Articles | Volume 16, issue 4
https://doi.org/10.5194/cp-16-1145-2020
© Author(s) 2020. 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-16-1145-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
03 Jul 2020
Research article |
| 03 Jul 2020
| 03 Jul 2020
Radionuclide wiggle matching reveals a nonsynchronous early Holocene climate oscillation in Greenland and western Europe around a grand solar minimum
Florian Mekhaldi
CORRESPONDING AUTHOR
Department of Geology – Quaternary Sciences, Lund University, 22362
Lund, Sweden
Markus Czymzik
Leibniz Institute for Baltic Sea Research Warnemünde (IOW), Marine Geology, 18119 Rostock, Germany
Florian Adolphi
Department of Geology – Quaternary Sciences, Lund University, 22362
Lund, Sweden
Physics Institute, Climate and Environmental Physics & Oeschger
Centre for Climate Change Research, University of Bern, 3012 Bern,
Switzerland
Jesper Sjolte
Department of Geology – Quaternary Sciences, Lund University, 22362
Lund, Sweden
Svante Björck
Department of Geology – Quaternary Sciences, Lund University, 22362
Lund, Sweden
Ala Aldahan
Department of Geology, United Arab Emirates University, 15551 Al Ain, UAE
Achim Brauer
GFZ German Research Centre for Geosciences, Climate Dynamics and
Landscape Evolution, 14473 Potsdam, Germany
Celia Martin-Puertas
Department of Geography, Royal Holloway University of London, Egham, TW20 0EX Surrey, UK
Göran Possnert
Tandem Laboratory, Uppsala University, 75120 Uppsala, Sweden
Raimund Muscheler
Department of Geology – Quaternary Sciences, Lund University, 22362
Lund, Sweden
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Our study presents the first seasonally laminated (varved) sediment record covering almost the entire Holocene in high mountainous arid Central Asia. The established floating varve chronology is confirmed by two terrestrial radiocarbon dates, whereby aquatic radiocarbon dates reveal decreasing reservoir ages up core. Changes in seasonal deposition characteristics are attributed to changes in runoff and precipitation and/or to evaporative summer conditions.
Svante Björck, Jesper Sjolte, Karl Ljung, Florian Adolphi, Roger Flower, Rienk H. Smittenberg, Malin E. Kylander, Thomas F. Stocker, Sofia Holmgren, Hui Jiang, Raimund Muscheler, Yamoah K. K. Afrifa, Jayne E. Rattray, and Nathalie Van der Putten
Clim. Past, 15, 1939–1958, https://doi.org/10.5194/cp-15-1939-2019, https://doi.org/10.5194/cp-15-1939-2019, 2019
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Southern Hemisphere westerlies play a key role in regulating global climate. A lake sediment record on a mid-South Atlantic island shows changes in the westerlies and hydroclimate 36.4–18.6 ka. Before 31 ka the westerlies shifted in concert with the bipolar seesaw mechanism in a fairly warm climate, followed by southerly westerlies and falling temperatures. After 27.5 ka temperatures dropped 3 °C with drier conditions and with shifting westerlies possibly triggering the variable LGM CO2 levels.
Hera Guðlaugsdóttir, Jesper Sjolte, Árný Erla Sveinbjörnsdóttir, and Hans Christian Steen-Larsen
Clim. Past Discuss., https://doi.org/10.5194/cp-2019-99, https://doi.org/10.5194/cp-2019-99, 2019
Revised manuscript not accepted
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In the North Atlantic four modes of climate variability dominate weather. Here we assess how these modes are affected after both equatorial and high latitude eruptions, known to influence temperature in the atmosphere. Main results show that the modes associated with extreme weather events tend to follow high latitude eruptions as opposed to equatorial eruptions. These modes have also become more frequent as a result of anthropogenic warming, providing an insight into the dominating mechanism.
Achim Brauer, Markus J. Schwab, Brian Brademann, Sylvia Pinkerneil, and Martin Theuerkauf
DEUQUA Spec. Pub., 2, 89–93, https://doi.org/10.5194/deuquasp-2-89-2019, https://doi.org/10.5194/deuquasp-2-89-2019, 2019
Tobias Erhardt, Emilie Capron, Sune Olander Rasmussen, Simon Schüpbach, Matthias Bigler, Florian Adolphi, and Hubertus Fischer
Clim. Past, 15, 811–825, https://doi.org/10.5194/cp-15-811-2019, https://doi.org/10.5194/cp-15-811-2019, 2019
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The cause of the rapid warming events documented in proxy records across the Northern Hemisphere during the last glacial has been a long-standing puzzle in paleo-climate research. Here, we use high-resolution ice-core data from to cores in Greenland to investigate the progression during the onset of these events on multi-annual timescales to test their plausible triggers. We show that atmospheric circulation changes preceded the warming in Greenland and the collapse of the sea ice by a decade.
François Klein, Nerilie J. Abram, Mark A. J. Curran, Hugues Goosse, Sentia Goursaud, Valérie Masson-Delmotte, Andrew Moy, Raphael Neukom, Anaïs Orsi, Jesper Sjolte, Nathan Steiger, Barbara Stenni, and Martin Werner
Clim. Past, 15, 661–684, https://doi.org/10.5194/cp-15-661-2019, https://doi.org/10.5194/cp-15-661-2019, 2019
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Antarctic temperature changes over the past millennia have been reconstructed from isotope records in ice cores in several studies. However, the link between both variables is complex. Here, we investigate the extent to which this affects the robustness of temperature reconstructions using pseudoproxy and data assimilation experiments. We show that the reconstruction skill is limited, especially at the regional scale, due to a weak and nonstationary covariance between δ18O and temperature.
Florian Adolphi, Christopher Bronk Ramsey, Tobias Erhardt, R. Lawrence Edwards, Hai Cheng, Chris S. M. Turney, Alan Cooper, Anders Svensson, Sune O. Rasmussen, Hubertus Fischer, and Raimund Muscheler
Clim. Past, 14, 1755–1781, https://doi.org/10.5194/cp-14-1755-2018, https://doi.org/10.5194/cp-14-1755-2018, 2018
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The last glacial period was characterized by a number of rapid climate changes seen, for example, as abrupt warmings in Greenland and changes in monsoon rainfall intensity. However, due to chronological uncertainties it is challenging to know how tightly coupled these changes were. Here we exploit cosmogenic signals caused by changes in the Sun and Earth magnetic fields to link different climate archives and improve our understanding of the dynamics of abrupt climate change.
Bernhard Aichner, Florian Ott, Michał Słowiński, Agnieszka M. Noryśkiewicz, Achim Brauer, and Dirk Sachse
Clim. Past, 14, 1607–1624, https://doi.org/10.5194/cp-14-1607-2018, https://doi.org/10.5194/cp-14-1607-2018, 2018
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Abundances of plant biomarkers are compared with pollen data in a 3000-year climate archive covering the Late Glacial to Holocene transition in northern Poland. Both parameters synchronously show the rapid onset (12680–12600 yr BP) and termination
(11580–11490 yr BP) of the Younger Dryas cold interval in the study area. This demonstrates the suitability of such proxies to record pronounced changes in vegetation cover without significant delay.
Jesper Sjolte, Christophe Sturm, Florian Adolphi, Bo M. Vinther, Martin Werner, Gerrit Lohmann, and Raimund Muscheler
Clim. Past, 14, 1179–1194, https://doi.org/10.5194/cp-14-1179-2018, https://doi.org/10.5194/cp-14-1179-2018, 2018
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Tropical volcanic eruptions and variations in solar activity have been suggested to influence the strength of westerly winds across the North Atlantic. We use Greenland ice core records together with a climate model simulation, and find stronger westerly winds for five winters following tropical volcanic eruptions. We see a delayed response to solar activity of 5 years, and the response to solar minima corresponds well to the cooling pattern during the period known as the Little Ice Age.
