<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Nicholas P. Webb</dc:contributor>
  <dc:contributor>Adrian Chappell</dc:contributor>
  <dc:contributor>Michael L. Kaplan</dc:contributor>
  <dc:contributor>Travis W. Nauman</dc:contributor>
  <dc:contributor>Gayle Loren Tyree</dc:contributor>
  <dc:contributor>Michael C. Duniway</dc:contributor>
  <dc:contributor>Brandon L. Edwards</dc:contributor>
  <dc:contributor>Sandra L. LeGrand</dc:contributor>
  <dc:contributor>Theodore W. Letcher</dc:contributor>
  <dc:contributor>S. McKenzie Skiles</dc:contributor>
  <dc:contributor>Patrick Naple</dc:contributor>
  <dc:contributor>Nathaniel W. Chaney</dc:contributor>
  <dc:contributor>Jiaxuan Cai</dc:contributor>
  <dc:creator>Saroj Dhital</dc:creator>
  <dc:date>2024</dc:date>
  <dc:description>&lt;p&gt;&lt;span&gt;Dust transported from rangelands of the Southwestern United States (US) to mountain snowpack in the Upper Colorado River Basin during spring (March-May) forces earlier and faster snowmelt, which creates problems for water resources and agriculture. To better understand the drivers of dust events, we investigated large-scale meteorology responsible for organizing two Southwest US dust events from two different dominant geographic locations: (a) the Colorado Plateau and (b) the northern Chihuahuan Desert. High-resolution Weather Research and Forecasting coupled with Chemistry model (WRF-Chem) simulations with the Air Force Weather Agency dust emission scheme incorporating a MODIS albedo-based drag-partition was used to explore land surface-atmosphere interactions driving two dust events. We identified commonalities in their meteorological setups. The meteorological analyses revealed that Polar and Sub-tropical jet stream interaction was a common upper-level meteorological feature before each of the two dust events. When the two jet streams merged, a strong northeast-directed pressure gradient upstream and over the source areas resulted in strong near-surface winds, which lifted available dust into the atmosphere. Concurrently, a strong mid-tropospheric flow developed over the dust source areas, which transported dust to the San Juan Mountains and southern Colorado snowpack. The WRF-Chem simulations reproduced both dust events, indicating that the simulations represented the dust sources that contributed to dust-on-snow events reasonably well. The representativeness of the simulated dust emission and transport in different geographic and meteorological conditions with our use of albedo-based drag partition provides a basis for additional dust-on-snow simulations to assess the hydrologic impact in the Southwest US.&lt;/span&gt;&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1029/2023JD040650</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Geophysical Union</dc:publisher>
  <dc:title>Synoptic analysis and WRF-Chem model simulation of dust events in the southwestern United States</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>