Impact of Convective Activity on Precipitation δ 18 O in Isotope‐Enabled General Circulation Models
The δ 18 O signal preserved in paleoarchives is widely used to reconstruct past climate conditions. In many speleothems, this signal is classically interpreted via the amount effect . However, recent work has shown that precipitation δ 18 O ( ) is greatly influenced by convective processes distinct...
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Veröffentlicht in: | Journal of geophysical research. Atmospheres 2018-12, Vol.123 (23) |
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Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
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