Minjie Zheng, Jesper Sjolte, Florian Adolphi, Bo Møllesøe Vinther, Hans Christian Steen-Larsen, Trevor James Popp, and Raimund Muscheler
Clim. Past, 14, 1067–1078, https://doi.org/10.5194/cp-14-1067-2018, https://doi.org/10.5194/cp-14-1067-2018, 2018
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We show the seasonal δ18O data from the NEEM site in northwestern Greenland over the last 150 years. We found that the NEEM summer δ18O signal correlates well with summer temperature in western coastal Greenland, while the NEEM winter δ18O signal correlates well with sea ice concentration in Baffin Bay. In contrast with the winter δ18O data from central/southern Greenland, we find no linkage of NEEM winter δ18O to winter NAO.
Markus Czymzik, Raimund Muscheler, Florian Adolphi, Florian Mekhaldi, Nadine Dräger, Florian Ott, Michał Słowinski, Mirosław Błaszkiewicz, Ala Aldahan, Göran Possnert, and Achim Brauer
Clim. Past, 14, 687–696, https://doi.org/10.5194/cp-14-687-2018, https://doi.org/10.5194/cp-14-687-2018, 2018
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Our results provide a proof of concept for facilitating 10Be in varved lake sediments as a novel synchronization tool required for investigating leads and lags of proxy responses to climate variability. They also point to some limitations of 10Be in these archives mainly connected to in-lake sediment resuspension processes.
Norel Rimbu, Monica Ionita, Markus Czymzik, Achim Brauer, and Gerrit Lohmann
Clim. Past Discuss., https://doi.org/10.5194/cp-2017-137, https://doi.org/10.5194/cp-2017-137, 2017
Manuscript not accepted for further review
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Multi-decadal to millennial flood frequency variations in the Mid- to Late Holocene in a flood layer record from Lake Ammersee is strongly related to the occurrence of extreme precipitation and temperatures in the northeastern Europe.
Annette Witt, Bruce D. Malamud, Clara Mangili, and Achim Brauer
Hydrol. Earth Syst. Sci., 21, 5547–5581, https://doi.org/10.5194/hess-21-5547-2017, https://doi.org/10.5194/hess-21-5547-2017, 2017
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Here we present a unique 9.5 m palaeo-lacustrine record of 771 palaeofloods which occurred over a period of 10 000 years in the Piànico–Sèllere basin (southern Alps) during an interglacial period in the Pleistocene (sometime between 400 000 and 800 000 years ago). We analyse the palaeoflood series correlation, clustering, and cyclicity properties, finding a long-range cyclicity with a period of about 2030 years superimposed onto a fractional noise.
Johann H. Jungclaus, Edouard Bard, Mélanie Baroni, Pascale Braconnot, Jian Cao, Louise P. Chini, Tania Egorova, Michael Evans, J. Fidel González-Rouco, Hugues Goosse, George C. Hurtt, Fortunat Joos, Jed O. Kaplan, Myriam Khodri, Kees Klein Goldewijk, Natalie Krivova, Allegra N. LeGrande, Stephan J. Lorenz, Jürg Luterbacher, Wenmin Man, Amanda C. Maycock, Malte Meinshausen, Anders Moberg, Raimund Muscheler, Christoph Nehrbass-Ahles, Bette I. Otto-Bliesner, Steven J. Phipps, Julia Pongratz, Eugene Rozanov, Gavin A. Schmidt, Hauke Schmidt, Werner Schmutz, Andrew Schurer, Alexander I. Shapiro, Michael Sigl, Jason E. Smerdon, Sami K. Solanki, Claudia Timmreck, Matthew Toohey, Ilya G. Usoskin, Sebastian Wagner, Chi-Ju Wu, Kok Leng Yeo, Davide Zanchettin, Qiong Zhang, and Eduardo Zorita
Geosci. Model Dev., 10, 4005–4033, https://doi.org/10.5194/gmd-10-4005-2017, https://doi.org/10.5194/gmd-10-4005-2017, 2017
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Climate model simulations covering the last millennium provide context for the evolution of the modern climate and for the expected changes during the coming centuries. They can help identify plausible mechanisms underlying palaeoclimatic reconstructions. Here, we describe the forcing boundary conditions and the experimental protocol for simulations covering the pre-industrial millennium. We describe the PMIP4 past1000 simulations as contributions to CMIP6 and additional sensitivity experiments.
Oliver Rach, Ansgar Kahmen, Achim Brauer, and Dirk Sachse
Clim. Past, 13, 741–757, https://doi.org/10.5194/cp-13-741-2017, https://doi.org/10.5194/cp-13-741-2017, 2017
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Currently, reconstructions of past changes in the hydrological cycle are usually qualitative, which is a major drawback for testing the accuracy of models in predicting future responses. Here we present a proof of concept of a novel approach to deriving quantitative paleohydrological data, i.e. changes in relative humidity, from lacustrine sediment archives, employing a combination of organic geochemical methods and plant physiological modeling.
Anne-Katrine Faber, Bo Møllesøe Vinther, Jesper Sjolte, and Rasmus Anker Pedersen
Atmos. Chem. Phys., 17, 5865–5876, https://doi.org/10.5194/acp-17-5865-2017, https://doi.org/10.5194/acp-17-5865-2017, 2017
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The recent decades loss of Arctic sea ice provide an interesting opportunity to study the impact of sea ice changes on the isotopic composition of Arctic precipitation. Using a climate model that can simulate water isotopes, we find that reduced sea ice extent yields more enriched isotope values while increased sea ice extent yields more
depleted isotope values. Results also show that the spatial distribution of the sea ice extent are important.
Markus Czymzik, Raimund Muscheler, and Achim Brauer
Clim. Past, 12, 799–805, https://doi.org/10.5194/cp-12-799-2016, https://doi.org/10.5194/cp-12-799-2016, 2016
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Integrating discharge data of the River Ammer back to 1926 and a 5500-year flood layer record from an annually laminated sediment core of the downstream Ammersee allowed investigating changes in the frequency of major floods in Central Europe on interannual to multi-centennial timescales. Significant correlations between flood frequency variations in both archives and changes in the activity of the Sun suggest a solar influence on the frequency of these hydrometeorological extremes.
Michael Sigl, Tyler J. Fudge, Mai Winstrup, Jihong Cole-Dai, David Ferris, Joseph R. McConnell, Ken C. Taylor, Kees C. Welten, Thomas E. Woodruff, Florian Adolphi, Marion Bisiaux, Edward J. Brook, Christo Buizert, Marc W. Caffee, Nelia W. Dunbar, Ross Edwards, Lei Geng, Nels Iverson, Bess Koffman, Lawrence Layman, Olivia J. Maselli, Kenneth McGwire, Raimund Muscheler, Kunihiko Nishiizumi, Daniel R. Pasteris, Rachael H. Rhodes, and Todd A. Sowers
Clim. Past, 12, 769–786, https://doi.org/10.5194/cp-12-769-2016, https://doi.org/10.5194/cp-12-769-2016, 2016
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Here we present a chronology (WD2014) for the upper part (0–2850 m; 31.2 ka BP) of the West Antarctic Ice Sheet (WAIS) Divide ice core, which is based on layer counting of distinctive annual cycles preserved in the elemental, chemical and electrical conductivity records. We validated the chronology by comparing it to independent high-accuracy, absolutely dated chronologies. Given its demonstrated high accuracy, WD2014 can become a reference chronology for the Southern Hemisphere.
