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dc.contributor.authorSchneidhofer, Petra
dc.contributor.authorTonning, Christer
dc.contributor.authorCannell, Rebecca J S
dc.contributor.authorNau, Erich
dc.contributor.authorHinterleitner, Alois
dc.contributor.authorVerhoeven, Geert J
dc.contributor.authorGustavsen, Lars
dc.contributor.authorPaasche, Knut
dc.contributor.authorNeubauer, Wolfgang
dc.contributor.authorGansum, Terje
dc.date.accessioned2024-04-02T11:03:50Z
dc.date.available2024-04-02T11:03:50Z
dc.date.created2024-02-07T11:37:15Z
dc.date.issued2023
dc.identifier.isbn978-3-928794-83-1
dc.identifier.urihttps://hdl.handle.net/11250/3124440
dc.description.abstractSoil moisture variation is complex and depends on a range of factors, which complicates the formulation of recommendations for GPR surveys. Low amounts of soil moisture produced GPR data of higher quality. However, precipitation rates as well as chronological sequence of precipitation/thawing processes and the GPR survey are of importance. Winter months can offer favorable conditions for GPR surveys if temperatures remain negative over a prolonged time period, allowing for frost to build in the ground. Results of the Borre Monitoring Project (BMP) are valid only for sites with similar settings as Borre; the monitoring approach, however, can be transferred to larger regions with more representative sites.en_US
dc.language.isoengen_US
dc.relation.ispartofAdvances in On- and Offshore Archaeological Prospection: Proceedings of the 15th International Conference on Archaeological Prospection
dc.titleHow much rain is too much for a GPR survey? Results of the Borre Monitoring Projecten_US
dc.title.alternativeHow much rain is too much for a GPR survey? Results of the Borre Monitoring Projecten_US
dc.typeChapteren_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber377-382en_US
dc.identifier.cristin2243996
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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