Articles | Volume 19, issue 7
https://doi.org/10.5194/cp-19-1397-2023
© Author(s) 2023. 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-19-1397-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
18 Jul 2023
Research article |
| 18 Jul 2023
| 18 Jul 2023
Earliest meteorological readings in San Fernando (Cádiz, Spain, 1799–1813)
Nieves Bravo-Paredes
Departamento de Física, Universidad de Extremadura, Badajoz,
Spain
María Cruz Gallego
Departamento de Física, Universidad de Extremadura, Badajoz,
Spain
Ricardo M. Trigo
Instituto Dom Luiz (IDL), Faculdade de Ciências da Universidade de Lisboa, 1749-016 Lisbon, Portugal
Departamento de Meteorologia, Universidade Federal do Rio de Janeiro, Rio de Janeiro, 21941-919, Brazil
Departamento de Física, Universidad de Extremadura, Badajoz,
Spain
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Francisco Javier Acero, Manuel Antón, Alejandro Jesús Pérez Aparicio, Nieves Bravo-Paredes, Víctor Manuel Sánchez Carrasco, María Cruz Gallego, José Agustín García, Marcelino Núñez, Irene Tovar, Javier Vaquero-Martínez, and José Manuel Vaquero
EGUsphere, https://doi.org/10.5194/egusphere-2023-2522, https://doi.org/10.5194/egusphere-2023-2522, 2023
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The month of June 1925 was detected as exceptional in the SW interior of Iberia due to the large number of thunderstorms and the significant impacts that caused, with serious losses in human lives and material resources. We analyzed this event from different, complementary perspectives: the reconstruction of the history of the events from newspapers; the study of monthly meteorological variables of the longest series available in Iberia; and the analysis of the meteorological synoptic situation.
Maite deCastro, Jose González-Cao, Nicolás deCastro, Juan J. Taboada, Jose M. Vaquero, and Moncho Gómez-Gesteira
Clim. Past Discuss., https://doi.org/10.5194/cp-2024-49, https://doi.org/10.5194/cp-2024-49, 2024
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Torrential rains in the Eastern Atlantic during 1768–1769 caused the worst agricultural crisis in Galicia and Northern Portugal. Using the EKF400v2 paleo-reanalysis dataset, it was found that the rainfall anomaly was positive in 11 out of 12 months. June 1768 saw the highest positive rain anomaly of the century, and September 1768 the second-highest. The atmospheric synoptic patterns show negative anomalies in sea level pressure and 500 hPa. These patterns induce surface low-pressure systems.
Tiago M. Ferreira, Ricardo M. Trigo, Tomás H. Gaspar, Joaquim G. Pinto, and Alexandre M. Ramos
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-130, https://doi.org/10.5194/nhess-2024-130, 2024
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Here we investigate the synoptic evolution associated with the occurrence of an atmospheric river leading to a 24 h record-breaking extreme precipitation event (120.3 mm) in Lisbon, Portugal, on 13 December 2022. The synoptic background allowed the formation, on 10 December, of an atmospheric river associated with a deep extratropical cyclone and with a high moisture content and an inflow of moisture, due to the warm conveyor belt, throughout its life cycle. The system made landfall on day 12.
Diego Fernández-Nóvoa, Alexandre M. Ramos, José González-Cao, Orlando García-Feal, Cristina Catita, Moncho Gómez-Gesteira, and Ricardo M. Trigo
Nat. Hazards Earth Syst. Sci., 24, 609–630, https://doi.org/10.5194/nhess-24-609-2024, https://doi.org/10.5194/nhess-24-609-2024, 2024
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The present study focuses on an in-depth analysis of floods in the lower section of the Tagus River from a hydrodynamic perspective by means of the Iber+ numerical model and on the development of dam operating strategies to mitigate flood episodes using the exceptional floods of February 1979 as a benchmark. The results corroborate the model's capability to evaluate floods in the study area and confirm the effectiveness of the proposed strategies to reduce flood impact in the lower Tagus valley.
Francisco Javier Acero, Manuel Antón, Alejandro Jesús Pérez Aparicio, Nieves Bravo-Paredes, Víctor Manuel Sánchez Carrasco, María Cruz Gallego, José Agustín García, Marcelino Núñez, Irene Tovar, Javier Vaquero-Martínez, and José Manuel Vaquero
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The month of June 1925 was detected as exceptional in the SW interior of Iberia due to the large number of thunderstorms and the significant impacts that caused, with serious losses in human lives and material resources. We analyzed this event from different, complementary perspectives: the reconstruction of the history of the events from newspapers; the study of monthly meteorological variables of the longest series available in Iberia; and the analysis of the meteorological synoptic situation.
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Animesh K. Gain, Yves Bühler, Pascal Haegeli, Daniela Molinari, Mario Parise, David J. Peres, Joaquim G. Pinto, Kai Schröter, Ricardo M. Trigo, María Carmen Llasat, and Heidi Kreibich
Nat. Hazards Earth Syst. Sci., 22, 985–993, https://doi.org/10.5194/nhess-22-985-2022, https://doi.org/10.5194/nhess-22-985-2022, 2022
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To mark the 20th anniversary of Natural Hazards and Earth System Sciences (NHESS), an interdisciplinary and international journal dedicated to the public discussion and open-access publication of high-quality studies and original research on natural hazards and their consequences, we highlight 11 key publications covering major subject areas of NHESS that stood out within the past 20 years.
