The Orbiting Carbon Observatory (OCO) mission
By David Crisp, R. Atlas, François-Marie Bréon, L. Brown, John P. Burrows, Philippe Ciais, Brian J. Connor, S. Doney, I. Fung, D. J. Jacob and 21 more. 2004
706 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/e7a7cfb7c20f4184ff220824abdceeddbbac57d4
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- Jonathan Tennyson
- Robert J. D. Spurr
- Kelly Chance
- V. Perevalov
- S. Tashkun
- Sergei N. Yurchenko
- Paul O. Wennberg
- L. Rothman
In Global and Planetary Change
- Jonathan Tennyson
- Robert J. D. Spurr
- Kelly Chance
- Paul O. Wennberg
- David Crisp
- V. Perevalov
- Christian Frankenberg
- Paul I. Palmer
Citations in the corpus
- Spaceborne observations of ocean glint reflectance and modeling of wave slope distributions (2006, background): “On the other hand, the intense sunglint contribution is needed for retrieving atmospheric column of various gases such as water vapor [Vespérini et al., 1999; Kleidman et al., 2000] or carbon dioxide [Crisp et al., 2004].”
- The Orbiting Carbon Observatory (OCO-2): spectrometer performance evaluation using pre-launch direct sun measurements (2014, background): “See Crisp et al. (2004), Pollock et al. Atmos.”
- The HITRAN 2008 molecular spectroscopic database (2005, methodology): “A notable effort is the set of extensive Fourier transform spectroscopy (FTS) experiments carried out by the Jet Propulsion Laboratory (JPL) [51–58] in order to support the OCO mission [8].”
- Filling-in of near-infrared solar lines by terrestrial fluorescence and other geophysical effects: simulations and space-based observations from SCIAMACHY and GOSAT (2012, positive): “The upcoming launch of the Orbiting Carbon Observatory-2 (OCO-2) (Crisp et al., 2004) will facilitate the use of solar Fraunhofer lines for fluorescence retrievals at wavelengths near the O 2 -”