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Evaluation of Atmospheric Aerosol Optical Depth Products at Ultraviolet Bands Derived from MODIS Products

机译:从MODIS产品获得的紫外线波段大气气溶胶光学深度产品的评估

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Solar ultraviolet (UV) radiation plays a significant role in climate, atmospheric chemical processes, and ecosystem balance. Aerosol optical depth (AOD) at UV wavelengths, the UV-AOD, is an important quantity for studying the extinction of UV radiation in the atmosphere. Ground-based UV-AOD observations, such as those from the AErosol RObotic NETwork (AERONET), are limited in spatial coverage. Current space derived UV-AOD from the Total Ozone Mapping Spectrometer (TOMS) or the Ozone Monitoring Instrument (OMI), on the other hand, are subject to large errors associated with low resolution, cloud contamination, assumed height of aerosol layer, and low sensitivity to aerosols in the lower troposphere. In this study, a new UV-AOD product is derived for the year 2009 by extrapolating the Moderate Resolution Imaging Spectra-radiometer (MODIS) visible bands AOD product (VIS-AOD) to 380 and 340 nm. Results are evaluated against UV-AOD measurements taken at AERONET sites. Over the oceans, four extrapolating methods are investigated by using two to five wavelengths. The best result, which has a correlation coefficient (R) of 0.90 at both wavelengths and root mean square errors (RMSE) of 0.062 and 0.068 at 380 and 340 nm, respectively, is achieved by combining a linear-extrapolation and a second-order polynomial fitting that takes into account the wavelength dependence of the à ngström exponent. Moreover, more than 80% of the data fall within the uncertainty range of ±0.05 ± 0.20τ. Over land, UV-AOD is extrapolated using the à ngström exponent derived from VIS-AODs at 470 and 660 nm, the only two wavelengths available from the MODIS AOD product. Compared with AERONET observations, the correlation coefficient is about 0.90 at both 380 and 340 nm, while the RMSE increases to 0.152 at 380 nm and 0.174 at 340 nm, due to the larger uncertainty of MODIS AOD over land. With the relatively low biases, this UV-AOD product will be valuable for climate and atmospheric chemistry research.Copyright 2012 American Association for Aerosol ResearchView full textDownload full textRelated var addthis_config = { ui_cobrand: "Taylor & Francis Online", services_compact: "citeulike,netvibes,twitter,technorati,delicious,linkedin,facebook,stumbleupon,digg,google,more", pubid: "ra-4dff56cd6bb1830b" }; Add to shortlist Link Permalink http://dx.doi.org/10.1080/02786826.2012.687475
机译:太阳紫外线(UV)在气候,大气化学过程和生态系统平衡中起着重要作用。 UV波长下的气溶胶光学深度(AOD),即UV-AOD,是研究大气中UV辐射消光的重要量。地面UV-AOD观测(例如来自AErosol机器人网络(AERONET)的观测)在空间覆盖范围上有限。另一方面,从总臭氧图谱仪(TOMS)或臭氧监测仪(OMI)提取的当前空间产生的UV-AOD会遇到与低分辨率,云污染,假定的气溶胶层高度和较低的误差有关的较大误差。对对流层下部的气溶胶敏感。在这项研究中,通过将中等分辨率成像光谱辐射仪(MODIS)的可见光波段AOD产品(VIS-AOD)外推到380和340 nm,得出了2009年的新UV-AOD产品。根据在AERONET站点进行的UV-AOD测量评估结果。在海洋上,使用2至5个波长研究了四种外推方法。通过结合线性外推法和二阶方法,可以获得最佳结果,在两个波长下的相关系数(R)均为0.90,在380和340 nm处的均方根误差(RMSE)分别为0.062和0.068。考虑到ngstrÃm指数的波长依赖性的多项式拟合。此外,超过80%的数据落在±0.05±0.20%的不确定性范围内。在陆地上,使用VIS-AOD在470和660 nm处获得的ngstrÃm指数外推UV-AOD,这是MODIS AOD产品仅有的两个波长。与AERONET观测相比,由于MODIS AOD在陆地上的不确定性较大,在380和340 nm处的相关系数均为0.90,而RMSE在380 nm和340 nm处分别提高至0.152和0.174。由于偏差相对较小,因此该UV-AOD产品将对气候和大气化学研究具有重要意义。版权所有2012美国气溶胶研究协会查看全文下载全文相关变量var addthis_config = {ui_cobrand:“泰勒和弗朗西斯在线”,service_compact:“ citeulike, netvibes,推特,technorati,可口,linkedin,facebook,stumbleupon,digg,google,更多”,发布:“ ra-4dff56cd6bb1830b”};添加到候选列表链接永久链接http://dx.doi.org/10.1080/02786826.2012.687475

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  • 来源
    《Aerosol Science and Technology》 |2012年第9期|p.1025-1034|共10页
  • 作者单位
  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-18 00:59:37

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