Joint retrieval of atmospheric temperature and water vapor from AIRS thermal infrared and OCO-2 near-infrared measurements
Abstract. Combining thermal-infrared emission measurement with near-infrared absorption measurement can be a pathway to improved remote sensing of temperature and water vapor profiles from the surface to the upper troposphere. The addition of near-infrared radiance data to the thermal can significantly enhance the information content close to the surface in the planetary boundary layer, and is effective in clear or near-clear daytime conditions over land and ocean glint. A proof-of-concept study is presented using thermal-infrared Atmospheric Infrared Sounder (AIRS) radiances combined with near-coincident, near-infrared radiances from the Orbiting Carbon Observatory-2 (OCO-2) in a joint optimal estimation retrieval. Results indicate a significant increase in information content and reduced retrieval error for both temperature and water vapor between the surface and ~800 mb. Comparisons of retrieved profiles to coincident radiosondes show limited-to-no reduction in biases of temperature and water vapor over the forecast-derived a priori near the surface, indicating that improvements in the forward-modelling and/or retrieval algorithm are needed.
Figure 11 was modified after submission, but the text on Page 17 describing it was not. The text "Figure 11 shows the sonde locations, with the numbers indicting the number of days where successful retrievals were made, and the coloring indicating the total number of matchups at that site at 918 mb" should read "Figure 11 shows the sonde locations, with the size of the dots indicting the number of days where successful retrievals were made, and the shading indicating the total number of matchups at that site at 918 mb."