Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-2031-2021
© Author(s) 2021. 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-17-2031-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
08 Oct 2021
Research article | Highlight paper |
| 08 Oct 2021
| 08 Oct 2021
Statistical characteristics of extreme daily precipitation during 1501 BCE–1849 CE in the Community Earth System Model
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Richard Blender
Meteorological Institute and Center for Earth System Research and Sustainability (CEN), University of Hamburg, Hamburg, Germany
Michael Sigl
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Martina Messmer
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Christoph C. Raible
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
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Anders Svensson, Dorthe Dahl-Jensen, Jørgen Peder Steffensen, Thomas Blunier, Sune O. Rasmussen, Bo M. Vinther, Paul Vallelonga, Emilie Capron, Vasileios Gkinis, Eliza Cook, Helle Astrid Kjær, Raimund Muscheler, Sepp Kipfstuhl, Frank Wilhelms, Thomas F. Stocker, Hubertus Fischer, Florian Adolphi, Tobias Erhardt, Michael Sigl, Amaelle Landais, Frédéric Parrenin, Christo Buizert, Joseph R. McConnell, Mirko Severi, Robert Mulvaney, and Matthias Bigler
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Thomas L. Frölicher, Luca Ramseyer, Christoph C. Raible, Keith B. Rodgers, and John Dunne
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In 1876, 1910, and 2005, Switzerland was impacted by extreme rainfall and floods. All events were linked to a Vb cyclone. We test a range of weather model setups (short spinup and standard physics are best) to understand the sensitivity of atmospheric dynamics. The simulated Vb cyclones are (not) well defined for 2005 and 1910 (1876). To reproduce the events, intense moisture flux from the right direction is needed. Storms that slightly deviate from an ideal path produce erroneous precipitation.
Dominic A. Winski, Tyler J. Fudge, David G. Ferris, Erich C. Osterberg, John M. Fegyveresi, Jihong Cole-Dai, Zayta Thundercloud, Thomas S. Cox, Karl J. Kreutz, Nikolas Ortman, Christo Buizert, Jenna Epifanio, Edward J. Brook, Ross Beaudette, Jeffrey Severinghaus, Todd Sowers, Eric J. Steig, Emma C. Kahle, Tyler R. Jones, Valerie Morris, Murat Aydin, Melinda R. Nicewonger, Kimberly A. Casey, Richard B. Alley, Edwin D. Waddington, Nels A. Iverson, Nelia W. Dunbar, Ryan C. Bay, Joseph M. Souney, Michael Sigl, and Joseph R. McConnell
Clim. Past, 15, 1793–1808, https://doi.org/10.5194/cp-15-1793-2019, https://doi.org/10.5194/cp-15-1793-2019, 2019
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A deep ice core was recently drilled at the South Pole to understand past variations in the Earth's climate. To understand the information contained within the ice, we present the relationship between the depth and age of the ice in the South Pole Ice Core. We found that the oldest ice in our record is from 54 302 ± 519 years ago. Our results show that, on average, 7.4 cm of snow falls at the South Pole each year.
Christoph C. Raible, Martina Messmer, Flavio Lehner, Thomas F. Stocker, and Richard Blender
Clim. Past, 14, 1499–1514, https://doi.org/10.5194/cp-14-1499-2018, https://doi.org/10.5194/cp-14-1499-2018, 2018
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Extratropical cyclones in winter and their characteristics are investigated in depth for the Atlantic European region from 850 to 2100 CE. During the Common Era, cyclone characteristics show pronounced variations mainly caused by internal variability of the coupled climate system. When anthropogenic forcing becomes dominant, a strong increase of extreme cyclone-related precipitation is found due to thermodynamics, though dynamical processes can play an important role during the last millennium.
Stefan Brönnimann, Jan Rajczak, Erich M. Fischer, Christoph C. Raible, Marco Rohrer, and Christoph Schär
Nat. Hazards Earth Syst. Sci., 18, 2047–2056, https://doi.org/10.5194/nhess-18-2047-2018, https://doi.org/10.5194/nhess-18-2047-2018, 2018
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Heavy precipitation events in Switzerland are expected to become more intense, but the seasonality also changes. Analysing a large set of model simulations, we find that annual maximum rainfall events become less frequent in late summer and more frequent in early summer and early autumn. The seasonality shift is arguably related to summer drying. Results suggest that changes in the seasonal cycle need to be accounted for when preparing for moderately extreme precipitation events.
Juan José Gómez-Navarro, Christoph C. Raible, Denica Bozhinova, Olivia Martius, Juan Andrés García Valero, and Juan Pedro Montávez
Geosci. Model Dev., 11, 2231–2247, https://doi.org/10.5194/gmd-11-2231-2018, https://doi.org/10.5194/gmd-11-2231-2018, 2018
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We carry out and compare two high-resolution simulations of the Alpine region in the period 1979–2005. We aim to improve the understanding of the local mechanisms leading to extreme events in this complex region. We compare both simulations to precipitation observations to assess the model performance, and attribute major biases to either model or boundary conditions. Further, we develop a new bias correction technique to remove systematic errors in simulated precipitation for impact studies.
Maida Zahid, Richard Blender, Valerio Lucarini, and Maria Caterina Bramati
Earth Syst. Dynam., 8, 1263–1278, https://doi.org/10.5194/esd-8-1263-2017, https://doi.org/10.5194/esd-8-1263-2017, 2017
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The southern part of Pakistan (Sindh province) has been exposed to frequent and intense temperature extremes recently and is highly vulnerable to their impacts due to lack of information on recurrence of extremes. In this paper for the first time we estimated the return levels of daily maximum temperatures and daily maximum wet-bulb temperatures over the different return periods in Sindh, which would help the local administrations to prioritize the regions in terms of adaptations.
PAGES Hydro2k Consortium
Clim. Past, 13, 1851–1900, https://doi.org/10.5194/cp-13-1851-2017, https://doi.org/10.5194/cp-13-1851-2017, 2017
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Water availability is fundamental to societies and ecosystems, but our understanding of variations in hydroclimate (including extreme events, flooding, and decadal periods of drought) is limited due to a paucity of modern instrumental observations. We review how proxy records of past climate and climate model simulations can be used in tandem to understand hydroclimate variability over the last 2000 years and how these tools can also inform risk assessments of future hydroclimatic extremes.
Martina Messmer, Juan José Gómez-Navarro, and Christoph C. Raible
Earth Syst. Dynam., 8, 477–493, https://doi.org/10.5194/esd-8-477-2017, https://doi.org/10.5194/esd-8-477-2017, 2017
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Low-pressure systems of type Vb may trigger heavy rainfall events over central Europe. This study aims at analysing the relative role of their moisture sources. For this, a set of sensitivity experiments encompassing changes in soil moisture and Atlantic Ocean and Mediterranean Sea SSTs are carried out with WRF. The latter moisture source stands out as the most relevant one. Furthermore, the regions most affected by Vb events in the future might be shifted from the Alps to the Balkan Peninsula.
