We develop monthly temperature series (mean, maximum and minimum) for the Scottish mainland (SMT), the northern and northwestern Scottish Isles (SIT, Orkneys, Shetlands and Outer Hebrides) and for Northern Ireland (NIT). The series were developed from eight long station records, five over SMT, two for SIT and one for NIT. The series are reliable back to 1866 for all three regions, but extensions to 1800 and 1827 for SMT and SIT are less so, likely due to direct solar insolation effects in the summer months. All three regions show long-term statistically significant seasonal warming over both 1861-2000 and 1901-2000, except for the winter season. For the calendar year, the temperature change explained by a linear trend over 1861-2000 is 0.69...
The first decadal-scale reconstruction of British coastal temperature anomalies spanning the last mi...
Daily temperature measurements from six meteorological stations along the coast and fjords of wester...
Mountain snowline is important as it is an easily identifiable measure of the phase state of water ...
This study presents a summer temperature reconstruction using Scots pine tree-ring chronologies for ...
Three independent mean temperature series for Armagh Observatory, covering the period 1796–2002 have...
This paper updates precipitation series forEngland and Wales, Scotland and Northern Ireland for 1990...
Three independent mean temperature series for Armagh Observatory, covering the period 1796 – 2002 ha...
Monthly sea surface temperature is provided for 14 locations around the UK for a 230 year period. Th...
Accurate long-term daily maximum and minimum air temperature series are needed to assess the frequen...
Despite the rich heritage of meteorological observations registered in Ireland, prior to this PhD re...
A continuous 305-year (1711–2016) monthly rainfall series (IoI_1711) is created for the Island of I...
The geographer and climatologist Gordon Manley produced a monthly temperature reduction for Durham U...
The Svalbard Airport composite series spanning the period from 1898 to the present represents one of...
We have analysed the trends in four long meteorological time series from Armagh Observatory and comp...
A continuous 305-year (1711–2016) monthly rainfall series (IoI_1711) is created for the Island of I...
The first decadal-scale reconstruction of British coastal temperature anomalies spanning the last mi...
Daily temperature measurements from six meteorological stations along the coast and fjords of wester...
Mountain snowline is important as it is an easily identifiable measure of the phase state of water ...
This study presents a summer temperature reconstruction using Scots pine tree-ring chronologies for ...
Three independent mean temperature series for Armagh Observatory, covering the period 1796–2002 have...
This paper updates precipitation series forEngland and Wales, Scotland and Northern Ireland for 1990...
Three independent mean temperature series for Armagh Observatory, covering the period 1796 – 2002 ha...
Monthly sea surface temperature is provided for 14 locations around the UK for a 230 year period. Th...
Accurate long-term daily maximum and minimum air temperature series are needed to assess the frequen...
Despite the rich heritage of meteorological observations registered in Ireland, prior to this PhD re...
A continuous 305-year (1711–2016) monthly rainfall series (IoI_1711) is created for the Island of I...
The geographer and climatologist Gordon Manley produced a monthly temperature reduction for Durham U...
The Svalbard Airport composite series spanning the period from 1898 to the present represents one of...
We have analysed the trends in four long meteorological time series from Armagh Observatory and comp...
A continuous 305-year (1711–2016) monthly rainfall series (IoI_1711) is created for the Island of I...
The first decadal-scale reconstruction of British coastal temperature anomalies spanning the last mi...
Daily temperature measurements from six meteorological stations along the coast and fjords of wester...
Mountain snowline is important as it is an easily identifiable measure of the phase state of water ...