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Central England temperature dataset, 1659 to 2014. The Central England Temperature (CET) record is a meteorological dataset originally published by Professor Gordon Manley in 1953 and subsequently extended and updated in 1974, following many decades of work.
Series of reliable temperature measurements in some regions began in the 1850—1880 time frame (this is called the instrumental temperature record). The longest-running temperature record is the Central England temperature data series, which starts in 1659. The longest-running quasi-global records start in 1850. [3]
The Central England temperature series continues to be updated each month by the UK Meteorological Office. During 1969–70 he was a Visiting Professor of Meteorology at Texas A&M University . For the rest of his life he continued working and publishing.
Last year also ranked the second warmest for the Central England Temperature, the world’s longest instrumental temperature series from 1659. Met Office senior scientist Mike Kendon said: “The ...
In an early attempt to show that climate had changed, Hubert Lamb's 1965 paper generalised from temperature records of central England together with historical, botanical, and archeological evidence to produce a qualitative estimate of temperatures in the North Atlantic region. Subsequent quantitative reconstructions used statistical techniques ...
Provisional data from the Met Office shows that 2022 has set a 139-year annual mean temperature record. ... this year has also been the warmest on record in the 364-year Central England series ...
English: Graphs of annual mean w:Central England temperature (CET) beginning in 1659, and of 10-year and 30-year moving averages. Source for version with data through 2018 (OUTDATED): mean CET ranked coldest to warmest from 1659 to 2019. w:Met Office, w:Hadley Centre for Climate Prediction and Research (31 July 2019).
The longest-running temperature record is the Central England temperature data series, which starts in 1659. The longest-running quasi-global records start in 1850. For temperature measurements in the upper atmosphere a variety of methods can be used.