Maris Aequor
Vide etiam paginam discretivam: Planum (discretiva)
Maris aequor est limes medianae altitudinis superficiei oceani. Adhibetur autem mensurae altitudinis, quae appellari potest super maris aequor.
De vocabulis
Columella locutionem hoc sensu utitur in libris de re rusticis: "ut in solo piscinae posita libella septem pedibus sublimius esse maris aequor ostendat" et "sin autem locus ubi uiuarium constituere censemus pari libra cum aequore maris est". Alibi autem aequor "mare placidum" saepe significat; ut apud Varronem: "aequor mare appellatum, quod aequatum cum commotum vento non est".
De mutatione
Crescit et decrescit maris aequor propter rationes diversas. Liquefactio glaciariorum eam crescere facit, glaciatio decrescere. Expectatur itaque ut calefactio globalis planum marinum augeat. Breviores mutationes (semel aut bis in die) a fluxu maris efficiuntur.
Notae
Bibliographia
- Anny Cazenave et al., "The rate of sea-level rise" in Nature Climate Change (23 Martii 2014)
- Anny Cazenave et al., "Chapter 13: Sea Level Change" in Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (2013)
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