the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 22 Jul 2019
Early instrumental meteorological measurements in Switzerland
Lucas Pfister
Franziska Hupfer
Yuri Brugnara
Lukas Munz
Leonie Villiger
Lukas Meyer
Mikhaël Schwander
Francesco Alessandro Isotta
Christian Rohr
Stefan Brönnimann
The decadal variability of weather and its extremes are still poorly understood. This is partly due to the scarcity of records, which, for many parts of the world, only allow for studies of 20th century weather. However, the 18th and early 19th centuries saw some pronounced climatic variations, with equally pronounced impacts on the environment and society. Considerable amounts of weather data are available even for that time but have not yet been digitised. Given recent progress in the quantitative reconstruction of subdaily weather, such data could form the basis of weather reconstructions. In Switzerland, measurements before 1864 (the start of the national network) have never been systematically compiled except for three prominent series (Geneva, Basel, Great St. Bernard Pass). Here we provide an overview of early instrumental meteorological measurements in Switzerland resulting from an archive survey. Our inventory encompasses 334 entries from 206 locations, providing an estimated 3640 station years and reaching back to the early 18th century. Most of the data sheets have been photographed and a considerable fraction is undergoing digitisation. This paper accompanies the online publication of the imaged data series and metadata. We provide a detailed inventory of the series, discuss their historical context, and provide the photographed data sheets. We demonstrate their usefulness on behalf of two historical cases and show how they complement the existing series in Europe. If similar searches in other countries yield similarly rich results, an extension of daily weather reconstructions for Europe back to the 1760s is possible.
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While decadal-to-multidecadal climate variability has become a major research focus in recent years, decadal variability in weather is still poorly understood. This is partly due to the fact that the observed record covers only an insufficient number and variety of decadal climatic anomalies and changes. Thus, there is a need to extend the record back in time. A monumental effort to draw historical daily weather maps was undertaken in the 1980s (Kington, 1988). A suite of recent, numerical approaches has targeted the reconstruction of weather based on early instrumental meteorological measurements, comprising data assimilation (e.g. the Twentieth Century Reanalysis, 20CR; Compo et al., 2011; or the coupled European reanalysis of the 20th century, CERA-20C; Laloyaux et al., 2018), daily weather-type reconstruction (Schwander et al., 2017; Delaygue et al., 2019), or analogue approaches (Yiou et al., 2014; Flückiger et al., 2017). These approaches allow, at least partly, for addressing changes in atmospheric dynamics. 20CR reaches back to the mid-19th century, i.e. the start of national weather services. Can we analyse weather variability even further back in time? In this paper we show, for the case of Switzerland, that rich, hitherto unknown data sources can still be found today in archives.
The 18th and early 19th centuries saw pronounced climatic variations in central Europe, such as a much-discussed warm and dry period around 1800 (e.g. Frank et al., 2007; Böhm et al., 2010), which was followed by an extremely cold period during the early 19th century (Brönnimann, 2015). Furthermore, a period of increased flood frequency occurred in the 19th century in Switzerland (Pfister, 1999; Schmocker-Fackel and Naef, 2010; see also Brönnimann et al., 2019). These climatic events had pronounced impacts on the environment and society (e.g. Summermatter, 2005; Stucki et al., 2018), which makes them interesting examples to study. Present climate risk management can make use of historical weather data and historical documents (Brönnimann et al., 2018a).
In Switzerland, a national meteorological network was initiated in December 1863 and maintained by the Schweizerische Naturforschende Gesellschaft (Swiss Society of Natural Sciences) before it became part of the Swiss federal administration (today MeteoSwiss) in 1881 (Hupfer, 2017). These data are well documented; a considerable fraction has been digitised and is electronically available (e.g. Begert et al., 2005). Three prominent series that reach further back than 1864 were re-evaluated (on the basis of daily or monthly mean values) in the 1950s (Bider et al., 1958; Schüepp, 1961), namely Geneva, Basel (both back to the mid-18th century), and Great St. Bernard Pass (back to 1819). These series have been important in climate science and for climate reconstruction, for which monthly resolved temperature series form the basis. They are also incorporated in the Austria-led database HISTALP (Auer et al., 2007). We have recently re-digitised these three long records based on original values rather than daily means (Füllemann et al., 2011) but not the full set of records that would possibly be available. In fact, measurements before 1864 have not been systematically compiled recently. Starting in 2005, MeteoSwiss registered its archive collections (in collaboration with the company GRAD GIS; project leader: Thomas Specker) and transferred them to the Swiss Federal Archives in Bern or the State Archives of the canton of Zurich (Fonds Naturforschende Gesellschaft in Zürich). The transfer to public archives and the cataloguing of these holdings made many Swiss records easier to access.
