Evaluation of aerosol mixing state classes in the GISS modelE-MATRIX climate model using single-particle mass spectrometry measurements

被引:45
作者
Bauer, Susanne E. [1 ]
Ault, Andrew P. [2 ]
Prather, Kimberly A. [2 ,3 ]
机构
[1] Columbia Univ, Ctr Climate Syst Res, Earth Inst, New York, NY 10025 USA
[2] NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[3] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
关键词
mixing state; GENERAL-CIRCULATION MODEL; LOS-ANGELES; SIZE DISTRIBUTIONS; PARTICULATE MATTER; SULFATE AEROSOLS; EVENTS; CHEMISTRY; VARIABILITY; NUCLEATION; TRANSPORT;
D O I
10.1002/jgrd.50700
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Aerosol particles in the atmosphere are composed of multiple chemical species. The aerosol mixing state, which describes how chemical species are mixed at the single-particle level, provides critical information on microphysical characteristics that determine the interaction of aerosols with the climate system. The evaluation of mixing state has become the next challenge. This study uses aerosol time-of-flight mass spectrometry (ATOFMS) data and compares the results to those of the Goddard Institute for Space Studies modelE-MATRIX (Multiconfiguration Aerosol TRacker of mIXing state) model, a global climate model that includes a detailed aerosol microphysical scheme. We use data from field campaigns that examine a variety of air mass regimens (urban, rural, and maritime). At all locations, polluted areas in California (Riverside, La Jolla, and Long Beach), a remote location in the Sierra Nevada Mountains (Sugar Pine) and observations from Jeju (South Korea), the majority of aerosol species are internally mixed. Coarse aerosol particles, those above 1 mu m, are typically aged, such as coated dust or reacted sea-salt particles. Particles below 1 mu m contain large fractions of organic material, internally mixed with sulfate and black carbon, and few external mixtures. We conclude that observations taken over multiple weeks characterize typical air mass types at a given location well; however, due to the instrumentation, we could not evaluate mass budgets. These results represent the first detailed comparison of single-particle mixing states in a global climate model with real-time single-particle mass spectrometry data, an important step in improving the representation of mixing state in global climate models.
引用
收藏
页码:9834 / 9844
页数:11
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