Spatial variability of δ18O during the past 1000 years in Northern Greenland
To reconstruct climate changes it is neccessary to have regionally representative data set. Stable water isotope records from the NGT cores are used to better understand the spatial variability of the climate in Northern Greenland. Questions: • How representative is a single record? • What ist the c...
Main Authors: | , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2013
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/37202/ https://epic.awi.de/id/eprint/37202/1/DACA_Poster_final.pdf https://hdl.handle.net/10013/epic.44891 https://hdl.handle.net/10013/epic.44891.d001 |
Summary: | To reconstruct climate changes it is neccessary to have regionally representative data set. Stable water isotope records from the NGT cores are used to better understand the spatial variability of the climate in Northern Greenland. Questions: • How representative is a single record? • What ist the correlation between the sites in Northern Greenland? |
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