期刊
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
卷 107, 期 D24, 页码 -出版社
AMER GEOPHYSICAL UNION
DOI: 10.1029/2002JD002204
关键词
dust; Asia; North America; aerosol; troposphere
[1] Using an elemental signature for Asian dust derived from events in April 1998, we probed a long-term set of routine aerosol samples to develop the first empirical assessment of the frequency and intensity of dust transport from Asia to midlatitude North America. Our data reveal a pattern of consistent, frequent transport that contradicts the episodic characterization derived from short-term studies and anecdotal reports. We find that fine (<2.5 mu m) Asian dust is a regular component of the troposphere over the eastern Pacific and western North America and is common, at least in spring, across North America. Typical Asian fine dust concentrations (24-hour average) are between 0.2 and 1 mu g/m(3) and only very rarely exceed 5 mu g/m(3). Our data also indicate that Asian dust is concentrated in an altitude zone ranging from about 500 to 3000 m MSL, consistent with isentropic transport processes previously observed in the western Pacific.
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