“…In contrast, Gibbs functions take multiple values in the T -p vicinity of the saturation curve where liquid and gas coexist so that in practice two separate Gibbs functions, g W and g V , respectively, are specified for liquid and vapour. Consistent with TEOS-10, there is an equation for the Gibbs function for liquid water under oceanographic conditions (Feistel, 2003;IAPWS SR7-09, 2009), an equation for the Gibbs function for liquid water at atmospheric pressure (Pátek et al, 2009;IAPWS SR6-08, 2011) and a virial expansion of the Gibbs function for water vapour . Recently, a Gibbs function for supercooled, metastable liquid water has also been developed (IAPWS G12-15, 2015) which is not included in TEOS-10.…”