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Journal articles on the topic 'Central England Temperature record'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

Brabson, B. B., and J. P. Palutikof. "The evolution of extreme temperatures in the Central England temperature record." Geophysical Research Letters 29, no. 24 (2002): 16–1. http://dx.doi.org/10.1029/2002gl015964.

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2

Chapman, S. C., E. J. Murphy, D. A. Stainforth, and N. W. Watkins. "Trends in Winter Warm Spells in the Central England Temperature Record." Journal of Applied Meteorology and Climatology 59, no. 6 (2020): 1069–76. http://dx.doi.org/10.1175/jamc-d-19-0267.1.

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AbstractAn important impact of climate change on agriculture and the sustainability of ecosystems is the increase of extended warm spells during winter. We apply crossing theory to the central England temperature time series of winter daily maximum temperatures to quantify how increased occurrence of higher temperatures translates into more frequent, longer-lasting, and more intense winter warm spells. We find since the late 1800s an overall two- to threefold increase in the frequency and duration of winter warm spells. A winter warm spell of 5 days in duration with daytime maxima above 13°C h

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3

Alan, D. Smith. "An Analysis of Climate Forcings from the Central England Temperature (CET) Record." British Journal of Environment & Climate Change 7, no. 2 (2017): 113–18. https://doi.org/10.9734/BJECC/2017/34589.

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The Central England Temperature (CET) record is the world's longest instrument-based temperature record and covers the years 1659-present. The temperature variation of 0.8°C between the Maunder Sunspot Minimum in the late 17<sup>th</sup> Century and the beginning of the Industrial Revolution in the mid-late 18<sup>th</sup> Century can be explained by fluctuations in solar output (TSI) alone. Thereafter, approximately one third of the temperature increase to the present may be attributed to increases in atmospheric CO<sub>2</sub>, with the anthropogenic contribution to Global Warming/Climate Ch

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4

Smith, Alan. "An Analysis of Climate Forcings from the Central England Temperature (CET) Record." British Journal of Environment and Climate Change 7, no. 2 (2017): 113–18. http://dx.doi.org/10.9734/bjecc/2017/34589.

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5

King, Andrew D., Geert Jan van Oldenborgh, David J. Karoly, Sophie C. Lewis, and Heidi Cullen. "Attribution of the record high Central England temperature of 2014 to anthropogenic influences." Environmental Research Letters 10, no. 5 (2015): 054002. http://dx.doi.org/10.1088/1748-9326/10/5/054002.

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6

Johnson, Robert W. "Enhanced wavelet analysis of solar magnetic activity with comparison to global temperature and the Central England Temperature record." Journal of Geophysical Research: Space Physics 114, A5 (2009): n/a. http://dx.doi.org/10.1029/2009ja014172.

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7

Isarin, René F. B., and Sjoerd J. P. Bohncke. "Mean July Temperatures during the Younger Dryas in Northwestern and Central Europe as Inferred from Climate Indicator Plant Species." Quaternary Research 51, no. 2 (1999): 158–73. http://dx.doi.org/10.1006/qres.1998.2023.

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AbstractWe estimated minimum mean July temperatures in northwestern and central Europe during the Younger Dryas (10,950–10,15014C yr B.P.) from distributions of climate indicator plant species, which were reconstructed from 140 pollen and plant macrofossil diagrams. Paleobotanical records, mainly from the central and eastern part of the study area, show that the coldest conditions occurred early in the Younger Dryas (before ∼10,55014C yr B.P.). For this phase, mean July temperatures at sea level of around 10°C are suggested for the northern part of the British Isles and for ice-free Scandinavi

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8

van der Schrier, Gerard, and Gerard J. M. Versteegh. "Internally and externally forced climate variability: A dynamical systems approach using the central England temperature record." Geophysical Research Letters 28, no. 5 (2001): 759–62. http://dx.doi.org/10.1029/2000gl011939.

