North Atlantic climate-ocean variations and sea level in Long Island Sound, Connecticut, since 500 cal yr A.D.
A record of detrended mean high water (MHW) variations from Hammock River marsh, Connecticut, is extended from ca. 850 to ca. 500 cal yr A.D. and correlated with summer-temperature reconstructions from northern Fennoscandia and northern Eurasia, Greenland Ice Sheet Project 2 δ
| Published in: | Quaternary Research |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
2001
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| Subjects: | |
| Online Access: | https://research.vu.nl/en/publications/3a25d96c-ccb1-485b-a22e-8318e5026a90 https://doi.org/10.1006/qres.1999.2099 |
| Summary: | A record of detrended mean high water (MHW) variations from Hammock River marsh, Connecticut, is extended from ca. 850 to ca. 500 cal yr A.D. and correlated with summer-temperature reconstructions from northern Fennoscandia and northern Eurasia, Greenland Ice Sheet Project 2 δ |
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