Articles | Volume 16, issue 2
https://doi.org/10.5194/cp-16-627-2020
© 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-16-627-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Droughts in the area of Poland in recent centuries in the light of multi-proxy data
Department of Meteorology and Climatology, Faculty of Earth Sciences and Spatial Management, Nicolaus Copernicus University, Toruń, Poland
Centre for Climate Change Research, Nicolaus Copernicus University, Toruń, Poland
Piotr Oliński
Department of Medieval History, Institute of History and Archival
Sciences, Faculty of History, Nicolaus Copernicus University, Toruń,
Poland
Centre for Climate Change Research, Nicolaus Copernicus University, Toruń, Poland
Marcin Koprowski
Department of Ecology and Biogeography, Faculty of Biological and Veterinary Sciences, Nicolaus Copernicus University, Toruń, Poland
Centre for Climate Change Research, Nicolaus Copernicus University, Toruń, Poland
Janusz Filipiak
Department of Meteorology and Climatology, Institute of Geography,
Faculty of Oceanography and Geography, University of Gdańsk, Gdańsk, Poland
Aleksandra Pospieszyńska
Department of Meteorology and Climatology, Faculty of Earth Sciences and Spatial Management, Nicolaus Copernicus University, Toruń, Poland
Centre for Climate Change Research, Nicolaus Copernicus University, Toruń, Poland
Waldemar Chorążyczewski
Department of Medieval History, Institute of History and Archival
Sciences, Faculty of History, Nicolaus Copernicus University, Toruń,
Poland
Centre for Climate Change Research, Nicolaus Copernicus University, Toruń, Poland
Radosław Puchałka
Department of Ecology and Biogeography, Faculty of Biological and Veterinary Sciences, Nicolaus Copernicus University, Toruń, Poland
Centre for Climate Change Research, Nicolaus Copernicus University, Toruń, Poland
Henryk Paweł Dąbrowski
Dendroarchaeological Laboratory, Archaeological Museum in Biskupin,
Biskupin, Poland
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Garima Singh, Rajmund Przybylak, Przemysław Wyszyński, Andrzej Araźny, and Konrad Chmist
EGUsphere, https://doi.org/10.5194/egusphere-2024-2719, https://doi.org/10.5194/egusphere-2024-2719, 2024
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This study aims to determine the nature of the climate in Labrador in historical times (late 18th century), which is crucial to understanding past climate changes in the Arctic and their causes. It is equally important to estimate the range of natural climate variability, which can help in correctly recognising the causes of present and future climate changes – especially the influence of man on climate. The analysis shows a significant warming from historical to present times.
Rajmund Przybylak, Garima Singh, Przemysław Wyszyński, Andrzej Araźny, and Konrad Chmist
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The purpose of this study is to recognise the nature of the climate in historical times (second half of 18th century) in Greenland. Such knowledge is important for validating Greenland temperature reconstructions based on both modelling works and various proxies. The two unique series of old meteorological observations from Greenland we used indicated that temperature in the study period was comparable to that of the early 20th-century Arctic warming but lower than that of the present day.
Rajmund Przybylak, Piotr Oliński, Marcin Koprowski, Elżbieta Szychowska-Krąpiec, Marek Krąpiec, Aleksandra Pospieszyńska, and Radosław Puchałka
Clim. Past, 19, 2389–2408, https://doi.org/10.5194/cp-19-2389-2023, https://doi.org/10.5194/cp-19-2389-2023, 2023
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The present paper upgrades our knowledge of Poland’s climate in the period 1001–1500 using multiproxy data. Four new climate reconstructions have been constructed – three based on dendrochronological data (since the 12th century) and one on documentary evidence (since the 15th century). The results should help improve the knowledge of climate change in Europe, particularly in central Europe.
Duncan Pappert, Mariano Barriendos, Yuri Brugnara, Noemi Imfeld, Sylvie Jourdain, Rajmund Przybylak, Christian Rohr, and Stefan Brönnimann
Clim. Past, 18, 2545–2565, https://doi.org/10.5194/cp-18-2545-2022, https://doi.org/10.5194/cp-18-2545-2022, 2022
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We present daily temperature and sea level pressure fields for Europe for the severe winter 1788/1789 based on historical meteorological measurements and an analogue reconstruction approach. The resulting reconstruction skilfully reproduces temperature and pressure variations over central and western Europe. We find intense blocking systems over northern Europe and several abrupt, strong cold air outbreaks, demonstrating that quantitative weather reconstruction of past extremes is possible.