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9

Duncan, Kirsty. "A COMPARISON OF THE TEMPERATURE RECORDS OF EDINBURGH AND CENTRAL ENGLAND." Weather 46, no. 6 (1991): 169–73. http://dx.doi.org/10.1002/j.1477-8696.1991.tb05735.x.

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10

González-Hidalgo, J. C., D. Peña-Angulo, and S. Beguería. "Temporal variations of trends in the Central England Temperature series." Cuadernos de Investigación Geográfica 46, no. 2 (2020): 345–69. http://dx.doi.org/10.18172/cig.4377.

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Variations in trend rates of annual values of the Central England Temperature series (CET) over the period1659-2017 were analysed using moving windows of different length, to identify the minimum period in which the trend expresses a climate signal not hidden by the noise produced by natural variability. Trend rates exhibit high variability and irregular shifting from positive to negative values unless very long window lengths (of 100 years or more) are used. In general, as the duration of the length of the temporal window analysed increases, the absolute range of the trend rates decreases and

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11

van Oldenborgh, G. J. "How unusual was autumn 2006 in Europe?" Climate of the Past Discussions 3, no. 3 (2007): 811–37. http://dx.doi.org/10.5194/cpd-3-811-2007.

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Abstract. The temperatures in large parts of Europe have been record high during the meteorological autumn of 2006. Compared to the 1961–1990 normals it was more than three degrees Celsius warmer from the North side of the Alps to southern Norway. This made it by far the warmest autumn on record in the United Kingdom, Belgium, the Netherlands, Denmark, Germany and Switzerland, with the records in Central England going back to 1659, in the Netherlands to 1706 and in Denmark to 1768. Also in most of Austria, southern Sweden, southern Norway and parts of Ireland the autumn was the warmest on reco

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12

van Oldenborgh, G. J. "How unusual was autumn 2006 in Europe?" Climate of the Past 3, no. 4 (2007): 659–68. http://dx.doi.org/10.5194/cp-3-659-2007.

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Abstract. The temperatures in large parts of Europe have been record high during the meteorological autumn of 2006. Compared to 1961–1990, the 2 m temperature was more than three degrees Celsius above normal from the North side of the Alps to southern Norway. This made it by far the warmest autumn on record in the United Kingdom, Belgium, the Netherlands, Denmark, Germany and Switzerland, with the records in Central England going back to 1659, in the Netherlands to 1706 and in Denmark to 1768. The deviations were so large that under the obviously false assumption that the climate does not chan

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13

Boyer, Tim, Ellen Bartow-Gillies, A. Abida, et al. "Introduction." Bulletin of the American Meteorological Society 104, no. 9 (2023): S1—S10. http://dx.doi.org/10.1175/2023bamsstateoftheclimate_intro.1.

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Abstract —J. BLUNDEN, T. BOYER, AND E. BARTOW-GILLIES Earth’s global climate system is vast, complex, and intricately interrelated. Many areas are influenced by global-scale phenomena, including the “triple dip” La Niña conditions that prevailed in the eastern Pacific Ocean nearly continuously from mid-2020 through all of 2022; by regional phenomena such as the positive winter and summer North Atlantic Oscillation that impacted weather in parts the Northern Hemisphere and the negative Indian Ocean dipole that impacted weather in parts of the Southern Hemisphere; and by more localized systems s

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14

Henriksson, S. V., P. Räisänen, J. Silen, H. Järvinen, and A. Laaksonen. "Power-law behavior in millennium climate simulations." Earth System Dynamics Discussions 3, no. 1 (2012): 391–416. http://dx.doi.org/10.5194/esdd-3-391-2012.

