Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1029/2018JD029558 |
Retrieval of Aerosol Size Distributions From In Situ Particle Counter Measurements: Instrument Counting Efficiency and Comparisons With Satellite Measurements | |
Deshler, Terry1,2; Luo, Beiping3; Kovilakam, Mahesh1,4; Peter, Thomas3; Kalnajs, Lars E.2 | |
2019-05-16 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES |
ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2019 |
卷号 | 124期号:9页码:5058-5087 |
文章类型 | Article |
语种 | 英语 |
国家 | USA; Switzerland |
英文摘要 | The method to derive aerosol size distributions from in situ stratospheric measurements from the University of Wyoming is modified to include an explicit counting efficiency function (CEF) to describe the channel-dependent instrument counting efficiency. This is motivated by Kovilakam and Deshler's (2015, ) discovery of an error in the calibration method applied to the optical particle counter (OPC40) developed in the late 1980s and used from 1991 to 2012. The method can be applied to other optical aerosol instruments for which counting efficiencies have been measured. The CEF employed is the integral of the Gaussian distribution representing the instrument response at any one aerosol channel, the aerosol counting efficiency. Results using the CEF are compared to previous derivations of aerosol size distributions (Deshler et al., 2003, ) applied to the measurements before and after Kovilakam and Deshler's correction of number concentration for the OPC40 calibration error. The CEF method is found, without any tuning parameter, to reproduce or improve upon the Kovilakam and Deshler's results, thus accounting for the calibration error without any external comparisons other than the laboratory determined counting efficiency at each aerosol channel. Moments of the new aerosol size distributions compare well with aerosol extinctions measured by Stratospheric Aerosol and Gas Experiment II and Halogen Occultation Experiment in the volcanic period 1991-1996, generally within 40%, the precision of OPC40 moments, and in the nonvolcanic period after 1996, generally within 20%. Stratospheric Aerosol and Gas Experiment II and Halogen Occultation Experiment estimates of aerosol surface area are generally in agreement with those derived using the new CEF method. Plain Language Summary Since 1971, balloon-borne instruments have been used to measure the size distribution of sub-micrometer-sized particles in the stratosphere. These particles, or aerosol, are important for two reasons: (1) They cool the planet by scattering sunlight back to space and (2) they facilitate chemical reactions, which destroy ozone. Ozone shields the Earth from harmful ultraviolet rays from the Sun. Stratospheric aerosol have also been measured from satellites since the 1980s using instruments which measure aerosol extinction, the extent to which sunlight is scattered or absorbed by stratospheric particles. The two measurement methods, satellite- and balloon-borne instruments, have had a long-standing discrepancy between satellite extinction measurements and balloon-borne measurements used to calculate extinction. This paper resolves that discrepancy through laboratory investigations of the counting efficiency of the balloon-borne instruments. When counting efficiency is included in the method to derive aerosol size distribution functions from the balloon-borne measurements, from which extinction and aerosol surface area can be calculated, the two measurement methods are in reasonable agreement. Resolving this discrepancy between the two instruments allows the local balloon-borne measurements to be used for testing the retrieval of aerosol surface area from the global satellite measurements. Stratospheric aerosol surface area is required for global climate models. Thus, this paper provides a basis to characterize the confidence, which can be placed in the global satellite estimates of aerosol surface area for the modeling community. |
英文关键词 | in situ aerosol measurements stratospheric aerosol extinction stratospheric aerosol surface area densities comparisons of in situ and remote aerosol measurements |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000469175600013 |
WOS关键词 | POLAR STRATOSPHERIC CLOUDS ; SAGE-II ; SULFURIC-ACID ; VERTICAL PROFILES ; VOLCANIC AEROSOL ; LIGHT-SCATTERING ; CONDENSATION NUCLEI ; OPTICAL-PROPERTIES ; LIDAR ; HALOE |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/183297 |
专题 | 气候变化 |
作者单位 | 1.Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA; 2.Lab Atmospher & Space Phys, Boulder, CO 80309 USA; 3.Swiss Fed Inst Technol, Dept Environm Syst Sci, Zurich, Switzerland; 4.NASA, Langley Res Ctr, Hampton, VA 23665 USA |
推荐引用方式 GB/T 7714 | Deshler, Terry,Luo, Beiping,Kovilakam, Mahesh,et al. Retrieval of Aerosol Size Distributions From In Situ Particle Counter Measurements: Instrument Counting Efficiency and Comparisons With Satellite Measurements[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2019,124(9):5058-5087. |
APA | Deshler, Terry,Luo, Beiping,Kovilakam, Mahesh,Peter, Thomas,&Kalnajs, Lars E..(2019).Retrieval of Aerosol Size Distributions From In Situ Particle Counter Measurements: Instrument Counting Efficiency and Comparisons With Satellite Measurements.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,124(9),5058-5087. |
MLA | Deshler, Terry,et al."Retrieval of Aerosol Size Distributions From In Situ Particle Counter Measurements: Instrument Counting Efficiency and Comparisons With Satellite Measurements".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 124.9(2019):5058-5087. |
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