Non-eustatic sea level changes from Mediterranean tide gages
Goldsmith, V. (1990). Non-eustatic sea level changes from Mediterranean tide gages, in: Paepe, R. et al. Greenhouse Effect, Sea Level and Drought. Proceedings of the NATO Advanced Research Workshop on Geohydrological Management of Sea Level and Mitigation of Drought, Fuerteventura, Canary Islands (Spain), March 1-7, 1989. NATO ASI Series C: Mathematical and Physical Sciences, 325: pp. 145-152. http://dx.doi.org/10.1007/978-94-009-0701-0_8
In: Paepe, R. et al. (Ed.) (1990). Greenhouse Effect, Sea Level and Drought. Proceedings of the NATO Advanced Research Workshop on Geohydrological Management of Sea Level and Mitigation of Drought, Fuerteventura, Canary Islands (Spain), March 1-7, 1989. Digitized reprint of the hardcover 1st edition 1990. NATO ASI Series C: Mathematical and Physical Sciences, 325. Kluwer Academic Publishers: Dordrecht. ISBN 978-94-009-0701-0. xix, 718 pp. http://dx.doi.org/10.1007/978-94-009-0701-0, more
In: NATO ASI Series C: Mathematical and Physical Sciences. D. Reidel: Dordrecht; Boston; Lancaster. ISSN 0258-2023, more
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Document type: Conference paper
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| Abstract |
As scientists have collected data on sea level changes, more and more attention has been focused on non-eustatic effects. The Mediterranean is an excellent example of this (e.g., Pirazzoli, 1987). Two examples of non-eustatic effects revealed in recent tide gage analyses include meteorological/oceanic effects (Goldsmith and Gilboa, 1987) and local neotectonics (Emery et al., 1987). In both examples, these effects largely outweigh, and mask, eustatic effects as revealed in monthly mean sea levels determined from tide gages in the Mediterranean. Moreover, The importance, and even dominance, of the non-eustatic effects involving sea level seasonality, local tectonics, and local sea level cycles in the order of tens of years, is consistent with studies conducted in other areas. |
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