- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
Online-Ressource
- Language
-
Englisch
- Bibliographic citation
-
Modelling sea-level fingerprints of glaciated regions with low mantle viscosity ; volume:12 ; number:3 ; year:2021 ; pages:783-795 ; extent:13
Earth System Dynamics ; 12, Heft 3 (2021), 783-795 (gesamt 13)
- Creator
-
Bartholet, Alan
Milne, Glenn A.
Latychev, Konstantin
- DOI
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10.5194/esd-12-783-2021
- URN
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urn:nbn:de:101:1-2021082606411503171132
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
2025-08-14T10:56:21+0200
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Bartholet, Alan
- Milne, Glenn A.
- Latychev, Konstantin
Other Objects (12)
Modelling sea-level fingerprints of glaciated regions with low mantle viscosity
Iterative solvers for modeling mantle convection with strongly varying viscosity
Variation in bridgmanite grain size accounts for the mid-mantle viscosity jump
How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior
Automatic Identification of Fingerprint Regions for Quick and Reliable Location Estimation
Determination of a consistent viscosity distribution in the Earth's mantle beneath northern and Central Europe
Effect of bridgmanite-ferropericlase grain size evolution on Earth’s average mantle viscosity: implications for mantle convection in early and present-day Earth
Effects of water load on geophysical signals due to glacial rebound and implications for mantle viscosity
Bridging the connection between effective viscosity and electrical conductivity through water content in the upper mantle
Mathematical modelling of mantle convection at a high Rayleigh number with variable viscosity and viscous dissipation
Viscosity
Mantle
Modelling sea-level fingerprints of glaciated regions with low mantle viscosity
Iterative solvers for modeling mantle convection with strongly varying viscosity
Variation in bridgmanite grain size accounts for the mid-mantle viscosity jump
How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior
Automatic Identification of Fingerprint Regions for Quick and Reliable Location Estimation
Determination of a consistent viscosity distribution in the Earth's mantle beneath northern and Central Europe
Effect of bridgmanite-ferropericlase grain size evolution on Earth’s average mantle viscosity: implications for mantle convection in early and present-day Earth
Effects of water load on geophysical signals due to glacial rebound and implications for mantle viscosity
Bridging the connection between effective viscosity and electrical conductivity through water content in the upper mantle
Mathematical modelling of mantle convection at a high Rayleigh number with variable viscosity and viscous dissipation
Viscosity
Mantle
Modelling sea-level fingerprints of glaciated regions with low mantle viscosity
Iterative solvers for modeling mantle convection with strongly varying viscosity
Variation in bridgmanite grain size accounts for the mid-mantle viscosity jump
How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior
Automatic Identification of Fingerprint Regions for Quick and Reliable Location Estimation
Determination of a consistent viscosity distribution in the Earth's mantle beneath northern and Central Europe
Effect of bridgmanite-ferropericlase grain size evolution on Earth’s average mantle viscosity: implications for mantle convection in early and present-day Earth
Effects of water load on geophysical signals due to glacial rebound and implications for mantle viscosity
Bridging the connection between effective viscosity and electrical conductivity through water content in the upper mantle
Mathematical modelling of mantle convection at a high Rayleigh number with variable viscosity and viscous dissipation
Viscosity