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Abstract. Using a method of discrete Fourier transform with varying starting point and length of time window and the long time series provided by millennium Earth System Model simulations, we get good fits to power laws between two characteristic oscillatory timescales of the model climate: multidecadal (50–80 yr) and El Nino (3–6 yr) timescales. For global mean temperature, we fit β ~ 0.35 in a relation S(f) ~ f−β in a simulation without external climate forcing and β over 0.7 in a simulation with external forcing included. We also fit a power law with β ~ 8 to the narrow frequency range betw

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15

Murphy, Conor, Ciaran Broderick, Timothy P. Burt, et al. "A 305-year continuous monthly rainfall series for the island of Ireland (1711–2016)." Climate of the Past 14, no. 3 (2018): 413–40. http://dx.doi.org/10.5194/cp-14-413-2018.

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Abstract. A continuous 305-year (1711–2016) monthly rainfall series (IoI_1711) is created for the Island of Ireland. The post 1850 series draws on an existing quality assured rainfall network for Ireland, while pre-1850 values come from instrumental and documentary series compiled, but not published by the UK Met Office. The series is evaluated by comparison with independent long-term observations and reconstructions of precipitation, temperature and circulation indices from across the British–Irish Isles. Strong decadal consistency of IoI_1711 with other long-term observations is evident thro

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16

Britain, Great, and D. Conway. "Recent climate variability and future climate change scenarios for." Progress in Physical Geography: Earth and Environment 22, no. 3 (1998): 350–74. http://dx.doi.org/10.1177/030913339802200303.

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This article reviews recent climatically extreme periods in Great Britain and presents results from the latest general circulation model (GCM) experiments showing the possible spatial patterns and magnitude of future climate change for this region. During the last decade the British Isles has seen record-breaking periods of above-average temperatures, alongside periods with above and below-average precipitation, combined with an increase in winter precipitation and a decrease in summer precipitation. The impacts of these anomalies, coupled with the possibility that future climate change may in

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17

West, David P., Mary K. Roden-Tice, Jaime K. Potter, and Nellie Q. Barnard. "Assessing the role of orogen-parallel faulting in post-orogenic exhumation: low-temperature thermochronology across the Norumbega Fault System, Maine." Canadian Journal of Earth Sciences 45, no. 3 (2008): 287–301. http://dx.doi.org/10.1139/e07-073.

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As a part of a regional effort to determine the extent of low-temperature thermochronological discontinuities across major orogen-parallel faults in northern New England, 41 apatite fission track (AFT) ages and 11 (U–Th)/He ages are used to constrain the ∼65 to 100 °C cooling history of rocks flanking a 160 km long segment of the Norumbega fault system in southern and south-central Maine. These data are used to evaluate the role of this structure in the late Mesozoic and younger exhumation history of the northern Appalachians. AFT ages flanking the fault system range from 159 to 95 Ma and reco

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18

Koumoutsaris, Symeon. "A hazard model of sub-freezing temperatures in the United Kingdom using vine copulas." Natural Hazards and Earth System Sciences 19, no. 3 (2019): 489–506. http://dx.doi.org/10.5194/nhess-19-489-2019.

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Abstract. Extreme cold weather events, such as the winter of 1962/63, the third coldest winter ever recorded in the Central England Temperature record, or more recently the winter of 2010/11, have significant consequences for the society and economy. This paper assesses the probability of such extreme cold weather across the United Kingdom (UK), as part of a probabilistic catastrophe model for insured losses caused by the bursting of pipes. A statistical model is developed in order to model the extremes of the Air Freezing Index (AFI), which is a common measure of the magnitude and duration of

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19

Nesbitt, A., S. Dorling, and R. Jones. "Climate resilience in the United Kingdom wine production sector: CREWS-UK." BIO Web of Conferences 15 (2019): 01011. http://dx.doi.org/10.1051/bioconf/20191501011.

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As cool climate viticulture rapidly expands, the England and Wales wine sector is winning international acclaim, particularly for its sparkling wines, and is attracting significant investment. Supported by warming climate trends during the growing season, wine producers are establishing new vineyards planted predominantly with Pinot Noir and Chardonnay. Grape-friendly weather conditions in 2018 led to a record harvest and may be a sign of good things to come. Long term (100-years) Growing Season Average Temperatures (GSTs) in south-east and south-central England have noticeably increased with

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20

Mateus, Carla, and Aaron Potito. "Development of a Quality-Controlled and Homogenised Long-Term Daily Maximum and Minimum Air Temperature Network Dataset for Ireland." Climate 9, no. 11 (2021): 158. http://dx.doi.org/10.3390/cli9110158.

