In 1839, Durham University (founded in
1832) resolved to establish an astronomical observatory. By 1841,
the Observatory building, designed by Anthony Salvin, was complete. As
at other astronomical observatories, meteorological observations were
necessary from the start because air temperature was needed for the
calculation of refraction. Mean values for pressure, temperature and
rainfall began to appear in the Durham Advertiser as early as 1841 and,
from 23 July 1843, observations were noted systematically in bound
volumes currently held in the University Library on Palace Green.
The meteorological station is located on a gently sloping south-facing
lawn in front of the Observatory building, on a ridge less than one
kilometre southwest from Durham Cathedral, at 54º 46’ 06” N, 1º 35’ 05”
W and 102 metres above sea level; the general situation of the site has
changed little over the years. At no time has there been need to move
the meteorological station, as has happened in many other cities, so
that Gordon Manley could be especially proud to create a temperature
series based on the second longest continuous record at one site at a
university in Britain, after that of the Radcliffe Observatory, Oxford
(where the record dates from 1766). Owing to some gaps in the record,
the long-term temperature record is presented from 1850 and the
rainfall record from 1952.
Gordon Manley’s original and seminal work on the temperature series
takes us back to the time when pens, pencils and “totting up”
prevailed. As head of the young Department of Geography from 1928, he
contributed papers on the climate of Durham and the north Pennines and
began his interest in establishing the Durham temperature series as
comparable to that of Oxford.
The complexity of problems met in standardising the temperature series
make his account (Manley 1941) a classic illustration of the fact that
it is seldom enough simply to accumulate instrumental measurements of
climatic conditions: “differences in exposure, in hours of observation,
in instrumental corrections and even in the observers’ predilections
must all be accounted for”. Manley’s work at Durham laid the foundation
for his Central England Temperature record, a series dating from 1694
and maintained to this day.
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