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dc.contributor.authorJones, RT
dc.contributor.authorReinhardt, LJ
dc.contributor.authorDearing, JA
dc.contributor.authorCrook, D
dc.contributor.authorChiverrell, RC
dc.contributor.authorWelsh, KE
dc.contributor.authorVergès, E
dc.date.accessioned2018-02-13T16:39:50Z
dc.date.issued2013-06-10
dc.description.abstractHistorical and documentary records from the Petit Lac d'Annecy, indicate that human activities have been the dominant 'geomorphic process' shaping the catchment during the late Holocene, with deforestation, agriculture and artificial drainage profoundly affecting both the pace and spatial distribution of soil erosion. The impact of past climatic change on the evolution of the catchment is less certain because of the lack of long-term climate records for the site. Previous attempts to use the sediment record from the lake to investigate the role past climate change may have played were hampered by the difficulty in isolating and disentangling the climatic signal preserved within the archive, because of overp rinting of human activity. This is a common problem in regions with a long history of human activity in the landscape. In this study we use a range of novel statistical techniques (including cross-correlation and cross spectral analysis) to assess the relative importance of climate in driving landscape dynamics. The statistical analysis is carried out on an updated high-resolution palaeo-environmental data set from the Petit Lac d'Annecy. The results of the statistical analysis indicate that regional climate phenomena such as the Atlantic multidecadal oscillation are partly responsible for landscape dynamics at Petit Lac d'Annecy throughout the late Holocene. We find that the Petit Lac d'Annecy catchment typically requires decades, or longer, to respond to changes in precipitation, reflecting the stochastic nature of river sediment storage and transport. The use of a 4 yr integrated lake core record effectively attenuates the 'signal shredding' effect of shorter-term internally generated sediment transport processes. Nonetheless, the lake record of climatically induced geormorphic process-responses is weak compared with the pervasive impact of human activities. © The Author(s) 2013.en_GB
dc.description.sponsorshipThis project was funded by the Leverhulme Trust (Grant No F/25/BQ). The reconstructed water-table record for Northern England Peatlands was accessed through the NOAA website (Charman and Hendon, 1999).en_GB
dc.identifier.citationVol. 23 (9), pp. 1329 - 1339en_GB
dc.identifier.doihttps://doi:10.1177/0959683613486940
dc.identifier.grantnumberF/25/BQen_GB
dc.identifier.urihttp://hdl.handle.net/10871/31469
dc.language.isoenen_GB
dc.publisherSAGE Publicationsen_GB
dc.rights© The Author(s) 2013en_GB
dc.titleDetecting climatic signals in an anthropogenically disturbed catchment: The late-Holocene record from the Petit Lac d'Annecy, French Alpsen_GB
dc.typeArticleen_GB
dc.date.available2018-02-13T16:39:50Z
dc.identifier.issn0959-6836
dc.descriptionThis is the author pre-print. The final version is available from SAGE Publications via the DOI in this record.en_GB
dc.identifier.journalHoloceneen_GB


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