Disentangling chlorophyll fluorescence from atmospheric scattering effects in O2 A‐band spectra of reflected sun‐light

By Christian Frankenberg, André Butz, Geoffrey C. Toon. 2011

229 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/d6a8d861d55f337c79e2a2306f1013a1b08c5b2e

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Citations in the corpus

The FLuorescence EXplorer Mission Concept—ESA’s Earth Explorer 8 (2017, background): “They include GOSAT (TANSO-FTS sensor), MetOp (GOME-2), and Envisat (SCIAMACHY and MERIS) (see [5], [6]).”
Observing Changing Ecological Diversity in the Anthropocene (2013, background): “…photosynthetic pigments (Ustin et al 2009), In addition to mapping process controls, preliminary studies show photosynthesis rates, and consequently key traits like resource use efficiencies, may be directly estimated spectroscopically by measuring chlorophyll fluorescence (Frankenberg et al 2011).”
Filling-in of near-infrared solar lines by terrestrial fluorescence and other geophysical effects: simulations and space-based observations from SCIAMACHY and GOSAT (2012, methodology): “(2011) and Frankenberg et al.(2011a); atmospheric correction is unnecessary as long as observations are made at wavelengths not affected by atmospheric absorption.”
Using field spectroscopy to assess the potential of statistical approaches for the retrieval of sun-induced chlorophyll fluorescence from ground and space (2013, methodology): “This single-retrieval error is comparable to the one reported in Frankenberg et al. (2011b) and in Guanter et al. (2012) for GOSAT-FTS retrievals, and is also comparable to the precision error estimated in Fig.”
The Orbiting Carbon Observatory-2: first 18 months of science data products (2016, methodology): “, 2016) and IMAP-DOAS (IDP) preprocessors (Frankenberg et al., 2011, 2012, 2014) were used for the selection of data to be processed to L2. To limit the demands on the computing system, no more than 6 % of data collected each day are processed to L2 in the v7 forward processing stream. The v7r proce”
Coupling between the terrestrial carbon and water cycles—a review (2019, methodology): “A global remote sensing of solarinduced chlorophyll fluorescence (SIF) has become widely available from satellites such as GOSAT, GOME-2, SCIAMACHY and OCO-2 (Frankenberg et al 2011a, 2011b, Joiner et al 2011a, 2012, 2013, Guanter et al 2012).”