GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE¶
Peltier. (2004). GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE: The ICE-5G (VM2) Model and GRACE. Annual Review of Earth and Planetary Sciences.
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Domain-specific¶
- Uplift
- Isostatic rebound is driven by unloading: when a mass that depressed the crust — an ice sheet, a sediment load, or eroded rock — is removed, the buoyant mantle responds by pushing the crust upward toward isostatic equilibrium; Scandinavia and Hudson Bay are rising at up to 1 cm per year as they recover from the Pleistocene ice sheets that melted between roughly 15,000 and 7,000 years ago
This sourceModels glacial isostatic adjustment as the solid Earth's response to the changing surface ice load (the ICE-5G (VM2) model).
Supported in partVerified against the publisher's abstract
“This review focuses upon the most recent advances that have been achieved in each of these areas, advances that have proven to be central to the construction of the refined model of the global process of glacial isostatic adjustment, denoted ICE-5G (VM2).”
- Isostatic rebound is driven by unloading: when a mass that depressed the crust — an ice sheet, a sediment load, or eroded rock — is removed, the buoyant mantle responds by pushing the crust upward toward isostatic equilibrium; Scandinavia and Hudson Bay are rising at up to 1 cm per year as they recover from the Pleistocene ice sheets that melted between roughly 15,000 and 7,000 years ago
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