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Accurate long-term daily maximum and minimum air temperature series are needed to assess the frequency, intensity, distribution, and duration of extreme climatic events. However, quality control and homogenisation procedures are required to minimise errors and inhomogeneities in climate series before the commencement of climate data analysis. A semi-automatic quality control procedure consisting of climate consistency, internal consistency, day-to-day step-change, and persistency tests was applied for 12 long-term series registered in Ireland from 1831–1968, Armagh Observatory (Northern Irelan

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21

Burt, Stephen. "Meteorological responses in the atmospheric boundary layer over southern England to the deep partial eclipse of 20 March 2015." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2077 (2016): 20150214. http://dx.doi.org/10.1098/rsta.2015.0214.

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A wide range of surface and near-surface meteorological observations were made at the University of Reading’s Atmospheric Observatory in central southern England (latitude 51.441° N, longitude 0.938° W, altitude 66 m above mean sea level) during the deep partial eclipse on the morning of 20 March 2015. Observations of temperature, humidity, radiation, wind speed and direction, and atmospheric pressure were made by computerized logging equipment at 1 Hz, supplemented by an automated cloud base recorder sampling at 1 min intervals and a high-resolution (approx. 10 m vertical interval) atmospheri

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22

Matthews, J. B., and J. B. R. Matthews. "Possible signals of poleward surface ocean heat transport, of Arctic basal ice melt, and of the twentieth century solar maximum in the 1904-2012 Isle of Man daily timeseries." Ocean Science Discussions 11, no. 1 (2014): 47–122. http://dx.doi.org/10.5194/osd-11-47-2014.

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Abstract. This is the second of two papers on observational timeseries of top of ocean heat capture. The first reports hourly and daily meridional central tropical Pacific top 3 m timeseries showing high Southern Hemisphere evaporation (2.67 m yr−1) and Northern Hemisphere trapped heat (12 MJ m−2 day−1). We suggested that wind drift/geostrophic stratified gyre circulation transported warm water to the Arctic and led to three phases of Arctic basal ice melt and fluxes of brackish nutrient-rich waters to north Atlantic on centennial timescales. Here we examine daily top metre 1904–2012 timeserie

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23

Greatbatch, Richard J., and Ping-ping Rong. "Discrepancies between Different Northern Hemisphere Summer Atmospheric Data Products." Journal of Climate 19, no. 7 (2006): 1261–73. http://dx.doi.org/10.1175/jcli3643.1.

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Abstract Northern Hemisphere summer (July–August) data from the NCEP–NCAR and ECMWF 40-yr Re-Analysis (ERA-40) reanalyses are compared with each other and with Trenberth's sea level pressure (SLP) dataset. Discrepancies in SLP and 500 hPa are mostly confined to a band connecting North Africa and Asia. In the NCEP–NCAR reanalysis, there is a negative offset in SLP over North Africa and Asia prior to the late 1960s, together with a similar problem in 500-hPa height, and in Trenberth's data there is a negative offset in SLP over Asia prior to the early 1990s. Both these offsets magnify the linear

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24

van der Schrier, Gerard, Richard P. Allan, Albert Ossó, et al. "The 1921 European drought: impacts, reconstruction and drivers." Climate of the Past 17, no. 5 (2021): 2201–21. http://dx.doi.org/10.5194/cp-17-2201-2021.