Already in 1864, Rudolf Wolf, the director of the Schweizerische Meteorologische Zentralanstalt (Swiss Central Meteorological Agency), gathered information about meteorological records in Switzerland dating back to the 16th century and pointed out their scientific value (MZA, 1864). The aim was to make several of these records accessible, but only few early instrumental data series were later published in some of the first Swiss meteorological annals in the 19th century. Unfortunately, they were mostly published in the form of daily mean values (within the EU project EMULATE, these daily data were digitised back to 1850 for Geneva, Zurich–Uetliberg, and Bern). In the 1920s, Billwiller (1927) published a more comprehensive inventory of Swiss meteorological records prior to 1864, compiling the available information on the series (but not the data). Individual studies have addressed some of the early records (e.g. Gisler, 1983). Gisler (1983, 1985) analysed instrumental series from Schaffhausen and Zurich, but they were only based on monthly mean values. Some of the shorter series have been analysed as an object of historical studies (e.g. Burri and Zenhäusern, 2009), but the original data have not been digitised. This is particularly true for instrumental measurements, while precipitation observations were sometimes digitised and incorporated into databases (e.g. EURO-CLIMHIST; see also Gimmi et al., 2007). Although meteorological networks in Switzerland in the mid-19th century have been analysed by historians (e.g. Pfister, 1975; Hupfer, 2015, 2019), no attempts have been undertaken to compile and digitise the data.
Here we report the results from a systematic survey of early instrumental meteorological measurements in Switzerland. Archive work brought to light more than 300 station records prior to 1864, some reaching back to the early 18th century. This paper accompanies the online publication of the photographed data sheets and metadata. A subsequent paper will describe the digitised records. Note that Switzerland serves as an example here of what could be found elsewhere in Europe.
The paper is organised as follows. Section 2 provides an overview of the history of meteorological measurement in Switzerland from the 18th century to the start of the national weather service. Section 3 describes the archive work and the resulting inventory. In Sect. 4 we demonstrate the usefulness of the photographed data sheets with two examples. Conclusions are drawn in Sect. 5.
In the mid-17th century, weather observation started to change from being qualitative to largely quantitative. Instrumental measurements were a trend that originated in the “quantifying spirit” of the Enlightenment, making instrumentation a new priority for scholars in Europe (Frängsmyr et al., 1990; Bourguet et al., 2002). However, instrumental measurements have only gradually replaced qualitative assessments of the weather. The instrumental method did not reach its supremacy in meteorological observation until the 19th century (Janković, 2001). The quantification process interacted with the development of meteorological instruments. The first thermometers were built in the early 1600s and the first barometers some decades later, with contributions from several well-known naturalists such as Descartes (Middleton, 1969; Golinski, 1999). Also, hygrometers and instruments for measuring precipitation, wind direction, and wind force came into use in the 17th century. Subsequently, these devices underwent technical changes, thus becoming an important part of the history of meteorological data.
Scholars took along meteorological instruments on travel, observing on mountains and other special locations that they thought deserved attention. Some also conducted regular instrumental measurements in their hometowns. In Switzerland, Johann Jakob Scheuchzer (1672–1733), a physician and professor of mathematics in Zurich who was well connected within the scholarly community of his time, made daily observations of atmospheric pressure, temperature, and precipitation. Starting in 1708, his records (with some interruptions until 1731) are the oldest instrumental series in the territory of today's Switzerland. Although the original diary is lost, many of Scheuchzer's results are known thanks to his publications in journals (Pfister, 1984). Scheuchzer's interest in weather data was part of his larger programme to collect all sorts of information on Swiss and alpine natural history (Pfister, 1975; Boscani Leoni, 2013, 2016). His efforts to get meteorological observations from peripheral regions had little success in general. Nevertheless, he managed to arrange measurements on St. Gotthard Pass: the Capuchin hospice agreed to read the barometer that Scheuchzer had installed there every day (Fischer, 1973). This allowed for corresponding observations between Zurich and St. Gotthard Pass (1728–1730). Observational programmes in order to compare meteorological measurements were also conceived by scientific societies or academies. The earliest example is the Florentine Accademia del Cimento, which sent thermometers to several places in Europe shortly after its foundation in 1657 (Hellmann, 1901, 1914). These data have been digitised and evaluated (Camuffo and Bertolin, 2012).