Duncan Pappert, Yuri Brugnara, Sylvie Jourdain, Aleksandra Pospieszyńska, Rajmund Przybylak, Christian Rohr, and Stefan Brönnimann
Clim. Past, 17, 2361–2379, https://doi.org/10.5194/cp-17-2361-2021, https://doi.org/10.5194/cp-17-2361-2021, 2021
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This paper presents temperature and pressure measurements from the 37 stations of the late 18th century network of the Societas Meteorologica Palatina, in addition to providing an inventory of the available observations, most of which have been digitised. The quality of the recovered series is relatively good, as demonstrated by two case studies. Early instrumental data such as these will help to explore past climate and weather extremes in Europe in greater detail.
Garima Singh, Rajmund Przybylak, Przemysław Wyszyński, Andrzej Araźny, and Konrad Chmist
EGUsphere, https://doi.org/10.5194/egusphere-2024-2719, https://doi.org/10.5194/egusphere-2024-2719, 2024
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This study aims to determine the nature of the climate in Labrador in historical times (late 18th century), which is crucial to understanding past climate changes in the Arctic and their causes. It is equally important to estimate the range of natural climate variability, which can help in correctly recognising the causes of present and future climate changes – especially the influence of man on climate. The analysis shows a significant warming from historical to present times.
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Rajmund Przybylak, Piotr Oliński, Marcin Koprowski, Elżbieta Szychowska-Krąpiec, Marek Krąpiec, Aleksandra Pospieszyńska, and Radosław Puchałka
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The present paper upgrades our knowledge of Poland’s climate in the period 1001–1500 using multiproxy data. Four new climate reconstructions have been constructed – three based on dendrochronological data (since the 12th century) and one on documentary evidence (since the 15th century). The results should help improve the knowledge of climate change in Europe, particularly in central Europe.
Rudolf Brázdil, Petr Dobrovolný, Christian Pfister, Katrin Kleemann, Kateřina Chromá, Péter Szabó, and Piotr Olinski
Clim. Past, 19, 1863–1890, https://doi.org/10.5194/cp-19-1863-2023, https://doi.org/10.5194/cp-19-1863-2023, 2023
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Duncan Pappert, Mariano Barriendos, Yuri Brugnara, Noemi Imfeld, Sylvie Jourdain, Rajmund Przybylak, Christian Rohr, and Stefan Brönnimann
Clim. Past, 18, 2545–2565, https://doi.org/10.5194/cp-18-2545-2022, https://doi.org/10.5194/cp-18-2545-2022, 2022
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We present daily temperature and sea level pressure fields for Europe for the severe winter 1788/1789 based on historical meteorological measurements and an analogue reconstruction approach. The resulting reconstruction skilfully reproduces temperature and pressure variations over central and western Europe. We find intense blocking systems over northern Europe and several abrupt, strong cold air outbreaks, demonstrating that quantitative weather reconstruction of past extremes is possible.
Duncan Pappert, Yuri Brugnara, Sylvie Jourdain, Aleksandra Pospieszyńska, Rajmund Przybylak, Christian Rohr, and Stefan Brönnimann
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This paper presents temperature and pressure measurements from the 37 stations of the late 18th century network of the Societas Meteorologica Palatina, in addition to providing an inventory of the available observations, most of which have been digitised. The quality of the recovered series is relatively good, as demonstrated by two case studies. Early instrumental data such as these will help to explore past climate and weather extremes in Europe in greater detail.
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Previous studies related to historical droughts in the Czech Lands showed that the summers of 1531–1540 could represent the driest summer decade of the past 500 years. To confirm this hypothesis, documentary data from central Europe were collected and presented for individual summers and complemented by maps of precipitation and drought distribution to document corresponding weather patterns and their various impacts. The main droughts occurred in 1532, 1534–1536, 1538, and particularly in 1540.