Gerard van der Schrier, Richard P. Allan, Albert Ossó, Pedro M. Sousa, Hans Van de Vyver, Bert Van Schaeybroeck, Roberto Coscarelli, Angela A. Pasqua, Olga Petrucci, Mary Curley, Mirosław Mietus, Janusz Filipiak, Petr Štěpánek, Pavel Zahradníček, Rudolf Brázdil, Ladislava Řezníčková, Else J. M. van den Besselaar, Ricardo Trigo, and Enric Aguilar
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Margarida L. R. Liberato, Irene Montero, Célia Gouveia, Ana Russo, Alexandre M. Ramos, and Ricardo M. Trigo
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Alexandre M. Ramos, Pedro M. Sousa, Emanuel Dutra, and Ricardo M. Trigo
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Sílvia A. Nunes, Carlos C. DaCamara, Kamil F. Turkman, Teresa J. Calado, Ricardo M. Trigo, and Maria A. A. Turkman
Nat. Hazards Earth Syst. Sci., 19, 1459–1470, https://doi.org/10.5194/nhess-19-1459-2019, https://doi.org/10.5194/nhess-19-1459-2019, 2019
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Portugal is recurrently affected by large wildfire events. We present a statistical model to estimate the probability that the summer burned area exceeds a given threshold. The model allows making outlooks of wildfire potential with up to 1 month in advance of the fire season. When applied to the 39-year period 1980-2018, only 1 severe (one weak) year is not anticipated as potentially severe (weak). The model will assist the fire community when planning prevention and combating fire events.
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Hist. Geo Space. Sci., 9, 133–139, https://doi.org/10.5194/hgss-9-133-2018, https://doi.org/10.5194/hgss-9-133-2018, 2018
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An analysis is made of the records made by Spanish observers of a notable aurora on 18 January 1770 in order to study the characteristics of this event. The records indicate that the phenomenon was observed in both continental and insular territories of Spain. In general, observers described the aurora as red in colour, from sunset to midnight. Calculations of the geomagnetic latitudes of the observation locations indicate this aurora was observed over a wide range of abnormally low latitudes.
Hisashi Hayakawa, José M. Vaquero, and Yusuke Ebihara
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Patrícia Páscoa, Célia M. Gouveia, Ana C. Russo, Roxana Bojariu, Sergio M. Vicente-Serrano, and Ricardo M. Trigo
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-264, https://doi.org/10.5194/hess-2018-264, 2018
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Julien Ruffault, Thomas Curt, Nicolas K. Martin-StPaul, Vincent Moron, and Ricardo M. Trigo
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Extreme wildfires events (EWE) have been recorded during the past year in the Mediterranean. By analyzing the climatic conditions associated with the French 2003 and 2016 fires seasons, we found that EWE were associated to two distinct climatic events whose frequencies are both expected to increase with global changes: hot droughts and long droughts. These results suggest that EWE are likely to become more common in the future and will certainly challenge fire management.
Miguel M. Pinto, Carlos C. DaCamara, Isabel F. Trigo, Ricardo M. Trigo, and K. Feridun Turkman
Nat. Hazards Earth Syst. Sci., 18, 515–529, https://doi.org/10.5194/nhess-18-515-2018, https://doi.org/10.5194/nhess-18-515-2018, 2018
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extremeclass of fire danger. The procedure is expected to assist in wildfire management and in decision making on prescribed burning.
Jorge Eiras-Barca, Alexandre M. Ramos, Joaquim G. Pinto, Ricardo M. Trigo, Margarida L. R. Liberato, and Gonzalo Miguez-Macho
Earth Syst. Dynam., 9, 91–102, https://doi.org/10.5194/esd-9-91-2018, https://doi.org/10.5194/esd-9-91-2018, 2018
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José M. Vaquero
Hist. Geo Space. Sci., 8, 53–56, https://doi.org/10.5194/hgss-8-53-2017, https://doi.org/10.5194/hgss-8-53-2017, 2017
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An analysis is given of the account of a
globe of fireobserved in Zafra (Spain) in the middle of the 16th century. During a strong storm, Conde Don Pedro observed what he described as a
globe of firethat was directed against the city and abruptly changed course. He attributed the change in course to a miracle. He described neither any damage nor sound.
Alexandre M. Ramos, Raquel Nieto, Ricardo Tomé, Luis Gimeno, Ricardo M. Trigo, Margarida L. R. Liberato, and David A. Lavers
Earth Syst. Dynam., 7, 371–384, https://doi.org/10.5194/esd-7-371-2016, https://doi.org/10.5194/esd-7-371-2016, 2016
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S. Pereira, A. M. Ramos, J. L. Zêzere, R. M. Trigo, and J. M. Vaquero
Nat. Hazards Earth Syst. Sci., 16, 371–390, https://doi.org/10.5194/nhess-16-371-2016, https://doi.org/10.5194/nhess-16-371-2016, 2016
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This work explores the meteorological conditions of the hydro-geomorphologic event of December 1909 that triggered the highest floods in more than 100 years at the Douro river's mouth and caused important social impacts over the Portuguese and Spanish territories.
The study of this extreme event contributes to a comprehensive and systematic synoptic evaluation of the second most deadly hydro-geomorphologic disaster event occurred in Portugal since 1865.
L. Gimeno, M. Vázquez, R. Nieto, and R. M. Trigo
Earth Syst. Dynam., 6, 583–589, https://doi.org/10.5194/esd-6-583-2015, https://doi.org/10.5194/esd-6-583-2015, 2015
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There appears to be a connection between two climate change indicators: an increase in evaporation over source regions and Arctic ice melting.