From the early 18th century on, attempts were made to publish compilations of data from different locations. When the Wrocław physician Johann Kanold invited other savants to submit their records for publication, Scheuchzer provided the Zurich data (1718–1726; see Steiger, 1933). Between 1718 and 1730, Kanold collected and printed meteorological information from more than 20 European cities in his Breslauer Sammlung (Hellmann, 1927; Feldman, 1990; Lüdecke, 2010). The Royal Society in London carried out a similar project, initiated in 1723 by its secretary, James Jurin, who issued an invitation to potential observers. During approximately 10 years, the Royal Society published Jurin's collected responses in its journal (Hellmann, 1914; Daston, 2008). Such undertakings illustrate the growing interest of 18th century scholars in comparing empirical details. As a result, exchanges across the political borders of Europe were stimulated.
In the second half of the 18th century, many projects were initiated to coordinate and publish meteorological observations, most of them by scientific, economic, or agricultural societies. Among the organisations with a meteorological programme was the Oekonomische Gesellschaft Bern (Economic Society of Bern). Soon after its foundation in 1759, the society equipped several stations in different regions with thermometers and barometers (OeGB, 1762; Pfister, 1975). In the following decade, three to eight locations sent in measurements, monthly means and extremes of which were printed in the society's journal. This observation network set up by the Oekonomische Gesellschaft was small regarding the number of stations and the geographic reach (all stations were in the territory of the Republic of Bern, including its Vaudois territories and those ruled in common with Fribourg). Identically equipped stations represented an innovative method initiated by such networks and soon also followed on a larger scale. The best-known 18th century initiative to establish an extended network of observers is the Mannheim-based Palatine Meteorological Society (Societas Meteorologica Palatina; see Cassidy, 1985; Kington, 1988; Wege and Winkler, 2005; Lüdecke, 2010). It was a state-subsidised project: the elector of Palatine and of Bavaria, Karl Theodor, provided the society's funds. Under his patronage, the court priest Johann Jakob Hemmer organised a network of over 30 stations in various parts of Europe. He also set up a station in Greenland and one in North America. All observers received a set of calibrated instruments (one barometer, two thermometers, and one hygrometer) together with instructions on observational procedures (e.g. the subdaily observation times were fixed for 07:00, 14:00, and 21:00 UTC+1). The registers were dispatched to Mannheim for publication in the society's journal called Ephemerides (12 volumes; 1781–1792). In the territory of today's Switzerland, two observers participated in the Palatine Society's network: the pastor and librarian Jean Senebier in Geneva and the Capuchin monk Onuphrius on the St. Gotthard Pass, succeeded by fellow monks (Billwiller, 1927; Pfister, 1984; Grenon, 2010).
The ambitious plan of standardising instruments and observing practices within these early networks of meteorological stations strived to improve the comparability of the measurements. Given the high individuality of instruments in the 18th century, it was extremely difficult to compare the observations (Daston, 2008). In this context, standardisation became an important issue. The participants of the late 18th and early 19th century networks observed with more precise instruments compared to most of the ones engaged outside coordinated projects. Also, they usually observed with more regularity (often subdaily at predetermined times) and submitted their tables to coordinators, who often published them in summaries or – less frequently – as full records. The growing amount of printed meteorological data was influenced by the expanding production of scholarly journals in the 18th century (for scholarly media culture, see Holenstein et al., 2013). By defining publishing criteria for meteorological observations, networks had a standardising effect. However, affiliation with a network did not necessarily guarantee high quality. Coordinators only had limited control over their observers. Many of them worked as volunteers and did not always follow their coordinators' guidelines, which were often poorly explained. Within a single network of stations, observations could vary significantly in reliability. Furthermore, not all networks had the resources to distribute instruments, which limited the degree of standardisation.