Juan José Gómez-Navarro, Eduardo Zorita, Christoph C. Raible, and Raphael Neukom
Clim. Past, 13, 629–648, https://doi.org/10.5194/cp-13-629-2017, https://doi.org/10.5194/cp-13-629-2017, 2017
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This contribution aims at assessing to what extent the analogue method, a classic technique used in other branches of meteorology and climatology, can be used to perform gridded reconstructions of annual temperature based on the limited information from available but un-calibrated proxies spread across different locations of the world. We conclude that it is indeed possible, albeit with certain limitations that render the method comparable to more classic techniques.
Stefan Brönnimann, Abdul Malik, Alexander Stickler, Martin Wegmann, Christoph C. Raible, Stefan Muthers, Julien Anet, Eugene Rozanov, and Werner Schmutz
Atmos. Chem. Phys., 16, 15529–15543, https://doi.org/10.5194/acp-16-15529-2016, https://doi.org/10.5194/acp-16-15529-2016, 2016
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The Quasi-Biennial Oscillation is a wind oscillation in the equatorial stratosphere. Effects on climate have been found, which is relevant for seasonal forecasts. However, up to now only relatively short records were available, and even within these the climate imprints were intermittent. Here we analyze a 108-year long reconstruction as well as four 405-year long simulations. We confirm most of the claimed QBO effects on climate, but they are small, which explains apparently variable effects.
Chantal Camenisch, Kathrin M. Keller, Melanie Salvisberg, Benjamin Amann, Martin Bauch, Sandro Blumer, Rudolf Brázdil, Stefan Brönnimann, Ulf Büntgen, Bruce M. S. Campbell, Laura Fernández-Donado, Dominik Fleitmann, Rüdiger Glaser, Fidel González-Rouco, Martin Grosjean, Richard C. Hoffmann, Heli Huhtamaa, Fortunat Joos, Andrea Kiss, Oldřich Kotyza, Flavio Lehner, Jürg Luterbacher, Nicolas Maughan, Raphael Neukom, Theresa Novy, Kathleen Pribyl, Christoph C. Raible, Dirk Riemann, Maximilian Schuh, Philip Slavin, Johannes P. Werner, and Oliver Wetter
Clim. Past, 12, 2107–2126, https://doi.org/10.5194/cp-12-2107-2016, https://doi.org/10.5194/cp-12-2107-2016, 2016
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Throughout the last millennium, several cold periods occurred which affected humanity. Here, we investigate an exceptionally cold decade during the 15th century. The cold conditions challenged the food production and led to increasing food prices and a famine in parts of Europe. In contrast to periods such as the “Year Without Summer” after the eruption of Tambora, these extreme climatic conditions seem to have occurred by chance and in relation to the internal variability of the climate system.
Stefan Muthers, Christoph C. Raible, Eugene Rozanov, and Thomas F. Stocker
Earth Syst. Dynam., 7, 877–892, https://doi.org/10.5194/esd-7-877-2016, https://doi.org/10.5194/esd-7-877-2016, 2016
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The Atlantic Meridional Overturning Circulation (AMOC) is an important oceanic circulation system which transports large amounts of heat from the tropics to the north. This circulation is strengthened when less solar irradiance reaches the Earth, e.g. due to reduced solar activity or geoengineering techniques. In climate models, however, this response is overestimated when chemistry–climate interactions and the following shift in the atmospheric circulation systems are not considered.
Niklaus Merz, Andreas Born, Christoph C. Raible, and Thomas F. Stocker
Clim. Past, 12, 2011–2031, https://doi.org/10.5194/cp-12-2011-2016, https://doi.org/10.5194/cp-12-2011-2016, 2016
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The last (Eemian) interglacial is studied with a global climate model focusing on Greenland and the adjacent high latitudes. A set of model experiments demonstrates the crucial role of changes in sea ice and sea surface temperatures for the magnitude of Eemian atmospheric warming. Greenland temperatures are found highly sensitive to sea ice changes in the Nordic Seas but rather insensitive to changes in the Labrador Sea. This behavior has important implications for Greenland ice core signals.
Amaelle Landais, Valérie Masson-Delmotte, Emilie Capron, Petra M. Langebroek, Pepijn Bakker, Emma J. Stone, Niklaus Merz, Christoph C. Raible, Hubertus Fischer, Anaïs Orsi, Frédéric Prié, Bo Vinther, and Dorthe Dahl-Jensen
Clim. Past, 12, 1933–1948, https://doi.org/10.5194/cp-12-1933-2016, https://doi.org/10.5194/cp-12-1933-2016, 2016
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The last lnterglacial (LIG; 116 000 to 129 000 years before present) surface temperature at the upstream Greenland NEEM deposition site is estimated to be warmer by +7 to +11 °C compared to the preindustrial period. We show that under such warm temperatures, melting of snow probably led to a significant surface melting. There is a paradox between the extent of the Greenland ice sheet during the LIG and the strong warming during this period that models cannot solve.
J. J. Gómez-Navarro, C. C. Raible, and S. Dierer
Geosci. Model Dev., 8, 3349–3363, https://doi.org/10.5194/gmd-8-3349-2015, https://doi.org/10.5194/gmd-8-3349-2015, 2015
S. Muthers, F. Arfeuille, C. C. Raible, and E. Rozanov
Atmos. Chem. Phys., 15, 11461–11476, https://doi.org/10.5194/acp-15-11461-2015, https://doi.org/10.5194/acp-15-11461-2015, 2015
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After volcanic eruptions different radiative and chemical processes take place in the stratosphere which perturb the ozone layer and cause pronounced dynamical changes. In idealized chemistry-climate model simulations the importance of these processes and the modulating role of the climate state is analysed. The chemical effect strongly differs between a preindustrial and present-day climate, but the effect on the dynamics is weak. Radiative processes dominate the dynamics in all climate states.
M. Messmer, J. J. Gómez-Navarro, and C. C. Raible
Earth Syst. Dynam., 6, 541–553, https://doi.org/10.5194/esd-6-541-2015, https://doi.org/10.5194/esd-6-541-2015, 2015
J. J. Gómez-Navarro, O. Bothe, S. Wagner, E. Zorita, J. P. Werner, J. Luterbacher, C. C. Raible, and J. P Montávez
Clim. Past, 11, 1077–1095, https://doi.org/10.5194/cp-11-1077-2015, https://doi.org/10.5194/cp-11-1077-2015, 2015
F. Lehner, F. Joos, C. C. Raible, J. Mignot, A. Born, K. M. Keller, and T. F. Stocker
Earth Syst. Dynam., 6, 411–434, https://doi.org/10.5194/esd-6-411-2015, https://doi.org/10.5194/esd-6-411-2015, 2015
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We present the first last-millennium simulation with the Community Earth System Model (CESM) including an interactive carbon cycle in both ocean and land component. Volcanic eruptions emerge as the strongest forcing factor for the preindustrial climate and carbon cycle. We estimate the climate-carbon-cycle feedback in CESM to be at the lower bounds of empirical estimates (1.3ppm/°C). The time of emergence for interannual global land and ocean carbon uptake rates are 1947 and 1877, respectively.
D. Zanchettin, O. Bothe, F. Lehner, P. Ortega, C. C. Raible, and D. Swingedouw
Clim. Past, 11, 939–958, https://doi.org/10.5194/cp-11-939-2015, https://doi.org/10.5194/cp-11-939-2015, 2015
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A discrepancy exists between reconstructed and simulated Pacific North American pattern (PNA) features during the early 19th century. Pseudo-reconstructions demonstrate that the available PNA reconstruction is potentially skillful but also potentially affected by a number of sources of uncertainty and deficiencies especially at multidecadal and centennial timescales. Simulations and reconstructions can be reconciled by attributing the reconstructed PNA features to internal variability.
