The importance of non-tidal water-level variability for reconstructing Holocene relative sea level
Salt-marsh sediment is an important geological archive for reconstructing Holocene relative sea level. The vertical uncertainty of these reconstructions is usually quantified as proportional to tidal range, resulting in a presumed primacy of microtidal regions for generating precise records. We anal...
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格式: | Article |
語言: | English |
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2024
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在線閱讀: | https://hdl.handle.net/10356/174625 |
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機構: | Nanyang Technological University |
語言: | English |
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