Abstract We provide an overview of data products from observations by the Japanese Venus Climate Orbiter, Akatsuki, and describe the definition and content of each data-processing level. Levels 1 and 2 consist of non-calibrated and calibrated radiance (or brightness temperature), respectively, as well as geometry information (e.g., illumination angles). Level 3 data are global-grid data in the regular longitude–latitude coordinate system, produced from the contents of Level 2. Non-negligible errors in navigational data and instrumental alignment can result in serious errors in the geometry calculations. Such errors cause mismapping of the data and lead to inconsistencies between radiances and illumination angles, along with errors in cloud-...
This is the derived data, presented in a publication entitled "Spatial and temporal variability of t...
Sensitivity studies indicate that among the diverse error sources of ground-based sky radiometer obs...
International audienceWe present new results of our studies of zonal and meridional winds in both he...
The data products derived and presented in the manuscript of "Planetary-scale variations in winds an...
Abstract The status and initial products of the 1-μm camera onboard the Akatsuki mission to Venus ar...
Astrometry satellites have common technological issues. (A) Astrometry satellites are requ...
Plain Language Summary Temperature profiles of the Venus atmosphere obtained by the Akatsuki radio o...
Abstract The Venus Climate Orbiter Akatsuki arrived at Venus in December 2015, and the Longwave Infr...
Abstract Since insertion into orbit on December 7, 2015, the Akatsuki orbiter has returned global im...
Abstract After the arrival of Akatsuki spacecraft of Japan Aerospace Exploration Agency at Venus in ...
The files contain the time series of the longitudinal gradient of Venusian cloud's brightness temper...
Abstract The first year (December 2015 to November 2016) of IR2 after Akatsuki’s successful insertio...
International audienceWe present new wind velocities and its variability at Venus cloud-tops (≈70 km...
Context. The Hayabusa2 spacecraft launched by Japan Aerospace Exploration Agency has been conducting...
The first Japanese infrared space mission AKARI successfully scanned the whole sky with it...
This is the derived data, presented in a publication entitled "Spatial and temporal variability of t...
Sensitivity studies indicate that among the diverse error sources of ground-based sky radiometer obs...
International audienceWe present new results of our studies of zonal and meridional winds in both he...
The data products derived and presented in the manuscript of "Planetary-scale variations in winds an...
Abstract The status and initial products of the 1-μm camera onboard the Akatsuki mission to Venus ar...
Astrometry satellites have common technological issues. (A) Astrometry satellites are requ...
Plain Language Summary Temperature profiles of the Venus atmosphere obtained by the Akatsuki radio o...
Abstract The Venus Climate Orbiter Akatsuki arrived at Venus in December 2015, and the Longwave Infr...
Abstract Since insertion into orbit on December 7, 2015, the Akatsuki orbiter has returned global im...
Abstract After the arrival of Akatsuki spacecraft of Japan Aerospace Exploration Agency at Venus in ...
The files contain the time series of the longitudinal gradient of Venusian cloud's brightness temper...
Abstract The first year (December 2015 to November 2016) of IR2 after Akatsuki’s successful insertio...
International audienceWe present new wind velocities and its variability at Venus cloud-tops (≈70 km...
Context. The Hayabusa2 spacecraft launched by Japan Aerospace Exploration Agency has been conducting...
The first Japanese infrared space mission AKARI successfully scanned the whole sky with it...
This is the derived data, presented in a publication entitled "Spatial and temporal variability of t...
Sensitivity studies indicate that among the diverse error sources of ground-based sky radiometer obs...
International audienceWe present new results of our studies of zonal and meridional winds in both he...