A comparison of similar aerosol measurements made on the NASA P3-B, DC-8, and NSFC-130 aircraft during TRACE-P and ACE-Asia

被引:19
|
作者
Moore, KG
Clarke, AD
Kapustin, VN
McNaughton, C
Anderson, BE
Winstead, EL
Weber, R
Ma, Y
Lee, YN
Talbot, R
Dibb, J
Anderson, T
Doherty, S
Covert, D
Rogers, D
机构
[1] Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Honolulu, HI 96822 USA
[2] NASA, Chem & Dynam Branch, Div Atmospher Sci, Langley Res Ctr, Hampton, VA 23681 USA
[3] NASA, GATS Inc, Langley Res Ctr, Hampton, VA 23681 USA
[4] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA
[5] Brookhaven Natl Lab, Dept Environm Sci, Upton, NY 11973 USA
[6] Univ New Hampshire, Inst Study Earth Oceans & Space, Durham, NH 03824 USA
[7] Univ Washington, Dept Atmospher Sci, Seattle, WA 98195 USA
[8] Natl Ctr Atmospher Res, RAF, Broomfield, CO 80021 USA
关键词
aerosols; special field campaigns; instrument comparison;
D O I
10.1029/2003JD003543
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Two major aircraft experiments occurred off the Pacific coast of Asia during spring 2001: the NASA sponsored Transport and Chemical Evolution over the Pacific (TRACE-P) and the National Science Foundation (NSF) sponsored Aerosol Characterization Experiment-Asia (ACE-Asia). Both experiments studied emissions from the Asian continent (biomass burning, urban/industrial pollution, and dust). TRACE-P focused on trace gases and aerosol during March/April and was based primarily in Hong Kong and Yokota Air Force Base, Japan, and involved two aircraft: the NASA DC-8 and the NASA P3-B. ACE-Asia focused on aerosol and radiation during April/May and was based in Iwakuni Marine Corps Air Station, Japan, and involved the NSF C-130. This paper compares aerosol measurements from these aircraft including aerosol concentrations, size distributions (and integral properties), chemistry, and optical properties. Best overall agreement (generally within RMS instrumental uncertainty) was for physical properties of the submircron aerosol, including condensation nuclei concentrations, scattering coefficients, and differential mobility analyzer and optical particle counter (OPC) accumulation mode size distributions. Larger differences (typically outside of the RMS uncertainty) were often observed for parameters related to the supermicron aerosols (total scattering and absorption coefficients, coarse mode Forward Scattering Spectrometer Probe and OPC size distributions/integral properties, and soluble chemical species usually associated with the largest particles, e.g., Na+, Cl-, Ca2+, and Mg2+), where aircraft sampling is more demanding. Some of the observed differences reflect different inlets ( e. g., low-turbulence inlet enhancement of coarse mode aerosol), differences in sampling lines, and instrument configuration and design. Means and variances of comparable measurements for horizontal legs were calculated, and regression analyses were performed for each platform and allow for an assessment of instrument performance. These results provide a basis for integrating aerosol data from these aircraft platforms for both the TRACE-P and ACE-Asia experiments.
引用
收藏
页码:D15S151 / 35
页数:35
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