S. Muthers, J. G. Anet, A. Stenke, C. C. Raible, E. Rozanov, S. Brönnimann, T. Peter, F. X. Arfeuille, A. I. Shapiro, J. Beer, F. Steinhilber, Y. Brugnara, and W. Schmutz
Geosci. Model Dev., 7, 2157–2179, https://doi.org/10.5194/gmd-7-2157-2014, https://doi.org/10.5194/gmd-7-2157-2014, 2014
K. M. Keller, F. Joos, and C. C. Raible
Biogeosciences, 11, 3647–3659, https://doi.org/10.5194/bg-11-3647-2014, https://doi.org/10.5194/bg-11-3647-2014, 2014
N. Merz, A. Born, C. C. Raible, H. Fischer, and T. F. Stocker
Clim. Past, 10, 1221–1238, https://doi.org/10.5194/cp-10-1221-2014, https://doi.org/10.5194/cp-10-1221-2014, 2014
J. G. Anet, S. Muthers, E. V. Rozanov, C. C. Raible, A. Stenke, A. I. Shapiro, S. Brönnimann, F. Arfeuille, Y. Brugnara, J. Beer, F. Steinhilber, W. Schmutz, and T. Peter
Clim. Past, 10, 921–938, https://doi.org/10.5194/cp-10-921-2014, https://doi.org/10.5194/cp-10-921-2014, 2014
C. C. Raible, F. Lehner, J. F. González-Rouco, and L. Fernández-Donado
Clim. Past, 10, 537–550, https://doi.org/10.5194/cp-10-537-2014, https://doi.org/10.5194/cp-10-537-2014, 2014
J. G. Anet, S. Muthers, E. Rozanov, C. C. Raible, T. Peter, A. Stenke, A. I. Shapiro, J. Beer, F. Steinhilber, S. Brönnimann, F. Arfeuille, Y. Brugnara, and W. Schmutz
Atmos. Chem. Phys., 13, 10951–10967, https://doi.org/10.5194/acp-13-10951-2013, https://doi.org/10.5194/acp-13-10951-2013, 2013
N. Merz, C. C. Raible, H. Fischer, V. Varma, M. Prange, and T. F. Stocker
Clim. Past, 9, 2433–2450, https://doi.org/10.5194/cp-9-2433-2013, https://doi.org/10.5194/cp-9-2433-2013, 2013
Related subject area
Subject: Atmospheric Dynamics | Archive: Modelling only | Timescale: Decadal-Seasonal
Extratropical circulation associated with Mediterranean droughts during the Last Millennium in CMIP5 simulations
Evaluation of statistical climate reconstruction methods based on pseudoproxy experiments using linear and machine-learning methods
Dynamics of the Mediterranean droughts from 850 to 2099 CE in the Community Earth System Model
A pseudoproxy assessment of data assimilation for reconstructing the atmosphere–ocean dynamics of hydroclimate extremes
Synoptic climatology and recent climate trends at Lake El'gygytgyn
Woon Mi Kim, Santos J. González-Rojí, and Christoph C. Raible
Clim. Past, 19, 2511–2533, https://doi.org/10.5194/cp-19-2511-2023, https://doi.org/10.5194/cp-19-2511-2023, 2023
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In this study, we investigate circulation patterns associated with Mediterranean droughts during the last millennium using global climate simulations. Different circulation patterns driven by internal interactions in the climate system contribute to the occurrence of droughts in the Mediterranean. The detected patterns are different between the models, and this difference can be a potential source of uncertainty in model–proxy comparison and future projections of Mediterranean droughts.
Zeguo Zhang, Sebastian Wagner, Marlene Klockmann, and Eduardo Zorita
Clim. Past, 18, 2643–2668, https://doi.org/10.5194/cp-18-2643-2022, https://doi.org/10.5194/cp-18-2643-2022, 2022
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A bidirectional long short-term memory (LSTM) neural network was employed for the first time for past temperature field reconstructions. The LSTM method tested in our experiments using a limited calibration and validation dataset shows worse reconstruction skills compared to traditional reconstruction methods. However, a certain degree of reconstruction performance achieved by the nonlinear LSTM method shows that skill can be achieved even when using small samples with limited datasets.
Woon Mi Kim and Christoph C. Raible
Clim. Past, 17, 887–911, https://doi.org/10.5194/cp-17-887-2021, https://doi.org/10.5194/cp-17-887-2021, 2021
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The analysis of the dynamics of western central Mediterranean droughts for 850–2099 CE in the Community Earth System Model indicates that past Mediterranean droughts were driven by the internal variability. This internal variability is more important during the initial years of droughts. During the transition years, the longevity of droughts is defined by the land–atmosphere feedbacks. In the future, this land–atmosphere feedbacks are intensified, causing a constant dryness over the region.
Nathan J. Steiger and Jason E. Smerdon
Clim. Past, 13, 1435–1449, https://doi.org/10.5194/cp-13-1435-2017, https://doi.org/10.5194/cp-13-1435-2017, 2017
M. Nolan, E. N. Cassano, and J. J. Cassano
Clim. Past, 9, 1271–1286, https://doi.org/10.5194/cp-9-1271-2013, https://doi.org/10.5194/cp-9-1271-2013, 2013
Cited articles
Allen, M. R. and Ingram, W. J.:
Constraints on future changes in climate and the hydrologic cycle,
Nature, 419, 228–232, https://doi.org/10.1038/nature01092, 2002. a, b, c, d
Asadieh, B. and Krakauer, N. Y.: Global trends in extreme precipitation: climate models versus observations, Hydrol. Earth Syst. Sci., 19, 877–891, https://doi.org/10.5194/hess-19-877-2015, 2015. a, b
Berger, A.:
Long-term variations of daily insolation and Quaternary climatic changes,
J. Atmos. Sci.,
35, 2362–2367, https://doi.org/10.1175/1520-0469(1978)035<2362:LTVODI>2.0.CO;2, 1978. a
Boer, G.:
Climate change and the regulation of the surface moisture and energy budgets,
Clim. Dynam.,
8, 225–239, https://doi.org/10.1007/BF00198617, 1993. a
Brázdil, R., Kundzewicz, Z. W., Benito, G., Demarée, G., Macdonald, N., and Roland, L. A.: Historical floods in Europe in the past millennium,
in: Changes in Flood Risk in Europe,
edited by: Kundzewicz, Z. W.,
IAHS Press, Wallingford, pp. 121–166, 2012. a
Büntgen, U., Tegel, W., Nicolussi, K., McCormick, M., Frank, D., Trouet, V., Kaplan, J. O., Herzig, F., Heussner, K.-U., Wanner, H., Luterbacher, J., and Esper, J.:
