Detailed Information on Publication Record
2024
Rethinking the Holocene temperature conundrum
ESSELL, Helen, Jan ESPER, Heinz WANNER and Ulf BÜNTGENBasic information
Original name
Rethinking the Holocene temperature conundrum
Authors
ESSELL, Helen, Jan ESPER, Heinz WANNER and Ulf BÜNTGEN (276 Germany, guarantor, belonging to the institution)
Edition
Climate Research, Inter-Research, 2024, 0936-577X
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10509 Meteorology and atmospheric sciences
Country of publisher
Germany
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 1.100 in 2022
Organization unit
Faculty of Science
UT WoS
001204492800001
Keywords in English
Holocene climates; Temperature reconstructions; Proxy archives; Model simulations; Orbital forcing; Paleoclimate research
Tags
Tags
International impact, Reviewed
Změněno: 3/5/2024 12:54, Mgr. Marie Šípková, DiS.
Abstract
V originále
Recent scholarship argues for more research to resolve the 'Holocene temperature conundrum', an apparent discrepancy between decreasing proxy-reconstructed and increasing model-simulated long-term temperature trends during the late Holocene. Here, we argue that the observed proxy-model offset likely results from inappropriate comparisons of different seasonal and spatial signals in the reconstructed and simulated palaeo-data. Since proxy archives have been used to reconstruct global annual mean temperatures, they have been compared against model simulations of the same seasonal and spatial domains. However, we suggest that most of the proxy-based large-scale reconstructions are biased towards Northern Hemisphere summer temperatures, and as such model comparisons have predominantly focused on the wrong target data. Further to advancing our understanding of long-term temperature trends, we recommend prioritising the refinement of proxy networks and climate reconstructions to preserve the full spectrum of naturally forced, interannual to multi-millennial variations needed to contextualise recent anthropogenic changes against past Holocene ranges.