The absence of historical sea-level data for the Pacific over the past 1,000 years hinders our understanding of late Neogene sea-level changes. Data from tectonically stable sites in various Pacific locations suggest that sea level was close to its present level around 1,000 years ago, rose to approximately 0.9 meters above present levels around 700 years ago during the Little Climatic Optimum, then fell during the Little Ice Age before gradually rising again over the past 200 years. Tags: Pacific, sea-level change, historical data, Little Climatic Optimum, Little Ice Age.
Field | Value |
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Publisher | External Partners |
Modified | 29 April 2024 |
Release Date | 14 November 2023 |
Source URL | https://www.jstor.org/stable/4298758 |
Identifier | 6dbd7cd7-82f5-473e-a384-83a73efa0d0e |
Spatial / Geographical Coverage Location | American Samoa |
Relevant Countries | American Samoa |
License |
Public
|
Contact Name | [email protected] |
POD Theme | Atmosphere and Climate, Coastal and Marine |