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The influence of large-scale climate patterns on sediment loss from agricultural land—exploration using an instrumented field and catchment scale platform

Bibliographic Data

ID15545780
AuthorsS J Granger (0000-0003-0183-0244, Rothamsted Research, corresponding author), Hari Ram Upadhayay (0000-0002-4851-4268, Rothamsted Research), Bruno Castelle (0000-0003-1740-7395, Environnements et Paléoenvironnements Océaniques et Continentaux), Ann L Collins (0000-0001-8790-8473, Rothamsted Research)
Year2025
Volume20
Issue4
Pages044023-044023
Publication date2025-03-06
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/adbd55
OpenAlexW4408177854
LanguageEN
References cited34

Accelerated soil erosion and sediment delivery are threats to water quality. In Western Europe, weather patterns are strongly influenced by large scale climate systems such as the North Atlantic Oscillation (NAOi). Recently, however, a new climate index has been developed, called the West Europe Pressure Anomaly (WEPAi), which may be more relevant for weather in North Western Europe. Recent attempts have tried to link variability in weather patterns as described by hydro-climatic indices and amplifications in the degradation of water quality. However, to our knowledge, no previous work has been undertaken on investigating their effects on suspended sediment concentrations (SSCs). A study was conducted in southwest England using long-term meteorological, monthly NAOi and WEPAi, and 15 min discharge and turbidity datasets collected from an instrumented field and catchment scale monitoring platform. Monthly winter precipitation totals, and air temperature were both found to be significantly positively related to NAOi, but not in the summer. Both variables were significant and more strongly related with the WEPAi for both seasons. Flow weighted mean SSCs calculated for both seasons over a 4 year period were compared to monthly NAOi and WEPAi. In winter months, no significant relationships were found at any scale for NAOi. However, significant positive relationships with the WEPAi were present regardless of catchment size. In the summer months there were no significant relationships with either climate indices. Large-scale climate drivers are important in the sediment responses of agricultural landscapes. An ability to forecast monthly climate scale drivers could enable farmers to better plan for those periods when hydro-sedimentological responses are likely to be elevated. More work is needed across a range of landscape typologies to confirm that the relationships observed hold true more widely

Agricultural land · Agriculture · Cartography · Drainage basin · Environmental resource management · Field (mathematics · Geography · Geomorphology · Geotechnical engineering · Hydrology (agriculture · Land use · Physical geography · Scale (ratio · Sediment · Environmental Science · Hydrology and Sediment Transport Processes · Hydrology and Watershed Management Studies · Soil erosion and sediment transport · Ecology · Geology

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