Warmer and wetter 6000 years ago?
- Univ. of Arizona, Tucson, AZ (United States)
The author discusses recent work on thermometer systems which can be used to study past climatic temperatures. The {sup 18}O/{sup 16}O isotope ratio of marine carbonates was originally expected to provide a definitive answer following its introduction. However this ratio has been shown to be a function of temperature and the isotope ratio in seawater, which has been seen to vary on glacial time scales. Recent work to link the {sup 18}O/{sup 16}O isotope ratio with the Sr/Ca ratio measurement in corals has shown promise to factor out some of this variability. One interpretation of recent work with 6000 year corals is that sea temperatures were 1.2{degrees}C warmer, and the extratropics should have been wetter. The authors discuss other interpretations, and additional work to validate the use of these types of thermometer systems.
- OSTI ID:
- 621409
- Journal Information:
- Science, Vol. 279, Issue 5353; Other Information: PBD: 13 Feb 1998
- Country of Publication:
- United States
- Language:
- English
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