The Importance of Long Climate Records (Second Edition)

A special issue of Climate (ISSN 2225-1154).

Deadline for manuscript submissions: 30 November 2025 | Viewed by 1274

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Guest Editor
National Research Council of Italy Institute of Atmospheric Sciences and Climate, Padua, Italy
Interests: climate change; indoor and outdoor microclimate; cultural heritage
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Institute of Polar Sciences (ISP) of the National Research Council (CNR) of Italy, c/o Campus Ca' Foscari, University of Venice, Via Torino 155, 30172 Venezia Mestre, VE, Italy
Interests: atmospheric physics; climatology and microclimatology; climate change; recovery and correction of meteorological series; polar sciences; radiation variability in the Arctic, Antarctic and remote areas

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Guest Editor
Institute of Atmospheric Sciences and Climate (ISAC) of the National Research Council (CNR) of Italy, Corso Stati Uniti 4, 35127 Padova, Italy
Interests: atmospheric physics; climatology; historic climatology; climate change; microclimate for conservation of cultural heritage

Special Issue Information

Dear Colleagues,

It is pertinent to celebrate past weather records, as they are vital in helping us identify aspects of climate change. The earliest temperature records and international network of meteorological observations, the Rete Medicea, started in 1654, founded by Ferdinand II de’ Medici, the Grand-Duke of Tuscany. Other international networks were organized by the Royal Society, London, in 1723, the Societé Royale de Médecine, Paris, in 1778, and the Societas Meteorologica Palatina, Mannheim, in 1781. Long records help us test hypotheses concerning climate change, where the pattern of change is slow and subtle, as well as new hypotheses when the beginning of a certain set of weather readings is unknown. They help us calibrate proxy series and transform and express them in normal units of temperature, precipitation, or other weather variables, thus extending our knowledge back in time, up until the pre-instrumental period. Early instrumental data are fundamental in reducing uncertainties and better knowing trends, accelerations, and both past and present changes in the climate, including the transition from the Little Ice Age to the pre-industrial situation and present-day global warming. Then, they can also be used to verify climate models, determine risk from extreme events, and improve future climate projections.

However, in the early instrumental period, records were scarce and taken using non-standard instruments and protocols. Methods, observing times, and exposures were different, and, in most cases, metadata are missing. Some international meteorological networks helped researchers adopt uniform practices and instruments. A turning point was reached in 1873, when the International Meteorological Committee was established to coordinate observing methods and protocols, substituted in 1950 by the World Meteorological Organization. The first challenge facing our field is to find and rescue data and metadata in a process whereby original records are catalogued and imaged. Data rescue includes copying, digitizing, archiving, and making early records usable, in cases where the originals were either handwritten, printed, or in graphical form. The next challenge is to recover them by deciphering, interpreting, and transforming early instrumental readings and their metadata to obtain high-quality datasets in modern units. After this process, an early series is ready for analysis to investigate the climate or conduct other studies.

This Special Issue will provide examples of climate change identification across a wide spectrum of weather observations, from temperature, precipitation, and sunshine to atmospheric pressure, wind, snow and ice, visibility, and fog. It will also encourage the discussion of metadata to show that each weather station needs to have strong accompanying records if they are to prove useful in the years and decades to come. In cases where significant changes have occurred and, typically, for all data recorded before the standardization which started with the foundation of the International Meteorological Committee in 1873, homogenization techniques must be employed. Examples of data rescue and recovery will hopefully be included in this Special Issue, as well as the following topics:

  • climate change;
  • metadata;
  • early instruments and screens;
  • early observation protocols;
  • transformation from early units and time references (e.g., day starting from twilight or from the apparent solar time (AST) to the coordinated universal time (UTC));
  • data homogenization;
  • proxy and instrumental data calibration, rescue, and recovering.

Prof. Dr. Dario Camuffo
Dr. Francesca Becherini
Dr. Antonio della Valle
Guest Editors

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Keywords

  • long weather records
  • climate change
  • metadata
  • homogenization
  • case studies from stations with century-scale records
  • recovery of early instrumental observations (e.g., 17th century, 18th century, and first half of the 19th century)
  • early instruments, protocols, calibrations, and units
  • instrumental and proxy data rescue and recovery
  • calibration of proxy and instrumental data

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23 pages, 11213 KiB  
Article
Three-Century Climatology of Cold and Warm Spells and Snowfall Events in Padua, Italy (1725–2024)
by Claudio Stefanini, Francesca Becherini, Antonio della Valle and Dario Camuffo
Climate 2025, 13(4), 70; https://doi.org/10.3390/cli13040070 - 30 Mar 2025
Viewed by 674
Abstract
Regular meteorological observations in Padua started in 1725 and have continued unbroken up to the present, making the series one of the longest in the world. Daily mean temperatures and precipitation amounts have recently been homogenized for the entire 1725–2024 period, making it [...] Read more.
Regular meteorological observations in Padua started in 1725 and have continued unbroken up to the present, making the series one of the longest in the world. Daily mean temperatures and precipitation amounts have recently been homogenized for the entire 1725–2024 period, making it possible to add new measurements without further work. Starting from the temperature series, the trends of cold and warm spells are investigated in this paper. The ongoing warming that started in the 1970s is extensively analyzed on the basis of the variability of the mean values and a magnitude index that captures both the duration and intensity of a spell and by investigating the frequency of extreme events by means of Intensity–Duration–Frequency curves. The periods with the greatest deviation from the climatological average are analyzed in detail: February 1740 and April 1755, the months with the largest negative and positive temperature anomalies, respectively, in the 300-year-long series. Moreover, the analysis of snow occurrences extracted from the original logs, together with the pressure observations from the long series of London and Uppsala, made it possible to evaluate the most typical synoptic situations leading to snow events in Padua for the whole period. Full article
(This article belongs to the Special Issue The Importance of Long Climate Records (Second Edition))
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