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Abstract. The European drought of 1921 is assessed in terms of its impacts on society and in terms of its physical characteristics. The development of impacts of the drought are categorized by a systematic survey of newspaper reports from five European newspapers covering the area from England to the Czech Republic and other parts of Europe. This is coupled to a reconstruction of daily temperature and precipitation based on meteorological measurements to quantify the drought severity and extent, and reanalysis data are used to identify its drivers. This analysis shows that the first impacts of

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25

Matthews, J. Brian. "Physics of Climate Change: Harmonic and exponential processes from in situ ocean time series observations show rapid asymmetric warming." JOURNAL OF ADVANCES IN PHYSICS 6, no. 2 (2014): 1135–71. http://dx.doi.org/10.24297/jap.v6i2.6960.

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Analyses of rare ocean timeseries in the top few meters show logarithmic and exponential processes control anthropogenic global warming (AGW) of which 93% is in the oceans. Processes result in asymmetric heat capture in the North and South tropical Pacific. A new Lagrangian paradigm established a global ocean surface freshwater and heat conveyor. Climate research wrongly assumed atmospheric pan-evaporation at sea as over land, a 10m well-mixed surface layer, and ignored that seawater density depends on both salinity and temperature. In situ observations show two different heat-capture and evap

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26

Folland, Chris K., Jeff Knight, Hans W. Linderholm, David Fereday, Sarah Ineson, and James W. Hurrell. "The Summer North Atlantic Oscillation: Past, Present, and Future." Journal of Climate 22, no. 5 (2009): 1082–103. http://dx.doi.org/10.1175/2008jcli2459.1.

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Abstract Summer climate in the North Atlantic–European sector possesses a principal pattern of year-to-year variability that is the parallel to the well-known North Atlantic Oscillation in winter. This summer North Atlantic Oscillation (SNAO) is defined here as the first empirical orthogonal function (EOF) of observed summertime extratropical North Atlantic pressure at mean sea level. It is shown to be characterized by a more northerly location and smaller spatial scale than its winter counterpart. The SNAO is also detected by cluster analysis and has a near-equivalent barotropic structure on

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27

DAVIES, NEIL S., JOHN C. GOSSE, ALEXANDRA ROUILLARD, et al. "WOOD JAMS OR BEAVER DAMS? PLIOCENE LIFE, SEDIMENT AND LANDSCAPE INTERACTIONS IN THE CANADIAN HIGH ARCTIC." PALAIOS 37, no. 6 (2022): 330–47. http://dx.doi.org/10.2110/palo.2021.065.

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ABSTRACT During the mid-Pliocene (Zanclean, ca. ∼ 3.9 Ma), parts of the Canadian High Arctic experienced mean annual temperatures that were 14–22°C warmer than today and supported diverse boreal-type forests. The landscapes of this vegetated polar region left behind a fragmented sedimentary record that crops out across several islands in the Canadian Arctic Archipelago as the Beaufort Formation and correlative strata. Paleoecological information from these strata provides a high-fidelity window onto Pliocene environments, and prominent fossil sites yield unparalleled insights into Cenozoic mam

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28

Probert-Jones, Richard. "Central England Temperature (CET)." Weather 68, no. 2 (2013): 54. http://dx.doi.org/10.1002/wea.2067.

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29

Parker, David. "Central England Temperature (CET)." Weather 68, no. 4 (2013): 111. http://dx.doi.org/10.1002/wea.2111.

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30

Syroka, J. "Scaling of Central England Temperature Fluctuations?" Atmospheric Science Letters 2, no. 1-4 (2001): 143–54. http://dx.doi.org/10.1006/asle.2002.0047.

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31

Karoly, David J., and Peter A. Stott. "Anthropogenic warming of central England temperature." Atmospheric Science Letters 7, no. 4 (2006): 81–85. http://dx.doi.org/10.1002/asl.136.

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32

Jones, D. E. "DAILY CENTRAL ENGLAND TEMPERATURE: RECENTLY CONSTRUCTED SERIES." Weather 42, no. 5 (1987): 130–33. http://dx.doi.org/10.1002/j.1477-8696.1987.tb06949.x.

