Item talk:Q301568
From geokb
{
"USGS Publications Warehouse": {
"@context": "https://schema.org",
"@type": "Article",
"additionalType": "Journal Article",
"name": "'Dust in the wind\u2019 from source-to-sink: Analysis of the 14-15 April 2015 storm in Utah",
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"propertyID": "USGS Publications Warehouse IndexID",
"value": "70211989",
"url": "https://pubs.usgs.gov/publication/70211989"
},
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"@type": "PropertyValue",
"propertyID": "USGS Publications Warehouse Internal ID",
"value": 70211989
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"propertyID": "DOI",
"value": "10.1016/j.aeolia.2019.06.002",
"url": "https://doi.org/10.1016/j.aeolia.2019.06.002"
}
],
"journal": {
"@type": "Periodical",
"name": "Aeolian Research",
"volumeNumber": "46",
"issueNumber": null
},
"inLanguage": "en",
"isPartOf": [
{
"@type": "CreativeWorkSeries",
"name": "Aeolian Research"
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"datePublished": "2020",
"dateModified": "2020-08-13",
"abstract": "On 14\u201315 April 2015, an intense intermountain cyclone in the western USA caused high winds and a dust storm that degraded air quality in the eastern Great Basin, and deposited dust-on-snow (DOS) in the Wasatch Range near Salt Lake City, Utah. We analyzed the storm and documented its \u201csource-to-sink\u201d development to relate the frontal passage with dust mobilization, air quality changes, and dust deposition on montane snowpack near Alta, Utah. This case study is first to track a dust storm and measure the elemental composition and radiative properties of the resulting DOS as a single specific event layer in Wasatch montane snowpack; prior studies have assessed seasonally aggregated DOS deposits. Dust plumes on MODIS imagery indicate mobilization from known regional \u201chotspots\u201d for aeolian activity, including clay- and silt-rich alluvium, modern playas, and disturbed areas within the Pleistocene Paleolake Bonneville Basin. This 2015 single event dust layer was 1\u20133\u202fcm thick with a median dust size of 10.81\u201312.55\u202f\u00b5m; its measured radiative properties are similar to aggregated dusts previously assessed in Wasatch snowpack. Dust from the 2015 DOS event is enriched in the elements As, Cd, Cu, and Mo by a 10\u00d7 factor relative to average elemental concentrations in the upper continental crust; its heavy metals (Cu, Pb, As, Cd, Mo, Zn) are probably derived from regional mine operations. Tracking elemental fluxes from source-to-sink is important for resolving environmental impacts, and informing future analysis of single storm dust loading, ecosystem impacts, and quantity and quality of meltwater-fed drinking water.",
"description": "100532, 15 p.",
"publisher": {
"@type": "Organization",
"name": "Elsevier"
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"author": [
{
"@type": "Person",
"name": "Nicoll, Kathleen",
"givenName": "Kathleen",
"familyName": "Nicoll"
},
{
"@type": "Person",
"name": "Hahnenberger, Maura",
"givenName": "Maura",
"familyName": "Hahnenberger",
"affiliation": [
{
"@type": "Organization",
"name": "Salt Lake Community College"
}
]
},
{
"@type": "Person",
"name": "Goldstein, Harland L. hgoldstein@usgs.gov",
"givenName": "Harland L.",
"familyName": "Goldstein",
"email": "hgoldstein@usgs.gov",
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"value": "0000-0002-6092-8818",
"url": "https://orcid.org/0000-0002-6092-8818"
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"@type": "Organization",
"name": "Geosciences and Environmental Change Science Center",
"url": "https://www.usgs.gov/centers/geosciences-and-environmental-change-science-center"
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"funder": [
{
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"name": "Geosciences and Environmental Change Science Center",
"url": "https://www.usgs.gov/centers/geosciences-and-environmental-change-science-center"
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"url": "https://geonames.org/4074035"
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