Abstract

Abstract. The eruption of Mount Tambora (Indonesia) in April 1815 is the largest documented volcanic eruption in history. It is associated with a large global cooling during the following year, felt particularly in parts of Europe and North America, where the year 1816 became known as the "year without a summer". This paper describes an effort made to collect surface meteorological observations from the early instrumental period, with a focus on the years of and immediately following the eruption (1815–1817). Although the collection aimed in particular at pressure observations, correspondent temperature observations were also recovered. Some of the series had already been described in the literature, but a large part of the data, recently digitised from original weather diaries and contemporary magazines and newspapers, is presented here for the first time. The collection puts together more than 50 sub-daily series from land observatories in Europe and North America and from ships in the tropics. The pressure observations have been corrected for temperature and gravity and reduced to mean sea level. Moreover, an additional statistical correction was applied to take into account common error sources in mercury barometers. To assess the reliability of the corrected data set, the variance in the pressure observations is compared with modern climatologies, and single observations are used for synoptic analyses of three case studies in Europe. All raw observations will be made available to the scientific community in the International Surface Pressure Databank.

Highlights

  • The measurement of atmospheric pressure has a long history, which begins with the famous experiment of Evangelista Torricelli in 1643

  • These projects marked an important development from earlier manual efforts, which sought to use historic barometric pressure observations to analyse changes in the atmospheric circulation but which were limited by an inability to automate the calculations (Cornes, 2014)

  • The latter was estimated in Moberg et al (2002) as negligible; it depends on the individual instrument

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Summary

Introduction

The measurement of atmospheric pressure has a long history, which begins with the famous experiment of Evangelista Torricelli in 1643. Between the 1990s and the 2000s, three European Unionfunded projects, ADVICE, IMPROVE and EMULATE (Jones et al, 1999; Camuffo and Jones, 2002; Ansell et al, 2006), triggered a large effort to digitise historical observations of temperature and pressure, those of long and continuous series, some longer than 250 years, which were in some cases corrected and homogenised. These projects marked an important development from earlier manual efforts, which sought to use historic barometric pressure observations to analyse changes in the atmospheric circulation but which were limited by an inability to automate the calculations (Cornes, 2014).

Data set description
Pressure and temperature measurement in the early 19th century
Cistern level correction for fixed-cistern barometers
Capillarity and drifts
Data processing
Unit conversion
Observation times
Conversion to pressure units and correction for local gravity
Reduction to mean sea level
Quality control
Interpolation on regular time steps
The post-Tambora period in monthly data sets
Storminess
Statistical correction
Summer 1816
April 1817
John Davy’s logbook
Findings
Conclusions
Full Text
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