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Matches in SemOpenAlex for { <https://semopenalex.org/work/W2012252040> ?p ?o ?g. }

• W2012252040 endingPage "734" @default.
• W2012252040 startingPage "731" @default.
• W2012252040 abstract "A multitracer study of a small aquifer in northern Switzerland indicates that the atmosphere in central Europe cooled by at least 5 degreesC during the last glacial period. The relation between oxygen isotope ratios (delta18O) and recharge temperatures reconstructed for this period is similar to the present-day one if a shift in the delta18O value of the oceans during the ice age is taken into account. This similarity suggests that the present-day delta18O-temperature relation can be used to reconstruct paleoclimate conditions in northern Switzerland. A gap in calculated groundwater age between about 17,000 and 25,000 years before the present indicates that during the last glacial maximum, local groundwater recharge was prevented by overlying glaciers." @default.
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• W2012252040 date "1998-10-23" @default.
• W2012252040 modified "2023-09-23" @default.
• W2012252040 title "Climate and Groundwater Recharge During the Last Glaciation in an Ice-Covered Region" @default.
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• W2012252040 doi "https://doi.org/10.1126/science.282.5389.731" @default.
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