Articles | Volume 18, issue 12
https://doi.org/10.5194/cp-18-2599-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-18-2599-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
15 Dec 2022
Research article | Highlight paper |
| 15 Dec 2022
| 15 Dec 2022
Reconstructing Holocene temperatures in time and space using paleoclimate data assimilation
School of Earth and Sustainability, Northern Arizona University,
Flagstaff, AZ, USA
Nicholas P. McKay
School of Earth and Sustainability, Northern Arizona University,
Flagstaff, AZ, USA
Nathan Steiger
Lamont-Doherty Earth Observatory, Columbia University, New York, NY, USA
Institute of Earth Sciences, Hebrew University, Jerusalem, Israel
Sylvia Dee
Department of Earth, Environmental, and Planetary Sciences, Rice
University, Houston, TX, USA
Chris Hancock
School of Earth and Sustainability, Northern Arizona University,
Flagstaff, AZ, USA
Ruza F. Ivanovic
School of Earth and Environment, University of Leeds, Leeds, UK
Lauren J. Gregoire
School of Earth and Environment, University of Leeds, Leeds, UK
Paul Valdes
School of Geographical Sciences, University of Bristol, Bristol, UK
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Cited
19 citations as recorded by crossref.
- The Historical Development of Large‐Scale Paleoclimate Field Reconstructions Over the Common Era J. Smerdon et al. 10.1029/2022RG000782
- A Greenland-wide empirical reconstruction of paleo ice sheet retreat informed by ice extent markers: PaleoGrIS version 1.0 T. Leger et al. 10.5194/cp-20-701-2024
- Unveiling the history and nature of paleostorms in the Holocene K. Minamidate & K. Goto 10.1016/j.earscirev.2024.104774
- Holocene warming trend based on peat brGDGTs records from southeastern humid to northwestern arid China S. Wei et al. 10.1016/j.palaeo.2023.111528
- Carbon and oxygen isotopes in mummified wood reveal warmer and wetter winters in the Siberian Arctic 3000 years ago B. Schubert et al. 10.1038/s41598-024-67947-1
- Sedimentary brGDGTs in China: An overview of modern observations and proposed land Holocene paleotemperature records T. Lin et al. 10.1016/j.earscirev.2024.104694
- A preliminary integrated analysis of regional paleoclimate variations in China over the past ∼ 21 ka H. Lu et al. 10.1016/j.gloplacha.2024.104510
- A continental reconstruction of hydroclimatic variability in South America during the past 2000 years M. Choblet et al. 10.5194/cp-20-2117-2024
- Relative importance of forcings and feedbacks in the Holocene temperature conundrum P. Hopcroft et al. 10.1016/j.quascirev.2023.108322
- Reconstructing 15 000 years of southern France temperatures from coupled pollen and molecular (branched glycerol dialkyl glycerol tetraether) markers (Canroute, Massif Central) L. d'Oliveira et al. 10.5194/cp-19-2127-2023
- Paleoclimate data assimilation with CLIMBER-X: An ensemble Kalman filter for the last deglaciation A. Masoum et al. 10.1371/journal.pone.0300138
- Revisiting the Holocene global temperature conundrum D. Kaufman & E. Broadman 10.1038/s41586-022-05536-w
- Environmental significance of <italic>δ</italic><sup>13</sup>C<sub>cell</sub> in living sedges in SWGT peatland, Chengbu County, Hunan Province Q. Qin et al. 10.1360/TB-2023-1022
- No Consistent Simulated Trends in the Atlantic Meridional Overturning Circulation for the Past 6,000 Years Z. Jiang et al. 10.1029/2023GL103078
- Rethinking the Holocene temperature conundrum H. Essell et al. 10.3354/cr01735
- High-frequency climate forcing causes prolonged cold periods in the Holocene E. van Dijk et al. 10.1038/s43247-024-01380-0
- Boreal forest cover was reduced in the mid-Holocene with warming and recurring wildfires M. Girardin et al. 10.1038/s43247-024-01340-8
- Climate and atmospheric circulation during the Early and Mid‐Holocene inferred from lake‐carbonate oxygen‐isotope records from western Ireland J. Holmes et al. 10.1002/jqs.3571
- Reconstructing Holocene temperatures in time and space using paleoclimate data assimilation M. Erb et al. 10.5194/cp-18-2599-2022
17 citations as recorded by crossref.