A. Bastos, C. M. Gouveia, R. M. Trigo, and S. W. Running
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S. Jerez, P. Jimenez-Guerrero, J. P. Montávez, and R. M. Trigo
Atmos. Chem. Phys., 13, 11195–11207, https://doi.org/10.5194/acp-13-11195-2013, https://doi.org/10.5194/acp-13-11195-2013, 2013
M. L. R. Liberato, J. G. Pinto, R. M. Trigo, P. Ludwig, P. Ordóñez, D. Yuen, and I. F. Trigo
Nat. Hazards Earth Syst. Sci., 13, 2239–2251, https://doi.org/10.5194/nhess-13-2239-2013, https://doi.org/10.5194/nhess-13-2239-2013, 2013
Related subject area
Subject: Atmospheric Dynamics | Archive: Historical Records | Timescale: Instrumental Period
Air temperature changes in SW Greenland in the second half of the 18th century
Early 20th century Southern Hemisphere cooling
Precipitation reconstructions for Paris based on the observations by Louis Morin, 1665–1713 CE
The weather diaries of the Kirch family: Leipzig, Guben, and Berlin (1677–1774)
Quantifying the contribution of forcing and three prominent modes of variability to historical climate
A 258-year-long data set of temperature and precipitation fields for Switzerland since 1763
Statistical reconstruction of daily temperature and sea level pressure in Europe for the severe winter 1788/89
Insights from 20 years of temperature parallel measurements in Mauritius around the turn of the 20th century
Unlocking weather observations from the Societas Meteorologica Palatina (1781–1792)
The 1921 European drought: impacts, reconstruction and drivers
The importance of input data quality and quantity in climate field reconstructions – results from the assimilation of various tree-ring collections
Reconstruction of the track and a simulation of the storm surge associated with the calamitous typhoon affecting the Pearl River Estuary in September 1874
Early instrumental meteorological measurements in Switzerland
The "dirty weather" diaries of Reverend Richard Davis: insights about early colonial-era meteorology and climate variability for northern New Zealand, 1839–1851
A collection of sub-daily pressure and temperature observations for the early instrumental period with a focus on the "year without a summer" 1816
East Asian Monsoon controls on the inter-annual variability in precipitation isotope ratio in Japan
Investigating uncertainties in global gridded datasets of climate extremes
HadISDH land surface multi-variable humidity and temperature record for climate monitoring
Pairwise homogeneity assessment of HadISD
Ensemble meteorological reconstruction using circulation analogues of 1781–1785
HadISDH: an updateable land surface specific humidity product for climate monitoring
Reconstruction of high resolution atmospheric fields for Northern Europe using analog-upscaling
Early Portuguese meteorological measurements (18th century)
Extreme climate, not extreme weather: the summer of 1816 in Geneva, Switzerland
Inferences on weather extremes and weather-related disasters: a review of statistical methods
Benchmarking homogenization algorithms for monthly data
The construction of a Central Netherlands temperature
Early ship-based upper-air data and comparison with the Twentieth Century Reanalysis
The influence of the circulation on surface temperature and precipitation patterns over Europe
Rajmund Przybylak, Garima Singh, Przemysław Wyszyński, Andrzej Araźny, and Konrad Chmist
Clim. Past, 20, 1451–1470, https://doi.org/10.5194/cp-20-1451-2024, https://doi.org/10.5194/cp-20-1451-2024, 2024
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The purpose of this study is to recognise the nature of the climate in historical times (second half of 18th century) in Greenland. Such knowledge is important for validating Greenland temperature reconstructions based on both modelling works and various proxies. The two unique series of old meteorological observations from Greenland we used indicated that temperature in the study period was comparable to that of the early 20th-century Arctic warming but lower than that of the present day.
Stefan Brönnimann, Yuri Brugnara, and Clive Wilkinson
Clim. Past, 20, 757–767, https://doi.org/10.5194/cp-20-757-2024, https://doi.org/10.5194/cp-20-757-2024, 2024
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The early 20th century warming – the first phase of global warming in the 20th century – started from a peculiar cold state around 1910. We digitised additional ship logbooks for these years to study this specific climate state and found that it is real and likely an overlap of several climatic anomalies, including oceanic variability (La Niña) and volcanic eruptions.
Thomas Pliemon, Ulrich Foelsche, Christian Rohr, and Christian Pfister
Clim. Past, 19, 2237–2256, https://doi.org/10.5194/cp-19-2237-2023, https://doi.org/10.5194/cp-19-2237-2023, 2023
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Louis Morin consistently recorded precipitation intensity and duration between 1665 and 1713. We use these records to reconstruct precipitation totals. This reconstruction is validated by several methods and then presented using precipitation indexes. What is exceptional about this dataset is the availability of a sub-daily resolution and the low number of missing data points over the entire observation period.
Stefan Brönnimann and Yuri Brugnara
Clim. Past, 19, 1435–1445, https://doi.org/10.5194/cp-19-1435-2023, https://doi.org/10.5194/cp-19-1435-2023, 2023
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We present the weather diaries of the Kirch family from 1677–1774 containing weather observations made in Leipzig and Guben and, from 1701 onward, instrumental observations made in Berlin. We publish the imaged diaries (10 445 images) and the digitized measurements (from 1720 onward). This is one of the oldest and longest meteorological records from Germany. The digitized pressure data show good agreement with neighbouring stations, highlighting their potential for weather reconstruction.