Norel Rimbu, Markus Czymzik, Monica Ionita, Gerrit Lohmann, and Achim Brauer
Clim. Past, 12, 377–385, https://doi.org/10.5194/cp-12-377-2016, https://doi.org/10.5194/cp-12-377-2016, 2016
I. Neugebauer, M. J. Schwab, N. D. Waldmann, R. Tjallingii, U. Frank, E. Hadzhiivanova, R. Naumann, N. Taha, A. Agnon, Y. Enzel, and A. Brauer
Clim. Past, 12, 75–90, https://doi.org/10.5194/cp-12-75-2016, https://doi.org/10.5194/cp-12-75-2016, 2016
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Micro-facies changes and elemental variations in deep Dead Sea sediments are used to reconstruct relative lake level changes for the early last glacial period. The results indicate a close link of hydroclimatic variability in the Levant to North Atlantic-Mediterranean climates during the time of the build-up of Northern Hemisphere ice shields. First petrographic analyses of gravels in the deep core question the recent hypothesis of a Dead Sea dry-down at the end of the last interglacial.
F. Adolphi and R. Muscheler
Clim. Past, 12, 15–30, https://doi.org/10.5194/cp-12-15-2016, https://doi.org/10.5194/cp-12-15-2016, 2016
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Here we employ common variations in tree-ring 14C and Greenland ice core 10Be records to synchronize the Greenland ice core (GICC05) and the radiocarbon (IntCal13) timescale over the Holocene. We propose a transfer function between both timescales that allows continuous comparisons between radiocarbon dated and ice core climate records at unprecedented chronological precision.
W. Clymans, L. Barão, N. Van der Putten, S. Wastegård, G. Gísladóttir, S. Björck, B. Moine, E. Struyf, and D. J. Conley
Biogeosciences, 12, 3789–3804, https://doi.org/10.5194/bg-12-3789-2015, https://doi.org/10.5194/bg-12-3789-2015, 2015
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Biogenic silica (BSi) is used as a proxy by soil scientists to identify biological effects on the Si cycle and by palaeoecologists to study environmental changes. We show the presence of tephra constituents can make measurements erroneous at low BSi concentrations, with repercussions for soil and palaeoecological studies. However, we also show that glass shards do not produce an identical dissolution signal to that of BSi, meaning they can be distinguished with appropriate experimental setups.
C. Martin-Puertas, A. Brauer, S. Wulf, F. Ott, S. Lauterbach, and P. Dulski
Clim. Past, 10, 2099–2114, https://doi.org/10.5194/cp-10-2099-2014, https://doi.org/10.5194/cp-10-2099-2014, 2014
B. Merz, J. Aerts, K. Arnbjerg-Nielsen, M. Baldi, A. Becker, A. Bichet, G. Blöschl, L. M. Bouwer, A. Brauer, F. Cioffi, J. M. Delgado, M. Gocht, F. Guzzetti, S. Harrigan, K. Hirschboeck, C. Kilsby, W. Kron, H.-H. Kwon, U. Lall, R. Merz, K. Nissen, P. Salvatti, T. Swierczynski, U. Ulbrich, A. Viglione, P. J. Ward, M. Weiler, B. Wilhelm, and M. Nied
Nat. Hazards Earth Syst. Sci., 14, 1921–1942, https://doi.org/10.5194/nhess-14-1921-2014, https://doi.org/10.5194/nhess-14-1921-2014, 2014
T. Swierczynski, S. Lauterbach, P. Dulski, and A. Brauer
Clim. Past, 9, 1601–1612, https://doi.org/10.5194/cp-9-1601-2013, https://doi.org/10.5194/cp-9-1601-2013, 2013
H. C. Steen-Larsen, S. J. Johnsen, V. Masson-Delmotte, B. Stenni, C. Risi, H. Sodemann, D. Balslev-Clausen, T. Blunier, D. Dahl-Jensen, M. D. Ellehøj, S. Falourd, A. Grindsted, V. Gkinis, J. Jouzel, T. Popp, S. Sheldon, S. B. Simonsen, J. Sjolte, J. P. Steffensen, P. Sperlich, A. E. Sveinbjörnsdóttir, B. M. Vinther, and J. W. C. White
Atmos. Chem. Phys., 13, 4815–4828, https://doi.org/10.5194/acp-13-4815-2013, https://doi.org/10.5194/acp-13-4815-2013, 2013
Related subject area
Subject: Atmospheric Dynamics | Archive: Terrestrial Archives | Timescale: Holocene
North Atlantic Oscillation polarity during the past 3000 years derived from sediments of a large lowland lake, Schweriner See, in NE Germany
Patterns of centennial to millennial Holocene climate variation in the North American mid-latitudes
Regional pollen-based Holocene temperature and precipitation patterns depart from the Northern Hemisphere mean trends
Mid-Holocene reinforcement of North Atlantic atmospheric circulation variability from a western Baltic lake sediment record
Holocene sea level and environmental change at the southern Cape – an 8.5 kyr multi-proxy paleoclimate record from Lake Voëlvlei, South Africa
Tree-ring-based spring precipitation reconstruction in the Sikhote-Alin' Mountain range
Hydrological variations in central China over the past millennium and their links to the tropical Pacific and North Atlantic oceans
Atmospheric blocking induced by the strengthened Siberian High led to drying in west Asia during the 4.2 ka BP event – a hypothesis
Hydro-climatic variability in the southwestern Indian Ocean between 6000 and 3000 years ago
Evidence for increased expression of the Amundsen Sea Low over the South Atlantic during the late Holocene
The 4.2 ka BP event: multi-proxy records from a closed lake in the northern margin of the East Asian summer monsoon
Drought and vegetation change in the central Rocky Mountains and western Great Plains: potential climatic mechanisms associated with megadrought conditions at 4200 cal yr BP
Placing the Common Era in a Holocene context: millennial to centennial patterns and trends in the hydroclimate of North America over the past 2000 years
Multi-century cool- and warm-season rainfall reconstructions for Australia's major climatic regions
Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks
Periodic input of dust over the Eastern Carpathians during the Holocene linked with Saharan desertification and human impact
Frequency and intensity of palaeofloods at the interface of Atlantic and Mediterranean climate domains
A 250-year periodicity in Southern Hemisphere westerly winds over the last 2600 years
Non-linear regime shifts in Holocene Asian monsoon variability: potential impacts on cultural change and migratory patterns
The influence of atmospheric circulation on the mid-Holocene climate of Europe: a data–model comparison
Late Holocene summer temperatures in the central Andes reconstructed from the sediments of high-elevation Laguna Chepical, Chile (32° S)
Effects of dating errors on nonparametric trend analyses of speleothem time series
Precipitation variability in the winter rainfall zone of South Africa during the last 1400 yr linked to the austral westerlies
Relationship between Holocene climate variations over southern Greenland and eastern Baffin Island and synoptic circulation pattern
Marie-Luise Adolph, Sambor Czerwiński, Mirko Dreßler, Paul Strobel, Marcel Bliedtner, Sebastian Lorenz, Maxime Debret, and Torsten Haberzettl
Clim. Past, 20, 2143–2165, https://doi.org/10.5194/cp-20-2143-2024, https://doi.org/10.5194/cp-20-2143-2024, 2024
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We reconstruct environmental changes derived from sediments of Schweriner See, a large lake in NE Germany, for the past 3000 years. We infer variations in North Atlantic large-scale atmospheric circulation systems, namely the North Atlantic Oscillation (NAO), by combining sedimentological, geochemical, and biological parameters. Our results suggest distinct shifts between positive and negative NAO phases affecting winter temperatures, precipitation, and westerly wind strength at our study site.
