The Orbiting Carbon Observatory (OCO-2) makes global measurements of CO2. This seminar reviews how the OCO-2 experiment retrieves CO2, and discusses physics (due to 3D cloud radiative effects) which is not included in the operational retrieval. Clouds outside of the OCO-2 footprints can scatter light towards observation footprints, and thereby increase observed radiances. Sun-cloud-observation footprint geometry can also lead to cloud shadowing (a decrease in radiance). Analysis of OCO-2 data files indicates that there are many more “cloud brightening” than “cloud shadowing” events. 3D and 1D radiative transfer calculations, and analysis of several years of OCO-2 and Moderate Resolution Imaging Spectrometer (MODIS) data files, indicate that a) retrievals are impacted when observations are within 4 km of clouds, and b) 40% of OCO-2 retrievals are within 4 km of clouds. 3D cloud effect biases are calculated over ocean and land for the northern and southern hemispheres. Mitigation of the 3D cloud effect biases is discussed in terms of a simple empirical look-up table algorithm.
Address Info: Please note that the doors to SPSC remain locked during business hours. If you are external to LASP, it would be helpful to alert us in advance by contacting Heather Mallander that you plan to attend so that we can let you in.