- The Historical Development of Large‐Scale Paleoclimate Field Reconstructions Over the Common Era J. Smerdon et al. 10.1029/2022RG000782
- A Greenland-wide empirical reconstruction of paleo ice sheet retreat informed by ice extent markers: PaleoGrIS version 1.0 T. Leger et al. 10.5194/cp-20-701-2024
- Unveiling the history and nature of paleostorms in the Holocene K. Minamidate & K. Goto 10.1016/j.earscirev.2024.104774
- Holocene warming trend based on peat brGDGTs records from southeastern humid to northwestern arid China S. Wei et al. 10.1016/j.palaeo.2023.111528
- Carbon and oxygen isotopes in mummified wood reveal warmer and wetter winters in the Siberian Arctic 3000 years ago B. Schubert et al. 10.1038/s41598-024-67947-1
- Sedimentary brGDGTs in China: An overview of modern observations and proposed land Holocene paleotemperature records T. Lin et al. 10.1016/j.earscirev.2024.104694
- A preliminary integrated analysis of regional paleoclimate variations in China over the past ∼ 21 ka H. Lu et al. 10.1016/j.gloplacha.2024.104510
- A continental reconstruction of hydroclimatic variability in South America during the past 2000 years M. Choblet et al. 10.5194/cp-20-2117-2024
- Relative importance of forcings and feedbacks in the Holocene temperature conundrum P. Hopcroft et al. 10.1016/j.quascirev.2023.108322
- Reconstructing 15 000 years of southern France temperatures from coupled pollen and molecular (branched glycerol dialkyl glycerol tetraether) markers (Canroute, Massif Central) L. d'Oliveira et al. 10.5194/cp-19-2127-2023
- Paleoclimate data assimilation with CLIMBER-X: An ensemble Kalman filter for the last deglaciation A. Masoum et al. 10.1371/journal.pone.0300138
- Revisiting the Holocene global temperature conundrum D. Kaufman & E. Broadman 10.1038/s41586-022-05536-w
- Environmental significance of <italic>δ</italic><sup>13</sup>C<sub>cell</sub> in living sedges in SWGT peatland, Chengbu County, Hunan Province Q. Qin et al. 10.1360/TB-2023-1022
- No Consistent Simulated Trends in the Atlantic Meridional Overturning Circulation for the Past 6,000 Years Z. Jiang et al. 10.1029/2023GL103078
- Rethinking the Holocene temperature conundrum H. Essell et al. 10.3354/cr01735
- High-frequency climate forcing causes prolonged cold periods in the Holocene E. van Dijk et al. 10.1038/s43247-024-01380-0
- Boreal forest cover was reduced in the mid-Holocene with warming and recurring wildfires M. Girardin et al. 10.1038/s43247-024-01340-8
2 citations as recorded by crossref.
- Climate and atmospheric circulation during the Early and Mid‐Holocene inferred from lake‐carbonate oxygen‐isotope records from western Ireland J. Holmes et al. 10.1002/jqs.3571
- Reconstructing Holocene temperatures in time and space using paleoclimate data assimilation M. Erb et al. 10.5194/cp-18-2599-2022
Latest update: 14 Nov 2024
Co-editor-in-chief
The manuscript presents a reconstruction of global temperature spanning the Holocene, which extends the scope of previous exercises in palaeoclimate data assimilation. The resulting reconstruction presents new insights into changes in global temperature over this period. Most notably, it confirms the results of previous studies that have shown a global cooling trend over the past 6,000 years. It also shows that a cooling trend is found even after allowing for potential biases in the proxies. These results are likely to be of considerable interest to the broader geoscience community.
The manuscript presents a reconstruction of global temperature spanning the Holocene, which...
Short summary
To look at climate over the past 12 000 years, we reconstruct spatial temperature using natural climate archives and information from model simulations. Our results show mild global mean warmth around 6000 years ago, which differs somewhat from past reconstructions. Undiagnosed seasonal biases in the data could explain some of the observed temperature change, but this still would not explain the large difference between many reconstructions and climate models over this period.
To look at climate over the past 12 000 years, we reconstruct spatial temperature using natural...
