干旱区生态环境知识资源中心(Arid): Dust-drought interactions over the last 15,000 years: A network of lake sediment records from the San Juan Mountains, Colorado

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DOI	10.1177/0959683619875192
	Dust-drought interactions over the last 15,000 years: A network of lake sediment records from the San Juan Mountains, Colorado
	Arcusa, Stephanie H.; McKay, Nicholas P.; Routson, Cody C.; Munoz, Samuel E.
通讯作者	Arcusa, SH (corresponding author), No Arizona Univ, Sch Earth & Sustainabil, POB 4099, Flagstaff, AZ 86011 USA.
来源期刊	HOLOCENE
ISSN	0959-6836
EISSN	1477-0911
出版年	2020
卷号	30 期号:4 页码:559-574
英文摘要	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 similar to 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.
英文关键词	Colorado Plateau drought dust Holocene land disturbance mixing model paleoclimate southwest
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000491949000001
WOS关键词	WESTERN UNITED-STATES ; AEOLIAN DUST ; ROCKY-MOUNTAINS ; HOLOCENE RECORD ; TIBETAN PLATEAU ; GLACIAL MAXIMUM ; MINERAL DUST ; EOLIAN DUST ; NEW-MEXICO ; DEEP-SEA
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向	Physical Geography ; Geology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/369273
作者单位	[Arcusa, Stephanie H.; McKay, Nicholas P.; Routson, Cody C.] No Arizona Univ, Sch Earth & Sustainabil, POB 4099, Flagstaff, AZ 86011 USA; [Munoz, Samuel E.] Northeastern Univ, Marine Sci Ctr, Dept Marine & Environm Sci, Boston, MA 02115 USA; [Munoz, Samuel E.] Northeastern Univ, Dept Civil & Environm Engn, Boston, MA 02115 USA
推荐引用方式 GB/T 7714	Arcusa, Stephanie H.,McKay, Nicholas P.,Routson, Cody C.,et al. Dust-drought interactions over the last 15,000 years: A network of lake sediment records from the San Juan Mountains, Colorado[J],2020,30(4):559-574.
APA	Arcusa, Stephanie H.,McKay, Nicholas P.,Routson, Cody C.,&Munoz, Samuel E..(2020).Dust-drought interactions over the last 15,000 years: A network of lake sediment records from the San Juan Mountains, Colorado.HOLOCENE,30(4),559-574.
MLA	Arcusa, Stephanie H.,et al."Dust-drought interactions over the last 15,000 years: A network of lake sediment records from the San Juan Mountains, Colorado".HOLOCENE 30.4(2020):559-574.