Bryan N. Shuman
Clim. Past, 20, 1703–1720, https://doi.org/10.5194/cp-20-1703-2024, https://doi.org/10.5194/cp-20-1703-2024, 2024
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A gap in understanding climate variation exists at centennial to millennial scales, particularly for warm climates. Such variations challenge detection. They exceed direct observation but are geologically short. Centennial to millennial variations that may have influenced North America were examined over the past 7 kyr. Significant patterns were detected from fossil pollen and sedimentary lake level changes, indicating ecological, hydrological, and likely human significance.
Ulrike Herzschuh, Thomas Böhmer, Manuel Chevalier, Raphaël Hébert, Anne Dallmeyer, Chenzhi Li, Xianyong Cao, Odile Peyron, Larisa Nazarova, Elena Y. Novenko, Jungjae Park, Natalia A. Rudaya, Frank Schlütz, Lyudmila S. Shumilovskikh, Pavel E. Tarasov, Yongbo Wang, Ruilin Wen, Qinghai Xu, and Zhuo Zheng
Clim. Past, 19, 1481–1506, https://doi.org/10.5194/cp-19-1481-2023, https://doi.org/10.5194/cp-19-1481-2023, 2023
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A mismatch between model- and proxy-based Holocene climate change may partially originate from the poor spatial coverage of climate reconstructions. Here we investigate quantitative reconstructions of mean annual temperature and annual precipitation from 1908 pollen records in the Northern Hemisphere. Trends show strong latitudinal patterns and differ between (sub-)continents. Our work contributes to a better understanding of the global mean.
Markus Czymzik, Rik Tjallingii, Birgit Plessen, Peter Feldens, Martin Theuerkauf, Matthias Moros, Markus J. Schwab, Carla K. M. Nantke, Silvia Pinkerneil, Achim Brauer, and Helge W. Arz
Clim. Past, 19, 233–248, https://doi.org/10.5194/cp-19-233-2023, https://doi.org/10.5194/cp-19-233-2023, 2023
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Productivity increases in Lake Kälksjön sediments during the last 9600 years are likely driven by the progressive millennial-scale winter warming in northwestern Europe, following the increasing Northern Hemisphere winter insolation and decadal to centennial periods of a more positive NAO polarity. Strengthened productivity variability since ∼5450 cal yr BP is hypothesized to reflect a reinforcement of NAO-like atmospheric circulation.
Paul Strobel, Marcel Bliedtner, Andrew S. Carr, Peter Frenzel, Björn Klaes, Gary Salazar, Julian Struck, Sönke Szidat, Roland Zech, and Torsten Haberzettl
Clim. Past, 17, 1567–1586, https://doi.org/10.5194/cp-17-1567-2021, https://doi.org/10.5194/cp-17-1567-2021, 2021
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This study presents a multi-proxy record from Lake Voёlvlei and provides new insights into the sea level and paleoclimate history of the past 8.5 ka at South Africa’s southern Cape coast. Our results show that sea level changes at the southern coast are in good agreement with the western coast of South Africa. In terms of climate our record provides valuable insights into changing sources of precipitation at the southern Cape coast, i.e. westerly- and easterly-derived precipitation contribution.
Olga Ukhvatkina, Alexander Omelko, Dmitriy Kislov, Alexander Zhmerenetsky, Tatyana Epifanova, and Jan Altman
Clim. Past, 17, 951–967, https://doi.org/10.5194/cp-17-951-2021, https://doi.org/10.5194/cp-17-951-2021, 2021
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We present the first precipitation reconstructions for three sites along a latitudinal gradient in the Sikhote-Alin' mountains (Russian Far East). The reconstructions are based on Korean pine tree rings. We found that an important limiting factor for this species growth was precipitation during the spring-to-early-summer period. The periodicity found in our reconstructions suggests the influence of El Niño–Southern Oscillation and Pacific Dedacadal Oscillation on the region's climate.
Fucai Duan, Zhenqiu Zhang, Yi Wang, Jianshun Chen, Zebo Liao, Shitao Chen, Qingfeng Shao, and Kan Zhao
Clim. Past, 16, 475–485, https://doi.org/10.5194/cp-16-475-2020, https://doi.org/10.5194/cp-16-475-2020, 2020
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We reconstruct a detailed history of the East Asian summer monsoon (EASM) using stalagmite records in central China during the last millennium. We estimate responses of the EASM to anthropogenic global warming by comparing its relative intensity between the Current Warm Period and Medieval Climate Anomaly, two recent warm periods. We also study potential links of the EASM to the tropical Pacific and North Atlantic oceans. This work advances our understanding of EASM dynamics.
Aurel Perşoiu, Monica Ionita, and Harvey Weiss
Clim. Past, 15, 781–793, https://doi.org/10.5194/cp-15-781-2019, https://doi.org/10.5194/cp-15-781-2019, 2019
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We present a reconstruction of winter climate around 4.2 ka cal BP in Europe, west Asia, and northern Africa that shows generally low temperatures and heterogeneously distributed precipitation. We hypothesize that in the extratropical Northern Hemisphere the 4.2 ka BP event was caused by the strengthening and expansion of the Siberian High, which effectively blocked the moisture-carrying westerlies from reaching west Asia and also resulted in outbreaks of northerly cold and dry winds.
Hanying Li, Hai Cheng, Ashish Sinha, Gayatri Kathayat, Christoph Spötl, Aurèle Anquetil André, Arnaud Meunier, Jayant Biswas, Pengzhen Duan, Youfeng Ning, and Richard Lawrence Edwards
Clim. Past, 14, 1881–1891, https://doi.org/10.5194/cp-14-1881-2018, https://doi.org/10.5194/cp-14-1881-2018, 2018
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The
4.2 ka eventbetween 4.2 and 3.9 ka has been widely discussed in the Northern Hemsiphere but less reported in the Southern Hemisphere. Here, we use speleothem records from Rodrigues in the southwestern Indian Ocean spanning from 6000 to 3000 years ago to investigate the regional hydro-climatic variability. Our records show no evidence for an unusual climate anomaly between 4.2 and 3.9 ka. Instead, it shows a multi-centennial drought between 3.9 and 3.5 ka.
Zoë A. Thomas, Richard T. Jones, Chris J. Fogwill, Jackie Hatton, Alan N. Williams, Alan Hogg, Scott Mooney, Philip Jones, David Lister, Paul Mayewski, and Chris S. M. Turney
Clim. Past, 14, 1727–1738, https://doi.org/10.5194/cp-14-1727-2018, https://doi.org/10.5194/cp-14-1727-2018, 2018
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We report a high-resolution study of a 5000-year-long peat record from the Falkland Islands. This area sensitive to the dynamics of the Amundsen Sea Low, which plays a major role in modulating the Southern Ocean climate. We find wetter, colder conditions between 5.0 and 2.5 ka due to enhanced southerly airflow, with the establishment of drier and warmer conditions from 2.5 ka to present. This implies more westerly airflow and the increased projection of the ASL onto the South Atlantic.
Jule Xiao, Shengrui Zhang, Jiawei Fan, Ruilin Wen, Dayou Zhai, Zhiping Tian, and Dabang Jiang
Clim. Past, 14, 1417–1425, https://doi.org/10.5194/cp-14-1417-2018, https://doi.org/10.5194/cp-14-1417-2018, 2018
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Multiple proxies of a sediment core at Hulun Lake in the northern margin of the EASM reveal a prominent dry event at the interval of 4210–3840 cal. yr BP that could be the regional manifestation of the 4.2 ka BP event. Future studies should be focused on the investigation of high-quality, high-resolution proxy records from climatically sensitive and geographically representative regions in order to explore the spatiotemporal pattern of the 4.2 ka BP event and the associated dynamic mechanism.
