Articles | Volume 8, issue 1
Clim. Past, 8, 353–371, 2012
https://doi.org/10.5194/cp-8-353-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue: Characterization of climatic variability in the Iberian Peninsula...
Clim. Past, 8, 353–371, 2012
https://doi.org/10.5194/cp-8-353-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article 29 Feb 2012
Research article | 29 Feb 2012
Early Portuguese meteorological measurements (18th century)
M. J. Alcoforado et al.
Related subject area
Subject: Atmospheric Dynamics | Archive: Historical Records | Timescale: Instrumental Period
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
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
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
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
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