Meteorological networks founded until the middle of the 19th century (before the era of official state observing systems) were all transitory. They seldom endured for more than 20 years (Edwards, 2010). Some never aimed at long-term series; others sought permanence but faced problems in resources. In the case of the Palatine Society, the project declined after the death of its first coordinator. The French Revolutionary Wars further contributed to the disintegration of the network. The last annual report was printed in 1795, 15 years after the promising start. The above-mentioned network of the Oekonomische Gesellschaft Bern was not a long-lasting one either: when the society as a whole became quite inactive for some time, its meteorological project was abandoned after 10 years of existence (1760–1770). Most networks had a high fluctuation of observers: only some of them pursued their measurements with tenacity over many years. The difficulties to build permanent structures persisted in the first half of the 19th century – despite the many endeavours to create and maintain networks with regional or cross-border dimensions.
Within the territory of today's Switzerland, the early initiative of the Oekonomische Gesellschaft Bern was followed by several attempts at observational network building (see Table 1): in the 1810s, the Naturforschende Gesellschaft (Society of Natural Sciences) in Aarau sent barometers to approximately 10 observers in different European cities but did not receive enough useful registers to publish a compilation (Hefty-Gysi, 1953). Some decades later, in the 1850s, the society set up a network inside the canton of Aargau. However, most of the 22 stations stopped observations after less than 3 years (Hartmann, 1911). The network of the Thurgauische Naturforschende Gesellschaft (Society of Natural Sciences of Thurgau) was short-lived as well (starting in 1855; see Bürgi, 2004). In the canton of Grisons, many members of the cantonal Naturforschende Gesellschaft Graubündens (Society of Natural Sciences of Grisons) participated in the observational system that Christian Gregor Brügger, a student and later secondary school teacher and natural history researcher, had initiated in 1856 (Hupfer, 2015). After Brügger left the region in 1859, the network lacked supervision and started to fall apart (although data were still collected). Some stations were incorporated into the national network starting in 1863. In the French-speaking part of Switzerland, the Société des sciences naturelles de Neuchâtel (Society of Natural Sciences of Neuchâtel) initiated a network in 1856 comprising six stations in the canton of Neuchâtel (Kopp, 1856). From these stations, however, only two persisted until integration into the national network. Another better-controlled network was operated by the observatory in Bern, which had equipped eight stations in cooperation with the Naturforschende Gesellschaft in Bern (Society of Natural Sciences of Bern) and the cantonal government (starting in 1860; see Wild, 1860).
Besides these regional projects, the Swiss Society of Natural Sciences (established in 1815, today the Swiss Academy of Sciences or SCNAT) aimed at a network at the national level. However, its first network with 12 stations, conceptualised by the Geneva observatory director Marc-Auguste Pictet in 1823, faced problems similar to those of other initiatives. It lacked a financed coordination centre and was confronted with high publication costs and a considerable drop-off rate amongst its observers. Finally, the society abandoned its project in 1836 and printed only the means and extremes of three stations (Basel 1826–1836, Bern 1826–1836, St. Gallen 1827–1832; see Merian et al., 1838). The society was to have more success with its second attempt, undertaken in the 1860s, with support from the Swiss Federal State.
In the period of repeated efforts for expanded and durable observational enterprises, there were far more persons involved than just those belonging to networks. Many observed as individuals and some on behalf of institutions such as universities or monasteries. Observations provided by institutions were often independent from the success or failure of meteorological networks. The Geneva observatory, for example, continued its measurements (started in 1772) regardless of whether it was participating in a network or not (Gautier, 1843). Other long series evolved in Basel where, among others, the university professors Johann Jakob d'Annone and Peter Merian observed for almost 50 years each (1755–1804 and 1826–1874, respectively; see Riggenbach, 1892; Bider et al., 1958). Merian in particular had an established status within the meteorological research community. However, the qualifications of 18th and 19th century observers ranged widely, spanning from university scholars such as Merian to persons without any scientific training. In the 18th century, thermometers and barometers became increasingly affordable, leading to wider public use (Golinski, 2007). This diversity limits the possibility of generalisations about the observers.
The interest in meteorological measurements derived from both theoretical and practical goals. Most observers saw their systematic observations as a contribution to a scientific understanding of weather and climate (see, for example, Pictet, 1780). They hoped that their records might eventually show regularities that would allow for the establishment of natural laws or discerning correlations with celestial motions (for the Palatine Society's goals see Cassidy, 1985; more general: Daston, 2008). Although the observation networks could not provide current weather information before the widespread introduction of the telegraph (invented in 1837), many organisers expected that their long-term data would help to predict the weather (Feldman, 1990). Others, particularly the Oekonomische Gesellschaft Bern, were interested in the impact of atmospheric conditions on plants, hoping to derive practical measures in their effort to improve agricultural methods (Carrard, 1763; Pfister, 1975). Another source of interest was medical, relating weather conditions to diseases, plagues, or mortality (Fleming, 1990).