Vachel A. Carter, Jacqueline J. Shinker, and Jonathon Preece
Clim. Past, 14, 1195–1212, https://doi.org/10.5194/cp-14-1195-2018, https://doi.org/10.5194/cp-14-1195-2018, 2018
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Between 4200 and 4000 cal yr BP, paleoecological evidence suggests a megadrought occurred in the central Rocky Mountains and western Great Plains. Modern climate analogues were used to explore potential climate mechanisms responsible for the ecological changes. Analogues illustrate that warm and dry conditions persisted through the growing season as a result of anomalously higher-than-normal heights centred over the Great Plains which suppressed moisture transport to the region.
Bryan N. Shuman, Cody Routson, Nicholas McKay, Sherilyn Fritz, Darrell Kaufman, Matthew E. Kirby, Connor Nolan, Gregory T. Pederson, and Jeannine-Marie St-Jacques
Clim. Past, 14, 665–686, https://doi.org/10.5194/cp-14-665-2018, https://doi.org/10.5194/cp-14-665-2018, 2018
Short summary
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A synthesis of 93 published records reveals that moisture availability increased over large portions of North America over the past 2000 years, the Common Era (CE). In many records, the second millennium CE tended to be wetter than the first millennium CE. The long-term changes formed the background for annual to multi-decade variations, such as "mega-droughts", and also provide a context for amplified rates of hydrologic change today.
Mandy Freund, Benjamin J. Henley, David J. Karoly, Kathryn J. Allen, and Patrick J. Baker
Clim. Past, 13, 1751–1770, https://doi.org/10.5194/cp-13-1751-2017, https://doi.org/10.5194/cp-13-1751-2017, 2017
Short summary
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To understand how climate change will influence Australian rainfall we must first understand the long-term context of droughts and floods. We reconstruct warm and cool season rainfall in Australia's eight major climatic regions for several centuries into the past, building the clearest picture yet of long-term rainfall variability across the Australian continent. We find recent rainfall increases in the warm season in the north, and declines in the cool season in the south, to be highly unusual.
Jasper G. Franke, Johannes P. Werner, and Reik V. Donner
Clim. Past, 13, 1593–1608, https://doi.org/10.5194/cp-13-1593-2017, https://doi.org/10.5194/cp-13-1593-2017, 2017
Short summary
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We apply evolving functional network analysis, a tool for studying temporal changes of the spatial co-variability structure, to a set of
Late Holocene paleoclimate proxy records covering the last two millennia. The emerging patterns obtained by our analysis are related to
long-term changes in the dominant mode of atmospheric circulation in the region, the North Atlantic Oscillation (NAO). We obtain a
qualitative reconstruction of the NAO long-term variability over the entire Common Era.
Jack Longman, Daniel Veres, Vasile Ersek, Ulrich Salzmann, Katalin Hubay, Marc Bormann, Volker Wennrich, and Frank Schäbitz
Clim. Past, 13, 897–917, https://doi.org/10.5194/cp-13-897-2017, https://doi.org/10.5194/cp-13-897-2017, 2017
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We present the first record of dust input into an eastern European bog over the past 10 800 years. We find significant changes in past dust deposition, with large inputs related to both natural and human influences. We show evidence that Saharan desertification has had a significant impact on dust deposition in eastern Europe for the past 6100 years.
B. Wilhelm, H. Vogel, C. Crouzet, D. Etienne, and F. S. Anselmetti
Clim. Past, 12, 299–316, https://doi.org/10.5194/cp-12-299-2016, https://doi.org/10.5194/cp-12-299-2016, 2016
Short summary
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The long-term response of the flood activity to both Atlantic and Mediterranean climatic influences was explored by reconstructing the Foréant record. Both influences result in a higher flood frequency during past cold periods. Atlantic influences seem to result in more frequent high-intensity flood events during past warm periods, suggesting an increase in flood intensity under the global warming. However, no high-intensity events occurred during the 20th century.
C. S. M. Turney, R. T. Jones, C. Fogwill, J. Hatton, A. N. Williams, A. Hogg, Z. A. Thomas, J. Palmer, S. Mooney, and R. W. Reimer
Clim. Past, 12, 189–200, https://doi.org/10.5194/cp-12-189-2016, https://doi.org/10.5194/cp-12-189-2016, 2016
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Southern Hemisphere westerly airflow is considered a major driver of Southern Ocean and global climate. Observational records, however, are limited. Here we present a new Falkland Islands record that exploits "exotic" South America pollen and charcoal to reconstruct changing airflow. We find stronger winds 2000–1000 cal. yr BP, associated with increased burning, and a 250-year periodicity, suggesting solar forcing. Our results have important implications for understanding late Holocene climates.
J. F. Donges, R. V. Donner, N. Marwan, S. F. M. Breitenbach, K. Rehfeld, and J. Kurths
Clim. Past, 11, 709–741, https://doi.org/10.5194/cp-11-709-2015, https://doi.org/10.5194/cp-11-709-2015, 2015
Short summary
Short summary
Paleoclimate records from cave deposits allow the reconstruction of Holocene dynamics of the Asian monsoon system, an important tipping element in Earth's climate. Employing recently developed techniques of nonlinear time series analysis reveals several robust and continental-scale regime shifts in the complexity of monsoonal variability. These regime shifts might have played an important role as drivers of migration, cultural change, and societal collapse during the past 10,000 years.
A. Mauri, B. A. S. Davis, P. M. Collins, and J. O. Kaplan
Clim. Past, 10, 1925–1938, https://doi.org/10.5194/cp-10-1925-2014, https://doi.org/10.5194/cp-10-1925-2014, 2014
R. de Jong, L. von Gunten, A. Maldonado, and M. Grosjean
Clim. Past, 9, 1921–1932, https://doi.org/10.5194/cp-9-1921-2013, https://doi.org/10.5194/cp-9-1921-2013, 2013
M. Mudelsee, J. Fohlmeister, and D. Scholz
Clim. Past, 8, 1637–1648, https://doi.org/10.5194/cp-8-1637-2012, https://doi.org/10.5194/cp-8-1637-2012, 2012
J. C. Stager, P. A. Mayewski, J. White, B. M. Chase, F. H. Neumann, M. E. Meadows, C. D. King, and D. A. Dixon
Clim. Past, 8, 877–887, https://doi.org/10.5194/cp-8-877-2012, https://doi.org/10.5194/cp-8-877-2012, 2012
B. Fréchette and A. de Vernal
Clim. Past, 5, 347–359, https://doi.org/10.5194/cp-5-347-2009, https://doi.org/10.5194/cp-5-347-2009, 2009
Cited articles
Adolphi, F. and Muscheler, R.: Synchronizing the Greenland ice core and radiocarbon timescales over the Holocene – Bayesian wiggle-matching of cosmogenic radionuclide records, Clim. Past, 12, 15–30, https://doi.org/10.5194/cp-12-15-2016, 2016.
Adolphi, F., Muscheler, R., Svensson, A., Aldahan, A., Possnert, G., Beer,
J., Sjolte, J., Björck, S., Matthes, K., and Thiéblemont, R.:
Persistent link between solar activity and Greenland climate during the Last
Glacial Maximum, Nat. Geosci., 7, 662–666, https://doi.org/10.1038/ngeo2225, 2014.