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33

Matthews, Dr J. Brian. "Isle of Man, Galapagos and sunspot data show net cooling hid double exponential ocean warming danger: +3Â°C in 2014, +4Â°C likely by 2016." JOURNAL OF ADVANCES IN PHYSICS 9, no. 2 (2015): 2355–71. http://dx.doi.org/10.24297/jap.v9i2.1436.

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Anthropogenic global warming (AGW) heat is trapped by the greenhouse gas (GHG) blanket, and the ocean surface layer. It is 93% in the ocean and drives atmospheric warming. The 111-year mean daily surface temperatures are 10.5Â±0.5Â°C at Port Erin (PE) Isle of Man compared with 9.6Â±4.8Â°C in Central England (CET) air. The Port Erin 5Â½-year max-min heat cycle synchronizes to the 11-year solar heat pump sunspot cycle. Tropical heat arrives 2 years after a solar maximum on wind-driven currents in the stratified sea surface. Runoff from bottom-up melted Arctic icesheets arrives 3Â½ year later at

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34

Parker, David E. "Anomalies of Central England Temperature Classified by Air Source." Journal of Climate 22, no. 5 (2009): 1069–81. http://dx.doi.org/10.1175/2008jcli2250.1.

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Abstract Daily anomalies of mean central England temperature (CET), relative to daily 1961–90 climatology, are analyzed in terms of the source of the air estimated from fields of mean sea level pressure. The average CET anomaly for a given source and calendar month during 1961–90 is taken as an estimate of the influence of atmospheric circulation for that source and calendar month, and the uncertainty in this influence is provided by the associated standard error. The atmospheric circulation influences are subtracted from the daily CET anomalies since the late nineteenth century to yield “resi

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35

Parker, D. E., T. P. Legg, and C. K. Folland. "A new daily central England temperature series, 1772–1991." International Journal of Climatology 12, no. 4 (1992): 317–42. http://dx.doi.org/10.1002/joc.3370120402.

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36

Turner, Charles. "The Eemian interglacial in the North European plain and adjacent areas." Netherlands Journal of Geosciences 79, no. 2-3 (2000): 217–31. http://dx.doi.org/10.1017/s0016774600023660.

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AbstractMany small deposits of Eemian age, including the stratotype, are found right across the North European plain. In adjacent areas, this interglacial is known by local names such as Ipswichian (Britain), Luhe or Ribains (France), Riss-Würm interglacial (Alps) and Mikulinian (Poland and Russia). It correlates primarily with MIS 5e of the deep-sea stratigraphy, though boundaries may not be exactly the same. Basins containing Eemian sediments rest directly on morainic deposits of all three Saalian ice advances, which must all, therefore, fall within MIS 6.Indicator species of both plants and

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37

Haupt, Harry, and Markus Fritsch. "Quantile Trend Regression and Its Application to Central England Temperature." Mathematics 10, no. 3 (2022): 413. http://dx.doi.org/10.3390/math10030413.

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The identification and estimation of trends in hydroclimatic time series remains an important task in applied climate research. The statistical challenge arises from the inherent nonlinearity, complex dependence structure, heterogeneity and resulting non-standard distributions of the underlying time series. Quantile regressions are considered an important modeling technique for such analyses because of their rich interpretation and their broad insensitivity to extreme distributions. This paper provides an asymptotic justification of quantile trend regression in terms of unknown heterogeneity a

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38

de Souza, Jeferson, Sílvio M. Duarte Queirós, and Alice M. Grimm. "Components of multifractality in the central England temperature anomaly series." Chaos: An Interdisciplinary Journal of Nonlinear Science 23, no. 2 (2013): 023130. http://dx.doi.org/10.1063/1.4811546.

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39

Matyasovszky, I. "Further results of the analysis of central England temperature data." Theoretical and Applied Climatology 39, no. 3 (1989): 126–36. http://dx.doi.org/10.1007/bf00868308.

