Titlebook: Sea Levels, Land Levels, and Tide Gauges; K. O. Emery,David G. Aubrey Book 1991 Springer-Verlag New York Inc. 1991 Coast.Ocean.Tide.enviro

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https://doi.org/10.1007/978-1-4613-9101-2Coast; Ocean; Tide; environment; global warming; sea level

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Previous Studies of Relative Sea Level from Tide Gauges,ach annual average tends to reinforce the others. Thus, a station record of many years is inherently stronger than a single radiocarbon date on organic or carbonate material that was deposited at a somewhat uncertain elevation above or below mean sea level.

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ble methods to monitor any change. During this century, and, in particular, the last three decades, tide-gauge records have been used to show these changes related to the world‘s oceans. Aubrey and Emery suggest, however, that tidal gauges should not be used unquestioningly as a benchmark for measur

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Detailed Mapping of Tide-Gauge Records in Specific Regions,er, the fall of relative sea level (rise of land) is mainly but not solely caused by removal of crustal loads by melting of glaciers. Many stations that show rise of relative sea level are at low latitudes where they probably are the result of tectonic uplift (mainly faults, folds, volcanoes) as well as rise in the ocean level.