Berggren, A.-M., Aldahan, A., Possnert, G., Haltia-Hovi, E., and Saarinen,
T.: 10Be and solar activity cycles in varved lake sediments, AD 1900–2006, J. Paleolimnol., 44, 559–569, https://doi.org/10.1007/s10933-010-9437-1, 2010.
Bos, J. A. A., van Geel, B., van der Plicht, J., and Bohncke, S. J. P.:
Preboreal climate oscillations in Europe: Wiggle-match dating and synthesis
of Dutch high-resolution multi-proxy records, Quaternary Sci. Rev., 26,
1927–1950, https://doi.org/10.1016/j.quascirev.2006.09.012, 2007.
Björck, S., Kromer, B., Johnsen, S., Bennike, O., Hammarlund, D.,
Lemdahl, G., Possnert, G., Rasmussen, T. L., Wohlfarth, B., Hammer, C. U.,
and Spurk, M.: Synchronized Terrestrial-Atmospheric Deglacial Records Around
the North Atlantic, Science, 274, 1155–1160,
https://doi.org/10.1126/science.274.5290.1155, 1996.
Björck, S., Rundgren, M., Ingólfsson, Ó., and Funder, S.: The
Preboreal oscillation around the Nordic Seas: terrestrial and lacustrine
responses, J. Quaternary Sci., 12, 455–465,
https://doi.org/10.1002/(SICI)1099-1417(199711/12)12:6<455::AID-JQS316>3.0.CO;2-S, 1997.
Björck, S., Muscheler, R., Kromer, B., Andresen, C. S., Heinemeier, J.,
Johnsen, S. J., Conley, D., Koç, N., Spurk, M., and Veski, S.:
High-resolution analyses of an early Holocene climate event may imply
decreased solar forcing as an important climate trigger, Geology, 29,
1107, https://doi.org/10.1130/0091-7613(2001)029<1107:HRAOAE>2.0.CO;2, 2001.
Brauer, A., Endres, C., Günter, C., Litt, T., Stebich, M., and Negendank,
J. F. W.: High resolution sediment and vegetation responses to Younger Dryas
climate change in varved lake sediments from Meerfelder Maar, Germany, Quaternary Sci. Rev., 18, 321–329, https://doi.org/10.1016/S0277-3791(98)00084-5, 1999.
Brauer, A., Endres, C., Zolitschka, B., and Negendank, J. F.: AMS radiocarbon
and varve chronology from the annually laminated sediment record of Lake
Meerfelder Maar, Germany, Radiocarbon, 42, 355–368, 2000.
Bronk Ramsey, C., van der Plicht, J., and Weninger, B.: “Wiggle matching”
radiocarbon dates, Radiocarbon, 43, 381–390, 2001.
Compo, G. P., Whitaker, J. S., Sardeshmukh, P. D., Matsui, N., Allan, R. J.,
Yin, X., Gleason, B. E., Vose, R. S., Rutledge, G., Bessemoulin, P.,
Brönnimann, S., Brunet, M., Crouthamel, R. I., Grant, A. N., Groisman,
P. Y., Jones, P. D., Kruk, M. C., Kruger, A. C., Marshall, G. J., Maugeri,
M., Mok, H. Y., Nordli, Ø., Ross, T. F., Trigo, R. M., Wang, X. L.,
Woodruff, S. D., and Worley, S. J.: The Twentieth Century Reanalysis Project,
Q. J. Roy. Meteor. Soc., 137, 1–28, https://doi.org/10.1002/qj.776, 2011.
Czymzik, M., Adolphi, F., Muscheler, R., Mekhaldi, F., Martin-Puertas, C.,
Aldahan, A., Oran Possnert, G. €and Brauer, A.: A varved lake
sediment record of the 10Be solar activity proxy for the
Lateglacial-Holocene transition, Quaternary Sci. Rev., 153, 31–39,
https://doi.org/10.1016/j.quascirev.2016.10.007, 2016.
Czymzik, M., Muscheler, R., Adolphi, F., Mekhaldi, F., Dräger, N., Ott, F., Słowinski, M., Błaszkiewicz, M., Aldahan, A., Possnert, G., and Brauer, A.: Synchronizing 10Be in two varved lake sediment records to IntCal13 14C during three grand solar minima, Clim. Past, 14, 687–696, https://doi.org/10.5194/cp-14-687-2018, 2018.
Dansgaard, W.: Stable isotopes in precipitation, Tellus, 16, 436–468,
https://doi.org/10.3402/tellusa.v16i4.8993, 1964.
Duchez, A., Hirschi, J. J.-M, Cunningham, S. A., Blaker, A. T., Bryden, H.
L., De Cuevas, B., Atkinson, C. P., Mccarthy, G. D., Frajka-Williams, E.,
Rayner, D., Smeed, D., and Mizielinski, M. S.: A new index for the Atlantic
Meridional Overturning Circulation at 26∘ N, J. Climate, 27,
6439–6455, https://doi.org/10.1175/JCLI-D-13-00052.1, 2014.
Dyke, A. S.: An outline of North American deglaciation with emphasis on
central and northern Canada, Developments in Quaternary Sciences, 2, 373–424,
https://doi.org/10.1016/S1571-0866(04)80209-4, 2004.
Finkel, R. C. and Nishiizumi, K.: Beryllium 10 concentrations in the
Greenland Ice Sheet Project 2 ice core from 3–40 ka, J. Geophys. Res., 102, 26699–26706, https://doi.org/10.1029/97JC01282, 1997.
Fisher, T. G., Smith, D. G., and Andrews, J. T.: Preboreal oscillation caused
by a glacial Lake Agassiz flood, Quaternary Sci. Rev., 21, 873–878,
https://doi.org/10.1016/S0277-3791(01)00148-2, 2002.
Frankignoul, C., Gastineau, G., and Kwon, Y. O.: The influence of the AMOC
variability on the atmosphere in CCSM3, J. Climate, 26, 9774–9790,
https://doi.org/10.1175/JCLI-D-12-00862.1, 2013.
Gray, L. J., Scaife, A. A., Mitchell, D. M., Osprey, S., Ineson, S.,
Hardiman, S., Butchart, N., Knight, J., Sutton, R., and Kodera, K.: A lagged
response to the 11 year solar cycle in observed winter Atlantic/European
weather patterns, J. Geophys. Res.-Atmos., 118, 13405–13420,
https://doi.org/10.1002/2013JD020062, 2013.
Haigh, J. D., Winning, A. R., Toumi, R., and Harder, J. W.: An influence of
solar spectral variations on radiative forcing of climate, Nature,
467, 696–699, https://doi.org/10.1038/nature09426, 2010.
Hald, M. and Hagen, S.: Early Preboreal cooling in the Nordic seas region
triggered by meltwater, Geology, 26, 615–618, https://doi.org/10.1130/0091-7613(1998)026<0615:EPCITN>2.3.CO;2, 1998.
Ineson, S., Scaife, A. A., Knight, J. R., Manners, J. C., Dunstone, N. J.,
Gray, L. J., and Haigh, J. D.: Solar forcing of winter climate variability in
the Northern Hemisphere, Nat. Geosci., 4, 753–757,
https://doi.org/10.1038/ngeo1282, 2011.
Kobashi, T., Severinghaus, J. P., and Barnola, J.-M.: 4±1.5 ∘C abrupt warming 11,270 yr ago identified from trapped air
in Greenland ice, Earth Planet. Sc. Lett., 268, 397–407,
https://doi.org/10.1016/j.epsl.2008.01.032, 2008.