Table 1Meteorological networks with stations in the territory of today's Switzerland.
Whereas the organisers of networks often explicitly outlined their motivation, little is known about the reasons for which individuals (connected to a network or not) started observations. The few testimonies reveal a desire to learn and to support knowledge production, often with a focus on their locality or region (Janković, 2001; Hupfer, 2015). In most cases, meteorological records were made by literate persons. However, well-off and almost exclusively male observers were often supported by household members who replaced them during their absences. Many observers not only monitored the weather, but were also involved in other investigations of nature such as phenological observations and botanical classifications. Some of them were well-known botanists, e.g. Laurent Garcin (1683–1752) and Abraham Gagnebin (1707–1800). A remarkable number of meteorological observers in 18th and 19th century Switzerland belonged to the liberal elite, among them the famous politician and author Heinrich Zschokke (1771–1848). Moreover, members of the clergy formed an important group among the observers. When pastors were moved to another church, they often took their instruments with them, e.g. Rudolf Ludwig Fankhauser (1796–1886), who carried out measurements in three different parishes in the canton of Bern. Clergymen, physicians, pharmacists, lawyers, or magistrates were not only typical meteorological observers, but were in general also strongly represented in Europe's natural history community. In the pre-20th century, this community was not limited to professional researchers, but also included many non-academics.
In December 1863, an important organisational transformation in meteorological measurement took place in Switzerland: a national observation network was started, organised by the Schweizerische Naturforschende Gesellschaft (Swiss Society of Natural Sciences) and supported by the Swiss Federal State (established in 1848). It encompassed 88 stations, incorporating many observation sites and observers from previous measurement initiatives, e.g. Aarau, Basel, and Geneva, as well as a great number of stations from the Brügger network in Grisons (Mousson, 1864). State funding provided the financial stability that had been lacking in the many previous attempts. The network was still a system of volunteer observers. However, its coordination was professionalised in the form of an administrative centre, the Schweizerische Meteorologische Zentralanstalt (Swiss Central Meteorological Agency, later MeteoSwiss). This state-supported institution pushed for the standardisation of both observers and instruments and adapted international agreements about the recording and communication of data (Hupfer, 2017, 2019; on internationalisation: Edwards, 2010). After a few years, in 1881, the meteorological agency became an official state institution responsible for climate monitoring and synoptic weather forecasting based on international telegraphic data exchange.
Figure 1Two examples of data sheets from Vevey and Schaffhausen from the Swiss Federal Archives (signatures: E3180-01#2005/90#202*; E3180-01#2005/90#231*).
The national observation networks that have emerged since the middle of the 19th century still form the basis of climate monitoring today. Compared to the 18th and early 19th century organisational structures, these state-founded networks can be considered quite stable. Over the long term, measuring practices have developed towards increased standardisation. However, the history of meteorological measurements is not only a success story, but also a history of many discontinued projects and unfulfilled expectations regarding both theoretical and practical aspects. Despite the less developed standards of the pre-1864 period, the inventoried series are informative for past weather events. What presents us with a challenge is the fact that measurement conditions were often not systematically documented. Therefore, it is necessary to not only make the data available, but also to examine the multiple contexts from which these observations originate.
Our archive search started from the above-mentioned previous compilations, most of which were published more than 100 years ago. Furthermore, we consulted the cantonal societies of natural sciences, checked their websites, and conducted an online search targeted at digitally available journals and publications from these societies (Ephemerides, journals of the natural sciences societies available at e-periodica). In a next step, digital libraries were searched for meteorological data (e.g. Munich Digitization Center MDZ, Google Books, e-periodica, e-manuscripta, and others), as were publications from MeteoSwiss (supplementary volumes of the MeteoSwiss annals). Moreover, we consulted a number of libraries and archives (Swiss Federal Archives, Cantonal Archive Aargau, Cantonal Library Aargau, University Library of Basel, Burgerbibliothek of Berne, University Library of Bern, Archive of the Monastery of Einsiedeln, Cantonal/University Library Fribourg, Cantonal Archive and Library of Geneva, Cantonal Library/Archive Grisons, University Library of Neuchâtel, City Archive Schaffhausen, Cantonal Library Vadiana St. Gallen, Cantonal Archive Vaud, Cantonal/University Library Lausanne, Cantonal Archive Zurich, City Library Zurich) and queried many more libraries and archives about meteorological data in their holdings. Two examples of data sheets from the Swiss Federal Archives are displayed in Fig. 1.