2500 years of European climate variability and human susceptibility,
Science,
331, 578–582, https://doi.org/10.1126/science.1197175, 2011. a
Byrne, M. P. and O'Gorman, P. A.:
The response of precipitation minus evapotranspiration to climate warming: Why the “wet-get-wetter, dry-get-drier” scaling does not hold over land,
J. Climate,
28, 8078–8092, https://doi.org/10.1175/JCLI-D-15-0369.1, 2015. a
Carn, S., Clarisse, L., and Prata, A. J.:
Multi-decadal satellite measurements of global volcanic degassing,
J. Volcanol. Geoth. Res.,
311, 99–134, https://doi.org/10.1016/j.jvolgeores.2016.01.002, 2016. a, b
Chadwick, R., Boutle, I., and Martin, G.:
Spatial patterns of precipitation change in CMIP5: Why the rich do not get richer in the tropics,
J. Climate,
26, 3803–3822, https://doi.org/10.1175/JCLI-D-12-00543.1, 2013. a
Champion, A. J., Hodges, K. I., Bengtsson, L. O., Keenlyside, N. S., and Esch, M.:
Impact of increasing resolution and a warmer climate on extreme weather from Northern Hemisphere extratropical cyclones,
Tellus A,
63, 893–906, https://doi.org/10.1111/j.1600-0870.2011.00538.x, 2011. a, b
Chen, H., Sun, J., and Li, H.:
Increased population exposure to precipitation extremes under future warmer climates,
Environ. Res. Lett.,
15, 034 048, https://doi.org/10.1088/1748-9326/ab751f, publisher: IOP Publishing, 2020. a
Chou, C. and Neelin, J. D.:
Mechanisms of global warming impacts on regional tropical precipitation,
J. Climate,
17, 2688–2701, https://doi.org/10.1175/1520-0442(2004)017<2688:MOGWIO>2.0.CO;2, 2004. a
Chou, C., Neelin, J. D., Chen, C.-A., and Tu, J.-Y.:
Evaluating the “rich-get-richer” mechanism in tropical precipitation change under global warming,
J. Climate,
22, 1982–2005, https://doi.org/10.1175/2008JCLI2471.1, 2009. a
Contractor, S., Donat, M. G., and Alexander, L. V.:
Changes in Observed Daily Precipitation over Global Land Areas since 1950,
J. Climate,
34, 3–19, https://doi.org/10.1175/JCLI-D-19-0965.1, 2021. a
Dai, A. and Wigley, T.:
Global patterns of ENSO-induced precipitation,
Geophys. Res. Lett.,
27, 1283–1286, https://doi.org/10.1029/1999GL011140, 2000. a
Dallmeyer, A., Claussen, M., Lorenz, S. J., Sigl, M., Toohey, M., and Herzschuh, U.: Holocene vegetation transitions and their climatic drivers in MPI-ESM1.2, Clim. Past Discuss. [preprint], https://doi.org/10.5194/cp-2021-51, in review, 2021. a
Dee, S. G., Cobb, K. M., Emile-Geay, J., Ault, T. R., Edwards, R. L., Cheng, H., and Charles, C. D.:
No consistent ENSO response to volcanic forcing over the last millennium,
Science,
367, 1477–1481, https://doi.org/10.1126/science.aax2000, 2020. a
Della-Marta, P. M., Mathis, H., Frei, C., Liniger, M. A., Kleinn, J., and Appenzeller, C.:
The return period of wind storms over Europe,
Int. J. Climatol.,
29, 437–459, https://doi.org/10.1002/joc.1794, 2009. a
DeMenocal, P. B.:
Cultural responses to climate change during the late Holocene,
Science,
292, 667–673, https://doi.org/10.1126/science.1059287, 2001. a
El Adlouni, S., Ouarda, T. B., Zhang, X., Roy, R., and Bobée, B.:
Generalized maximum likelihood estimators for the nonstationary generalized extreme value model, Water Resour. Res.,
43, W03410, https://doi.org/10.1029/2005WR004545, 2007. a
European Centre for Medium-Range Weather Forecasts: ERA5 Reanalysis, Research Data Archive at the National Center for Atmospheric Research, Computational and Information Systems Laboratory, updated monthly,
https://doi.org/10.5065/D6X34W69, 2017. a
Fasullo, J. T., Phillips, A., and Deser, C.:
Evaluation of leading modes of climate variability in the CMIP archives,
J. Climate,
33, 5527–5545, https://doi.org/10.1175/JCLI-D-19-1024.1, 2020. a
Fischer, E. M. and Knutti, R.:
Observed heavy precipitation increase confirms theory and early models,
Nat. Clim. Change,
6, 986–991, https://doi.org/10.1038/nclimate3110, 2016. a, b
Flato, G., Marotzke, J., Abiodun, B., Braconnot, P., Chou, S. C., Collins, W., Cox, P., Driouech, F., Emori, S., Eyring, V., Forest, C., Gleckler, P., Guilyardi, E., Jakob, C., Kattsov, V., Reason, C., and Rummukainen, M.:
Evaluation of climate models,
in: Climate change 2013: the physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Stocker, T. F., Qin, D., Plattner, G.-K., Tignor, M., Allen, S. K., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P. M., Cambridge University Press, Cambridge, UK and New York, NY, USA, 741–866, 2014. a, b
Gao, C., Robock, A., and Ammann, C.:
Volcanic forcing of climate over the past 1500 years: An improved ice core-based index for climate models,
J. Geophys. Res.-Atmos.,
113, D23111, https://doi.org/10.1029/2008JD010239, 2008. a, b, c
Giles, D. E., Feng, H., and Godwin, R. T.:
Bias-corrected maximum likelihood estimation of the parameters of the generalized Pareto distribution,
Commun. Stat. Theory,
45, 2465–2483, https://doi.org/10.1080/03610926.2014.887104, 2016. a
Gilleland, E. and Katz, R. W.:
extRemes 2.0: An extreme value analysis package in R,
J. Stat. Softw.,
72, 1–39, https://doi.org/10.18637/jss.v072.i08, 2016. a
Gilleland, E. R.: Extreme Value Analysis, available at: https://CRAN.R-project.org/package=extRemes, last access: 1 May 2021. a
Glaser, R., Riemann, D., Schönbein, J., Barriendos, M., Brázdil, R., Bertolin, C., Camuffo, D., Deutsch, M., Dobrovolný, P., van Engelen, A., Enzi, S., Halíčková, M., Koenig, S. J., Kotyza, O., Limanówka, D., Macková, J., Sghedoni, M., Martin, B., and Himmelsbach, I.:
The variability of European floods since AD 1500,
Climatic Change,
101, 235–256, https://doi.org/10.1007/s10584-010-9816-7, 2010. a
Heffernan, J. E. and Stephenson, A. G.: ismev: An Introduction to Statistical Modeling of Extreme Values [code], available at: https://CRAN.R-project.org/package=ismev (last access: 1 May 2021), 2018. a
