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Department of Energy Office of Science Biological and Environmental Research 1 CESD Overview Objective Study the impacts of dust on the North American summer monsoon system Approach WRF-Chem is used to conduct numerical experiments over 15 years using the MADE/SORGAM aerosol scheme coupled with the GOCART dust emission scheme Simulations performed for April- September 1995-2009 at 36 km horizontal resolution with and without dust Impact Simulated dust concentration and AOD compared well with observations Dust from the U.S. Southwest deserts induces surface cooling of 1 W m -2 and atmospheric heating of 0.4 W m -2 Dust heating of 0.3 K day -1 in the lower atmosphere strengthens the Desert Dust Impact on the Summer Monsoon System over Southwestern North America Zhao C, X Liu, and LR Leung. 2012. “ Impact of the Desert Dust on the Summer Monsoon System O ver Southwestern North America ,” Atmospheric Chemistry and Physics, 12, 3717-3731, DOI:10.5194/acp-12-3717-2012. Dust induced diabatic heating over the desert (contours) and precipitation changes over Texas and New Mexico. Dust induced change of zonal and meridional moisture fluxes in the monsoon system.

Objective Study the impacts of dust on the North American summer monsoon system Approach

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Page 1: Objective Study the impacts of dust on the North American summer monsoon system Approach

Department of Energy • Office of Science • Biological and Environmental Research1 CESD Overview

Objective● Study the impacts of dust on the North

American summer monsoon system

Approach● WRF-Chem is used to conduct numerical

experiments over 15 years using the MADE/SORGAM aerosol scheme coupled with the GOCART dust emission scheme

● Simulations performed for April-September 1995-2009 at 36 km horizontal resolution with and without dust

Impact● Simulated dust concentration and AOD

compared well with observations● Dust from the U.S. Southwest deserts

induces surface cooling of 1 W m-2 and atmospheric heating of 0.4 W m-2

● Dust heating of 0.3 K day-1 in the lower atmosphere strengthens the low-level meridional winds, leading to a 10-40% increase in the NAM precipitation

Desert Dust Impact on the Summer Monsoon System over Southwestern North America

Zhao C, X Liu, and LR Leung. 2012. “Impact of the Desert Dust on the Summer Monsoon System Over Southwestern North America,” Atmospheric Chemistry and Physics, 12, 3717-3731, DOI:10.5194/acp-12-3717-2012.

Dust induced diabatic heating over the desert (contours) and precipitation changes over Texas and New Mexico.

Dust induced change of zonal and meridional moisture fluxes in the monsoon system.