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dc.contributor.advisorWilson, Rob
dc.contributor.authorRydval, Miloš
dc.coverage.spatial219en_US
dc.date.accessioned2016-03-14T16:16:34Z
dc.date.available2016-03-14T16:16:34Z
dc.date.issued2016-06-22
dc.identifier.urihttp://hdl.handle.net/10023/8418
dc.description.abstractThis thesis focuses on reconstructing past temperatures using Scots pine (Pinus sylvestris L.) tree-ring chronologies developed from Scotland. The research aims to fill a spatial and temporal gap in understanding northwest European climate dynamics, thus providing the context for assessing future climate changes in this region. Development of both a spatially complete reconstruction from an extensive network of 44 'living' Scottish tree-ring chronologies for the last few centuries, but also a near-millennium length chronology from central Scotland using mainly lake-derived 'subfossil' wood material was undertaken. Before reconstruction development, a combination of treegrowth modelling and disturbance removal methodologies was utilised in order to understand the drivers of pine growth in the Scottish Highlands, and to assess and remove anthropogenic disturbance and other non-climatic influences on growth. The advantages and limitations of utilising the relatively new 'Blue Intensity' (BI) parameter was also explored and assessed, particularly in relation to its possible utilization as a more affordable surrogate for maximum latewood density in the development of temperature reconstructions and for crossdating validation of undated samples. Although BI showed much promise for dendroclimatology, elimination of low frequency biases resulting from sample discolouration still requires further attention. Chronologies from the Cairngorms in central Scotland were identified as most suitable for reconstruction development, while reconstructions based on chronologies from other areas in the west were found to be weaker due to a range of factors including disturbance. In order to maximise reconstruction strength, BI and ring width (RW) data were combined to produce composite high-frequency BI / low-frequency RW chronologies. Although it was possible to develop an ~800 year reconstruction of temperature from central Scotland, there is substantial potential to further extend this reconstruction back in time.en_US
dc.language.isoenen_US
dc.publisherUniversity of St Andrewsen
dc.subjectDendrochronologyen_US
dc.subjectDendroclimatologyen_US
dc.subjectPalaeoclimatologyen_US
dc.subjectTemperature reconstructionen_US
dc.subjectTree ringsen_US
dc.subjectScots pineen_US
dc.subjectScotlanden_US
dc.subject.lccQC884.5S3R8
dc.titleDendroclimatic reconstruction of late Holocene summer temperatures in the Scottish Highlandsen_US
dc.typeThesisen_US
dc.contributor.sponsorCarnegie Trust for the Universities of Scotlanden_US
dc.type.qualificationlevelDoctoralen_US
dc.type.qualificationnamePhD Doctor of Philosophyen_US
dc.publisher.institutionThe University of St Andrewsen_US


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