Hersbach, H., Bell, B., Berrisford, P., Hirahara, S., Horányi, A., Muñoz–Sabater, J., Nicolas, J., Peubey, C., Radu, R., Schepers, D., Simmons, A., Soci, C., Abdalla, S., Abellan, X., Balsamo, G., Bechtold, P., Biavati, G., Bidlot, J., Bonavita, M., Chiara, G. D., Dahlgren, P., Dee, D., Diamantakis, M., Dragani, R., Flemming, J., Forbes, R., Fuentes, M., Geer, A., Haimberger, L., Healy, S., Hogan, R. J., Hólm, E., Janisková, M., Keeley, S., Laloyaux, P., Lopez, P., Lupu, C., Radnoti, G., Rosnay, P. d., Rozum, I., Vamborg, F., Villaume, S., and Thépaut, J.-N.:
The ERA5 global reanalysis,
Q. J.Roy. Meteorol. Soc.,
146, 1999–2049, https://doi.org/10.1002/qj.3803, 2020. a, b
Hodell, D. A., Curtis, J. H., and Brenner, M.:
Possible role of climate in the collapse of Classic Maya civilization,
Nature,
375, 391–394, https://doi.org/10.1038/375391a0, 1995. a
Hofmann, D. J.:
Perturbations to the global atmosphere associated with the El Chichon volcanic eruption of 1982,
Rev. Geophys.,
25, 743–759, https://doi.org/10.1029/RG025i004p00743, 1987. a
Huang, B., Thorne, P. W., Banzon, V. F., Boyer, T., Chepurin, G., Lawrimore, J. H., Menne, M. J., Smith, T. M., Vose, R. S., and Zhang, H.-M.:
NOAA Extended Reconstructed Sea Surface Temperature (ERSST), Version 5, NOAA National Centers for Environmental Information [dataset],
https://doi.org/10.7289/V5T72FNM, 2017. a
Hunke, E. C., Lipscomb, W. H., Turner, A. K., Jeffery, N., and Elliott, S.:
Cice: the los alamos sea ice model documentation and software user's manual version 4.1 la-cc-06-012, T-3
Fluid Dynamics Group, Los Alamos National Laboratory, 675, 500, 2010. a
Hurrell, J. W., Holland, M. M., Gent, P. R., Ghan, S., Kay, J. E., Kushner, P. J., Lamarque, J.-F., Large, W. G., Lawrence, D., Lindsay, K., Lipscomb, W. H., Long, M. C., Mahowald, N., Marsh, D. R., Neale, R. B., Rasch, P., Vavrus, S., Vertenstein, M., Bader, D., Collins, W. D., Hack, J. J., Kiehl, J., and Marshall, S.:
The community earth system model: a framework for collaborative research,
B. Am. Meteorol. Soc.,
94, 1339–1360, https://doi.org/10.1175/BAMS-D-12-00121.1, 2013. a
Hurtt, G. C., Chini, L. P., Frolking, S., Betts, R., Feddema, J., Fischer, G., Fisk, J., Hibbard, K., Houghton, R., Janetos, A., Jones, C. D., Kindermann, G., Kinoshita, T., Kees Klein Goldewijk, Riahi, K., Shevliakova, E., Smith S., Stehfest, E., Thomson, A., Thornton, P., van Vuuren, D. P., and Wang, Y. P.:
Harmonization of land-use scenarios for the period 1500–2100: 600 years of global gridded annual land-use transitions, wood harvest, and resulting secondary lands,
Climatic Change,
109, 117–161, https://doi.org/10.1007/s10584-011-0153-2, 2011. a
Iles, C. E. and Hegerl, G. C.:
The global precipitation response to volcanic eruptions in the CMIP5 models,
Environ. Res. Lett.,
9, 104012, https://doi.org/10.1088/1748-9326/9/10/104012, 2014. a, b
Iles, C. E., Hegerl, G. C., Schurer, A. P., and Zhang, X.:
The effect of volcanic eruptions on global precipitation,
J. Geophys. Res.-Atmos.,
118, 8770–8786, https://doi.org/10.1002/jgrd.50678, 2013. a, b
Jacobeit, J., Glaser, R., Luterbacher, J., and Wanner, H.:
Links between flood events in central Europe since AD 1500 and large-scale atmospheric circulation modes, Geophys. Res. Lett., 30, 1172, https://doi.org/10.1029/2002GL016433, 2003. a
Joos, F. and Spahni, R.:
Rates of change in natural and anthropogenic radiative forcing over the past 20,000 years,
P. Natl. Acad. Sci. USA,
105, 1425–1430, https://doi.org/10.1073/pnas.0707386105, 2008. a, b, c, d
Jungclaus, J. H., Bard, E., Baroni, M., Braconnot, P., Cao, J., Chini, L. P., Egorova, T., Evans, M., González-Rouco, J. F., Goosse, H., Hurtt, G. C., Joos, F., Kaplan, J. O., Khodri, M., Klein Goldewijk, K., Krivova, N., LeGrande, A. N., Lorenz, S. J., Luterbacher, J., Man, W., Maycock, A. C., Meinshausen, M., Moberg, A., Muscheler, R., Nehrbass-Ahles, C., Otto-Bliesner, B. I., Phipps, S. J., Pongratz, J., Rozanov, E., Schmidt, G. A., Schmidt, H., Schmutz, W., Schurer, A., Shapiro, A. I., Sigl, M., Smerdon, J. E., Solanki, S. K., Timmreck, C., Toohey, M., Usoskin, I. G., Wagner, S., Wu, C.-J., Yeo, K. L., Zanchettin, D., Zhang, Q., and Zorita, E.:
The PMIP4 contribution to CMIP6 – Part 3: The last millennium, scientific objective, and experimental design for the PMIP4 past1000 simulations, Geosci. Model Dev., 10, 4005–4033, https://doi.org/10.5194/gmd-10-4005-2017, 2017. a, b, c
Kawai, H., Yukimoto, S., Koshiro, T., Oshima, N., Tanaka, T., Yoshimura, H., and Nagasawa, R.: Significant improvement of cloud representation in the global climate model MRI-ESM2, Geosci. Model Dev., 12, 2875–2897, https://doi.org/10.5194/gmd-12-2875-2019, 2019. a
Kenyon, J. and Hegerl, G. C.:
Influence of Modes of Climate Variability on Global Precipitation Extremes,
J. Climate,
23, 6248–6262, https://doi.org/10.1175/2010JCLI3617.1, 2010. a, b
Khaliq, M. N., Ouarda, T. B., Ondo, J.-C., Gachon, P., and Bobée, B.:
Frequency analysis of a sequence of dependent and/or non-stationary hydro-meteorological observations: A review,
J. Hydrol.,
329, 534–552, https://doi.org/10.1016/j.jhydrol.2006.03.004, 2006. a
Kharin, V. V., Zwiers, F. W., Zhang, X., and Wehner, M.:
Changes in temperature and precipitation extremes in the CMIP5 ensemble,
Climatic Change,
119, 345–357, https://doi.org/10.1007/s10584-013-0705-8, 2013. a, b
Kim, W. M.: wmk21/EVT-D-statistics-comparison: EVT-D-statistics-comparison (EVT-D-statistics), Zenodo [code], https://doi.org/10.5281/zenodo.5553094, 2021. a
Kim, W. M. and Raible, C. C.: Dynamics of the Mediterranean droughts from 850 to 2099 CE in the Community Earth System Model, Clim. Past, 17, 887–911, https://doi.org/10.5194/cp-17-887-2021, 2021. a
Kim, W. M., Blender, R., Sigl, M., Messmer, M., and Raible, C. C.: Data for publication “Statistical characteristics of extreme daily precipitation during 1501 BCE–1849 CE in the Community Earth System Model”, Zenodo [data set], https://doi.org/10.5281/zenodo.5513689, 2021. a
