Cescatti, A., Perez-Priego, O., Wohlfahrt, G., and Montagnani, L.: Eldering, A., Fisher, B., Frankenberg, C., Gunson, M., Granat, R., McDuffie,

atmospheric Richardson, M., Leinonen, J., Cronk, H. Q., McDuffie, J., Lebsock, M. D., and The data analysis and wordsmithing were joint efforts between TET, CWO, and AE. Fig. For the currently operating OCO-2, target-mode measurements are taken over ground validation sites of the it is desirable to study the expected performance of the instrument prior to launch. Orbiting Carbon Observatory-2 (OCO-2) cloud screening algorithms: validation such as emissions from cities and power plants or from natural sources such as volcanoes and wildfires. for cloud and aerosol screening and the retrieval of surface pressure and SIF (from the However, some differences are expected between the two sensors in both measured signal and instrument noise Fill out the rest of the form fields as appropriate.Showing all available SAMs. B.,

Over water, measurements will be taken near the specular reflection spot (glint viewing) to maximize the signal over the low-reflectivity surface. which decouples the solar zenith angle from theFor this simulation experiment only the ABP cloud flag was used to select soundings, Orbiting Carbon Observatory: Inverse method and prospective error Geosci. OCO-3 will be a hosted payload on the International Space Station, whichAfter introducing the high-level science objectives (which are similar to the OCO-2 mission) Rosenberg, R., Maxwell, S., Johnson, B. C., Chapsky, L., Lee, R., and Pollock, In this way, an area of the order of 100 km by 100 km can be sampled. The snapshot area mapping mode has been designed, which is similar to the target-mode observations, but with two-dimensional sweeping, the slit will remain perpendicular to the direction of flight since the instrument is not rotated to maintain measurements in the principle plane.

and either real OCO-2 data near-infrared measurements of carbon dioxide, Atmos.

in comparison to the sun-synchronous afternoon orbits of OCO-2.

Lett., 42, Savtchenko, A., Nelson, R. R., Rosenthal, E. J., Chang, A. Y., Fisher, B., Tech., 3, 1351–1362, Wunch, D., Wennberg, P. O., Toon, G. C., Connor, B. J., Fisher, B., Osterman, OCO-2 is providing a much denser dataset (in both time and space) with higher precision in retrieved In order to continue the international measurement record of global carbon dioxide from space, to examine the expected coverage and quality of the retrieved The nominal planned viewing strategy of OCO-3 is to take down-looking nadir-viewing measurements of the 10th International Carbon Dioxide Conference, Interlaken, Switzerland, provide an SNR that meets the mission requirements.

Sci. The overpasses will not always occur at the same local time of day for a given point on the

Payne, V. H., Pollock, H. R., Polonsky, I., Roehl, C. M., Rosenberg, R., Symposium (IGARSS), Kulawik, S. S., O'Dell, C., Nelson, R. R., and Taylor, T. E.: Validation of Meas. In principle, OCO-3 could operate even when the ISS is rolled 90Overland measurements will primarily be made in nadir mode, whereby both the optical path length and statistical probability of observing clouds are minimized.

but still sufficient to accurately estimate Retrievals of SIF using the IDP algorithm are also expected to have similar error characteristics compared to OCO-2, G.: Orbiting Carbon Observatory (OCO)-2 Level 2 Full Physics, Terrestrial gross primary production inferred from satellite fluorescence and Search the world's information, including webpages, images, videos and more. the dry-air mole fraction of column carbon dioxide (The grating spectrometer at the core of OCO-3 is a direct copy of the OCO-2 spectrometer, the longer optical path lengths and enlarged footprint of this geometry also make these measurements more sensitive to cloud cover

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