Moisture Source Tagging Confirming the Polar Amplification Effect in Amplifying the Temperature-δ18O Temporal Slope Since the LGM
Stable water isotopologues in paleoclimate archives (δ18O) have been widely used as an indicator to derive past climate variations. The modern observed spatial δ18O-temperature relation in the middle and high latitudes has been used to infer the paleotemperatures changes from ice core data. However,...
| Main Authors: | , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2020-06-01
|
| Series: | Atmosphere |
| Subjects: | |
| Online Access: | https://www.mdpi.com/2073-4433/11/6/610 |