Kjeldsen, T. R., Macdonald, N., Lang, M., Mediero, L., Albuquerque, T., Bogdanowicz, E., Brázdil, R., Castellarin, A., David, V., Fleig, A., Gül, G. O., Kriauciuniene, J., Kohnová, S., Merz, B., Nicholson, O., Roald, L. A., Salinas, J. L., Sarauskiene, D., Šraj, M., Strupczewski, W., Szolgay, J., Toumazis, A., Vanneuville, W., Veijalainen, N., and Wilson, D.:
Documentary evidence of past floods in Europe and their utility in flood frequency estimation,
J. Hydrol.,
517, 963–973, https://doi.org/10.1016/j.jhydrol.2014.06.038, 2014. a
Kopparla, P., Fischer, E. M., Hannay, C., and Knutti, R.:
Improved simulation of extreme precipitation in a high-resolution atmosphere model,
Geophys. Res. Lett.,
40, 5803–5808, https://doi.org/10.1002/2013GL057866, 2013. a, b
Lawrence, D. M., Oleson, K. W., Flanner, M. G., Thornton, P. E., Swenson, S. C., Lawrence, P. J., Zeng, X., Yang, Z.-L., Levis, S., Sakaguchi, K., Bonan, G. B., and Slater, A. G.:
Parameterization improvements and functional and structural advances in version 4 of the Community Land Model,
J. Adv. Model. Earth Sy.,
3, M03001, https://doi.org/10.1029/2011MS00045, 2011. a
Lehner, F., Joos, F., Raible, C. C., Mignot, J., Born, A., Keller, K. M., and Stocker, T. F.: Climate and carbon cycle dynamics in a CESM simulation from 850 to 2100 CE, Earth Syst. Dynam., 6, 411–434, https://doi.org/10.5194/esd-6-411-2015, 2015. a
Machado, M. J., Botero, B. A., López, J., Francés, F., Díez-Herrero, A., and Benito, G.: Flood frequency analysis of historical flood data under stationary and non-stationary modelling, Hydrol. Earth Syst. Sci., 19, 2561–2576, https://doi.org/10.5194/hess-19-2561-2015, 2015. a
Mann, H. B.: Nonparametric tests against trend, Econometrica,
13, 245–259, https://doi.org/10.2307/1907187, 1945. a
Mann, H. B. and Whitney, D. R.:
On a test of whether one of two random variables is stochastically larger than the other, Ann. Math. Stat.,
18, 50–60, https://doi.org/10.1214/aoms/1177730491, 1947. a
Matthes, K., Funke, B., Andersson, M. E., Barnard, L., Beer, J., Charbonneau, P., Clilverd, M. A., Dudok de Wit, T., Haberreiter, M., Hendry, A., Jackman, C. H., Kretzschmar, M., Kruschke, T., Kunze, M., Langematz, U., Marsh, D. R., Maycock, A. C., Misios, S., Rodger, C. J., Scaife, A. A., Seppälä, A., Shangguan, M., Sinnhuber, M., Tourpali, K., Usoskin, I., van de Kamp, M., Verronen, P. T., and Versick, S.: Solar forcing for CMIP6 (v3.2), Geosci. Model Dev., 10, 2247–2302, https://doi.org/10.5194/gmd-10-2247-2017, 2017. a, b
McConnell, J. R., Sigl, M., Plunkett, G., Burke, A., Kim, W. M., Raible, C. C., Wilson, A. I., Manning J. G., Ludlow F., Chellman N. J., Innes H. M., Yang Z., Larsen J. F., Schaefer J. R., Kipfstuhl S., Mojtabavi S., Wilhelms F., Opel T., Meyer H., and Steffensen J. P.:
Extreme climate after massive eruption of Alaska's Okmok volcano in 43 BCE and effects on the late Roman Republic and Ptolemaic Kingdom,
P. Natl. Acad. Sci. USA,
117, 15443–15449, https://doi.org/10.1073/pnas.2002722117, 2020. a
McGregor, S. and Timmermann, A.:
The effect of explosive tropical volcanism on ENSO,
J. Climate,
24, 2178–2191, https://doi.org/10.1175/2010JCLI3990.1, 2011. a, b
McGregor, S., Khodri, M., Maher, N., Ohba, M., Pausata, F. S., and Stevenson, S.:
The effect of strong volcanic eruptions on ENSO,
in: El Niño Southern Oscillation in a Changing Climate,
edited by: McPhaden, M. J., Santoso, A., and Cai, W.,
John Wiley & Sons, Inc., Hoboken, NJ, USA and the American Geophysical Union Washington, D.C., USA, 267–287, https://doi.org/10.1002/9781119548164.ch12, 2020. a, b
Meinshausen, M., Vogel, E., Nauels, A., Lorbacher, K., Meinshausen, N., Etheridge, D. M., Fraser, P. J., Montzka, S. A., Rayner, P. J., Trudinger, C. M., Krummel, P. B., Beyerle, U., Canadell, J. G., Daniel, J. S., Enting, I. G., Law, R. M., Lunder, C. R., O'Doherty, S., Prinn, R. G., Reimann, S., Rubino, M., Velders, G. J. M., Vollmer, M. K., Wang, R. H. J., and Weiss, R.: Historical greenhouse gas concentrations for climate modelling (CMIP6), Geosci. Model Dev., 10, 2057–2116, https://doi.org/10.5194/gmd-10-2057-2017, 2017. a, b, c, d
Myhre, G., Alterskjær, K., Stjern, C. W., Hodnebrog, Ø., Marelle, L., Samset, B. H., Sillmann, J., Schaller, N., Fischer, E., Schulz, M., and Stohl, A.:
Frequency of extreme precipitation increases extensively with event rareness under global warming,
Sci. Rep.-UK,
9, 16063, https://doi.org/10.1038/s41598-019-52277-4, 2019. a, b, c
Neale, R. B., Chen, C.-C., Gettelman, A., Lauritzen, P. H., Park, S., Williamson, D. L., Conley, A. J., Garcia, R., Kinnison, D., and Lamarque, J.-F.: Description of the NCAR community atmosphere model (CAM 5.0), NCAR Tech. Note NCAR/TN-486+ STR, 1, Technical report, National Center for Atmospheric Research (NCAR), USA, 1–12, 2010. a
Ohba, M., Shiogama, H., Yokohata, T., and Watanabe, M.:
Impact of strong tropical volcanic eruptions on ENSO simulated in a coupled GCM,
J. Climate,
26, 5169–5182, https://doi.org/10.1175/JCLI-D-12-00471.1, 2013. a
Oman, L., Robock, A., Stenchikov, G., Schmidt, G. A., and Ruedy, R.:
Climatic response to high-latitude volcanic eruptions,
J. Geophys. Res.-Atmos.,
110, D13103, https://doi.org/10.1029/2004JD005487, 2005. a
Otto-Bliesner, B. L., Brady, E. C., Fasullo, J., Jahn, A., Landrum, L., Stevenson, S., Rosenbloom, N., Mai, A., and Strand, G.:
Climate variability and change since 850 CE: An ensemble approach with the Community Earth System Model,
B. Am. Meteorol. Soc.,
97, 735–754, https://doi.org/10.1175/BAMS-D-14-00233.1, 2016. a
O'Gorman, P. A.:
Sensitivity of tropical precipitation extremes to climate change,
Nat. Geosci.,
5, 697–700, https://doi.org/10.1038/ngeo1568, 2012. a