Andrew P. Schurer, Gabriele C. Hegerl, Hugues Goosse, Massimo A. Bollasina, Matthew H. England, Michael J. Mineter, Doug M. Smith, and Simon F. B. Tett
Clim. Past, 19, 943–957, https://doi.org/10.5194/cp-19-943-2023, https://doi.org/10.5194/cp-19-943-2023, 2023
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We adopt an existing data assimilation technique to constrain a model simulation to follow three important modes of variability, the North Atlantic Oscillation, El Niño–Southern Oscillation and the Southern Annular Mode. How it compares to the observed climate is evaluated, with improvements over simulations without data assimilation found over many regions, particularly the tropics, the North Atlantic and Europe, and discrepancies with global cooling following volcanic eruptions are reconciled.
Noemi Imfeld, Lucas Pfister, Yuri Brugnara, and Stefan Brönnimann
Clim. Past, 19, 703–729, https://doi.org/10.5194/cp-19-703-2023, https://doi.org/10.5194/cp-19-703-2023, 2023
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Climate reconstructions give insights into monthly and seasonal climate variability of the past few hundred years. However, to understand past extreme weather events and to relate them to impacts, for example to periods of extreme floods, reconstructions on a daily timescale are needed. Here, we present a reconstruction of 258 years of high-resolution daily temperature and precipitation fields for Switzerland covering the period 1763 to 2020, which is based on instrumental measurements.
Duncan Pappert, Mariano Barriendos, Yuri Brugnara, Noemi Imfeld, Sylvie Jourdain, Rajmund Przybylak, Christian Rohr, and Stefan Brönnimann
Clim. Past, 18, 2545–2565, https://doi.org/10.5194/cp-18-2545-2022, https://doi.org/10.5194/cp-18-2545-2022, 2022
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We present daily temperature and sea level pressure fields for Europe for the severe winter 1788/1789 based on historical meteorological measurements and an analogue reconstruction approach. The resulting reconstruction skilfully reproduces temperature and pressure variations over central and western Europe. We find intense blocking systems over northern Europe and several abrupt, strong cold air outbreaks, demonstrating that quantitative weather reconstruction of past extremes is possible.
Samuel O. Awe, Martin Mahony, Edley Michaud, Conor Murphy, Simon J. Noone, Victor K. C. Venema, Thomas G. Thorne, and Peter W. Thorne
Clim. Past, 18, 793–820, https://doi.org/10.5194/cp-18-793-2022, https://doi.org/10.5194/cp-18-793-2022, 2022
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We unearth and analyse 2 decades of highly valuable measurements made on Mauritius at the Royal Alfred Observatory, where several distinct thermometer combinations were in use and compared, at the turn of the 20th century. This series provides unique insights into biases in early instrumental temperature records. Differences are substantial and for some instruments exhibit strong seasonality. This reinforces the critical importance of understanding early instrumental series biases.
Duncan Pappert, Yuri Brugnara, Sylvie Jourdain, Aleksandra Pospieszyńska, Rajmund Przybylak, Christian Rohr, and Stefan Brönnimann
Clim. Past, 17, 2361–2379, https://doi.org/10.5194/cp-17-2361-2021, https://doi.org/10.5194/cp-17-2361-2021, 2021
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This paper presents temperature and pressure measurements from the 37 stations of the late 18th century network of the Societas Meteorologica Palatina, in addition to providing an inventory of the available observations, most of which have been digitised. The quality of the recovered series is relatively good, as demonstrated by two case studies. Early instrumental data such as these will help to explore past climate and weather extremes in Europe in greater detail.
Gerard van der Schrier, Richard P. Allan, Albert Ossó, Pedro M. Sousa, Hans Van de Vyver, Bert Van Schaeybroeck, Roberto Coscarelli, Angela A. Pasqua, Olga Petrucci, Mary Curley, Mirosław Mietus, Janusz Filipiak, Petr Štěpánek, Pavel Zahradníček, Rudolf Brázdil, Ladislava Řezníčková, Else J. M. van den Besselaar, Ricardo Trigo, and Enric Aguilar
Clim. Past, 17, 2201–2221, https://doi.org/10.5194/cp-17-2201-2021, https://doi.org/10.5194/cp-17-2201-2021, 2021
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The 1921 drought was the most severe drought to hit Europe since the start of the 20th century. Here the climatological description of the drought is coupled to an overview of its impacts, sourced from newspapers, and an analysis of its drivers. The area from Ireland to the Ukraine was affected but hardest hit was the triangle between Brussels, Paris and Lyon. The drought impacts lingered on until well into autumn and winter, affecting water supply and agriculture and livestock farming.
Jörg Franke, Veronika Valler, Stefan Brönnimann, Raphael Neukom, and Fernando Jaume-Santero
Clim. Past, 16, 1061–1074, https://doi.org/10.5194/cp-16-1061-2020, https://doi.org/10.5194/cp-16-1061-2020, 2020
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This study explores the influence of the input data choice on spatial climate reconstructions. We compare three tree-ring-based data sets which range from small sample size, small spatial coverage and strict screening for temperature sensitivity to the opposite. We achieve the best spatial reconstruction quality by combining all available input data but rejecting records with little and uncertain climatic information and considering moisture availability as an additional growth limitation.
Hing Yim Mok, Wing Hong Lui, Dick Shum Lau, and Wang Chun Woo
Clim. Past, 16, 51–64, https://doi.org/10.5194/cp-16-51-2020, https://doi.org/10.5194/cp-16-51-2020, 2020
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Using available information from historical documents, the maximum storm surge and storm tide at Hong Kong during the passage of a typhoon in 1874 were determined by reconstructing the possible typhoon track and found to be higher than all existing records since the 1883 establishment of the Hong Kong Observatory. This reveals that a more detailed frequency analysis of extreme sea levels taking the 1874 typhoon into account is essential for realistic storm surge risk assessments in Hong Kong.
