Differential optical absorption spectroscopy

By Ulrich Platt, J. Stutz. 2008

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A fast and sensitive new satellite SO2 retrieval algorithm based on principal component analysis: Application to the ozone monitoring instrument (2013, neutral): “…2019-10-21T00:56:54+00:00Z I(λ)/I0(λ), can be modeled with the weak absorption BeerLambert law [e.g., Platt and Stutz, 2008] as 1n I λð Þ I0 λð Þ ¼ ∑ n g¼1 Sgσg λð Þ P λð Þ RRS λð Þ; (1) where I(λ) and I0(λ) are the Earthshine radiance and solar…”
Inversion of tropospheric profiles of aerosol extinction and HCHO and NO 2 mixing ratios from MAX-DOAS observations in Milano during the summer of 2003 and comparison with independent data sets (2011, methodology): “Absolute concentrations can be determined from the measured column densities by knowing the length of the absorption path between the sending and receiving telescope (see Platt and Stutz, 2008) and an array of retro reflectors.”
The version 3 OMI NO 2 standard product (2017, methodology): “To calculate stratospheric and tropospheric AMFs, we use a pre-computed dimensionless scattering weight vector W (also known as the BoxAMF; Platt and Stutz, 2008).”
2 µm Laser Sources and Their Possible Applications (2010, background): “Most of these rely on differential optical absorption spectroscopy DOAS (Platt & Stutz, 2008).”