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- W3109236862 abstract "Oxygen-isotope records offer an alternative way to quantitatively reconstruct paleoclimate, which, at first view, is independent of an ecosystem’s reaction to climate change. The ice core records from high latitude inland ice, where the former precipitation and its isotopic composition (δ18OP) are preserved in an almost original state, are widely accepted as valuable sources of paleoclimate information. Worldwide systematic observation of δ18OP (Rozanski et al. 1992), starting in the late sixties, together with the incorporation of the water isotopes in several generations of general circulation models (Hoffmann et al. 1998; Jouzel et al. 1987) and models of intermediate complexity have, not only increased the confidence in δ18OP as a powerful paleotemperature indicator in a number of key regions, but have also demonstrated its importance as a primary hydrometeorological parameter in regions where temperature dependence is less evident or absent." @default.
- W3109236862 created "2020-12-07" @default.
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- W3109236862 date "2020-11-08" @default.
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- W3109236862 title "Air-Interface: δ18O Records of Past Meteoric Water Using Benthic Ostracods from Deep Lakes" @default.
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- W3109236862 doi "https://doi.org/10.1007/978-3-030-24982-3_15" @default.
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