Lucas Pfister, Franziska Hupfer, Yuri Brugnara, Lukas Munz, Leonie Villiger, Lukas Meyer, Mikhaël Schwander, Francesco Alessandro Isotta, Christian Rohr, and Stefan Brönnimann
Clim. Past, 15, 1345–1361, https://doi.org/10.5194/cp-15-1345-2019, https://doi.org/10.5194/cp-15-1345-2019, 2019
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The 18th and early 19th centuries saw pronounced climatic variations with impacts on the environment and society. Although instrumental meteorological data for that period exist, only a small fraction has been the subject of research. This study provides an overview of early instrumental meteorological records in Switzerland resulting from an archive survey and demonstrates the great potential of such data. It is accompanied by the online publication of the imaged data series and metadata.
Andrew M. Lorrey and Petra R. Chappell
Clim. Past, 12, 553–573, https://doi.org/10.5194/cp-12-553-2016, https://doi.org/10.5194/cp-12-553-2016, 2016
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The meteorological diary of Reverend Richard Davis (1839–1844; 1848–1851) is the earliest continuous daily instrumental weather observation record for New Zealand. It pre-dates James Hector's meteorological network by more than 20 years, and it contains evidence that temperatures for May–August were on average colder than present day in Northland. Some weather extremes Davis also witnessed may have been more frequent in the mid-1800s relative to the modern era, including frost, ice and snow.
Y. Brugnara, R. Auchmann, S. Brönnimann, R. J. Allan, I. Auer, M. Barriendos, H. Bergström, J. Bhend, R. Brázdil, G. P. Compo, R. C. Cornes, F. Dominguez-Castro, A. F. V. van Engelen, J. Filipiak, J. Holopainen, S. Jourdain, M. Kunz, J. Luterbacher, M. Maugeri, L. Mercalli, A. Moberg, C. J. Mock, G. Pichard, L. Řezníčková, G. van der Schrier, V. Slonosky, Z. Ustrnul, M. A. Valente, A. Wypych, and X. Yin
Clim. Past, 11, 1027–1047, https://doi.org/10.5194/cp-11-1027-2015, https://doi.org/10.5194/cp-11-1027-2015, 2015
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A data set of instrumental pressure and temperature observations for the early instrumental period (before ca. 1850) is described. This is the result of a digitisation effort involving the period immediately after the eruption of Mount Tambora in 1815, combined with the collection of already available sub-daily time series. The highest data availability is therefore for the years 1815 to 1817. An analysis of pressure variability and of case studies in Europe is performed for that period.
N. Kurita, Y. Fujiyoshi, T. Nakayama, Y. Matsumi, and H. Kitagawa
Clim. Past, 11, 339–353, https://doi.org/10.5194/cp-11-339-2015, https://doi.org/10.5194/cp-11-339-2015, 2015
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This study demonstrates that the intensity of the East Asian summer and winter monsoon is the primary driver of variations of summer and winter precipitation isotopes in central Japan. Japan lies in the northeast limits of the East Asian monsoon region. Understanding the past monsoon changes in Japan is important for determining whether the isotopic variability recorded in Chinese stalagmite reflects the East Asian summer monsoon intensity or rainfall variability in the Indian summer monsoon.
R. J. H. Dunn, M. G. Donat, and L. V. Alexander
Clim. Past, 10, 2171–2199, https://doi.org/10.5194/cp-10-2171-2014, https://doi.org/10.5194/cp-10-2171-2014, 2014
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Observational data sets contain uncertainties, e.g. from the instrument accuracy, as well as from the fact that usually only a single method is used in processing. We have performed an assessment of the size of the uncertainties associated with choices in the method used. The largest effects come from changes which affect the station network or the gridding method used. However, for the temperature indices in places with many stations, these changes have little effect on the long-term behaviour.
K. M. Willett, R. J. H. Dunn, P. W. Thorne, S. Bell, M. de Podesta, D. E. Parker, P. D. Jones, and C. N. Williams Jr.
Clim. Past, 10, 1983–2006, https://doi.org/10.5194/cp-10-1983-2014, https://doi.org/10.5194/cp-10-1983-2014, 2014
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We have developed HadISDH, a new gridded global land monthly mean climate montitoring product for humidity and temperature from 1973 to then end of 2013 (updated annually) based entirely on in situ observations. Uncertainty estimates are provided. Over the period of record significant warming and increases in water vapour have taken place. The specific humidity trends have slowed since a peak in 1998 concurrent with decreasing relative humidity from 2000 onwards.
