[1] Thompson B A, harteck P, Reeves R R.Ultraviolet absorption coefficients of CO2, CO, O2, H2O, N2O, NH3, NO, SO2 and CH4 between 1850 and 4000 A.Journal of Geophysical Research, 1963,68(24): 6431～6436

[2] McGee T J,Jr J B. SO2.Absorption cross sections in the near U.V.J Quant Spectrosc Radiat Tranfer, 1987,37(2): 165～182

[3] Molina L T, Molina M J.Absolute Absorption Cross Sections of Ozone in the 185 to 350 nm wavelength range.Journal of Geophysical Research, 1986,91(13):14501～14508

[4] Platt U,Perner D.Simultaneous measurements of atmospheric CH2O, O3 and NO2 by differential optical absorption. Geophys Res, 1979 ,84(C10): 6329～6335

[7] Davidson J A,et al.Visible-ultraviolet absorption cross sections for NO2 as a function of temperature.Journal of Geophysical Research,1988,93(D6): 7105～7112

[8] Bass A M.Temperature dependent absorption cross sections for formaldehyde(CH2O): The effect of formaldehyde on stratospheric chlorine chemistry.Planet Space Sci, 1980,28(7): 675～679

[11] Stutz J,Platt U. Numerical analysis and estimation of the statistical error of differential optical absorption spectroscopy measurements with least-squares methods.Applied Optics, 1996,35(30):6041～6053