Detailed Information on Publication Record
2023
A frequency-optimised temperature record for the Holocene
ESSELL, Helen, Paul J KRUSIC, Jan ESPER, Sebastian WAGNER, Pascale BRACONNOT et. al.Basic information
Original name
A frequency-optimised temperature record for the Holocene
Authors
ESSELL, Helen, Paul J KRUSIC, Jan ESPER, Sebastian WAGNER, Pascale BRACONNOT, Johann JUNGCLAUS, Francesco MUSCHITIELLO, Clive OPPENHEIMER and Ulf BÜNTGEN (276 Germany, guarantor, belonging to the institution)
Edition
Environmental Research Letters, IOP Publishing Ltd, 2023, 1748-9326
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
10509 Meteorology and atmospheric sciences
Country of publisher
United Kingdom of Great Britain and Northern Ireland
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 6.700 in 2022
RIV identification code
RIV/00216224:14310/23:00132414
Organization unit
Faculty of Science
UT WoS
001087599000001
Keywords in English
climate reconstructions; global warming; Holocene climate; paleoclimate; proxy archives; temperature changes
Tags
Tags
International impact, Reviewed
Změněno: 5/12/2023 11:39, Mgr. Marie Šípková, DiS.
Abstract
V originále
Existing global mean surface temperature reconstructions for the Holocene lack high-frequency variability that is essential for contextualising recent trends and extremes in the Earth's climate system. Here, we isolate and recombine archive-specific climate signals to generate a frequency-optimised record of interannual to multi-millennial temperature changes for the past 12 000 years. Average temperatures before ∼8000 years BP and after ∼4000 years BP were 0.26 (±2.84) °C and 0.07 (±2.11) °C cooler than the long-term mean (0–12 000 years BP), while the Holocene Climate Optimum ∼7000–4000 years BP was 0.40 (±1.86) °C warmer. Biased towards Northern Hemisphere summer temperatures, our multi-proxy record captures the spectral properties of transient Earth system model simulations for the same spatial and season domain. The new frequency-optimised trajectory emphasises the importance and complex interplay of natural climate forcing factors throughout the Holocene, with an approximation of the full range of past temperature changes providing novel insights for policymakers addressing the risks of recent anthropogenic warming.