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40

Yin, J. J., D. X. Yuan, H. C. Li, et al. "Variation in the Asian monsoon intensity and dry-wet condition since the Little Ice Age in central China revealed by an aragonite stalagmite." Climate of the Past Discussions 10, no. 2 (2014): 1305–35. http://dx.doi.org/10.5194/cpd-10-1305-2014.

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Abstract. Highlight: this paper focuses on the climate variability in central China since 1300 AD, involving: 1. A well-dated, 1.5 year resolution stalagmite δ18O record from Lianhua Cave, central China; 2. Links of the δ18O record with regional dry-wet condition, monsoon intensity, and temperature over eastern China; 3. Correlations among drought events in the Lianhua record, solar irradiation, and ENSO index. We present a highly precisely 230Th/U dated, 1.5 year resolution δ18O record of an aragonite stalagmite (LHD1) collected from Lianhua Cave in Wuling mountain area of central China. The

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41

Colman, Andrew. "Prediction of summer central England temperature from preceding North Atlantic winter sea surface temperature." International Journal of Climatology 17, no. 12 (1997): 1285–300. http://dx.doi.org/10.1002/(sici)1097-0088(199710)17:12<1285::aid-joc198>3.0.co;2-9.

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42

Tan, L., Y. Cai, Z. An, L. Yi, H. Zhang, and S. Qin. "Climate patterns in north central China during the last 1800 yr and their possible driving force." Climate of the Past 7, no. 3 (2011): 685–92. http://dx.doi.org/10.5194/cp-7-685-2011.

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Abstract. We synthesized high-resolution precisely-dated stalagmite records and historical document records from north central China to reconstruct a decadal resolution precipitation record during the last 1800 years (190–1980 AD). The synthesized precipitation record shows coincident variations and significant positive correlations with the temperature reconstructions on centennial- to multidecadal-scale, suggesting warm-humid/cool-dry was the main climate pattern in north central China over the past 1800 years. Solar activity may be the dominant force that drove the same-phase variations of

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43

Taricco, C., M. Ghil, S. Alessio, and G. Vivaldo. "Two millennia of climate variability in the Central Mediterranean." Climate of the Past 5, no. 2 (2009): 171–81. http://dx.doi.org/10.5194/cp-5-171-2009.

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Abstract. This experimental work addresses the need for high-resolution, long and homogeneous climatic time series that facilitate the study of climate variability over time scales of decades to millennia. We present a high-resolution record of foraminiferal δ18O from a Central-Mediterranean sediment core that covers the last two millennia. The record was analyzed using advanced spectral methods and shows highly significant oscillatory components with periods of roughly 600, 350, 200, 125 and 11 years. Over the last millennium, our data show several features related to known climatic periods,

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Taricco, C., M. Ghil, and G. Vivaldo. "Two millennia of climate variability in the Central Mediterranean." Climate of the Past Discussions 4, no. 5 (2008): 1089–113. http://dx.doi.org/10.5194/cpd-4-1089-2008.

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Abstract. This experimental work addresses the need for high-resolution, long and homogeneous climatic time series that facilitate the study of climate variability over time scales of decades to millennia. We present a high-resolution record of foraminiferal δ18O from a Central Mediterranean sediment core that covers the last two millennia. The record was analyzed using advanced spectral methods and shows highly significant oscillatory components with periods of roughly 600, 350, 200, 125 and 11 years. Comparison with the spectra of composite temperature-proxy series over the last millennium r

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Yao, T., K. Duan, B. Xu, N. Wang, X. Guo, and X. Yang. "Ice core precipitation record in central Tibetan plateau since AD 1600." Climate of the Past Discussions 4, no. 1 (2008): 233–48. http://dx.doi.org/10.5194/cpd-4-233-2008.

