Umfang:
Online-Ressource
ISSN:
1814-9332
Inhalt:
Abstract Δ Δ n = 480) in glaciated massifs in the state, excluding areas in southern Alaska that were covered by the Cordilleran Ice Sheet. The data show a trend of increasing ELAs from the southwest to the northeast during both the LGM and the LIA, indicating a consistent southern Bering Sea and northernmost Pacific Ocean precipitation source. Our LGM–LIA Δ Δ - ± - Δ 〈 ∘ C. Our results are consistent with a growing number of local climate proxy reconstructions and global data assimilation syntheses that indicate mild summer temperature across Beringia during the LGM. Limited LGM summer temperature depressions could be explained by the influence of Northern Hemisphere ice sheets on atmospheric circulation.
In:
volume:20
In:
number:1
In:
year:2024
In:
pages:91-106
In:
extent:16
In:
Climate of the past, Katlenburg-Lindau : Copernicus Ges., 2005-, 20, Heft 1 (2024), 91-106 (gesamt 16), 1814-9332
Sprache:
Englisch
DOI:
10.5194/cp-20-91-2024
URN:
urn:nbn:de:101:1-2024011803302785596061
URL:
https://doi.org/10.5194/cp-20-91-2024
URL:
https://nbn-resolving.org/urn:nbn:de:101:1-2024011803302785596061
URL:
https://d-nb.info/1316312070/34
URL:
https://cp.copernicus.org/articles/20/91/2024/cp-20-91-2024.pdf
URL:
https://cp.copernicus.org/articles/20/91/2024/