Y. Brugnara, R. Auchmann, S. Brönnimann, R. J. Allan, I. Auer, M. Barriendos, H. Bergström, J. Bhend, R. Brázdil, G. P. Compo, R. C. Cornes, F. Dominguez-Castro, A. F. V. van Engelen, J. Filipiak, J. Holopainen, S. Jourdain, M. Kunz, J. Luterbacher, M. Maugeri, L. Mercalli, A. Moberg, C. J. Mock, G. Pichard, L. Řezníčková, G. van der Schrier, V. Slonosky, Z. Ustrnul, M. A. Valente, A. Wypych, and X. Yin
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A data set of instrumental pressure and temperature observations for the early instrumental period (before ca. 1850) is described. This is the result of a digitisation effort involving the period immediately after the eruption of Mount Tambora in 1815, combined with the collection of already available sub-daily time series. The highest data availability is therefore for the years 1815 to 1817. An analysis of pressure variability and of case studies in Europe is performed for that period.
Related subject area
Subject: Proxy Use-Development-Validation | Archive: Historical Records | Timescale: Centennial-Decadal
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Clim. Past, 20, 137–150, https://doi.org/10.5194/cp-20-137-2024, https://doi.org/10.5194/cp-20-137-2024, 2024
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This study examines the relationship between temperature and precipitation as explanatory variables for the probability of death due to waterborne and airborne diseases in historical urban space. The lagged effects of temperature and precipitation on waterborne and airborne diseases were significant, except for the smooth lagged average monthly temperature effect for the latter. There was also significant spatial heterogeneity in the prevalence of deaths due to waterborne and airborne diseases.
Fredrik Charpentier Ljungqvist, Bo Christiansen, Jan Esper, Heli Huhtamaa, Lotta Leijonhufvud, Christian Pfister, Andrea Seim, Martin Karl Skoglund, and Peter Thejll
Clim. Past, 19, 2463–2491, https://doi.org/10.5194/cp-19-2463-2023, https://doi.org/10.5194/cp-19-2463-2023, 2023
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We study the climate signal in long harvest series from across Europe between the 16th and 18th centuries. The climate–harvest yield relationship is found to be relatively weak but regionally consistent and similar in strength and sign to modern climate–harvest yield relationships. The strongest climate–harvest yield patterns are a significant summer soil moisture signal in Sweden, a winter temperature and precipitation signal in Switzerland, and spring temperature signals in Spain.
Yuri Brugnara, Chantal Hari, Lucas Pfister, Veronika Valler, and Stefan Brönnimann
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We digitized dozens of weather journals containing temperature measurements from in and around Bern and Zurich. They cover over a century before the creation of a national weather service in Switzerland. With these data we could create daily temperature series for the two cities that span the last 265 years. We found that the pre-industrial climate on the Swiss Plateau was colder than suggested by previously available instrumental data sets and about 2.5 °C colder than the present-day climate.
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Clim. Past, 18, 2345–2356, https://doi.org/10.5194/cp-18-2345-2022, https://doi.org/10.5194/cp-18-2345-2022, 2022
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This study investigates the possibility of inferring information on aerosol optical depth from photographs of historic paintings. The idea – which has been applied in previous studies – is very interesting because it would provide an archive of the atmospheric aerosol loading covering many centuries. We show that twilight colours depend not only on the aerosol optical thickness, but also on several other parameters, making a quantitative estimate of aerosol optical depth very difficult.
Rudolf Brázdil, Petr Zahradník, Péter Szabó, Kateřina Chromá, Petr Dobrovolný, Lukáš Dolák, Miroslav Trnka, Jan Řehoř, and Silvie Suchánková
Clim. Past, 18, 2155–2180, https://doi.org/10.5194/cp-18-2155-2022, https://doi.org/10.5194/cp-18-2155-2022, 2022
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George C. D. Adamson, David J. Nash, and Stefan W. Grab
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Descriptions of climate held in archives are a valuable source of past climate variability, but there is a large potential for error in assigning quantitative indices (e.g. −2, v. dry to +2, v. wet) to descriptive data. This is the first study to examine this uncertainty. We gave the same dataset to 71 postgraduate students and 6 professional scientists, findings that error can be minimized by taking an average of indices developed by eight postgraduates and only two professional climatologists.