Kodera, K.: Solar cycle modulation of the North Atlantic Oscillation:
Implication in the spatial structure of the NAO, Geophys. Res. Lett., 29,
59-1–59-4, https://doi.org/10.1029/2001GL014557, 2002.
Lane, C. S., Brauer, A., Martín-Puertas, C., Blockley, S. P. E., Smith,
V. C., and Tomlinson, E. L.: The Late Quaternary tephrostratigraphy of
annually laminated sediments from Meerfelder Maar, Germany, Quaternary Sci. Rev., 122, 192–206, https://doi.org/10.1016/j.quascirev.2015.05.025, 2015.
Lockwood, M., Bell, C., Woollings, T., Harrison, R. G., Gray, L. J., and
Haigh, J. D.: Top-down solar modulation of climate: evidence for
centennial-scale change, Environ. Res. Lett., 5, 34008,
https://doi.org/10.1088/1748-9326/5/3/034008, 2010.
Löfverström, M. and Lora, J. M.: Abrupt regime shifts in the North
Atlantic atmospheric circulation over the last deglaciation, Geophys. Res.
Lett., 44, 8047–8055, https://doi.org/10.1002/2017GL074274, 2017.
Magny, M., Vannière, B., de Beaulieu, J.-L., Bégeot, C., Heiri, O.,
Millet, L., Peyron, O., and Walter-Simonnet, A.-V.: Early-Holocene climatic
oscillations recorded by lake-level fluctuations in west-central Europe and
in central Italy, Quaternary Sci. Rev., 26, 1951–1964,
https://doi.org/10.1016/j.quascirev.2006.04.013, 2007.
Martin-Puertas, C., Brauer, A., Dulski, P., and Brademann, B.: Testing
climate-proxy stationarity throughout the Holocene: an example from the
varved sediments of Lake Meerfelder Maar (Germany), Quaternary Sci. Rev., 58,
56–65, https://doi.org/10.1016/j.quascirev.2012.10.023, 2012a.
Martin-Puertas, C., Matthes, K., Brauer, A., Muscheler, R., Hansen, F.,
Petrick, C., Aldahan, A., Possnert, G., and van Geel, B.: Regional
atmospheric circulation shifts induced by a grand solar minimum, Nat.
Geosci., 5, 397–401, https://doi.org/10.1038/ngeo1460, 2012b.
Martin-Puertas, C., Tjallingii, R., Bloemsma, M., and Brauer, A.: Varved
sediment responses to early Holocene climate and environmental changes in
Lake Meerfelder Maar (Germany) obtained from multivariate analyses of micro
X-ray fluorescence core scanning data, J. Quaternary Sci., 32, 427–436,
https://doi.org/10.1002/jqs.2935, 2017.
Masson-Delmotte, V., Landais, A., Stievenard, M., Cattani, O., Falourd, S.,
Jouzel, J., Johnsen, S. J., Dahl-Jensen, D., Sveinsbjornsdottir, A., White,
J. W. C., Popp, T., and Fischer, H.: Holocene climatic changes in Greenland:
Different deuterium excess signals at Greenland Ice Core Project (GRIP) and
NorthGRIP, J. Geophys. Res., 110, D14102, https://doi.org/10.1029/2004JD005575, 2005.
Matthes, K., Kuroda, Y., Kodera, K., and Langematz, U.: Transfer of the solar
signal from the stratosphere to the troposphere: Northern winter, J.
Geophys. Res., 111, D06108, https://doi.org/10.1029/2005JD006283, 2006.
McCarthy, G. D., Haigh, I. D., Hirschi, J. J. M., Grist, J. P., and Smeed,
D. A.: Ocean impact on decadal Atlantic climate variability revealed by
sea-level observations, Nature, 521, 508–510, https://doi.org/10.1038/nature14491,
2015.
Mekhaldi, F.: 10Be concentrations from lake Meerfelder Maar during the earliest part of the Holocene, PANGAEA, https://doi.org/10.1594/PANGAEA.907808, 2019.
Merz, N., Raible, C. C., and Woollings, T.: North Atlantic Eddy-Driven Jet in
Interglacial and Glacial Winter Climates, J. Climate, 28, 3977–3997,
https://doi.org/10.1175/JCLI-D-14-00525.1, 2015.
Moffa-Sánchez, P., Born, A., Hall, I. R., Thornalley, D. J. R., and
Barker, S.: Solar forcing of North Atlantic surface temperature and salinity
over the past millennium, Nat. Geosci., 7, 275–278, https://doi.org/10.1038/ngeo2094, 2014.
Muscheler, R., Beer, J., Wagner, G., Laj, C., Kissel, C., Raisbeck, G. M.,
Yiou, F., and Kubik, P. W.: Changes in the carbon cycle during the last
deglaciation as indicated by the comparison of 10Be and 14C records, Earth Planet. Sci. Lett., 219, 325–340, https://doi.org/10.1016/S0012-821X(03)00722-2, 2004.
Muscheler, R., Kromer, B., Björck, S., Svensson, A., Friedrich, M.,
Kaiser, K. F., and Southon, J.: Tree rings and ice cores reveal 14C
calibration uncertainties during the Younger Dryas, Nat. Geosci., 1, 263–267, https://doi.org/10.1038/ngeo128, 2008.
Muscheler, R., Adolphi, F., and Knudsen, M. F.: Assessing the differences
between the IntCal and Greenland ice-core time scales for the last 14,000
years via the common cosmogenic radionuclide variations, Quaternary Sci. Rev., 106, 81–87, https://doi.org/10.1016/j.quascirev.2014.08.017, 2014.
Ortega, P., Lehner, F., Swingedouw, D., Masson-Delmotte, V., Raible, C. C.,
Casado, M., and Yiou, P.: A model-tested North Atlantic Oscillation
reconstruction for the past millennium, Nature, 523, 71–74, https://doi.org/10.1038/nature14518, 2015.
Pedro, J. B., Mcconnell, J. R., Van Ommen, T. D., Fink, D., Curran, M. A.
J., Smith, A. M., Simon, K. J., Moy, A. D., and Das, S. B.: Solar and climate
influences on ice core 10Be records from Antarctica and Greenland during the neutron monitor era, Earth Planet. Sc. Lett., 355–356, 174–186,
https://doi.org/10.1016/j.epsl.2012.08.038, 2012.
Rach, O., Brauer, A., Wilkes, H., and Sachse, D.: Delayed hydrological
response to Greenland cooling at the onset of the Younger Dryas in western
Europe, Nat. Geosci., 7, 109–112, https://doi.org/10.1038/ngeo2053, 2014.
Rasmussen, S. O., Andersen, K. K., Svensson, A. M., Steffensen, J. P.,
Vinther, B. M., Clausen, H. B., Siggaard-Andersen, M.-L., Johnsen, S. J.,
Larsen, L. B., Dahl-Jensen, D., Bigler, M., Röthlisberger, R., Fischer,
H., Goto-Azuma, K., Hansson, M. E., and Ruth, U.: A new Greenland ice core
chronology for the last glacial termination, J. Geophys. Res., 111,
D06102, https://doi.org/10.1029/2005JD006079, 2006.
Rasmussen, S. O., Vinther, B. M., Clausen, H. B., and Andersen, K. K.: Early
Holocene climate oscillations recorded in three Greenland ice cores, Quaternary Sci. Rev., 26, 1907–1914, https://doi.org/10.1016/j.quascirev.2007.06.015,
2007.
