Dust-drought interactions over the last 15,000 years

A network of lake sediment records from the San Juan Mountains, Colorado

Bibliographic Data

ID12268245
AuthorsStéphanie Arcusa (0000-0003-0694-9623, Northern Arizona University, corresponding author), Nicholas P Mckay (0000-0003-3598-5113, Northern Arizona University), Cody Routson (0000-0001-8694-7809, Northern Arizona University), Cody C Routson (Northern Arizona University), Samuel E Munoz (0000-0002-0994-0483, Northeastern University)
Year2019
Volume30
Issue4
Pages559-574
Publication date2019-09-18
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683619875192
OpenAlexW2974690912
LanguageEN
Citations received2
References cited106

Millions of people in the arid Southwest United States rely on snow-fed Colorado River water. Dust deposition on snow accelerates snowmelt, posing a challenge for water managers who also need to grapple with increased likelihood of drought due to climate change. Dust production is thought to increase during drought, but the impact of drought on dust deposition is unclear. To answer this question, total dust mass accumulation rate (DMAR) reconstructions were developed from sediment cores from three lakes in the San Juan Mountains, Colorado, spanning the last ~15,000 years. Monte-Carlo end-member analysis of particle size and elemental composition, which incorporates measurement and model uncertainties, was combined with age uncertainty to estimate DMAR for each lake. We also synthesize the records providing the first Holocene DMAR reconstruction for the region. The records show little relation between periods of frequent and severe drought (e.g. during medieval megadroughts) and periods of higher DMAR, although there is considerable uncertainty at short timescales. We find instead that sediment availability, modulated by natural or human-mediated geomorphic processes that generate sediment, and transport mechanisms are the key drivers. DMAR was highest during the Late Glacial-Interglacial Transition (LGIT, 15–11 kyr BP) and in the last 250 years, periods when sediment availability was enhanced. DMAR increased by 60% (16–85% 75% highest density region range) compared with the late-Holocene baseline starting in the 1770s and peaking in the 1840s, associated with the intensification of human activities. Human-induced dustiness also represents the highest interval of dust deposition in the last 11,000 years. Our results demonstrate that although the Colorado Plateau is naturally prone to dustiness, drought is a secondary driver of dust accumulation in the mountains. This suggests that land-use management decisions aimed at reducing land disturbance can mitigate future dust accumulation, despite projected increases in regional aridity

Arid · Climate change · Deposition (geology · Geography · Geomorphology · Holocene · Hydrology (agriculture · Physical geography · Range (aeronautics · Sediment · Snow · Snowmelt · Aeolian processes and effects · Environmental Science · Geology and Paleoclimatology Research · Soil erosion and sediment transport · Geology · Oceanography · Paleontology

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