experimental
Entry: iceberg calving induced tsunami
URI: https://registry.epos-eu.org/ncl/FAIR-Incubator/tcs-TSU/93
Iceberg calving is one of the main contributors to ice sheet mass balance and is responsible for most of the mass loss of the largest Earth's ice sheets (Antarctica, Greenland). It consists in the sudden deatchment of an iceberg from a glacier front due to a fracture. Iceberg calving can occur bith above and below sea level. Gravity and buoyancy are the main driving forces that determine the way the iceberg moves into the water and excites tsunami waves (tyically a combination of vertical movements, capsizing and overturning).
Core metadata
| is a | Concept |
| submitted by | Tendry R |
| accepted on | 11 Mar 2022 00:16:15.025 | 11 Mar 2022 00:13:52.335 |
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All metadata properties
| date accepted |
11 Mar 2022 00:16:15.025
| 11 Mar 2022 00:13:52.335
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| date submitted |
11 Mar 2022 00:08:28.292
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| definition |
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| description |
Iceberg calving is one of the main contributors to ice sheet mass balance and is responsible for most of the mass loss of the largest Earth's ice sheets (Antarctica, Greenland). It consists in the sudden deatchment of an iceberg from a glacier front due to a fracture. Iceberg calving can occur bith above and below sea level. Gravity and buoyancy are the main driving forces that determine the way the iceberg moves into the water and excites tsunami waves (tyically a combination of vertical movements, capsizing and overturning).
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| item class |
Concept
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| label |
iceberg calving induced tsunami
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| notation |
93
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| register |
tcs tSU
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| status |
status experimental
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| submitter |
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| type |
register item
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| version info |
3
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Definition
| description |
Iceberg calving is one of the main contributors to ice sheet mass balance and is responsible for most of the mass loss of the largest Earth's ice sheets (Antarctica, Greenland). It consists in the sudden deatchment of an iceberg from a glacier front due to a fracture. Iceberg calving can occur bith above and below sea level. Gravity and buoyancy are the main driving forces that determine the way the iceberg moves into the water and excites tsunami waves (tyically a combination of vertical movements, capsizing and overturning).
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| label |
iceberg calving induced tsunami
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| notation |
93
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| type |
Concept
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