From the known meteorological records, the vast majority could be located (see Fig. 2). Apart from instrumental measurements, a considerable number of qualitative weather descriptions, as well as phenological records, was found but has not been inventoried. The archive work revealed that many more series exist than the ones known so far. If original records could be found (the majority of the series), they were photographed together with all available metadata. For certain series, transcripts and printed versions were photographed instead of missing original manuscripts. In some cases, we could not locate the data but found information about the station or observer, or we found data only in statistical form and not as raw data. In these cases, the metadata were collected as completely as possible, enabling future users to better track the data.
Figure 2Number of possibly available measurement series (grey) and number of series for which subdaily data were found (green) as a function of the year. The peak around 1860 is due to the Brügger network in Grisons, encompassing around 90 locations. From 1864 onwards, only series starting prior to this date that have not been included in the national network are depicted.
For each series, the time period and resolution, variables measured, location, observer, and sources of any information are stored in our inventory. Long series are thus often fragmented in many short, sometimes overlapping sequences. The full inventory is published in the Supplement; an abridged version is given in Table 2. Some basic characteristics, such as the length of the records and the start year, are visualised in Figs. 3 and 4.
Figure 3Map of the available stations in Switzerland before 1864 showing the length of the series.
Figure 4Maps of the available stations over time. Measurement series starting in the indicated period are shown as red dots, while grey dots represent stations with continuing observations.
Table 2Summary inventory of all stations with at least 10 years of data, summarised per station (variables: p – pressure, T – temperature, w – wind, R – precipitation, d−1 – the number of measurements per day). Station names are sorted by the start year of the series and indicated in the corresponding local language.
The number of series found – over 300 – was much larger than anticipated. While many series (e.g. those of the Grisons network) were rather short, we also found several long series, as well as segments that could possibly be combined into long series (see Fig. 3). In addition to the three long (>200 years) series that are presently available – Geneva, Basel, and Great St. Bernard Pass – many other long series could possibly be generated such as Zurich, Schaffhausen, Aarau, Bern, St. Gallen, and others. Our inventory encompasses 334 entries from 206 locations, providing an estimated 3640 station years reaching back to the early 18th century.
Based on this information, the data to be photographed and digitised were prioritised. Long series had a higher priority than short series, and series from the 18th century had higher priority than those from the 19th century. In total, temperature, pressure, and (if available) precipitation, as well as other variables for more than 50 measurement series have been digitised. The digitised data, along with a description of the quality assurance, will be described in a subsequent paper. The focus here is on the inventoried and photographed series, as they provide rich additional information (e.g. weather descriptions, rainfall, wind, etc.) that is not digitised but can be accessed online. With the permission of the respective archives and libraries, the images of the meteorological series and corresponding metadata are published at the open-access repository Zenodo (https://doi.org/10.5281/zenodo.3066836). The images are structured in folders following the full inventory in the Supplement with series ordered alphabetically by location and chronologically for each location. Each published series has an ID assigned to facilitate locating the series on the repository. For series that are already published online, a link is indicated in the inventory.
4.1 The cold surge in December 1788
In Europe, the winter of 1788/89 was one of the most severe during the last 300 years. The cold surge led to the freezing of the Venetian Lagoon, as well as many lakes, and had vast impacts on society and the economy (e.g. Lamb, 1995; Camuffo, 1987). In Switzerland, the winter began early, with below-freezing temperatures in the lowlands starting from 22 November. Apart from a brief warming around Christmas (a period of stormy weather), temperatures remained low until 8 January. In the CAP7 weather type classification of Schwander et al. (2017), which, based on station data, extends the MeteoSwiss CAP9 weather types back into the past (Weusthoff, 2011), and most of the days during this period were of type 6 (“North”), most others were type 1 (“North East, indifferent”), type 4 (“East, indifferent”), or type 5 (“High Pressure”). These types indicate the flow of cold, continental air towards Switzerland. Over Christmas, winds turned south-westerly (“West Cyclonic” type 7), then back to northerly and to easterly.
