Synoptic analysis and simulation of an unusual dust event over the Atacama Desert

Abstract An unusual dust event over the Atacama Desert occurred in July 2016. Here, a synoptic study of the event is carried out using the NCEP FNL analysis data and WRF‐chem simulations. The “zonalization” of a mid‐tropospheric trough leads to the formation of a horizontal convergence band over the...

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Main Authors: Mark Reyers, Mehdi Hamidi, Yaping Shao
Format: Article
Language:English
Published: Wiley 2019-06-01
Series:Atmospheric Science Letters
Subjects:
Online Access:https://doi.org/10.1002/asl.899
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author Mark Reyers
Mehdi Hamidi
Yaping Shao
author_facet Mark Reyers
Mehdi Hamidi
Yaping Shao
author_sort Mark Reyers
collection DOAJ
description Abstract An unusual dust event over the Atacama Desert occurred in July 2016. Here, a synoptic study of the event is carried out using the NCEP FNL analysis data and WRF‐chem simulations. The “zonalization” of a mid‐tropospheric trough leads to the formation of a horizontal convergence band over the Northern Atacama and thus downward wind below it. As the descending air masses warm adiabatically, strong temperature contrasts to the colder air over the western Andes occur and intensify the down‐valley winds, thus leading to extraordinary strong easterly winds in the Atacama. Simulations with WRF‐chem indicate that these surface winds are sufficient for large‐scale dust emission, and simulated dust plumes traveling far over the eastern South Pacific agree well with the observations. As the integrated dust load is comparable with the load observed in major dust sources of the world, our findings highlight the importance of such unusual events.
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spelling doaj.art-a276e64c53984326a7ff79980480a0582022-12-21T23:25:35ZengWileyAtmospheric Science Letters1530-261X2019-06-01206n/an/a10.1002/asl.899Synoptic analysis and simulation of an unusual dust event over the Atacama DesertMark Reyers0Mehdi Hamidi1Yaping Shao2Institute for Geophysics and Meteorology University of Cologne Cologne GermanyFaculty of Civil Engineering Babol Noshirvani University of Technology Babol IranInstitute for Geophysics and Meteorology University of Cologne Cologne GermanyAbstract An unusual dust event over the Atacama Desert occurred in July 2016. Here, a synoptic study of the event is carried out using the NCEP FNL analysis data and WRF‐chem simulations. The “zonalization” of a mid‐tropospheric trough leads to the formation of a horizontal convergence band over the Northern Atacama and thus downward wind below it. As the descending air masses warm adiabatically, strong temperature contrasts to the colder air over the western Andes occur and intensify the down‐valley winds, thus leading to extraordinary strong easterly winds in the Atacama. Simulations with WRF‐chem indicate that these surface winds are sufficient for large‐scale dust emission, and simulated dust plumes traveling far over the eastern South Pacific agree well with the observations. As the integrated dust load is comparable with the load observed in major dust sources of the world, our findings highlight the importance of such unusual events.https://doi.org/10.1002/asl.899analysisAtacama Desertdust eventdynamic/processessimulationwind
spellingShingle Mark Reyers
Mehdi Hamidi
Yaping Shao
Synoptic analysis and simulation of an unusual dust event over the Atacama Desert
Atmospheric Science Letters
analysis
Atacama Desert
dust event
dynamic/processes
simulation
wind
title Synoptic analysis and simulation of an unusual dust event over the Atacama Desert
title_full Synoptic analysis and simulation of an unusual dust event over the Atacama Desert
title_fullStr Synoptic analysis and simulation of an unusual dust event over the Atacama Desert
title_full_unstemmed Synoptic analysis and simulation of an unusual dust event over the Atacama Desert
title_short Synoptic analysis and simulation of an unusual dust event over the Atacama Desert
title_sort synoptic analysis and simulation of an unusual dust event over the atacama desert
topic analysis
Atacama Desert
dust event
dynamic/processes
simulation
wind
url https://doi.org/10.1002/asl.899
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