2012 IEEE International Geoscience and Remote Sensing Symposium 2012
DOI: 10.1109/igarss.2012.6352020
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FLEX: ESA's Earth Explorer 8 candidate mission

Abstract: In this paper we present the scientific objectives of the FLEX mission and the underlying rationale. It sketches the basic ideas of the new measurement concept, which is making use of the tandem configuration of FLEX with GMES/Sentinel-3, and outlines the most important instrument and system requirements. We will describe the envisaged instrument configuration that is in line with the measurement objectives, and which is supported by the latest results of the scientific investigations.

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Cited by 31 publications
(24 citation statements)
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“…Recently, a new retrieval of red SIF from GOME‐2 instrument was developed (Joiner et al, 2016), which is noisy but could yield important additional information on LUE. New fluorescence observations at higher spatial and temporal resolution and with higher signal‐to‐noise ratio, such as from OCO‐2 (Frankenberg et al, 2014; Li et al, 2017; Schimel et al, 2015), Florescence Explorer (FLEX) (Kraft et al, 2012), TROPOspheric Monitoring Instrument (TROPOMI) (Guanter et al, 2015), or Geostationary Carbon Cycle Observatory (GeoCARB) (O'Brien et al, 2016), might help better retrieve changes in LUE, maybe in combination with this RSIF product. In addition, SIF observations at other spectral frequencies and at higher temporal resolution (diurnal) might yield critical information regarding variations in SIF yield and LUE.…”
Section: Discussionmentioning
confidence: 99%
“…Recently, a new retrieval of red SIF from GOME‐2 instrument was developed (Joiner et al, 2016), which is noisy but could yield important additional information on LUE. New fluorescence observations at higher spatial and temporal resolution and with higher signal‐to‐noise ratio, such as from OCO‐2 (Frankenberg et al, 2014; Li et al, 2017; Schimel et al, 2015), Florescence Explorer (FLEX) (Kraft et al, 2012), TROPOspheric Monitoring Instrument (TROPOMI) (Guanter et al, 2015), or Geostationary Carbon Cycle Observatory (GeoCARB) (O'Brien et al, 2016), might help better retrieve changes in LUE, maybe in combination with this RSIF product. In addition, SIF observations at other spectral frequencies and at higher temporal resolution (diurnal) might yield critical information regarding variations in SIF yield and LUE.…”
Section: Discussionmentioning
confidence: 99%
“…These include the Greenhouse gases Observing SATellite (GOSAT) [32][33][34][35], the Global Ozone Monitoring Experiment 2 (GOME-2) [21,36], the SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY (SCIAMACHY) [33,37], and the Orbiting Carbon Observatory 2 (OCO-2) [38]. Future instruments capable of measuring SiF are the TROPOspheric Monitoring Instrument (TROPOMI) [39] and the dedicated FLuorescence EXplorer mission (FLEX) [40]. From the current instruments, particularly the GOME-2 instruments profit from a good spatial coverage and the availability of long historical records: GOME-2 on Metop-A has been fully operational since 2007 and GOME-2 on Metop-B since 2013.…”
Section: Introductionmentioning
confidence: 99%
“…Clerbaux et al, 2009 ;Menut et al, 2017 pour les aspects composition atmosphérique), Polder et Calipso (aérosols et nuages, voir Tanré et al, 2011 ;Zeng et al, 2011et Winker et al, 2009 ; voir aussi encadré 6). De futures missions/ instruments sont aujourd'hui en phase A, B ou C, comme par exemple Iasi-NG (Crevoisier et al, 2014), Biomass (Scipal et al, 2010), Flex (Kraft et al, 2012), CFOsat (Caudal et al, 2014), Swarm (Mandéa, 2016), Swot (Gaultier et al, 2016), Merlin et Microcarb (voir Chevallier et al, 2017, pour plus …”
Section: Le Rôle De L'europe Et De La Franceunclassified