the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Air temperature changes in Wrocław (SW Poland) in 1773–81 based on a newly discovered series of meteorological measurements
Abstract. The article presents a description of a newly discovered series of meteorological measurements made in Wrocław (SW Poland) in 1773–81 and its importance for climate analysis. The series is the third-oldest available for Wrocław. The 1773–81 observations were made by Johann Ephraim Scheibel on the premises of the Gymnasium that belonged to the Church of St Elizabeth (central Wrocław). Meteorological observations of air temperature and atmospheric pressure were made three times a day (morning, midday and evening) – or twice a day (morning and evening) for atmospheric precipitation, wind (including direction and force) and humidity. The meteorological registers were published in the newspaper Oekonomische Nachrichten der Patriotischen Gesellschaft in Schlesien issued in Wrocław in the years 1773–81. Between 1773 and 1776, the meteorological data were published in each weekly edition of the newspaper. From 1777 onwards, the data were published for the entire month and in three-month blocks in the last two years. In addition to the measurements, J. E. Scheibel also published, in the same source, between one and three pages of weather descriptions for each month or block of two to three months. The air temperature in Wrocław during the period 1773–81 was 1.2 °C and 0.3 °C warmer than in the respective equivalent periods 100 and 200 years later (i.e., 1873–81 and 1973–81) but 2.1 °C colder than in the most recent period (2013–21). The increase in temperature between the study period and the most recent period was greatest in summer (2.8 °C) and smallest in spring (1.4 °C).
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Status: open (until 27 Feb 2026)
- RC1: 'Comment on egusphere-2025-6326', Christian Pfister, 20 Jan 2026 reply
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RC2: 'Comment on egusphere-2025-6326', Thomas Pliemon, 25 Jan 2026
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RC3: 'Comment on egusphere-2025-6326', Anonymous Referee #3, 02 Feb 2026
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In this paper, the authors describe a newly recovered series of temperature observations from a site in Wrocław covering the period 1773–1781. Such series are extremely valuable because—despite the inherent limitations of early instrumental observations—they provide data at a much higher temporal resolution than is achievable with most proxy records. In particular, they capture the full seasonal cycle, whereas many proxy series are restricted to specific parts of the year (for example, growing-season temperatures).
The period studied is also of particular interest, as it coincides with a time when the competing influences of solar variability and volcanic forcing remain poorly constrained, and which broadly corresponds to a phase of relatively cooler average temperatures.
The temperature observations presented appear to be highly reliable and to have been recorded using a responsive instrument. I was pleased to see the comparison with temperature estimates from the ModE-RA reanalysis, and I fully agree with the authors that assimilation of these data into palaeoreanalysis products would further enhance their value, particularly if combined with the construction of a longer regional temperature series.
The paper primarily consists of a description of the data and an evaluation of the observations against other available series. As such, it represents an incremental contribution; nevertheless, it is a valuable one and fits well within the remit of the journal.
Specific comments
Line 21: “atmospheric” is not needed before “precipitation”.
Line 44: The definition of the aims of historical climatology is too limited. For example, Brázdil et al. (2005, p. 366, doi:10.1007/s10584-005-5924-1) describe three aims of historical climatology:
(i) reconstructing temporal and spatial patterns of weather and climate, as well as climate-related natural disasters, for the period prior to the establishment of national meteorological networks (mainly over the last millennium);
(ii) investigating the vulnerability of past societies and economies to climate variability, climate extremes, and natural disasters;
(iii) exploring past discourses and social representations of climate.Line 160: It would be useful to place the link to the data in a more prominent location, for example in a dedicated section at the end of the paper titled “Data Availability”, with a brief description of the repository.
Line 142: Change “exposition” to “exposure”.
Figure 4: The morning and Tmin curves are shown in the same colour; please revise the figure to allow clear visual distinction.
Figure 9: Please invert the sign of the difference so that, for example, the grey bars represent positive values.
Around page 15: Please include a time series (1773–1781) showing the difference between the ModE-RA series representative of Wrocław and the newly recovered temperature series. This could be included as a supplementary figure if space is limited.
Line 404: Please explain why the reconstructed temperature series should be expected to outperform the palaeoreanalysis.
Citation: https://doi.org/10.5194/egusphere-2025-6326-RC3
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The article presents a recently discovered series of meteorological measurements made in Wrocław (SW Poland) in 1773–81 comprising daily observations of air temperature and atmospheric pressure, precipitation, wind force and direction.. The analysis focuses on air temperature extending the regular temperature series for Wrocław back to 1773. the scientific methods and assumptions valid and clearly outlined? The paper is clearly structured and the figures are of high quality. As a result, the Wroclaw series will be the longest temperature series in Poland.
The article should be published with minor revisions.