Physical and chemical properties of surface and column aerosols at a rural New England site during MODIS overpass

被引:42
作者
Slater, JF
Dibb, JE
Campbell, JW
Moore, TS
机构
[1] Univ New Hampshire, Inst Study Earth Oceans & Space, Climate Change Res Ctr, Durham, NH 03824 USA
[2] Univ New Hampshire, Dept Earth Sci, Durham, NH 03824 USA
[3] Univ New Hampshire, Inst Study Earth Oceans & Space, Ocean Proc Anal Lab, Durham, NH 03824 USA
基金
美国国家航空航天局; 美国海洋和大气管理局;
关键词
MODIS; chemical composition of aerosols; aerosol optical depth comparison; fine particle mass concentration;
D O I
10.1016/j.rse.2004.05.011
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Surface-based measurements of aerosol optical depth at a rural site in southern New Hampshire (43.11 degreesN, 70.95 degreesW) are compared to retrievals of the same parameter by the Moderate Resolution Imaging Spectrometer (MODIS) during April-August, 2001. Hourly averages of aerosol optical depth (AOD) were derived using a multi-filter rotating shadowband radiometer (MFRSR) at the time of NASA's Terra satellite overpass. The MODIS Level 2 aerosol product at a wavelength of 550 nm was directly compared to the MFRSR interpolated AOD at 550 nm. We were able to compare the two AOD measurement platforms on 46 days (out of a possible 128 days) and observed a good agreement between the two methods (R = 0.81; slope 0.95 +/- 0.10). However, there were I I days during this study period when MODIS measured AOD at the site, but the MFRSR did not due to excessive cloud cover. There were also 7 days when clear skies prevailed at the site during the time of MODIS overpass, but there was no AOD retrieved by MODIS. Surface measurements of fine particle (PM2.5) mass, chemical composition, and optical properties were also performed during summer 2001. A good correlation (R = 0.87) between fine particle mass and AOD measured by the MFRSR was observed. A comparison between fine particle light extinction at the surface and MFRSR AOD (at the same wavelength) also showed good agreement (R = 0.80). Aerosol chemical analysis revealed that ammonium sulfate was the main aerosol component during times of very high turbidity, while organic carbon dominated during times of below-average turbidity. (C) 2004 Elsevier Inc. All rights reserved.
引用
收藏
页码:173 / 180
页数:8
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