Rudolf Brázdil, Petr Dobrovolný, Jiří Mikšovský, Petr Pišoft, Miroslav Trnka, Martin Možný, and Jan Balek
Clim. Past, 18, 935–959, https://doi.org/10.5194/cp-18-935-2022, https://doi.org/10.5194/cp-18-935-2022, 2022
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The paper deals with 520-year series (1501–2020 CE) of temperature, precipitation, and four drought indices reconstructed from documentary evidence and instrumental observations for the Czech Lands. Basic features of their fluctuations, long-term trends, and periodicities as well as attribution to changes in external forcings and climate variability modes are analysed. Representativeness of Czech reconstructions at European scale is evaluated. The paper shows extreme character of past decades.
Santiago Gorostiza, Maria Antònia Martí Escayol, and Mariano Barriendos
Clim. Past, 17, 913–927, https://doi.org/10.5194/cp-17-913-2021, https://doi.org/10.5194/cp-17-913-2021, 2021
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How did cities respond to drought during the 17th century? This article studies the strategies followed by the city government of Barcelona during the severely dry period from 1620 to 1650. Beyond the efforts to expand urban water supply sources and to improve the maintenance of the system, the city government decided to compile knowledge about water infrastructure into a book and to restrict access to it. This management strategy aimed to increase the city's control over water.
LingYun Tang, Neil Macdonald, Heather Sangster, Richard Chiverrell, and Rachel Gaulton
Clim. Past, 16, 1917–1935, https://doi.org/10.5194/cp-16-1917-2020, https://doi.org/10.5194/cp-16-1917-2020, 2020
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A historical drought series (since 1200 CE) for Shenyang, NE China, shows 20th century droughts comparable in magnitude to recent severe droughts. Drought resilience driven by early 20th century societal/cultural changes reduced loss of life compared with the 1887 and 1891 droughts. A longer temporal analysis from integrated precipitation and historical records shows an earlier onset to droughts. Regional standardised precipitation indices could provide early warnings for drought development.
Siying Chen, Yun Su, Xiuqi Fang, and Jia He
Clim. Past, 16, 1873–1887, https://doi.org/10.5194/cp-16-1873-2020, https://doi.org/10.5194/cp-16-1873-2020, 2020
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Private diaries are important sources of historical data for research on climate change. Through a case study of Yunshan Diary, authored by Bi Guo of the Yuan dynasty of China, this article demonstrates how to delve into climate information in ancient diaries, mainly including species distribution records, phenological records and daily weather descriptions. This article considers how to use these records to reconstruct climate change and extreme climatic events on various timescales.
Rüdiger Glaser and Michael Kahle
Clim. Past, 16, 1207–1222, https://doi.org/10.5194/cp-16-1207-2020, https://doi.org/10.5194/cp-16-1207-2020, 2020
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A new study on droughts in Germany since 1500 reveals the long-term trend of single extreme events, as well as drier periods. Extreme droughts appeared in 1540, 1590, 1615, 1706, 1834, 1893, 1921, 1949 and 2018. Like today, droughts had manifold impacts such as harvest failures, water deficits, low water levels and forest fires. This had different societal consequences ranging from famine, disease, rising prices, migration and riots leading to subsidies and discussions on climate change.
Kathleen Pribyl
Clim. Past, 16, 1027–1041, https://doi.org/10.5194/cp-16-1027-2020, https://doi.org/10.5194/cp-16-1027-2020, 2020
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Droughts pose a climatic hazard that can have a profound impacts on past societies. Using documentary sources, this paper studies the occurrence and impacts of spring–summer droughts in pre-industrial England from 1200 to 1700. The impacts most relevant to human livelihood, including the agricultural and pastoral sectors of agrarian production, and public health are evaluated.
Sarir Ahmad, Liangjun Zhu, Sumaira Yasmeen, Yuandong Zhang, Zongshan Li, Sami Ullah, Shijie Han, and Xiaochun Wang
Clim. Past, 16, 783–798, https://doi.org/10.5194/cp-16-783-2020, https://doi.org/10.5194/cp-16-783-2020, 2020
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This study provides the opportunity to extend climatic records to preindustrial periods in northern Pakistan. The reconstructed March–August PDSIs for the past 424 years, going back to 1593 CE, enable scientists to know how these areas were prone to climatic extremes in the past. The instrumental data are limited in Pakistan; however, the Cedrus deodara tree that preserves physical characteristics of past climatic variabilities can provide insight into the trend of climatic changes.
