Overview of Akatsuki data products: definition of data levels, method and accuracy of geometric correction

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 geo...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Earth, planets, and space planets, and space, 2017-12, Vol.69 (1), p.1-16, Article 167
Hauptverfasser: Ogohara, Kazunori, Takagi, Masahiro, Murakami, Shin-ya, Horinouchi, Takeshi, Yamada, Manabu, Kouyama, Toru, Hashimoto, George L., Imamura, Takeshi, Yamamoto, Yukio, Kashimura, Hiroki, Hirata, Naru, Sato, Naoki, Yamazaki, Atsushi, Satoh, Takehiko, Iwagami, Naomoto, Taguchi, Makoto, Watanabe, Shigeto, Sato, Takao M., Ohtsuki, Shoko, Fukuhara, Tetsuya, Futaguchi, Masahiko, Sakanoi, Takeshi, Kameda, Shingo, Sugiyama, Ko-ichiro, Ando, Hiroki, Lee, Yeon Joo, Nakamura, Masato, Suzuki, Makoto, Hirose, Chikako, Ishii, Nobuaki, Abe, Takumi
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung: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-motion vectors. Thus, we carefully correct the boresight pointing of each camera by fitting an ellipse to the observed Venusian limb to provide improved longitude–latitude maps for Level 3 products, if possible. The accuracy of the pointing correction is also estimated statistically by simulating observed limb distributions. The results show that our algorithm successfully corrects instrumental pointing and will enable a variety of studies on the Venusian atmosphere using Akatsuki data.
ISSN:1880-5981
1343-8832
1880-5981
DOI:10.1186/s40623-017-0749-5