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dc.contributor.authorThomson, Marcus J
dc.contributor.authorMacdonald, Glen M
dc.identifier.citationThomson , M J & Macdonald , G M 2020 , ' Climate and growing season variability impacted the intensity and distribution of Fremont maize farmers during and after the Medieval Climate Anomaly based on a statistically downscaled climate model ' , Environmental Research Letters , vol. 15 , no. 10 , 105002 .
dc.identifier.otherPURE: 270724596
dc.identifier.otherPURE UUID: 38fc9cd3-ce62-4b89-96e9-a3f3156c76ce
dc.identifier.othercrossref: 10.1088/1748-9326/aba57e
dc.identifier.otherWOS: 000574297000001
dc.identifier.otherScopus: 85092661004
dc.descriptionFunding for MJT was provided by the Department of Geography, UCLA, and the Department of Interior Southwest Climate Science Center, the Institute of the Environment and Sustainability (IoES) at UCLA, and fellowships from the John Muir Memorial fund. Part of this research was conducted during a Mikhelavich Award fellowship at the International Institute for Applied Systems Analysis (IIASA), in Laxenburg, Austria. GMM was partly supported by a University of St Andrews Global Fellowship.en
dc.description.abstractThe rise and decline of many complex, pre-European maize-farming cultures in the American Southwest coincides with the warm, climatically quiescent Medieval Climate Anomaly (MCA, ca. 850–1350 CE) and transition to the cool, hydrologically variable Little Ice Age (LIA, ca. 1350–1850 CE). The effects of drought on early subsistence agriculture in the Southwest is well studied, but the impact of temperature stress and variability on the growth of maize crops and which areas were most resilient to such stress remain open questions. We statistically downscaled outputs from a paleo-climate model experiment (CESM1 LME) to map changes to cumulative growing degree days for maize (GDD, 30/10 °C) and precipitation over Utah between 850 and 1449 CE, and downscaled GDD changes to local Fremont Culture archaeological site occupations from radiocarbon-dated contexts mapped as spatially discrete kernel density estimates of summed probability distributions (SPDs). We then analyzed correspondences between Fremont SPDs and GDD/precipitation between 850 and 1449 CE. In general, we found (1) high Fremont occupation intensity coincident with GDD that is less volatile than the long term average, and low occupation intensity coincident with, or following, periods of volatile GDD; (2) intensified occupation of high-elevation sites during the MCA, followed by a retreat to lower elevation sites coincident with a sudden rise in annual temperature volatility and increasing drought conditions; and (3) these occupation changes occurred in spite of the greater temperatures and variability in GDD at low-elevation sites. We found evidence that increased inter-annual variability of growing seasons prior to the onset of the LIA, was likely a determinant of Fremont subsistence strategy decision making, and high-elevation site occupation. The most resilient Fremont occupations in the face of these challenges were sited where growing season lengths were least variable.
dc.relation.ispartofEnvironmental Research Lettersen
dc.rightsCopyright © 2020 The Author(s). Published by IOP Publishing Ltd. Original content from this work may be used under the terms of the Creative Commons Attribution 3.0 license. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.en
dc.subjectZea maysen
dc.subjectGrowing degree daysen
dc.subjectTemperature variabilityen
dc.subjectGE Environmental Sciencesen
dc.subjectSDG 13 - Climate Actionen
dc.titleClimate and growing season variability impacted the intensity and distribution of Fremont maize farmers during and after the Medieval Climate Anomaly based on a statistically downscaled climate modelen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. School of Geography & Sustainable Developmenten
dc.description.statusPeer revieweden

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