R. J. H. Dunn, K. M. Willett, C. P. Morice, and D. E. Parker
Clim. Past, 10, 1501–1522, https://doi.org/10.5194/cp-10-1501-2014, https://doi.org/10.5194/cp-10-1501-2014, 2014
P. Yiou, M. Boichu, R. Vautard, M. Vrac, S. Jourdain, E. Garnier, F. Fluteau, and L. Menut
Clim. Past, 10, 797–809, https://doi.org/10.5194/cp-10-797-2014, https://doi.org/10.5194/cp-10-797-2014, 2014
K. M. Willett, C. N. Williams Jr., R. J. H. Dunn, P. W. Thorne, S. Bell, M. de Podesta, P. D. Jones, and D. E. Parker
Clim. Past, 9, 657–677, https://doi.org/10.5194/cp-9-657-2013, https://doi.org/10.5194/cp-9-657-2013, 2013
F. Schenk and E. Zorita
Clim. Past, 8, 1681–1703, https://doi.org/10.5194/cp-8-1681-2012, https://doi.org/10.5194/cp-8-1681-2012, 2012
M. J. Alcoforado, J. M. Vaquero, R. M. Trigo, and J. P. Taborda
Clim. Past, 8, 353–371, https://doi.org/10.5194/cp-8-353-2012, https://doi.org/10.5194/cp-8-353-2012, 2012
R. Auchmann, S. Brönnimann, L. Breda, M. Bühler, R. Spadin, and A. Stickler
Clim. Past, 8, 325–335, https://doi.org/10.5194/cp-8-325-2012, https://doi.org/10.5194/cp-8-325-2012, 2012
H. Visser and A. C. Petersen
Clim. Past, 8, 265–286, https://doi.org/10.5194/cp-8-265-2012, https://doi.org/10.5194/cp-8-265-2012, 2012
V. K. C. Venema, O. Mestre, E. Aguilar, I. Auer, J. A. Guijarro, P. Domonkos, G. Vertacnik, T. Szentimrey, P. Stepanek, P. Zahradnicek, J. Viarre, G. Müller-Westermeier, M. Lakatos, C. N. Williams, M. J. Menne, R. Lindau, D. Rasol, E. Rustemeier, K. Kolokythas, T. Marinova, L. Andresen, F. Acquaotta, S. Fratianni, S. Cheval, M. Klancar, M. Brunetti, C. Gruber, M. Prohom Duran, T. Likso, P. Esteban, and T. Brandsma
Clim. Past, 8, 89–115, https://doi.org/10.5194/cp-8-89-2012, https://doi.org/10.5194/cp-8-89-2012, 2012
G. van der Schrier, A. van Ulden, and G. J. van Oldenborgh
Clim. Past, 7, 527–542, https://doi.org/10.5194/cp-7-527-2011, https://doi.org/10.5194/cp-7-527-2011, 2011
S. Brönnimann, G. P. Compo, R. Spadin, R. Allan, and W. Adam
Clim. Past, 7, 265–276, https://doi.org/10.5194/cp-7-265-2011, https://doi.org/10.5194/cp-7-265-2011, 2011
P. D. Jones and D. H. Lister
Clim. Past, 5, 259–267, https://doi.org/10.5194/cp-5-259-2009, https://doi.org/10.5194/cp-5-259-2009, 2009
Cited articles
Alcoforado, M. J., Vaquero, J. M., Trigo, R. M., and Taborda, J. P.: Early Portuguese meteorological measurements (18th century), Clim. Past, 8, 353–371, https://doi.org/10.5194/cp-8-353-2012, 2012.
Auer, I., Böhm, R., Jurkovic, A., Lipa, W., Orlik, A., Potzmann, R.,
Schöner, W., Ungersböck, M., Matulla, C., Briffa, K., Jones, P.,
Efthymiadis, D., Brunetti, M., Nanni, T., Maugeri, M., Mercalli, L., Mestre,
O., Moisselin, J-M., Begert, M., Müller-Westermeier, G., Kveton, V.,
Bochnicek, O., Stastny, P., Lapin, M., Szalai, S., Szentimrey, T., Cegnar,
T., Dolinar, M., Gajic-Capka, M., Zaninovic, K., Majstorovic, Z., and
Nieplova, E.: HISTALP – historical instrumental climatological surface time
series of the Greater Alpine Region, Int. J. Climatol., 27, 17–46,
https://doi.org/10.1002/joc.1377, 2007.
Barriendos, M., Martín-Vide, J., Peña, J. C., and Rodríguez,
R.: Daily Meteorological Observations in Cádiz – San Fernando. Analysis
of the Documentary Sources and the Instrumental Data Content (1786–1996),
Clim. Change, 53, 151–170, https://doi.org/10.1023/A:1014991430122, 2002.
Bližňák, V., Valente, M. A., and Bethke, J.: Homogenization of
time series from Portugal and its former colonies for the period from the
late 19th to the early 21st century, Int. J. Climatol, 35, 2400–2418,
https://doi.org/10.1002/joc.4151, 2015.
Bravo-Paredes, N., Gallego, M. C., Trigo, R. M., and Vaquero, J. M.: [Data] Earliest meteorological readings in San Fernando (Cádiz, Spain), Zenodo [data set], https://doi.org/10.5281/zenodo.7104289, 2022.
Brönnimann, S., Brugnara, Y., Allan, R. J., Brunet, M., Compo, G. P.,
Crouthamel, R. I., Jones, P. D., Jourdain, S., Luterbacher, J., Siegmund,
P., Valente, M. A., and Wilkinson, C. W.: A roadmap to climate data rescue
services, Geosci. Data J., 5, 28–39, https://doi.org/10.1002/gdj3.56, 2018.
