string>
</affiliations>
</json:item>
<json:item>
<name>M. Baringer</name>
<affiliations>
<json:string>Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration, Florida, Miami, USA</json:string>
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</json:item>
<json:item>
<name>N. L. Bindoff</name>
<affiliations>
<json:string>IMAS, University of Tasmania, Hobart, Tasmania, Australia</json:string>
<json:string>CSIRO Marine and Atmospheric Research, Centre for Australian Weather and Climate Research, Hobart, Tasmania, Australia</json:string>
<json:string>Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Tasmania, Hobart, Australia</json:string>
</affiliations>
</json:item>
<json:item>
<name>T. Boyer</name>
<affiliations>
<json:string>National Oceanographic Data Center, NOAA, Maryland, Silver Spring, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>L. J. Cheng</name>
<affiliations>
<json:string>Chinese Academy of Science, Institute of Atmospheric Physics, Bejing, China</json:string>
</affiliations>
</json:item>
<json:item>
<name>J. A. Church</name>
<affiliations>
<json:string>CSIRO Marine and Atmospheric Research, Centre for Australian Weather and Climate Research, Tasmania, Hobart, Australia</json:string>
</affiliations>
</json:item>
<json:item>
<name>J. L. Conroy</name>
<affiliations>
<json:string>School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Georgia, Atlanta, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>C. M. Domingues</name>
<affiliations>
<json:string>Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Tasmania, Hobart, Australia</json:string>
</affiliations>
</json:item>
<json:item>
<name>J. T. Fasullo</name>
<affiliations>
<json:string>National Center for Atmospheric Research, Colorado, Boulder, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>J. Gilson</name>
<affiliations>
<json:string>Scripps Institution of Oceanography, California, La Jolla, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>G. Goni</name>
<affiliations>
<json:string>Atlantic Oceanographic and Meteorological Laboratory, National Oceanic and Atmospheric Administration, Florida, Miami, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>S. A. Good</name>
<affiliations>
<json:string>Met Office Hadley Centre, Exeter, UK</json:string>
</affiliations>
</json:item>
<json:item>
<name>J. M. Gorman</name>
<affiliations>
<json:string>School of Engineering, University of St. Thomas, Minneapolis, St. Paul, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>V. Gouretski</name>
<affiliations>
<json:string>Klima Campus, Hamburg University, Hamburg, Germany</json:string>
</affiliations>
</json:item>
<json:item>
<name>M. Ishii</name>
<affiliations>
<json:string>Climate Research Department, Meteorological Research Institute, Tsukuba, Japan</json:string>
</affiliations>
</json:item>
<json:item>
<name>G. C. Johnson</name>
<affiliations>
<json:string>Pacific Marine Environmental Laboratory, NOAA, Washington, Seattle, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>S. Kizu</name>
<affiliations>
<json:string>Department of Geophysics, Tohoku University, Sendai, Japan</json:string>
</affiliations>
</json:item>
<json:item>
<name>J. M. Lyman</name>
<affiliations>
<json:string>Pacific Marine Environmental Laboratory, NOAA, Seattle, Washington, USA</json:string>
<json:string>Joint Institute for Marine and Atmospheric Research, University of Hawai'i at Manoa, Hawaii, Honolulu, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>A. M. Macdonald</name>
<affiliations>
<json:string>Woods Hole Oceanographic Institution, Massachusettes, Woods Hole, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>W. J. Minkowycz</name>
<affiliations>
<json:string>Department of Mechanical and Industrial Engineering, University of Illinois at Chicago, Illinois, Chicago, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>S. E. Moffitt</name>
<affiliations>
<json:string>Bodega Marine Laboratory, Bodega, California, USA</json:string>
<json:string>Graduate Group in Ecology, University of California, California, Davis, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>M. D. Palmer</name>
<affiliations>
<json:string>Met Office Hadley Centre, Exeter, UK</json:string>
</affiliations>
</json:item>
<json:item>
<name>A. R. Piola</name>
<affiliations>
<json:string>Departamento Oceanografia, Servicio de Hidrografia Naval and Departamento de Ciencias de la Atmosfera y los Oceanos/UMI IFAECI, Universidad de Buenos Aires, Buenos Aires, Argentina</json:string>
</affiliations>
</json:item>
<json:item>
<name>F. Reseghetti</name>
<affiliations>
<json:string>ENEA–Italian National Agency for New Technologies, Energy Sustainable Economic Development, UTMAR‐OSS, La Spezia, Italy</json:string>
</affiliations>
