Articles | Volume 13, issue 3
Clim. Past, 13, 267–301, 2017
https://doi.org/10.5194/cp-13-267-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Clim. Past, 13, 267–301, 2017
https://doi.org/10.5194/cp-13-267-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
29 Mar 2017
Research article
| 29 Mar 2017
Was the Little Ice Age more or less El Niño-like than the Medieval Climate Anomaly? Evidence from hydrological and temperature proxy data
Lilo M. K. Henke et al.
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Cited
15 citations as recorded by crossref.
- 300 years of hydrological records and societal responses to droughts and floods on the Pacific coast of Central America A. Guevara-Murua et al. 10.5194/cp-14-175-2018
- A Century of Reduced ENSO Variability During the Medieval Climate Anomaly A. Lawman et al. 10.1029/2019PA003742
- Did Modern Precipitation Drivers Influence Centennial Trends in the Highlands of the Atacama Desert During the Most Recent Millennium? I. Jara et al. 10.1029/2021GL095927
- The Medieval Climate Anomaly in South America S. Lüning et al. 10.1016/j.quaint.2018.10.041
- Teleconnections and relationship between the El Niño–Southern Oscillation (ENSO) and the Southern Annular Mode (SAM) in reconstructions and models over the past millennium C. Dätwyler et al. 10.5194/cp-16-743-2020
- Enhanced North American ENSO Teleconnections During the Little Ice Age Revealed by Paleoclimate Data Assimilation S. Dee et al. 10.1029/2020GL087504
- The Medieval Climate Anomaly in Antarctica S. Lüning et al. 10.1016/j.palaeo.2019.109251
- Large-scale climate signals of a European oxygen isotope network from tree rings D. Balting et al. 10.5194/cp-17-1005-2021
- Multi‐Centennial‐Scale Variations of South American Summer Monsoon Intensity in the Southern Central Andes (24–27°S) During the Late Holocene S. Kock et al. 10.1029/2019GL084157
- Last millennium intensification of decadal and interannual river discharge cycles into the Southwestern Atlantic Ocean increases shelf productivity L. Perez et al. 10.1016/j.gloplacha.2020.103367
- A PMIP3 narrative of modulation of ENSO teleconnections to the Indian summer monsoon by background changes in the Last Millennium C. Tejavath et al. 10.1007/s00382-019-04718-z
- Variation of the summer Asian westerly jet over the last millennium based on the PMIP3 simulations N. Jiang et al. 10.1177/0959683619883011
- Modes of climate variability: Synthesis and review of proxy-based reconstructions through the Holocene A. Hernández et al. 10.1016/j.earscirev.2020.103286
- Calibration Uncertainties of Tropical Pacific Climate Reconstructions over the Last Millennium K. Yun & A. Timmermann 10.1175/JCLI-D-18-0524.1
- Patterns of Resource Use and Isotopic Niche Overlap Among Guanaco (Lama guanicoe), Pampas Deer (Ozotoceros bezoarticus) and Marsh Deer (Blastocerus dichotomus) in the Pampas. Ecological, Paleoenvironmental and Archaeological Implications D. Loponte & M. Corriale 10.1080/14614103.2019.1585646
15 citations as recorded by crossref.
- 300 years of hydrological records and societal responses to droughts and floods on the Pacific coast of Central America A. Guevara-Murua et al. 10.5194/cp-14-175-2018
- A Century of Reduced ENSO Variability During the Medieval Climate Anomaly A. Lawman et al. 10.1029/2019PA003742
- Did Modern Precipitation Drivers Influence Centennial Trends in the Highlands of the Atacama Desert During the Most Recent Millennium? I. Jara et al. 10.1029/2021GL095927
- The Medieval Climate Anomaly in South America S. Lüning et al. 10.1016/j.quaint.2018.10.041
- Teleconnections and relationship between the El Niño–Southern Oscillation (ENSO) and the Southern Annular Mode (SAM) in reconstructions and models over the past millennium C. Dätwyler et al. 10.5194/cp-16-743-2020
- Enhanced North American ENSO Teleconnections During the Little Ice Age Revealed by Paleoclimate Data Assimilation S. Dee et al. 10.1029/2020GL087504
- The Medieval Climate Anomaly in Antarctica S. Lüning et al. 10.1016/j.palaeo.2019.109251
- Large-scale climate signals of a European oxygen isotope network from tree rings D. Balting et al. 10.5194/cp-17-1005-2021
- Multi‐Centennial‐Scale Variations of South American Summer Monsoon Intensity in the Southern Central Andes (24–27°S) During the Late Holocene S. Kock et al. 10.1029/2019GL084157
- Last millennium intensification of decadal and interannual river discharge cycles into the Southwestern Atlantic Ocean increases shelf productivity L. Perez et al. 10.1016/j.gloplacha.2020.103367
- A PMIP3 narrative of modulation of ENSO teleconnections to the Indian summer monsoon by background changes in the Last Millennium C. Tejavath et al. 10.1007/s00382-019-04718-z
- Variation of the summer Asian westerly jet over the last millennium based on the PMIP3 simulations N. Jiang et al. 10.1177/0959683619883011
- Modes of climate variability: Synthesis and review of proxy-based reconstructions through the Holocene A. Hernández et al. 10.1016/j.earscirev.2020.103286
- Calibration Uncertainties of Tropical Pacific Climate Reconstructions over the Last Millennium K. Yun & A. Timmermann 10.1175/JCLI-D-18-0524.1
- Patterns of Resource Use and Isotopic Niche Overlap Among Guanaco (Lama guanicoe), Pampas Deer (Ozotoceros bezoarticus) and Marsh Deer (Blastocerus dichotomus) in the Pampas. Ecological, Paleoenvironmental and Archaeological Implications D. Loponte & M. Corriale 10.1080/14614103.2019.1585646
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Discussed (final revised paper)
Latest update: 07 Dec 2022
Short summary
To understand future ENSO behaviour we must look at the past, but temperature and rainfall proxies (e.g. tree rings, sediment cores) appear to show different responses. We tested this by making separate multi-proxy ENSO reconstructions for precipitation and temperature and found no evidence of a disagreement between ENSO-driven changes in precipitation and temperature. While this supports our physical understanding of ENSO, the lack of good proxy data must be addressed to further explore this.
To understand future ENSO behaviour we must look at the past, but temperature and rainfall...
