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The International thermodynamic equation of ... - unesdoc - Unesco

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ΣΑ = Δρ/0Σ– A Summary for Policy Makers2010ΣΑ<strong>The</strong> <strong>International</strong><strong>The</strong>rmodynamicEquation <strong>of</strong> SeawaterAdvantages <strong>of</strong> TEOS-108© CSIRO<strong>The</strong> more prominent advantages <strong>of</strong> TEOS-10compared with EOS-80 are: lation<strong>of</strong> internal energy, entropy, enthalpy,potential enthalpy and the chemical potentials<strong>of</strong> seawater as well as the freezingtemperature, and the latent heats <strong>of</strong> freezingand <strong>of</strong> evaporation. <strong>The</strong>se quantities werenot available from the <strong>International</strong> Equation<strong>of</strong> State 1980 but are essential for the accurateaccounting <strong>of</strong> “heat” in the ocean andfor the consistent and accurate treatment <strong>of</strong>air-sea and ice-sea heat fluxes. For example,a new temperature variable, ConservativeTemperature, can be defined as being proportionalto potential enthalpy and is a valuablemeasure <strong>of</strong> the “heat” content per unit mass<strong>of</strong> seawater for use in physical oceanographyand in climate studies, as it is approximatelytwo orders <strong>of</strong> magnitude more conservativethan both potential temperature and entropy. varying composition <strong>of</strong> seawater can systematicallybe taken into account through theuse <strong>of</strong> Absolute Salinity. In the open ocean,this has a non-trivial effect on the horizontaldensity gradient computed from the <strong>equation</strong><strong>of</strong> state, and thereby on the ocean velocitiesand heat transports calculated via the“thermal wind” relation. the new approach are totally consistent witheach other, and can now account for propertiessuch as speed <strong>of</strong> sound and the compressibility<strong>of</strong> water with depth. measured in SI units. Moreover the treatment<strong>of</strong> freshwater fluxes in ocean models will beconsistent with the use <strong>of</strong> Absolute Salinity,but is only approximately so for PracticalSalinity. seawater supports marine physicochemicalstudies such as the solubility <strong>of</strong> sea saltconstituents, alkalinity, pH, and ocean acidificationfrom risingspheric CO 2 .concentrations <strong>of</strong> atmo-

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