Arid
DOI10.1016/j.atmosenv.2016.06.076
Increasing aeolian dust deposition to snowpacks in the Rocky Mountains inferred from snowpack, wet deposition, and aerosol chemistry
Clow, David W.1; Williams, Mark W.2; Schuster, Paul F.3
通讯作者Clow, David W.
来源期刊ATMOSPHERIC ENVIRONMENT
ISSN1352-2310
EISSN1873-2844
出版年2016
卷号146页码:183-194
英文摘要

Mountain snowpacks are a vital natural resource for similar to 1.5 billion people in the northern Hemisphere, helping to meet human and ecological demand for water in excess of that provided by summer rain. Springtime warming and aeolian dust deposition accelerate snowmelt, increasing the risk of water shortages during late summer, when demand is greatest. While climate networks provide data that can be used to evaluate the effect of warming on snowpack resources, there are no established regional networks for monitoring aeolian dust deposition to snow. In this study, we test the hypothesis that chemistry of snow, wet deposition, and aerosols can be used as a surrogate for dust deposition to snow. We then analyze spatial patterns and temporal trends in inferred springtime dust deposition to snow across the Rocky Mountains, USA, for 1993-2014. Geochemical evidence, including strong correlations (r(2) >= 0.94) between Ca2+, alkalinity, and dust concentrations in snow deposited during dust events, indicate that carbonate minerals in dust impart a strong chemical signature that can be used to track dust deposition to snow. Spatial patterns in chemistry of snow, wet deposition, and aerosols indicate that dust deposition increases from north to south in the Rocky Mountains, and temporal trends indicate that winter/spring dust deposition increased by 81% in the southern Rockies during 1993-2014. Using a multivariate modeling approach, we determined that increases in dust deposition and decreases in springtime snowfall combined to accelerate snowmelt timing in the southern Rockies by approximately 7-18 days between 1993 and 2014. Previous studies have shown that aeolian dust emissions may have doubled globally during the 20th century, possibly due to drought and land-use change. Climate projections for increased aridity in the southwestern U.S., northern Africa, and other mid-latitude regions of the northern Hemisphere suggest that aeolian dust emissions may continue to increase, compounding the risk that climate warming poses to snowpack water resources in arid/semi-arid regions of the world. Published by Elsevier Ltd.


英文关键词Aeolian Carbonate Dust Snow Trends Snowmelt
类型Article ; Proceedings Paper
语种英语
国家USA
收录类别SCI-E ; CPCI-S
WOS记录号WOS:000388051700017
WOS关键词BIOLOGICAL SOIL CRUSTS ; SAHARAN DUST ; ATMOSPHERIC DEPOSITION ; WIND EROSION ; CLIMATE ; DESERT ; COLORADO ; IMPACTS ; TRENDS ; SOLUTES
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
来源机构United States Geological Survey
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/191621
作者单位1.US Geol Survey, Colorado Water Sci Ctr, Denver Fed Ctr, MS 415, Denver, CO 80225 USA;
2.Univ Colorado, Dept Geog, UCB 360, Boulder, CO 80309 USA;
3.US Geol Survey, Natl Res Program, 3215 Marine St, Boulder, CO 80303 USA
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Clow, David W.,Williams, Mark W.,Schuster, Paul F.. Increasing aeolian dust deposition to snowpacks in the Rocky Mountains inferred from snowpack, wet deposition, and aerosol chemistry[J]. United States Geological Survey,2016,146:183-194.
APA Clow, David W.,Williams, Mark W.,&Schuster, Paul F..(2016).Increasing aeolian dust deposition to snowpacks in the Rocky Mountains inferred from snowpack, wet deposition, and aerosol chemistry.ATMOSPHERIC ENVIRONMENT,146,183-194.
MLA Clow, David W.,et al."Increasing aeolian dust deposition to snowpacks in the Rocky Mountains inferred from snowpack, wet deposition, and aerosol chemistry".ATMOSPHERIC ENVIRONMENT 146(2016):183-194.
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