Articles | Volume 18, issue 7
https://doi.org/10.5194/cp-18-1541-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-18-1541-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Jul 2022
Research article |
| 05 Jul 2022
| 05 Jul 2022
On the economic impact of droughts in central Europe: the decade from 1531 to 1540 from the Polish perspective
Stanisław Leszczycki Institute of Geography and Spatial Organization, Polish Academy of Sciences, Warsaw, 00-818, Poland
Piotr Guzowski
Faculty of History and International Relations, University of Białystok, Białystok, 15-420, Poland
Radosław Poniat
Faculty of History and International Relations, University of Białystok, Białystok, 15-420, Poland
Maciej T. Radomski
Institute of Archaeology and Ethnology, Polish Academy of Sciences, Warsaw, 00-140, Poland
Monika Kozłowska-Szyc
Faculty of History and International Relations, University of Białystok, Białystok, 15-420, Poland
Tomasz Panecki
Tadeusz Manteuffel Institute of History, Polish Academy of Sciences, Warsaw, 00-272, Poland
Sandra Słowińska
Stanisław Leszczycki Institute of Geography and Spatial Organization, Polish Academy of Sciences, Warsaw, 00-818, Poland
Bogusława Kruczkowska
Department of Soil Science, Institute of Agriculture, Warsaw University of Life Sciences – SGGW, Warsaw, 02-776, Poland
Michał Targowski
Faculty of History, Nicolaus Copernicus University in Toruń, Toruń, 87–100, Poland
Centre for Climate Change Research, Nicolaus Copernicus University in Toruń, Toruń, 87-100, Poland
Dagmara Adamska
Faculty of Historical and Pedagogical Sciences, History Department, University of Wrocław, Wrocław, 50-139, Poland
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Katarzyna Słomska-Przech, Aniela Rząsa, and Tomasz Panecki
Abstr. Int. Cartogr. Assoc., 5, 13, https://doi.org/10.5194/ica-abs-5-13-2022, https://doi.org/10.5194/ica-abs-5-13-2022, 2022
Tomasz Panecki and Tomasz Królik
Abstr. Int. Cartogr. Assoc., 5, 37, https://doi.org/10.5194/ica-abs-5-37-2022, https://doi.org/10.5194/ica-abs-5-37-2022, 2022
Katarzyna Słomska-Przech, Tomasz Panecki, and Wojciech Pokojski
Abstr. Int. Cartogr. Assoc., 5, 66, https://doi.org/10.5194/ica-abs-5-66-2022, https://doi.org/10.5194/ica-abs-5-66-2022, 2022
Tomasz Panecki and Tomasz Królik
Abstr. Int. Cartogr. Assoc., 3, 229, https://doi.org/10.5194/ica-abs-3-229-2021, https://doi.org/10.5194/ica-abs-3-229-2021, 2021
Katarzyna Słomska-Przech, Dawid Maciuszek, Aniela Rząsa, and Tomasz Panecki
Abstr. Int. Cartogr. Assoc., 3, 270, https://doi.org/10.5194/ica-abs-3-270-2021, https://doi.org/10.5194/ica-abs-3-270-2021, 2021
Tomasz Panecki
Abstr. Int. Cartogr. Assoc., 1, 287, https://doi.org/10.5194/ica-abs-1-287-2019, https://doi.org/10.5194/ica-abs-1-287-2019, 2019
Tomasz Panecki and Wojciech Pokojski
Abstr. Int. Cartogr. Assoc., 1, 288, https://doi.org/10.5194/ica-abs-1-288-2019, https://doi.org/10.5194/ica-abs-1-288-2019, 2019
Related subject area
Subject: Climate Modelling | Archive: Historical Records | Timescale: Holocene
Asymmetric changes in temperature in the Arctic during the Holocene based on a transient run with the Community Earth System Model (CESM)
The blue suns of 1831: was the eruption of Ferdinandea, near Sicily, one of the largest volcanic climate forcing events of the nineteenth century?
