1968
DOI: 10.1002/j.1477-8696.1968.tb03086.x
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The Radcliffe Meteorological Station*

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Cited by 15 publications
(4 citation statements)
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“…The new Stornoway rainfall observations therefore represent a big improvement in coverage for the HadUK-Grid. The DWR observations for Oxford, however, are in very good agreement with HadUK-Grid ( Figure 11) since MIDAS has similar daily observations from the same site (the Radcliffe Observatory; Smith, 1968;Burt and Burt, 2019). The DWR observations are often slightly less than the gridded data which may be an artefact of the interpolation used to create the gridded dataset or slightly different observing times for the MIDAS data.…”
Section: Rainfall Observationsmentioning
confidence: 61%
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“…The new Stornoway rainfall observations therefore represent a big improvement in coverage for the HadUK-Grid. The DWR observations for Oxford, however, are in very good agreement with HadUK-Grid ( Figure 11) since MIDAS has similar daily observations from the same site (the Radcliffe Observatory; Smith, 1968;Burt and Burt, 2019). The DWR observations are often slightly less than the gridded data which may be an artefact of the interpolation used to create the gridded dataset or slightly different observing times for the MIDAS data.…”
Section: Rainfall Observationsmentioning
confidence: 61%
“…Documents labelled with an asterisk are both referred to an Annual Reports in the main text of this paper. After 1920, when control of the Met Office passed from the Board of Trade to the Air Ministry (Walker, 2011) stations in Aberdeen (Geddes, 1955), Liverpool (Reynolds, 1954), Oxford (Smith, 1968) and Valentia (Murphy, 1990) were already known, but further investigation was required to locate other stations (Table 1). Some stations are not in the location that their name in the DWR may suggest.…”
Section: British and Irish Stationsmentioning
confidence: 99%
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“…A contribution to meteorology by Spencer Cowper was experimenting with ways of measuring rainfall at Corpus Christi College in 1758 and 1760. 39 He made numerous but irregular observations of temperature, rainfall, winds and cloud from 1760 until 1804, when his health and eyesight were failing. 40 As discussed below, he advised others on instruments and methods of observing and became involved, albeit marginally, in a project to create a network of weather observers across Britain.…”
mentioning
confidence: 99%