Observational and energetics constraints on the non-conservation of potential/Conservative Temperature and implications for ocean modelling
• We link nonconservation of potential temperature to surface buoyancy fluxes. • We link nonconservation of potential enthalpy to work of expansion/contraction. • We show that heat nonconservation is fundamental to total energy conservation. • Simple change to OGCM sufficient to retain potential tem...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Tailleux, Rémi [verfasserIn] |
|---|
| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Umfang: |
12 |
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| Übergeordnetes Werk: |
Enthalten in: Laser sharpening evaluation of diamond wheels based on 3D recognition - Zhou, Wei ELSEVIER, 2022, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:88 ; year:2015 ; pages:26-37 ; extent:12 |
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10.1016/j.ocemod.2015.02.001 |
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| 520 | |a • We link nonconservation of potential temperature to surface buoyancy fluxes. • We link nonconservation of potential enthalpy to work of expansion/contraction. • We show that heat nonconservation is fundamental to total energy conservation. • Simple change to OGCM sufficient to retain potential temperature nonconservation. • Potential viable alternative to switching from potential to Conservative Temperature. | ||
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Observational and energetics constraints on the non-conservation of potential/Conservative Temperature and implications for ocean modelling |
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• We link nonconservation of potential temperature to surface buoyancy fluxes. • We link nonconservation of potential enthalpy to work of expansion/contraction. • We show that heat nonconservation is fundamental to total energy conservation. • Simple change to OGCM sufficient to retain potential temperature nonconservation. • Potential viable alternative to switching from potential to Conservative Temperature. |
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• We link nonconservation of potential temperature to surface buoyancy fluxes. • We link nonconservation of potential enthalpy to work of expansion/contraction. • We show that heat nonconservation is fundamental to total energy conservation. • Simple change to OGCM sufficient to retain potential temperature nonconservation. • Potential viable alternative to switching from potential to Conservative Temperature. |
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• We link nonconservation of potential temperature to surface buoyancy fluxes. • We link nonconservation of potential enthalpy to work of expansion/contraction. • We show that heat nonconservation is fundamental to total energy conservation. • Simple change to OGCM sufficient to retain potential temperature nonconservation. • Potential viable alternative to switching from potential to Conservative Temperature. |
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Observational and energetics constraints on the non-conservation of potential/Conservative Temperature and implications for ocean modelling |
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