Northern Hemisphere atmospheric pattern enhancing Eastern Mediterranean Transient-type events during the past 1000 years
Synergy of the westerly winds and monsoons in the lake evolution of global closed basins since the Last Glacial Maximum and implications for hydrological change in central Asia
A regional climate palaeosimulation for Europe in the period 1500–1990 – Part 2: Shortcomings and strengths of models and reconstructions
Simulated climate variability in the region of Rapa Nui during the last millennium
Hongyue Zhang, Jesper Sjolte, Zhengyao Lu, Jian Liu, Weiyi Sun, and Lingfeng Wan
Clim. Past, 19, 665–680, https://doi.org/10.5194/cp-19-665-2023, https://doi.org/10.5194/cp-19-665-2023, 2023
Short summary
Short summary
Based on proxy data and modeling, the Arctic temperature has an asymmetric cooling trend with more cooling over the Atlantic Arctic than the Pacific Arctic during the Holocene, dominated by orbital forcing. There is a seasonal difference in the asymmetric cooling trend, which is dominated by the DJF (December, January, and February) temperature variability. The Arctic dipole mode of sea level pressure and sea ice play a major role in asymmetric temperature changes.
Christopher Garrison, Christopher Kilburn, David Smart, and Stephen Edwards
Clim. Past, 17, 2607–2632, https://doi.org/10.5194/cp-17-2607-2021, https://doi.org/10.5194/cp-17-2607-2021, 2021
Short summary
Short summary
An unidentified eruption in 1831 was one of the largest volcanic climate forcing events of the nineteenth century. We use reported observations of a blue sun to reconstruct the transport of an aerosol plume from that eruption and, hence, identify it as the 1831 eruption of Ferdinandea, near Sicily. We propose that, although it was only a modest eruption, its volcanic plume was enriched with sulfur from sedimentary deposits and that meteorological conditions helped it reach the stratosphere.
Aleix Cortina-Guerra, Juan José Gomez-Navarro, Belen Martrat, Juan Pedro Montávez, Alessandro Incarbona, Joan O. Grimalt, Marie-Alexandrine Sicre, and P. Graham Mortyn
Clim. Past, 17, 1523–1532, https://doi.org/10.5194/cp-17-1523-2021, https://doi.org/10.5194/cp-17-1523-2021, 2021
Short summary
Short summary
During late 20th century a singular Mediterranean circulation episode called the Eastern Mediterranean Transient (EMT) event occurred. It involved changes on the seawater physical and biogeochemical properties, which can impact areas broadly. Here, using paleosimulations for the last 1000 years we found that the East Atlantic/Western Russian atmospheric mode was the main driver of the EMT-type events in the past, and enhancement of this mode was coetaneous with low solar insolation.
Yu Li and Yuxin Zhang
Clim. Past, 16, 2239–2254, https://doi.org/10.5194/cp-16-2239-2020, https://doi.org/10.5194/cp-16-2239-2020, 2020
Short summary
Short summary
Monsoons and westerly winds interact with each other in the middle to low latitudes. We track millennial-scale evolution characteristics of monsoons and westerly winds over the past 21 000 years. In the monsoon-dominated regions of Asia, a humid climate prevails in the past 6000–10 000 years, while in the westerly-wind-dominated regions of Asia, the climate is relatively humid around 21 000 years and 6000 years ago.
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
C. Junk and M. Claussen
Clim. Past, 7, 579–586, https://doi.org/10.5194/cp-7-579-2011, https://doi.org/10.5194/cp-7-579-2011, 2011
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Short summary
We wanted to take an in-depth look at how climate events affected the economy of early modern Poland. We focused on analysing all available sources of a fiscal nature for this period. In addition, we analysed available materials on the export of primary agricultural products. Our results have shown that the economic system in Poland at that time coped effectively with periodic droughts, and it was only the great drought of 1540 that significantly shook the state's economy.
We wanted to take an in-depth look at how climate events affected the economy of early modern...