</json:item>
<json:item>
<name>K. Schuckmann</name>
<affiliations>
<json:string>Ifremer, Toulon, France</json:string>
</affiliations>
</json:item>
<json:item>
<name>K. E. Trenberth</name>
<affiliations>
<json:string>National Center for Atmospheric Research, Colorado, Boulder, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>I. Velicogna</name>
<affiliations>
<json:string>Department of Earth System Science, University of California, Irvine, California, USA</json:string>
<json:string>Jet Propulsion Laboratory, California Institute of Technology, California, Pasadena, USA</json:string>
</affiliations>
</json:item>
<json:item>
<name>J. K. Willis</name>
<affiliations>
<json:string>Jet Propulsion Laboratory, California Institute of Technology, California, Pasadena, USA</json:string>
</affiliations>
</json:item>
</author>
<subject>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>global warming</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>ocean heat content</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>Argo float</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>thermosteric sea level rise</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>expendable bathythermograph</value>
</json:item>
<json:item>
<lang>
<json:string>eng</json:string>
</lang>
<value>Earth energy balance</value>
</json:item>
</subject>
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<json:string>ROG20022</json:string>
</articleId>
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<json:string>eng</json:string>
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<abstract>The evolution of ocean temperature measurement systems is presented with a focus on the development and accuracy of two critical devices in use today (expendable bathythermographs and conductivity‐temperature‐depth instruments used on Argo floats). A detailed discussion of the accuracy of these devices and a projection of the future of ocean temperature measurements are provided. The accuracy of ocean temperature measurements is discussed in detail in the context of ocean heat content, Earth's energy imbalance, and thermosteric sea level rise. Up‐to‐date estimates are provided for these three important quantities. The total energy imbalance at the top of atmosphere is best assessed by taking an inventory of changes in energy storage. The main storage is in the ocean, the latest values of which are presented. Furthermore, despite differences in measurement methods and analysis techniques, multiple studies show that there has been a multidecadal increase in the heat content of both the upper and deep ocean regions, which reflects the impact of anthropogenic warming. With respect to sea level rise, mutually reinforcing information from tide gauges and radar altimetry shows that presently, sea level is rising at approximately 3 mm yr−1 with contributions from both thermal expansion and mass accumulation from ice melt. The latest data for thermal expansion sea level rise are included here and analyzed.</abstract>
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<title>A review of global ocean temperature observations: Implications for ocean heat content estimates and climate change</title>
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<json:string>article</json:string>
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<title>Reviews of Geophysics</title>
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<doi>
<json:string>10.1002/(ISSN)1944-9208</json:string>
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<issn>
<json:string>8755-1209</json:string>
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<eissn>
<json:string>1944-9208</json:string>
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<json:string>ROG</json:string>
</publisherId>
<volume>51</volume>
<issue>3</issue>
<pages>
<first>450</first>
<last>483</last>
<total>34</total>
</pages>
<genre>
<json:string>journal</json:string>
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<subject>
<json:item>
<value>GEODESY AND GRAVITY</value>
</json:item>
<json:item>
<value>Ocean monitoring with geodetic techniques</value>
</json:item>
<json:item>
<value>Global change from geodesy</value>
</json:item>
<json:item>
<value>GLOBAL CHANGE</value>
</json:item>
<json:item>
<value>Oceans</value>
</json:item>
<json:item>
<value>Sea level change</value>
</json:item>
<json:item>
<value>Climate variability</value>
</json:item>
<json:item>
<value>ATMOSPHERIC PROCESSES</value>
</json:item>
<json:item>
<value>Climate change and variability</value>
</json:item>
<json:item>
<value>Climatology</value>
</json:item>
<json:item>
<value>OCEANOGRAPHY: GENERAL</value>
</json:item>
<json:item>
<value>Ocean observing systems</value>