As a side note, this cold winter (together with a preceding drought and the following flood-rich spring) worsened the economic crisis (increased costs) and supply situation in France. Without overemphasising the role of weather, it arguably did play a role in paving the ground for the French Revolution in the following summer.
During this period, the Palatina network was active, providing data from two Swiss stations (Geneva and St. Gotthard Pass at 2091 m a.s.l.). Additional data were photographed and digitised from four stations: Sutz, Bern (two series for January 1789), Basel, and a second independent series from Geneva. Figure 5 shows excerpts of two data sheets. According to our inventory, further data might be available for Chur, Glarus, Winterthur, and Zurich, as well as from additional observers from Basel and Geneva. However, we have not yet entirely located these data.
Raw temperature series from digitised available locations are shown in Fig. 6, together with the daily weather types. Temperature series agree very well with each other over this period. All mutual correlations are between 0.89 and 0.99 except for St. Gotthard Pass, which often lies above the inversion layer that covers the Swiss Plateau and therefore shows a clearly different behaviour. All lowland series show a cooling, with negative temperatures from late November onwards. During the very cold phases, temperatures at St. Gotthard Pass were not far below those on the Swiss Plateau, which indicates stable conditions or an inversion. Conversely, the gradient is larger during phases of cyclonic weather (e.g. type 7); i.e. the Christmas warming was clearly less pronounced at St. Gotthard Pass than in the lowlands. The change from northerly to south-westerly winds back in late December can clearly be seen in the observations from Bern (Fig. 5), while at St. Gotthard Pass (possibly due to channelling, which remains to be studied), winds remained north-westerly throughout the second half of December.
Figure 5Excerpts of data sheets from Bern and St. Gotthard Pass for the second half of December 1788. For St. Gotthard Pass, the wind was noted as “NW” for every single day; not shown (Burgerbibliothek of Berne: Mss.h.h.XX.5.2; LMU Munich library: 0001/4 Phys.861(1888)).
Figure 6Temperature at Geneva, Basel, Bern, Sutz, and St. Gotthard Pass in November to January 1788/89. If several observations were made per day, we show the sunrise temperature. Note that these are the digitised raw data in degrees Réaumur. The series from Basel was shifted upward by 10∘ for visualisation. The bottom bar indicates the weather type according to Schwander et al. (2017).
This brief example demonstrates that daily weather can indeed be reconstructed from the combination of all digitised records. Adding pressure information and records from neighbouring countries could possibly allow for a more detailed view on late 18th century daily weather in central Europe.
4.2 The heavy precipitation event on 4 and 5 July 1817
Precipitation measurements are sparse in the early 19th century. Although we did not systematically collect non-measured precipitation information, the descriptions in our photographed data sheets reveal interesting insights. An example is the flood event in July 1817, when Lake Constance reached the highest level since the beginning of measurements (see Rössler and Brönnimann, 2018). Though melting snow contributed (at high altitudes consisting of a triple snowpack with winter snow from 1815 to 1816, which could not melt during the cold summer of 1816 but was covered by summer snow, on top of which lay the winter 1816–1817 snowpack), it is very unlikely to have been a main cause, according to model simulations (Rössler and Brönnimann, 2018). Rather, a heavy precipitation event in early July must have triggered the flood.
The only available precipitation series in Switzerland is from Geneva and indicates 29 mm on 5 July. This is clearly not sufficient to judge whether a heavy precipitation event affected Switzerland. However, using not just the measurements but also the weather observations and comments (which were not the focus of the project and hence not systematically collected), more can indeed be said. Our photographed data sheets indicate rain all day long in Aarau on 4 and 5 July and in St. Gallen on 5 July. The monastery of Einsiedeln (see Fig. 7) noted strong precipitation already on 1 and 2 July (“pluvia, serenum”), two thunderstorms on 4 July (“vespere tempestas, noctu repetita”), and again rain on 5 July (“pluvia, pluvia”). The observer at Schaffhausen also noted strong thunderstorms on 4 July (“trübe, starkes Gewitter, Regen”) and rain on 5 July (“fast beständig starker Regen”); the notes from Marschlins concerning early July (with no clear date) indicate terrible weather with many thunderstorms (“furchtbare Witterung mit viel Gewitter”), Vevey noted thunderstorms with hail and rain (“Gewitter mit Hagel/Regen”), and Bern had rain on 4 and 5 July, with thunderstorms.