Brönnimann, S., Allan, R., Ashcroft, L., Baer, S., Barriendos, M.,
Brázdil, R., Brugnara, Y., Brunet, M., Brunetti, M., Chimani, B.,
Cornes, R., Domínguez-Castro, F., Founda, D., Gergis, J., Grab, S.,
Hannak, L., García-Herrera, R., Huhtamaa, H., Jacobsen, K. S., Jones,
P., Jourdain, S., Kiss, A., Lin, K. E., Lorrey, A., Lundstad, E.,
Luterbacher, J., Moberg, A., Mauelshagen, F., Maugeri, M., Maughan, N.,
Neukom, R., Nicholson, S., Noone, S., Nordli, Ø., Ólafsdóttir,
K. B., Pearce, P. R., Pfister, L., Pribyl, K., Przybylak, R., Pudmenzky, C.,
Rasol, D., Reichenbach, D., Řezníčková, L., Rodrigo, F. S.,
Rohde, R., Rohr, C., Skrynyk, O., Slonosky, V., Thorne, P., Valente, M. A.,
Vaquero, J. M., Westcottt, N. E., Williamson, F., and Wyszyński, P.:
Unlocking pre-1850 instrumental meteorological records: A global inventory,
B. Am. Meteorol. Soc. 100, ES389–ES413,
https://doi.org/10.1175/BAMS-D-19-0040.1, 2019.
Brugnara, Y., Pfister, L., Villiger, L., Rohr, C., Isotta, F. A., and Brönnimann, S.: Early instrumental meteorological observations in Switzerland: 1708–1873, Earth Syst. Sci. Data, 12, 1179–1190, https://doi.org/10.5194/essd-12-1179-2020, 2020.
Calvo, N., Gallego, D., García-Herrera, R., Gullón, A., Portela, M.
J., Prieto, M. R., and Ribera, P.: El clima de Cádiz en la primera mitad
del silgo XIX según los parte de la Vigía, edited by:
García-Herrera, R., Servicio de Publicaciones de la Fundación
Unicaja, Málaga, Spain, ISBN 978-84-95979-69-8, 2008.
Camuffo, D. and Jones, P.: Improved Understanding of Past Climatic
Variability from Early Daily European Instrumental Sources, in: Improved
Understanding of Past Climatic Variability from Early Daily European
Instrumental Sources, vol. 53, edited by: Camuffo, D. and Jones, P.,
Springer, Dordrecht, 1–4,
https://doi.org/10.1007/978-94-010-0371-1_1, 2002.
Cornes, R. C., Jones, P. D., Briffa, K. R., and Osborn, T. J.: A daily
series of mean sea-level pressure for Paris, 1670–2007, Int. J. Climatol.,
32, 1135–1150, https://doi.org/10.1002/joc.2349, 2012.
Domínguez-Castro, F., Vaquero, J. M., Rodrigo, F. S., Farrona, A. M.
M., Gallego, M. C., García-Herrera, R., Barriendos, M., and
Sanchez-Lorenzo, A.: Early Spanish meteorological records (1780–1850), Int.
J. Climatol., 34, 593–603, https://doi.org/10.1002/joc.3709, 2014.
Domínguez-Castro, F., Vaquero, J. M., Gallego, M. C., Farrona, A. M.
M., Antuña-Marrero, J. C., Cevallos, E. E., García-Herrera, R., de
la Guía, C., Mejía, R. D., Naranjo, J. M., Prieto, M. R., Ramos
Guadalupe, L. E., Seiner, L., Trigo, R. M., and Villacís, M.: Early
meteorological records from Latin- America and the Caribbean during the 18th and 19th centuries, Sci. Data, 4, 1–10,
https://doi.org/10.1038/sdata.2017.169, 2017.
Dunnington, D.: Ggspatial: spatial data framework for ggplot2, R package
version 1.1.1, https://CRAN.R-project.org/package=ggspatial (Last access: 4 July 2023), 2020.
Farrona, A. M. M., Trigo, R. M., Gallego, M. C., and Vaquero, J. M.: The
meteorological observations of Bento Sanches Dorta, Rio de Janeiro, Brazil:
1781–1788, Clim. Change, 115, 579–595,
https://doi.org/10.1007/s10584-012-0467-8, 2012.
Gallego, D., García-Herrera, R., Calvo, N., and Ribera, P.: A new meteorological record for Cádiz (Spain) 1806–1852: Implications for climatic reconstructions. J. Geophys. Res.-Atmos., 112, D12108, https://doi.org/10.1029/2007JD008517, 2007.
García-Herrera, R., Prieto, L., Gallego, D., Hernández, E., Gimeno,
L., Können, G., Koek, F., Wheeler, D., Wilkinson, C., Prieto, M.,
Báez, C., and Woodruff, S: CLIWOC multilingual meteorological
dictionary, https://epic.awi.de/id/eprint/17064/ (last access: 4 July 2023), 2003.
Jones, P. D., Davies, T. D., Lister, D. H., Slonosky, V., Jónsson, T.,
Bärring, L., Jönsson, P., Maheras, P., Kolyva-Machera, F.,
Barriendos, M., Martin-Vide, J., Rodriguez, R., Alcoforado, M. J., Wanner,
H., Pfister, C., Luterbacher, J., Rickli, R., Schuepbach, E., Kaas, E.,
Schmith, T., Jacobeip, J., and Beck, C.: Monthly mean pressure
reconstructions for Europe for the 1780–1995 period, Int. J. Climatol., 19,
347–364, https://doi.org/10.1002/(SICI)1097-0088(19990330)19:4<347::AID-JOC363>3.0.CO;2-S, 1999.
Können, G. P. and Brandsma, T.: Instrumental pressure observations from
the end of the 17th century: Leiden (The Netherlands), Int. J. Climatol.,
25, 1139–1145, https://doi.org/10.1002/joc.1192, 2005.
Lafuente, A. and Sellés, M.: El Observatorio de Cádiz (1753–1831),
Ministerio de Defensa, Instituto de Historia y Cultura Naval, Madrid, ISBN 84-505-7563-X, 1988.