</json:item>
<json:item>
<value>Instruments and techniques</value>
</json:item>
<json:item>
<value>Climate and interannual variability</value>
</json:item>
<json:item>
<value>NATURAL HAZARDS</value>
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<json:item>
<value>Oceanic</value>
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<json:item>
<value>OCEANOGRAPHY: PHYSICAL</value>
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<json:item>
<value>Decadal ocean variability</value>
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<json:item>
<value>Sea level: variations and mean</value>
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<json:item>
<value>Regular Article</value>
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<json:string>I. Velicogna</json:string>
<json:string>L. Conroy</json:string>
<json:string>Martin Sippican</json:string>
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<json:string>N. Larson</json:string>
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<region>California</region>
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<orgName>Graduate Group in Ecology</orgName>
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<p>The evolution of ocean temperature measurement systems is presented with a focus on the development and accuracy of two critical devices in use today (expendable bathythermographs and conductivity‐temperature‐depth instruments used on Argo floats). A detailed discussion of the accuracy of these devices and a projection of the future of ocean temperature measurements are provided. The accuracy of ocean temperature measurements is discussed in detail in the context of ocean heat content, Earth's energy imbalance, and thermosteric sea level rise. Up‐to‐date estimates are provided for these three important quantities. The total energy imbalance at the top of atmosphere is best assessed by taking an inventory of changes in energy storage. The main storage is in the ocean, the latest values of which are presented. Furthermore, despite differences in measurement methods and analysis techniques, multiple studies show that there has been a multidecadal increase in the heat content of both the upper and deep ocean regions, which reflects the impact of anthropogenic warming. With respect to sea level rise, mutually reinforcing information from tide gauges and radar altimetry shows that presently, sea level is rising at approximately 3 mm yr
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with contributions from both thermal expansion and mass accumulation from ice melt. The latest data for thermal expansion sea level rise are included here and analyzed.</p>
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<correspondenceTo>Corresponding author: J. P. Abraham, School of Engineering, University of St. Thomas, 2115 Summit Ave., St. Paul, MN 55105‐1079, USA. (
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<p>The evolution of ocean temperature measurement systems is presented with a focus on the development and accuracy of two critical devices in use today (expendable bathythermographs and conductivity‐temperature‐depth instruments used on Argo floats). A detailed discussion of the accuracy of these devices and a projection of the future of ocean temperature measurements are provided. The accuracy of ocean temperature measurements is discussed in detail in the context of ocean heat content, Earth's energy imbalance, and thermosteric sea level rise. Up‐to‐date estimates are provided for these three important quantities. The total energy imbalance at the top of atmosphere is best assessed by taking an inventory of changes in energy storage. The main storage is in the ocean, the latest values of which are presented. Furthermore, despite differences in measurement methods and analysis techniques, multiple studies show that there has been a multidecadal increase in the heat content of both the upper and deep ocean regions, which reflects the impact of anthropogenic warming. With respect to sea level rise, mutually reinforcing information from tide gauges and radar altimetry shows that presently, sea level is rising at approximately 3 mm yr
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<affiliation>CSIRO Marine and Atmospheric Research, Centre for Australian Weather and Climate Research, Hobart, Tasmania, Australia</affiliation>
<affiliation>Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Tasmania, Hobart, Australia</affiliation>
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   |texte=   A review of global ocean temperature observations: Implications for ocean heat content estimates and climate change
}}

Wicri

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