Ernesto Tejedor, Martín de Luis, Mariano Barriendos, José María Cuadrat, Jürg Luterbacher, and Miguel Ángel Saz
Clim. Past, 15, 1647–1664, https://doi.org/10.5194/cp-15-1647-2019, https://doi.org/10.5194/cp-15-1647-2019, 2019
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We developed a new dataset of historical documents by compiling records (rogation ceremonies) from 13 cities in the northeast of the Iberian Peninsula (IP). These records were transformed into quantitative continuous data to develop drought indices (DIs). We regionalized them by creating three DIs (Ebro Valle, Mediterranean, and Mountain), which cover the period from 1650 to 1899 CE. We identified extreme drought years and periods which help to understand climate variability in the IP.
Thomas Labbé, Christian Pfister, Stefan Brönnimann, Daniel Rousseau, Jörg Franke, and Benjamin Bois
Clim. Past, 15, 1485–1501, https://doi.org/10.5194/cp-15-1485-2019, https://doi.org/10.5194/cp-15-1485-2019, 2019
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In this paper we present the longest grape harvest date (GHD) record reconstructed to date, i.e. Beaune (France, Burgundy) 1354–2018. Drawing on unedited archive material, the series is validated using the long Paris temperature series that goes back to 1658 and was used to assess April-to-July temperatures from 1354 to 2018. The distribution of extremely early GHD is uneven over the 664-year-long period of the series and mirrors the rapid global warming from 1988 to 2018.
Salvador Gil-Guirado, Juan José Gómez-Navarro, and Juan Pedro Montávez
Clim. Past, 15, 1303–1325, https://doi.org/10.5194/cp-15-1303-2019, https://doi.org/10.5194/cp-15-1303-2019, 2019
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The historical climatology has remarkable research potentialities. However, historical climatology has some methodological limitations. This study presents a new methodology (COST) that allows us to perform climate reconstructions with monthly resolution. The variability of the climatic series obtained are coherent with previous studies. The new proposed method is objective and is not affected by social changes, which allows us to perform studies in regions with different languages and cultures.
Rudolf Brázdil, Petr Dobrovolný, Miroslav Trnka, Ladislava Řezníčková, Lukáš Dolák, and Oldřich Kotyza
Clim. Past, 15, 1–24, https://doi.org/10.5194/cp-15-1-2019, https://doi.org/10.5194/cp-15-1-2019, 2019
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The paper analyses extreme droughts of the pre-instrumental period (1501–1803) over the territory of the recent Czech Republic. In total, 16 droughts were selected for spring, summer and autumn each and 14 droughts for summer half-year (Apr–Sep). They are characterized by very low values of drought indices, high temperatures, low precipitation and by the influence of high-pressure situations. Selected extreme droughts are described in more detail. Effect of droughts on grain prices are studied.
Rudolf Brázdil, Andrea Kiss, Jürg Luterbacher, David J. Nash, and Ladislava Řezníčková
Clim. Past, 14, 1915–1960, https://doi.org/10.5194/cp-14-1915-2018, https://doi.org/10.5194/cp-14-1915-2018, 2018
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The paper presents a worldwide state of the art of droughts fluctuations based on documentary data. It gives an overview of achievements related to different kinds of documentary evidence with their examples and an overview of papers presenting long-term drought chronologies over the individual continents, analysis of the most outstanding drought events, the influence of external forcing and large-scale climate drivers, and human impacts and responses. It recommends future research directions.
Shanna Lyu, Zongshan Li, Yuandong Zhang, and Xiaochun Wang
Clim. Past, 12, 1879–1888, https://doi.org/10.5194/cp-12-1879-2016, https://doi.org/10.5194/cp-12-1879-2016, 2016
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This study presents a 414-year growing season minimum temperature reconstruction based on Korean pine tree-ring series at Laobai Mountain, northeast China. It developed a more than 400-year climate record in this area for the first time. This reconstruction showed six cold periods, seven warm periods, and natural disaster records of extreme climate events.
Pierre Brigode, François Brissette, Antoine Nicault, Luc Perreault, Anna Kuentz, Thibault Mathevet, and Joël Gailhard
Clim. Past, 12, 1785–1804, https://doi.org/10.5194/cp-12-1785-2016, https://doi.org/10.5194/cp-12-1785-2016, 2016
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In this paper, we apply a new hydro-climatic reconstruction method on the Caniapiscau Reservoir (Canada), compare the obtained streamflow time series against time series derived from dendrohydrology by other authors on the same catchment, and study the natural streamflow variability over the 1881–2011 period. This new reconstruction is based on a historical reanalysis of global geopotential height fields and aims to produce daily streamflow time series (using a rainfall–runoff model).