Luterbacher, J., Rickli, R., Tinguely, C., Xoplaki, E., Schüpbach, E.,
Dietrich, D., Hüsler, J., Ambühl, M., Pfister, C., Beeli, P.,
Dietrich, U., Dannecker, A., Davies, T. D., Jones, P. D., Slonosky, V.,
Ogilvie, A. E. J., Maheras, P., Kolyva-Machera, F., Martin-Vide, J.,
Barriendos, M., Alcoforado, M. J., Nunes, M. F., Jónsson, T., Glaser,
R., Jacobeit, J., Beck, C., Philipp, A., Beyer, U., Kaas, E., Schmith, T.,
Bärring, L., Jönsson, P., Rácz, L., and Wanner, H.: Monthly mean
pressure reconstruction for the Late Maunder Minimum Period (AD 1675–1715),
Int. J. Climatol., 20, 1049–1066,
https://doi.org/10.1002/1097-0088(200008)20:10<1049::AID-JOC521>3.0.CO;2-6, 2000.
Morozova, A. L. and Valente, M. A.: Homogenization of Portuguese long-term temperature data series: Lisbon, Coimbra and Porto, Earth Syst. Sci. Data, 4, 187–213, https://doi.org/10.5194/essd-4-187-2012, 2012.
Pfister, L., Hupfer, F., Brugnara, Y., Munz, L., Villiger, L., Meyer, L., Schwander, M., Isotta, F. A., Rohr, C., and Brönnimann, S.: Early instrumental meteorological measurements in Switzerland, Clim. Past, 15, 1345–1361, https://doi.org/10.5194/cp-15-1345-2019, 2019.
Picas, J., Grab, S., and Allan, R.: A 19th century daily surface pressure
series for the Southwestern Cape region of South Africa: 1834–1899, Int. J.
Climatol., 39, 1404–1414, https://doi.org/10.1002/joc.5890, 2019.
Pujazón, C.: Resumen de las observaciones pluviométricas efectuadas
en los años 1805 a 1899, Instituto y Observatorio de Marina, San
Fernando, Cádiz, 1899.
Rodrigo, F. S.: Completing the early instrumental weather record from
Cádiz (Southern Spain): New data from 1799 to 1803, Clim. Change, 111,
697–704, https://doi.org/10.1007/s10584-011-0174-x, 2012.
Rodrigo, F. S.: Early meteorological data in southern Spain during the
Dalton Minimum, Int. J. Climatol., 39, 3593–3607,
https://doi.org/10.1002/joc.6041, 2019.
Slonosky, V.: The Meteorological Observations of Jean-François Gaultier,
Quebec, Canada: 1742–56, J. Climate, 16, 2232–2247,
https://doi.org/10.1175/1520-0442(2003)16<2232:TMOOJG>2.0.CO;2, 2003.
Slonosky, V. C., Jones, P. D., and Davies, T. D.: Instrumental pressure
observations and atmospheric circulation from the 17th and 18th centuries:
London and Paris, Int. J. Climatol., 21, 285–298,
https://doi.org/10.1002/joc.611, 2001.
Sousa, R.: Notas para una Climatología de Cádiz, Ministerio de
Transportes, Turismo y Comunicaciones, Madrid, ISBN 84-505-6878-1, 1987.
Valler, V., Franke, J., Brugnara, Y., and Brönnimann, S.: An updated
global atmospheric paleo-reanalysis covering the last 400 years, Geosci.
Data J., 1–19, https://doi.org/10.1002/gdj3.121, 2021.
Vaquero, J. M., Bravo-Paredes, N., Obregón, M. A., Carrasco, V. M. S.,
Valente, M. A., Trigo, R. M., Domínguez-Castro, F.,
Montero-Martín, J., Vaquero-Martínez, J., Antón, M.,
García, J. A., and Gallego, M. C.: Recovery of early meteorological
records from Extremadura region (SW Iberia): The “CliPastExtrem” (v1.0)
database, Geosci. Data J., 9, 1–14, https://doi.org/10.1002/gdj3.131, 2022.
Wheeler, D.: Early instrumental weather data from Cadiz: A study of late
eighteenth and early nineteenth century records, Int. J. Climatol., 15,
801–810, https://doi.org/10.1002/joc.3370150707, 1995.
WMO: Guide to meteorological instruments and methods of observation; WMO-No.
8: Measurement of Meteorological Variables, 525–552, ISBN 978-92-63-100085, 2018.
Zaiki, M., Kimura, K., and Mikami, T.: A statistical estimate of daily mean
temperature derived from a limited number of daily observations, Geophys.
Res. Lett., 29, 39.1–39.4,
https://doi.org/10.1029/2001GL014378, 2002.
Zaiki, M., Können, G. P., Tsukahara, T., Jones, P. D., Mikami, T., and
Matsumoto, K.: Recovery of nineteenth-century Tokyo/Osaka meteorological
data in Japan, Int. J. Climatol., 26, 399–423,
https://doi.org/10.1002/joc.1253, 2006.
Short summary
We present the earliest records made in San Fernando, very close to Cádiz (SW Spain). Several previous works have already recovered a significant number of meteorological records of interest in these localities. However, more than 40 000 daily meteorological observations recorded at the Royal Observatory of the Spanish Navy (located in San Fernando) were previously unnoticed and remained neither digitized nor studied. We analyze in detail these newly recovered meteorological readings.
We present the earliest records made in San Fernando, very close to Cádiz (SW Spain). Several...
