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Thirty-six borehole temperature–depth profiles were analysed to\udreconstruct the ground surface temperature history (GSTH) of eastern Tasmania\udfor the past 5 centuries. We used the singular value decomposition method\udto invert borehole temperatures to produce temperature histories. The quality\udof borehole data was classified as high or low based on model misfit. The\udquality of the borehole data was not dependent on topography or land use.\udAnalysis reveals that three to five high-quality borehole temperature–depth\udprofiles were adequate to reconstruct robust paleotemperature records from\udany area.\ud  \udAverage GSTH reconstructed from Tasmanian boreholes shows temperature\udincreases about 1.2 ± 0.2 °C during the past 5 centuries.\udReconstructed temperatures were consistent with meteorological records and\udother proxy records from Tasmania during their period of overlap.\udTemperature changes were greatest around the north-east coast and decreased\udtowards the centre of Tasmania. The extension of the East Australian Current (EAC) further south and its strengthening around the north-east coast of Tasmania\udover the past century was considered a prime driver of warmer temperatures\udobserved in north-east Tasmania

Late Holocene temperature variability in Tasmania inferred from borehole temperature data