A method of data supplementing Global PBL SO2 based on OMI
Chongyang Kang
Department of Education, Sichuan Tecnology and Business University
Xiaofang Yang
Department of Education, Sichuan Tecnology and Business University
Zhuoying He
Department of Education, Sichuan Tecnology and Business University
Kedi Mi
Department of Library, Sichuan Tecnology and Business University
Jie Hu
Department of Library, Sichuan Tecnology and Business University
Xiaorong Yu
Department of Library, Sichuan Tecnology and Business University
DOI: https://doi.org/10.59429/esta.v12i1.9648
Keywords: PBL SO2; OMI; The function derivative; Verification; SO2 column
Abstract
Sulfur dioxide(SO2) is an important pollutant gas that affects environment of our lives. Although we had made lots of detections, but still can not receive the distribution of SO2 in the world. Compared with great success in UV-vis spectrometers from remote sensing in OMI and OMPS, can provide SO2 data in a huge range and daily, but cannot receive data as there is no sunshine, this is difficult for researchers to do their study in global or area in high latitudes. In this paper, we tried to supplement the PBL SO2 in the whole world, based on the data of OMISO2, by the function derivative algorithm to segment approximation, and verified the method in the area, where OMI SO2 data are complete. The results show that the spatial distribution of SO2 in the global atmospheric boundary layer is obviously latitudinal zonality. SO2 columns and its variation trend are the same or similar in the same latitude during the year. Through verification we found that the partition below 5° latitude seldom affect the estimation, The accuracy is good in the region where there is no SO2 columns mutation, more than 90% of the grids which differences between the estimation and the truth are in a range of [-0.2DU, 0.2DU], less than the multi-day OMI monthly error of 0.2DU, the function is suitable in this situation, and the estimation will be biased in the region where the volcanic eruption, causes the monthly average SO2 columns mutation, but choosing data from the month nearby with no volcanic eruption can helps to eliminate the effects of volcanic eruptions and also can estimate the areas affected by volcanic eruptions.
References
[1] Zhang Y, Li C, Krotkov N A, J., 2017.Continuation of long-term global SO2 pollution monitoring from OMI to OMPS. Atmospheric Measurement Techniques. 10(4),1-21. http://www.atmos-meas-tech.net/10/1495/2017/amt-10-1495-2017-supplement.pdf
[2] Robock A, J., 2000. Volcanic eruptions and climate. Reviews of Geophysics. 38(2),191–219.http://eos.ubc.ca/~mjelline/453website/eosc453/E_prints/1998RG000054.pdf
[3] Koike M, Kondo Y, Kita K, J., 2003.Export of anthropogenic reactive nitrogen and sulfur compounds from the East Asia region in spring. Journal of Geophysical Research Atmospheres. 108(20):1887-1902. http://onlinelibrary.wiley.com/doi/10.1029/2002JD003284.pdf
[4] Lee C, Richter A, Weber M, J., 2008.SO2 Retrieval from SCIAMACHY using the Weighting Function DOAS (WFDOAS) Technique: comparison with Standard DOAS retrieval. Atmospheric Chemistry & Physics Discussions. 8(3), 6137-6145.https://www.cosis.net/members/meetings/abstracts/file.php/8/21445/jpdf/EAE03-J-08369.pdf
[5] Bell M L, Davis D L, J., 2001.Reassessment of the lethal London fog of 1952: novel indicators of acute and chronic consequences of acute exposure to air pollution. Environmental Health Perspectives Supplements.109 Suppl 3 (Suppl 3),389-394. http://120.52.51.19/europepmc.org/articles/PMC1240556/pdf/ehp109s-000389.pdf
[6] Lan Lan, D., 2013. Effects on Air Pollution on Public Health in Jinchang[D]. Lanzhou University.http://xueshu.baidu.com/usercenter/paper/show?paperid=2a21c570cbe216e9d5c5211411bc3719&site=xueshu_se
[7] Nyberg F, Gustavsson P, JRup L, J., 2000. Urban Air Pollution and Lung Cancer in Stockholm.Epidemiology 11(5),487-495.http://www.alarik.se/documents/LUCAS_Epidemiology2000nr11.pdf
[8] Yun Y , Gao R , Yue H , J., 2015. Synergistic effects of particulate matter (PM10) and SO2 on human nonsmall cell lung cancer A549 via ROS-mediated NFκB activation. Journal of Environmental Sciences, 31,146-153.http://or.nsfc.gov.cn/bitstream/00001903-5/199292/1/1000013192735.pdf