J. Zheng, Z. Hua, Y. Liu, and Z. Hao
Clim. Past, 11, 1553–1561, https://doi.org/10.5194/cp-11-1553-2015, https://doi.org/10.5194/cp-11-1553-2015, 2015
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In this paper we reconstruct the annual temperature anomalies in South Central China from 1850 to 2008, using phenodates of plants, snowfall days, and five tree-ring width chronologies. It is found that rapid warming has occurred since the 1990s, with an abrupt change around 1997, leading to unprecedented variability in warming; a cold interval dominated the 1860s, 1890s, and 1950s; warm decades occurred around 1850, 1870, and 1960; and the warmest decades were the 1990s–2000s.
R. Brázdil, P. Dobrovolný, M. Trnka, O. Kotyza, L. Řezníčková, H. Valášek, P. Zahradníček, and P. Štěpánek
Clim. Past, 9, 1985–2002, https://doi.org/10.5194/cp-9-1985-2013, https://doi.org/10.5194/cp-9-1985-2013, 2013
Q. Ge, Z. Hao, J. Zheng, and X. Shao
Clim. Past, 9, 1153–1160, https://doi.org/10.5194/cp-9-1153-2013, https://doi.org/10.5194/cp-9-1153-2013, 2013
H.-J. Lüdecke, A. Hempelmann, and C. O. Weiss
Clim. Past, 9, 447–452, https://doi.org/10.5194/cp-9-447-2013, https://doi.org/10.5194/cp-9-447-2013, 2013
V. Daux, I. Garcia de Cortazar-Atauri, P. Yiou, I. Chuine, E. Garnier, E. Le Roy Ladurie, O. Mestre, and J. Tardaguila
Clim. Past, 8, 1403–1418, https://doi.org/10.5194/cp-8-1403-2012, https://doi.org/10.5194/cp-8-1403-2012, 2012
Z.-X. Hao, J.-Y. Zheng, Q.-S. Ge, and W.-C. Wang
Clim. Past, 8, 1023–1030, https://doi.org/10.5194/cp-8-1023-2012, https://doi.org/10.5194/cp-8-1023-2012, 2012
F. Domínguez-Castro, P. Ribera, R. García-Herrera, J. M. Vaquero, M. Barriendos, J. M. Cuadrat, and J. M. Moreno
Clim. Past, 8, 705–722, https://doi.org/10.5194/cp-8-705-2012, https://doi.org/10.5194/cp-8-705-2012, 2012
P. Yiou, I. García de Cortázar-Atauri, I. Chuine, V. Daux, E. Garnier, N. Viovy, C. van Leeuwen, A. K. Parker, and J.-M. Boursiquot
Clim. Past, 8, 577–588, https://doi.org/10.5194/cp-8-577-2012, https://doi.org/10.5194/cp-8-577-2012, 2012
R. Brázdil, K. Chromá, H. Valášek, and L. Dolák
Clim. Past, 8, 467–481, https://doi.org/10.5194/cp-8-467-2012, https://doi.org/10.5194/cp-8-467-2012, 2012
F. Domínguez-Castro, R. García-Herrera, P. Ribera, and M. Barriendos
Clim. Past, 6, 553–563, https://doi.org/10.5194/cp-6-553-2010, https://doi.org/10.5194/cp-6-553-2010, 2010
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in: The Polish Climate in the European Context. An Historical Overview,
edited by: Przybylak, R., Majorowicz, J., Brázdil, R., and Kejna, M., Dordrecht, Heidelberg, London, New York, 191–218,
https://doi.org/10.1007/978-90-481-3167-9, 2010.
Short summary
The paper presents the main features of droughts in Poland in the period 996–2015 based on proxy data (documentary and dendrochronological) and instrumental measurements of precipitation. More than 100 droughts were found in documentary sources from the mid-15th century to the end of the 18th century with a maximum in the second halves of the 17th and, particularly, the 18th century. The long-term frequency of droughts in Poland has been stable for the last two or three centuries.
The paper presents the main features of droughts in Poland in the period 996–2015 based on...