PAGES Hydro2k Consortium: Comparing proxy and model estimates of hydroclimate variability and change over the Common Era, Clim. Past, 13, 1851–1900, https://doi.org/10.5194/cp-13-1851-2017, 2017. a
Pall, P., Allen, M. R., and Stone, D. A.:
Testing the Clausius–Clapeyron constraint on changes in extreme precipitation under CO2 warming,
Clim. Dynam.,
28, 351–363, https://doi.org/10.1007/s00382-006-0180-2, 2007. a, b, c, d
Papalexiou, S. M. and Montanari, A.:
Global and regional increase of precipitation extremes under global warming,
Water Resour. Res.,
55, 4901–4914, https://doi.org/10.1029/2018WR024067, 2019. a
Pendergrass, A. G., Lehner, F., Sanderson, B. M., and Xu, Y.:
Does extreme precipitation intensity depend on the emissions scenario?,
Geophys. Res. Lett.,
42, 8767–8774, https://doi.org/10.1002/2015GL065854, 2015. a
Pfahl, S.: Characterising the relationship between weather extremes in Europe and synoptic circulation features, Nat. Hazards Earth Syst. Sci., 14, 1461–1475, https://doi.org/10.5194/nhess-14-1461-2014, 2014. a
Pfahl, S. and Wernli, H.:
Quantifying the relevance of cyclones for precipitation extremes,
J. Climate,
25, 6770–6780, https://doi.org/10.1175/JCLI-D-11-00705.1, 2012. a
Pfahl, S., O'Gorman, P. A., and Fischer, E. M.:
Understanding the regional pattern of projected future changes in extreme precipitation,
Nat. Clim. Change,
7, 423–427, https://doi.org/10.1038/nclimate3287, 2017. a
Pongratz, J., Reick, C., Raddatz, T., and Claussen, M.:
A reconstruction of global agricultural areas and land cover for the last millennium,
Global Biogeochem. Cy.,
22, GB3018, https://doi.org/10.1029/2007GB003153, 2008. a, b, c
Robock, A.:
Volcanic eruptions and climate,
Rev. Geophys.,
38, 191–219, https://doi.org/10.1029/1998RG000054, 2000. a
Roderick, M. L., Sun, F., Lim, W. H., and Farquhar, G. D.: A general framework for understanding the response of the water cycle to global warming over land and ocean, Hydrol. Earth Syst. Sci., 18, 1575–1589, https://doi.org/10.5194/hess-18-1575-2014, 2014. a
Scher, S., Haarsma, R. J., Vries, H. d., Drijfhout, S. S., and Delden, A. J. v.:
Resolution dependence of extreme precipitation and deep convection over the Gulf Stream,
J. Adv. Model. Earth Sy.,
9, 1186–1194, https://doi.org/10.1002/2016MS000903, 2017. a, b
Schmidt, G. A., Jungclaus, J. H., Ammann, C. M., Bard, E., Braconnot, P., Crowley, T. J., Delaygue, G., Joos, F., Krivova, N. A., Muscheler, R., Otto-Bliesner, B. L., Pongratz, J., Shindell, D. T., Solanki, S. K., Steinhilber, F., and Vieira, L. E. A.: Climate forcing reconstructions for use in PMIP simulations of the last millennium (v1.0), Geosci. Model Dev., 4, 33–45, https://doi.org/10.5194/gmd-4-33-2011, 2011. a, b
Schneider, D. P., Ammann, C. M., Otto-Bliesner, B. L., and Kaufman, D. S.:
Climate response to large, high-latitude and low-latitude volcanic eruptions in the Community Climate System Model,
J. Geophys. Res.-Atmos.,
114, D15101, https://doi.org/10.1029/2008JD011222, 2009. a
Schurer, A. P., Hegerl, G. C., Mann, M. E., Tett, S. F., and Phipps, S. J.:
Separating forced from chaotic climate variability over the past millennium,
J. Climate,
26, 6954–6973, https://doi.org/10.1175/JCLI-D-12-00826.1, 2013. a
Scoccimarro, E., Gualdi, S., Bellucci, A., Zampieri, M., and Navarra, A.:
Heavy Precipitation Events in a Warmer Climate: Results from CMIP5 Models,
J. Climate,
26, 7902–7911, https://doi.org/10.1175/JCLI-D-12-00850.1, 2013. a, b
Shields, C. A., Kiehl, J. T., and Meehl, G. A.:
Future changes in regional precipitation simulated by a half-degree coupled climate model: Sensitivity to horizontal resolution,
J. Adv. Model. Earth Sy.,
8, 863–884, https://doi.org/10.1002/2015MS000584, 2016. a
Sigl, M., Winstrup, M., McConnell, J. R., Welten, K. C., Plunkett, G., Ludlow, F., Büntgen, U., Caffee, M., Chellman, N., Dahl-Jensen, D., and Fischer, H.:
Timing and climate forcing of volcanic eruptions for the past 2,500 years,
Nature,
523, 543–549, https://doi.org/10.1038/nature14565, 2015. a, b
Sigl, M., Toohey, M., McConnell, J. R., Cole-Dai, J., and Severi, M.:
HolVol: Reconstructed volcanic stratospheric sulfur injections and aerosol optical depth for the Holocene (9500 BCE to 1900 CE),
PANGAEA, https://doi.org/10.1594/PANGAEA.928646, 2021. a, b, c, d
Sillmann, J., Stjern, C. W., Myhre, G., and Forster, P. M.:
Slow and fast responses of mean and extreme precipitation to different forcing in CMIP5 simulations,
Geophys. Res. Lett.,
44, 6383–6390, https://doi.org/10.1002/2017GL073229, 2017. a
Silva, A. T., Naghettini, M., and Portela, M. M.:
On some aspects of peaks-over-threshold modeling of floods under nonstationarity using climate covariates,
Stoch. Env. Res. Risk A.,
30, 207–224, https://doi.org/10.1007/s00477-015-1072-y, 2016. a
Smith, R., Jones, P., Briegleb, B., Bryan, F., Danabasoglu, G., Dennis, J., Dukowicz, J., Eden, C., Fox-Kemper, B., Gent, P., Hecht, M., Jayne, S., Jochum, M., Large, W., Lindsay, K., Maltrud, M., Norton, N., Peacock, S., Vertenstein, M., and Yeager, S.:
The parallel ocean program (POP) reference manual ocean component of the community climate system model (CCSM) and community earth system model (CESM), LAUR-01853, 141, Technical report, Los Alamos National Laboratory (LANL), USA, 1–140, 2010. a
Steinschneider, S., Ho, M., Cook, E. R., and Lall, U.:
Can PDSI inform extreme precipitation?: An exploration with a 500 year long paleoclimate reconstruction over the U.S.,
Water Resour. Res.,
52, 3866–3880, https://doi.org/10.1002/2016WR018712, 2016. a, b
Stephens, G. L., L'Ecuyer, T., Forbes, R., Gettelmen, A., Golaz, J.-C., Bodas–Salcedo, A., Suzuki, K., Gabriel, P., and Haynes, J.:
Dreary state of precipitation in global models,
J. Geophys. Res.-Atmos., 115, D24211, https://doi.org/10.1029/2010JD014532, 2010. a, b