Rasmussen, S. O., Bigler, M., Blockley, S. P., Blunier, T., Buchardt, S. L.,
Clausen, H. B., Cvijanovic, I., Dahl-Jensen, D., Johnsen, S. J., Fischer,
H., Gkinis, V., Guillevic, M., Hoek, W. Z., Lowe, J. J., Pedro, J. B., Popp,
T., Seierstad, I. K., Steffensen, J. P., Svensson, A. M., Vallelonga, P.,
Vinther, B. M., Walker, M. J. C., Wheatley, J. J., and Winstrup, M.: A
stratigraphic framework for abrupt climatic changes during the Last Glacial
period based on three synchronized Greenland ice-core records: refining and
extending the INTIMATE event stratigraphy, Quaternary Sci. Rev., 106, 14–28,
https://doi.org/10.1016/j.quascirev.2014.09.007, 2014.
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey,
C. B., Buck, C. E., Cheng, H., Edwards, R. L., Friedrich, M., Grootes, P.
M., Guilderson, T. P., Haflidason, H., Hajdas, I., Hatté, C., Heaton, T.
J., Hoffmann, D. L., Hogg, A. G., Hughen, K. A., Kaiser, K. F., Kromer, B.,
Manning, S. W., Niu, M., Reimer, R. W., Richards, D. A., Scott, E. M.,
Southon, J. R., Staff, R. A., Turney, C. S. M., and van der Plicht, J.:
IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal
BP, Radiocarbon, 55, 1869–1887, https://doi.org/10.2458/azu_js_rc.55.16947, 2013.
Seierstad, I. K., Abbott, P. M., Bigler, M., Blunier, T., Bourne, A. J.,
Brook, E., Buchardt, S. L., Buizert, C., Clausen, H. B., Cook, E.,
Dahl-Jensen, D., Davies, S. M., Guillevic, M., Johnsen, S. J., Pedersen, D.
S., Popp, T. J., Rasmussen, S. O., Severinghaus, J. P., Svensson, A., and
Vinther, B. M.: Consistently dated records from the Greenland GRIP, GISP2
and NGRIP ice cores for the past 104 ka reveal regional millennial-scale
δ18O gradients with possible Heinrich event imprint, Quaternary Sci. Rev., 106, 29–46, https://doi.org/10.1016/j.quascirev.2014.10.032, 2014.
Simpson, I. R., Blackburn, M., Haigh, J. D., Simpson, I. R., Blackburn, M.,
and Haigh, J. D.: The Role of Eddies in Driving the Tropospheric Response to
Stratospheric Heating Perturbations, J. Atmos. Sci., 66, 1347–1365,
https://doi.org/10.1175/2008jas2758.1, 2009.
Sjolte, J., Sturm, C., Adolphi, F., Vinther, B. M., Werner, M., Lohmann, G., and Muscheler, R.: Solar and volcanic forcing of North Atlantic climate inferred from a process-based reconstruction, Clim. Past, 14, 1179–1194, https://doi.org/10.5194/cp-14-1179-2018, 2018.
Southon, J.: A First Step to Reconciling the GRIP and GISP2 Ice-Core
Chronologies, 0–14,500 yr B.P., Quaternary Res., 57, 32–37,
https://doi.org/10.1006/qres.2001.2295, 2002.
Steig, E. J., Grootes, P. M., and Stuiver, M.: Seasonal Precipitation Timing
and Ice Core Records. Science, 266, 1885–1886,
https://doi.org/10.1126/science.266.5192.1885, 1994.
Stroeven, A. P., Hättestrand, C., Kleman, J., Heyman, J., Fabel, D.,
Fredin, O., Goodfellow, B. W., Harbor, J. M., Jansen, J. D., Olsen, L.,
Caffee, M. W., Fink, D., Lundqvist, J., Rosqvist, G. C., Strömberg, B.,
and Jansson, K. N.: Deglaciation of Fennoscandia, Quaternary Sci. Rev., 147,
91–121, https://doi.org/10.1016/j.quascirev.2015.09.016, 2016.
Stuiver, M. and Polach, H. A.: Discussion Reporting of 14C Data,
Radiocarbon, 19, 355–363, https://doi.org/10.1017/S0033822200003672, 1977.
Svalgaard, L. and Schatten, K. H.: Reconstruction of the Sunspot Group
Number: The Backbone Method, Sol. Phys., 291, 2653–2684,
https://doi.org/10.1007/s11207-015-0815-8, 2016.
Svensson, A., Andersen, K. K., Bigler, M., Clausen, H. B., Dahl-Jensen, D., Davies, S. M., Johnsen, S. J., Muscheler, R., Parrenin, F., Rasmussen, S. O., Röthlisberger, R., Seierstad, I., Steffensen, J. P., and Vinther, B. M.: A 60 000 year Greenland stratigraphic ice core chronology, Clim. Past, 4, 47–57, https://doi.org/10.5194/cp-4-47-2008, 2008.
van der Plicht, J., van Geel, B., Bohncke, S. J. P., Bos, J. A. A., Blaauw,
M., Speranza, A. O. M., Muscheler, R., and Björck, S.: The Preboreal
climate reversal and a subsequent solar-forced climate shift, J. Quaternary Sci., 19, 263–269, https://doi.org/10.1002/jqs.835, 2004.
Vinther, B. M., Clausen, H. B., Johnsen, S. J., Rasmussen, S. O., Andersen,
K. K., Buchardt, S. L., Dahl-Jensen, D., Seierstad, I. K.,
Siggaard-Andersen, M.-L., Steffensen, J. P., Svensson, A., Olsen, J., and
Heinemeier, J.: A synchronized dating of three Greenland ice cores
throughout the Holocene, J. Geophys. Res., 111, D13102,
https://doi.org/10.1029/2005JD006921, 2006.
Vinther, B. M., Buchardt, S. L., Clausen, H. B., Dahl-Jensen, D., Johnsen,
S. J., Fisher, D. A., Koerner, R. M., Raynaud, D., Lipenkov, V., Andersen,
K. K., Blunier, T., Rasmussen, S. O., Steffensen, J. P., and Svensson, A. M.:
Holocene thinning of the Greenland ice sheet, Nature, 461, 385–388,
https://doi.org/10.1038/nature08355, 2009.
von Grafenstein U., Erlenkeuser, H., Brauer, A., Jouzel, J., and Johnsen, S.
J.: A mid-european decadal isotope-climate record from 15,500 to 5000 years
B.P., Science, 284, 1654–1657, https://doi.org/10.1126/science.284.5420.1654, 1999.
Vonmoos, M., Beer, J., and Muscheler, R.: Large variations in Holocene solar
activity: Constraints from 10Be in the Greenland Ice Core Project ice core, J. Geophys. Res., 111, A10105, https://doi.org/10.1029/2005JA011500, 2006.
White, J. W. C., Barlow, L. K., Fisher, D., Grootes, P. M., Jouzel, J.,
Johnsen, S. J., Stuiver, M., and Clausen, H. B.: Stable isotope stacks from
GRIP and GISP ice cores, PANGAEA, https://doi.org/10.1594/PANGAEA.716878, 2009.
Woollings, T., Lockwood, M., Masato, G., Bell, C., and Gray, L.: Enhanced
signature of solar variability in Eurasian winter climate, Geophys. Res. Lett., 37, L20805, https://doi.org/10.1029/2010GL044601, 2010.
Short summary
Due to chronology uncertainties within paleoclimate archives, it is unclear how climate oscillations from different records relate to one another. By using radionuclides to synchronize Greenland ice cores and a German lake record over 11 000 years, we show that two oscillations observed in these records were not synchronous but terminated and began with the onset of a grand solar minimum. Both this and changes in ocean circulation could have played a role in the two climate oscillations.
Due to chronology uncertainties within paleoclimate archives, it is unclear how climate...
