[1] [1] J. Sandsten, P. Weibring, H. Edner et al. Real-time gas-correlation imaging employing thermal background radiation[J]. Opt. Express, 2000, 6(4): 92-103

[2] [2] L. Falko, H. Gerd, P. Ulrich. Ground-based imaging differential optical absorption spectroscopy of atmospheric gases[J]. Appl. Opt., 2004, 43(24): 4711-4717

[3] [3] N. Bobrowski, G. Honninger, F. Lohberger et al.. IDOAS: A new monitoring technique to study the 2D distribution of volcanic gas emissions[J]. Journal of Volcanology and Geothermal Research, 2006, 150(4): 329-338

[4] [4] Li Ang, Xie Pinhua, Liu Wenqing et al.. Monitoring of total emission volume from pollution sources based on passive differential optical absorption Spectroscopy[J]. Acta Optica Sinica, 2007, 27(9): 1537-1542

[5] [5] Peng Fumin, Xie Pinhua, Zhang Yinghua et al.. Effect of spectra resolution on measurement of trace gases in atmosphere by differential optical absorption spectroscopy [J]. Acta Optica Sinica, 2008, 28(9): 1643-1648

[6] [6] Zhou Bin, Liu Wenqing, Qi Feng et al.. Error analysis in differential optical absorption spectroscopy[J]. Acta Optica Sinca, 2002, 22(8): 957-961

[7] [7] Y. Yoshii, H. Kuze, N. Takeuchi. Long-path measurement of atmospheric NO2 with an obstruction flashlight and a charge-coupled-device spectrometer [J]. Appl. Opt., 2003, 42(21): 4362-4368

[8] [8] Li Suwen, Xie Pinhua, Li Yujin et al.. Wavelet tra nsform baesd differential optical absorption spectroscopy data processing[J]. Acta Optica Sinca, 2006, 26(11): 1601-1604

[9] [9] Shen Yi, Zhou Bin, Wang Shansha et al.. Measurement of NO2 in cigarette main smoke by differential optical absorption spectroscopy[J]. Acta Optica Sinca, 2008, 28(10): 1934-1937

[10] [10] I. B. Konovalov, M. Beekmann R, J. P. Vautard et al.. Comparison and evaluation of modelled and GOME measurement derived tropospheric NO2 columns over Western and Eastern Europe[J]. Atmos. Chem. Phys., 2005, 5(1): 169-190

[11] [11] H. Bovensmann, J. P. Burrows, M. Buchwitz et al.. SCIAMACHY: Mission objectives and measurement modes[J]. J. Atmos.Sci., 1999, 56(2): 127-150

[12] [12] J. Skupin, S. Noёl, M. W. Wuttke et al.. SCIAMACHY solar irradiance observation in the spectral range from 240 to 2380 nm[J]. Adv. Space Res., 2005, 35: 370-375

[13] [13] J. K. Louisa, J. L. Roland, J. R. John et al.. Comparison of OMI and ground-based in situ and MAX-DOAS measurements of tropospheric nitrogen dioxide in an urban area[J]. J. Geophys. Res., 2008, 113: D16S39

[14] [14] R. Dirksen, M. Dobber, R. Voors et al.. Prelaunch characterization of the ozone monitoring instrument transfer function in the spectral domain[J]. Appl. Optics, 2006, 45(17): 3972-3981

[15] [15] Wang Shaolin, Xie Jun, Cao Kaifa et al.. Monitoring O3 in atmosphere by Raman-differentail absorption method[J]. Chinese J. Lasers, 2008, 35(5): 739-743

[16] [16] Si Fuqi, Xie Pinhua, Klaus-Peter Heue et al.. Hyperspectral imaging differential optical absorption spectroscopy[J]. Acta Physica Sinica, 57: 6018-6023

[17] [17] S. Solomon, A. L. Schmeltekopf. On the interpretation of zenith sky absorption measurements[J]. J. Geophys. Res., 1987, 92: 8311-8319

[18] [18] Ministry of Environmental Protection of The People’s Republic of China. GB13223-2003 Emission Standard of Air Pollutants for fossil power plants[S]. Beijing: Standards Pressof China, 2003. 214