Stevenson, S., Otto-Bliesner, B., Fasullo, J., and Brady, E.:
“El Niño like” hydroclimate responses to last millennium volcanic eruptions,
J. Climate,
29, 2907–2921, https://doi.org/10.1175/JCLI-D-15-0239.1, 2016. a, b, c
Stevenson, S., Fasullo, J. T., Otto-Bliesner, B. L., Tomas, R. A., and Gao, C.:
Role of eruption season in reconciling model and proxy responses to tropical volcanism,
P. Natl. Acad. Sci. USA,
114, 1822–1826, https://doi.org/10.1073/pnas.1612505114, 2017. a
Stevenson, S., Overpeck, J. T., Fasullo, J., Coats, S., Parsons, L., Otto-Bliesner, B., Ault, T., Loope, G., and Cole, J.:
Climate variability, volcanic forcing, and last millennium hydroclimate extremes,
J. Climate,
31, 4309–4327, https://doi.org/10.1175/JCLI-D-17-0407.1, 2018. a
Sun, Q., Zhang, X., Zwiers, F., Westra, S., and Alexander, L. V.:
A global, continental, and regional analysis of changes in extreme precipitation,
J. Climate,
34, 243–258, https://doi.org/10.1175/JCLI-D-19-0892.1, 2021. a
Sun, X., Renard, B., Thyer, M., Westra, S., and Lang, M.:
A global analysis of the asymmetric effect of ENSO on extreme precipitation,
J. Hydrol.,
530, 51–65, https://doi.org/10.1016/j.jhydrol.2015.09.016, 2015. a
Thiombiano, A. N., El Adlouni, S., St-Hilaire, A., Ouarda, T. B., and El-Jabi, N.:
Nonstationary frequency analysis of extreme daily precipitation amounts in Southeastern Canada using a peaks-over-threshold approach,
Theor. Appl. Climatol.,
129, 413–426, https://doi.org/10.1007/s00704-016-1789-7, 2017. a, b
Toohey, M., Stevens, B., Schmidt, H., and Timmreck, C.: Easy Volcanic Aerosol (EVA v1.0): an idealized forcing generator for climate simulations, Geosci. Model Dev., 9, 4049–4070, https://doi.org/10.5194/gmd-9-4049-2016, 2016. a
Trenberth, K. E., Dai, A., Rasmussen, R. M., and Parsons, D. B.:
The Changing Character of Precipitation,
B. Am. Meteorol. Soc.,
84, 1205–1218, https://doi.org/10.1175/BAMS-84-9-1205, 2003. a, b, c, d
Usoskin, I., Hulot, G., Gallet, Y., Roth, R., Licht, A., Joos, F., Kovaltsov, G., Thébault, E., and Khokhlov, A.:
Evidence for distinct modes of solar activity,
Astron. Astrophys.,
562, L10, https://doi.org/10.1051/0004-6361/201423391, 2014. a, b, c
Usoskin, I., Gallet, Y., Lopes, F., Kovaltsov, G., and Hulot, G.:
Solar activity during the Holocene: the Hallstatt cycle and its consequence for grand minima and maxima,
Astron. Astrophys.,
587, A150, https://doi.org/10.1051/0004-6361/201527295, 2016. a
Van Haren, R., Haarsma, R. J., Van Oldenborgh, G. J., and Hazeleger, W.:
Resolution dependence of European precipitation in a state-of-the-art atmospheric general circulation model,
J. Climate,
28, 5134–5149, https://doi.org/10.1175/JCLI-D-14-00279.1, 2015. a, b
Vieira, L. E. A., Solanki, S. K., Krivova, N. A., and Usoskin, I.:
Evolution of the solar irradiance during the Holocene,
Astron. Astrophys.,
531, A6, https://doi.org/10.1051/0004-6361/201015843, 2011. a, b, c
Wang, T., Guo, D., Gao, Y., Wang, H., Zheng, F., Zhu, Y., Miao, J., and Hu, Y.:
Modulation of ENSO evolution by strong tropical volcanic eruptions,
Clim. Dynam.,
51, 2433–2453, https://doi.org/10.1007/s00382-017-4021-2, 2018. a, b
Wang, X., Jiang, D., and Lang, X.:
Future extreme climate changes linked to global warming intensity,
Sci. Bull.,
62, 1673–1680, https://doi.org/10.1016/j.scib.2017.11.004, 2017. a, b, c, d
Wanner, H., Beer, J., Bütikofer, J., Crowley, T. J., Cubasch, U., Flückiger, J., Goosse, H., Grosjean, M., Joos, F., Kaplan, J. O., Küttel, M., Müller, S. A., Prentice, I. C., Solomina, O., Stocker, T. F., Tarasov, P., Wagner, M., and Widmann, M.:
Mid- to Late Holocene climate change: an overview,
Quaternary Sci. Rev.,
27, 1791–1828, https://doi.org/10.1016/j.quascirev.2008.06.013, 2008. a
Westra, S., Alexander, L. V., and Zwiers, F. W.:
Global increasing trends in annual maximum daily precipitation,
J. Climate,
26, 3904–3918, https://doi.org/10.1175/JCLI-D-12-00502.1, 2013. a
Wilhelm, B., Arnaud, F., Sabatier, P., Crouzet, C., Brisset, E., Chaumillon, E., Disnar, J.-R., Guiter, F., Malet, E., Reyss, J.-L., Tachikawa, K., Bard, E., and Delannoy, J.-J.:
1400 years of extreme precipitation patterns over the Mediterranean French Alps and possible forcing mechanisms,
Quaternary Res.,
78, 1–12, https://doi.org/10.1016/j.yqres.2012.03.003, 2012. a
Yang, F., Kumar, A., Schlesinger, M. E., and Wang, W.:
Intensity of hydrological cycles in warmer climates,
J. Climate,
16, 2419–2423, https://doi.org/10.1175/2779.1, 2003. a
Yang, T., Li, H., Wang, W., Xu, C.-Y., and Yu, Z.:
Statistical downscaling of extreme daily precipitation, evaporation, and temperature and construction of future scenarios,
Hydrol. Process.,
26, 3510–3523, https://doi.org/10.1002/hyp.8427, 2012. a
Zheng, J., Yu, Y., Zhang, X., and Hao, Z.: Variation of extreme drought and flood in North China revealed by document-based seasonal precipitation reconstruction for the past 300 years, Clim. Past, 14, 1135–1145, https://doi.org/10.5194/cp-14-1135-2018, 2018.
a
Zhong, Y., Jahn, A., Miller, G., and Geirsdottir, A.:
Asymmetric Cooling of the Atlantic and Pacific Arctic During the Past Two Millennia: A Dual Observation-Modeling Study,
Geophys. Res. Lett.,
45, 12–497, https://doi.org/10.1029/2018GL079447, 2018. a
Short summary
To understand the natural characteristics and future changes of the global extreme daily precipitation, it is necessary to explore the long-term characteristics of extreme daily precipitation. Here, we used climate simulations to analyze the characteristics and long-term changes of extreme precipitation during the past 3351 years. Our findings indicate that extreme precipitation in the past is associated with internal climate variability and regional surface temperatures.
To understand the natural characteristics and future changes of the global extreme daily...