[9] Bovensmann H , Buchwitz M , Noel S, J., 2004.SCIAMACHY on ENVISAT: in-flight optical performance and first results. Proceedings of SPIE - The International Society for Optical Engineering, 5235,160-173. https://www.mendeley.com/catalogue/sciamachy-envisat-inflight-optical-performance-firstresults/1198735.pdf
[10] Krotkov N A, Carn S A, Krueger A J, J., 2006. Band residual difference algorithm for retrieval of SO2from the aura ozone monitoring instrument (OMI). IEEE Transactions on Geoscience & Remote Sensing. 44(5),1259-1266.http://ieeexplore.ieee.org/stamp/stamp.jsp?tp=&arnumber=1624604.pdf
[11] Yang K, Dickerson R R, Carn S A, J., 2013.First observations of SO2 from the satellite Suomi NPP OMPS: Widespread air pollution events over China. Geophysical Research Letters. 40(18),4957-4962.https://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/20140013038.pdf
[12] Carn, S. A, J., 2003. Prodigious sulfur dioxide emissions from Nyamuragira volcano, D.R. Congo. Geophysical Research Letters, 30(23),2211-2215.http://www.geo.mtu.edu/~gbluth/Publications/carn_2003_grl.pdf
[13] Khokhar M F, Frankenberg C, Roozendael M V, J., 2005. Satellite observations of atmospheric SO2, from volcanic eruptions during the time-period of 1996–2002. Advances in Space Research. 36(5),879-887. http://citeseerx.ist.psu.edu/viewdoc/download;jsessionid=62BB5EB4B52A443C9467A00B81177723?doi =10.1.1.497.9333&rep=rep1&type=pdf
[14] Michael Eisinger, J., 1998. Tropospheric Sulfur Dioxide observed by the ERS-2 GOME Instrument. GEOPHYSICAL RESEARCH LETTERS. 25(22),4177-4180.
http://doas-bremen.de/paper/grl_98_eisinger.pdf
[15] Fioletov V E, Mclinden C A, Krotkov N, J., 2011. Estimation of SO2 emissions using OMI retrievals. GEOPHYSICAL RESEARCH LETTERS. 38,L21811.
https://so2.gsfc.nasa.gov/pdfs/Fioletov_2011GL049402.pdf
[16] Krotkov N A, Mclinden C A, Li C, J., 2016. Aura OMI observations of regional SO2 and NO2 pollution changes from 2005 to 2015. Atmospheric Chemistry & Physics. 16(7),4605-4629. https://www.atmos-chem-phys-discuss.net/15/26555/2015/acp-2015-674-manuscript-version2.pdf
[17] Jiang J, D., 2012.Atmospheric SO2 Concentration Monitoring and Emission Estimation in China Based on OMI Satellite Data and Numerical Simulations. Nanjing Normal University.http://xueshu.baidu.com/usercenter/paper/show?paperid=21b2914213953202a590a59dbebb61a1&site=x
ueshu_se
[18] Xue D, Yin J, J., 2013.Meteorological influence on predicting surface SO₂ concentration from satellite remote sensing in Shanghai, China. Environmental Monitoring & Assessment, 186(5),2895.http://dx.doi.org/10.1007/s10661-013-3588-2.pdf
[19] Zhao Jun, Zhang Bincai, Fan Jieping, J., 2011. The Analysis of SO2 value Changes in the Atmospheric Boundary Layer over Lanzhou and Surrounding Areas based on the OMI Product.Remote sensing Technology and Application. 26(6),808-813.http://xueshu.baidu.com/usercenter/paper/showpaperid=4d0f4d0d9f4587faf89cbf9def2a6516&site=xueshu_se
[20] Kang Chongyang, Zhao jun, Song guofu, J., 2018. Study on the spatial pattern of SO2 in China’s atmospheric boundary layer based on OMI data. CHINA ENVIRONMENTAL SCIENCECE. 38(2), 435-443.http://xueshu.baidu.com/usercenter/paper/show?paperid=bd50f4c9c66075e42b6ab2b94efd8f63&site=xueshu_se
[21] Wang Mingxing, Zhen Xunhua, M., 2005. Atmospheric Chemistry Introduction. Meteorological Press.
[22] Yang K, Krotkov N A, Krueger A J, J., 2007.Retrieval of large volcanic SO2 s from the Aura Ozone Monitoring Instrument: Comparison and limitations. Journal of Geophysical Research Atmospheres, 112(D24),24-43.https://so2.gsfc.nasa.gov/pdfs/Yang_OMISO2_2007JD008825.pdf
[23] Li C, Joiner J, Krotkov N A, J., 2009. Retrieval of vertical columns of sulfur dioxide from SCIAMACHY and OMI: Air mass factor algorithm development, validation, and error analysis.114, D22303.http://www.iup.uni-bremen.de/doas/paper/jgr_09_lee.pdf
[24] Huang Meisheng, J., 1988.Use the formula to calculate the position of the sun and the latitude and longitude of the polar day and night. Middle School Geography Teaching Reference. (5),11-12.http://xueshu.baidu.com/usercenter/paper/show?paperid=013d8e417049f890ef80daefa781693b&site=xueshu_se