Figure 7Excerpts of data sheets from Einsiedeln, Schaffhausen, and Aarau for early July 1817 (Klosterarchiv Einsiedeln: KAE.A.39/6; Swiss Federal Archives: E3180-01#2005/90#201*; State Archives Aargau: NL.A-0197).
All sites indicate a drop in pressure and also temperature. The wind was mainly from the west or south-west. Existing weather type classifications indicate that 4 and 5 July were of the “Low Pressure” type (in Geneva; Auchmann et al., 2012) or “West Cyclonic” (in CAP7; Schwander et al., 2017).
All this additional information hints at the passage of a synoptic-scale system (with antecedent rain and arguably saturated soils), which was accompanied by large thunderstorm activity (including hail) due to embedded convection. This fits very well with several of the weather patterns identified to lead to heavy precipitation events (Stucki et al., 2012). From this evidence we can conclude that it is not unlikely that a heavy precipitation event affected much of the Swiss pre-alpine region and thus could have acted as a trigger for the 1817 flooding. The examples demonstrate the usefulness of the photographed sheets, which provide information that can then be combined with information from historical databases such as EURO-CLIMHIST.
The climate of the late 18th and 19th centuries includes specific periods that are of strong interest to present-day climate science. Studying these events requires instrumental data; however, Swiss measurements before 1864 have never been systematically explored. The earliest Swiss measurements go back to Enlightenment scientists. The observers belonged to the liberal elite; some were members of the clergy, and they were typically well embedded in a European network of scientists. Two Swiss stations were part of the Palatina network. From the mid-18th century onwards and throughout the first half of the 19th century, numerous regional meteorological networks were founded, but they all remained transitory. Only with support from the Swiss Federal State could a national network finally be realised (on the importance of such context knowledge for science and applications, see Brönnimann and Wintzer, 2019).
In our study we have compiled information on more than 300 station records from Switzerland prior to 1864. The inventory is added to the global registry of the Copernicus Data Rescue Services (Brönnimann et al., 2018b), and the images are published at the open-access repository Zenodo (https://doi.org/10.5281/zenodo.3066836). Two examples illustrate the usefulness not only of the digitised data, but also of the images provided, for reconstructing daily weather as far back as the 18th century.
Part of the data (temperature, pressure, and precipitation measurements) will be digitised and made available publicly. They can be used for various applications, including data assimilation for producing dynamical reanalyses. The example of Switzerland also suggests that the amount of European early instrumental data might have been underestimated up to now, probably because the focus of climatology was mostly on long series. In fact, focusing on pressure measurements for the period 1815–1817, Brugnara et al. (2015) compiled and digitised more than 50 pressure series from Europe and North America and located many more. This was sufficient for a dynamical reanalysis (Brohan et al., 2016). Taken together, this suggests that at a European scale, a 250-year daily weather reconstruction should be possible. However, this requires further data rescue efforts, such as those coordinated in the Atmospheric Circulation Reconstructions over the Earth (ACRE) initiative (Allan et al., 2011).
Photographed meteorological series and metadata are published at the open-access repository Zenodo (https://doi.org/10.5281/zenodo.3066836; Pfister, 2019) under a Creative Commons BY-NC-ND licence. The images are organised by station name alphabetically and can be found via the identification number listed in the inventory published as the Supplement to this paper.
The supplement related to this article is available online at: https://doi.org/10.5194/cp-15-1345-2019-supplement.
LP, SB, and LV organised the archive survey. LP, LMu, LV, and LMe photographed and inventoried the data. FH conducted the research on meteorological measurement history together with FI, CR, and SB. YB, LV, and LP organised the digitisation of the measurements. SB, CR, and FH analysed the case studies with contributions from MS. Figures and tables were provided by SB, LP, and YB.
The authors declare that they have no conflict of interest.
This work has been supported by the Swiss National Science Foundation projects CHIMES (169676) and RE-USE (162668) and by the European Union (H2020; ERC grant number 787574 PALAEO-RA). We thank all students who helped in digitising the historical data.
This research has been supported by the Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung (grant nos. 169676 and 162668) and the European Research Council (PALAEO-RA (grant no. 787574)).
This paper was edited by Marit-Solveig Seidenkrantz and reviewed by Alba Gilabert Gallart and Alexander Sterin.
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