4.3 Review

An Overview of Mineral Dust Modeling over East Asia

Journal

JOURNAL OF METEOROLOGICAL RESEARCH
Volume 31, Issue 4, Pages 633-653

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s13351-017-6142-2

Keywords

East Asia; dust aerosol; dust modeling; dust emissions; long-range dust transport; dust radiative forcing

Funding

  1. National Natural Science Foundation of China [41405003, 41521004]
  2. Office of Science, U.S. Department of Energy (DOE)
  3. DOE by Battelle Memorial Institute [DE-AC05-76RL01830]

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East Asian dust (EAD) exerts considerable impacts on the energy balance and climate/climate change of the earth system through its influence on solar and terrestrial radiation, cloud properties, and precipitation efficiency. Providing an accurate description of the life cycle and climate effects of EAD is therefore critical to better understanding of climate change and socioeconomic development in East Asia and even worldwide. Dust modeling has undergone substantial development since the late 1990s, associated with improved understanding of the role of EAD in the earth system. Here, we review the achievements and progress made in recent decades in terms of dust modeling research, including dust emissions, long-range transport, radiative forcing (RF), and climate effects of dust particles over East Asia. Numerous efforts in dust/EAD modeling have been directed towards furnishing more sophisticated physical and chemical processes into the models on higher spatial resolutions. Meanwhile, more systematic observations and more advanced retrieval methods for instruments that address EAD related science issues have made it possible to evaluate model results and quantify the role of EAD in the earth system, and to further reduce the uncertainties in EAD simulations. Though much progress has been made, large discrepancies and knowledge gaps still exist among EAD simulations. The deficiencies and limitations that pertain to the performance of the EAD simulations referred to in the present study are also discussed.

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