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Abstract. Lack of reliable long-term precipitation record from northern Tibetan Plateau has constrained the understanding of precipitation variation in this region. An ice core drilled from the Puruogangri Ice Field on central Tibetan Plateau in the year 2000 helped reveal the precipitation variations since AD 1600. Analysis of the annual accumulation data presented precipitation changes from AD 1600, indicative of wet and dry periods in the past 400 year in the central Tibetan Plateau. Accordingly, the 18th and 20th centuries experienced high precipitation period, whilst the 19th century expe

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Schultze, Hans-Peter, and John Chorn. "Palaeoniscoid (Actinopterygii, Pisces) vertebrae from the Late Paleozoic of central North America." Journal of Paleontology 60, no. 3 (1986): 744–57. http://dx.doi.org/10.1017/s0022336000022265.

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Actinopterygian vertebral centra are more common in the Pennsylvanian and Early Permian of central North America than was previously known. The oldest record dates from the Early Carboniferous of England. Stratigraphic occurrence, co-occurring vertebrate fauna, histology, and external morphology contradict a previous interpretation as centra of “holosteans.” The centra are assigned here to Palaeoniscoidea indet. Besides centra in haplolepids, these are the only known actinopterygian centra from the Paleozoic. The so-called caudal centra in Pygopterus are the bases of hypurals.

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Jagt, J. W. M., J. Lindgren, M. Machalski, and A. Radwański. "New records of the tylosaurine mosasaur Hainosaurus from the Campanian-Maastrichtian (Late Cretaceous) of central Poland." Netherlands Journal of Geosciences 84, no. 3 (2005): 303–6. http://dx.doi.org/10.1017/s0016774600021077.

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AbstractTwo isolated mosasaur teeth, one from the upper Campanian of Piotrawin, the other from the upper Maastrichtian at Nasilów (Wisla River valley, central Poland), recently described as Plioplatecarpinae sp. A and Plioplatecarpinae sp. B, respectively, are reassigned to the tylosaurine genus Hainosaurus Dollo, 1885. The present record thus adds to the list of Hainosaurus species known to date from elsewhere in Europe (Sweden, Belgium and England).

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Ajioka, T., M. Yamamoto, K. Takemura, A. Hayashida, and H. Kitagawa. "Water pH and temperature in Lake Biwa from MBT'/CBT indices during the last 280 000 years." Climate of the Past 10, no. 5 (2014): 1843–55. http://dx.doi.org/10.5194/cp-10-1843-2014.

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Abstract. We generated a 280 000 yr record of water pH and temperature in Lake Biwa, central Japan, by analysing the methylation index (MBT′) and cyclisation ratio (CBT) of branched tetraethers in sediments from piston and borehole cores. Our aim was to understand the responses of precipitation and air temperature in central Japan to the East Asian monsoon variability on orbital timescales. Because the water pH in Lake Biwa is determined by phosphorus and alkali cation inputs, the record of water pH should indicate the changes in precipitation and temperature in central Japan. Comparison with

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Affolter, Stéphane, Anamaria Häuselmann, Dominik Fleitmann, R. Lawrence Edwards, Hai Cheng, and Markus Leuenberger. "Central Europe temperature constrained by speleothem fluid inclusion water isotopes over the past 14,000 years." Science Advances 5, no. 6 (2019): eaav3809. http://dx.doi.org/10.1126/sciadv.aav3809.

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The reasons for the early Holocene temperature discrepancy between northern hemispheric model simulations and paleoclimate reconstructions—known as the Holocene temperature conundrum—remain unclear. Using hydrogen isotopes of fluid inclusion water extracted from stalagmites from the Milandre Cave in Switzerland, we established a mid-latitude European mean annual temperature reconstruction for the past 14,000 years. Our Milandre Cave fluid inclusion temperature record (MC-FIT) resembles Greenland and Mediterranean sea surface temperature trends but differs from recent reconstructions obtained f

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Blenkinsop, S., P. D. Jones, S. R. Dorling, and T. J. Osborn. "Observed and modelled influence of atmospheric circulation on central England temperature extremes." International Journal of Climatology 29, no. 11 (2009): 1642–60. http://dx.doi.org/10.1002/joc.1807.

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