IASI AND IASI NG, MERLIN, MICROCARB FOR CH 4 AND CO 2 OBS. IN THE TROPOSPHERE

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CEOS-ACC- Séoul, October 14th, 2016 IASI AND IASI NG, MERLIN, MICROCARB FOR CH 4 AND CO 2 OBS. IN THE TROPOSPHERE Prepared by C. DENIEL, CNES, France (carole.deniel@cnes.fr) With contributions from C. CREVOISIER (LMD), B. BOUSQUET, F CHEVALIER & FM BREON (LSCE) Presented by C. Clerbaux, LATMOS/CNRS, France & 1 17/10/2016

French contribution to GG observation IASI IASI-NG Passive FTIR IASI-A, IASI-B IASI-C 2018 IASI-NG Phase C/D Operational mission (NRT + continuity) S5 component Merlin Lidar DLR-CNES collaboration Phase B completed Demonstrator CNES in charge of platform, system, launcher, and part of ground segment DLR in charge of payload, and part of ground segment Microcarb Passive spectrometer SWIR Context COP21 Phase A completed Demontrator Climate sentinel Cathy Clerbaux

CO 2 SURFACE FLUXES: ECMWF CO 2 forecast Total column average atmospheric CO 2 Vegetation (CTESSEL) Fires (GFAS) Ocean (inventory) Anthropogenic (inventory) IFS TRANSPORT PBL mixing Advection Convection CHEMISTRY Oxidation of CO (not yet represented in model) [ppm] Above background CO 2 Below background CO 2 Credit: S. Massart/A. Agusti-Panareda, JN Thépaut

TIR vs NIR/SWIR Cathy Clerbaux

IASI on MetOp

CO 2 (ppm) Greenhouse gases: CO 2 and CH 4 with IASI Objective: to better understand surface sources and sinks of greenhouse gases and the related processes (transport, flux). IASI contribution: mid-tropospheric columns of CO 2, CH 4 over both land and sea, day and night. AIRS (2003-2007) IASI (2007-2012) Trend: +2.1 ppm yr -1 AIRS (2003-2007) IASI (2007-2012) Methods: non linear inference scheme for CO 2 and CH 4 Chédin et al., 2003; Crevoisier et al., GRL, 2004; ACP 2009; ACP 2012. 6

Greenhouse gases: CO 2 with IASI

Seasonal maps of mid-tropospheric IASI CH 4 Average over July 2007-June 2015 Jan-Feb-Mar Apr-May-Jun Jul-Aug-Sep Oct-Nov-Dec Near-real time (D+1) delivery to Copernicus Atmospheric Service

Greenhouse gases: CH 4 with IASI CH 4 flying carpet Year (2007 2014) 9

Greenhouse gases: CO 2 and CH 4 and CO Long-term variations of CH 4 [30N:60N] Time series & (ppbv) Trend Growth rate (ppbv.year -1 ) [30N:Eq] [30S:Eq] [60S:30S] Latitude band Averaged growth rate (ppbv.year-1) IASI surface stations increase of CH 4 (ppbv) (Jul 2007-Dec 2014) [60N:30N] 4.54 +/- 7.15 4.90 +/- 3.96 ~ 33 [30N:Eq] 5.49 +/- 8.46 6.52 +/ 2.90 ~ 41 [30S:Eq] 5.31 +/- 5.92 5.53 +/ 4.25 ~ 39 [60S:30S] 3.12 +/- 2.42 5.37+/- 2.28 ~ 23 10

IASI-NG on MetOp-SG

The IASI-NG mission Carbon monoxide 2006 2012 2018 2021 2028 2035 IASI-A IASI-B IASI-C IASI-NG-A IASI-NG-B IASI-NG-C Objectives of the mission: To assure the continuity of IASI for NWP, atmospheric chemistry and climate applications. To improve the characterization of the lower part of the troposphere, the UT/LS region and, more generally, of the full atmospheric column. To improve the precision of the retrievals and to allow the detection of new species. Improvement of spectral resolution and radiometric noise. IASI-NG Characteristics: -spectral coverage: 645-2760 cm 1 (similar to IASI). -spectral resolution: 0.25 cm 1 after apodisation (0.50 cm -1 for IASI) -spectral sampling: 0.125 cm 1 (0.25 cm -1 for IASI). -reduction of the radiometric noise by at least a factor of ~2 as compared to IASI. -spatial sampling: 12km FOV.

Pressure (hpa) IASI-NG: Mid-tropospheric columns of CO 2 and CHCarbon 4 monoxide Carbon dioxide Spectral bands for IASI-NG Improvement of the CO 2 precision 15 µm 30 % 4.3 µm 0 % 15 + 4.3 µm 45 % IASI-NG will enable the use of 4.3 µm channels, giving access to a lower part of the atmosphere, with a much improved precision. Spectral bands for IASI-NG Methane Improvement of the CO 2 precision 7.7 µm 44 % Less interference with water vapor lines. 10 100 1000 CO 2 weighting function 15 µm 4.3 µm both IASI IASI-NG Strong and needed complementarity with SWIR obs. (UVNS/Sentinel5).

MICROCARB: CO 2 (Artist view based on CNES Myriade enhanced plat form) Passive SWIR (Short Wave Infra Red) spectrometer Mass < 200 kg High rate telemetry: 156 Mbits/s On board Data storage: 800 Gbits Agility Hydrazine propulsion Steerable solar generator 14 17/10/2016

MICROCARB : Operating modes Nadir Glint Target Over lands Over oceans For calibration (TCCON) Scan capacity Mechanism integrated in the instrument (rotating mirror. One axis) Across the track: ± 200 km Permits to acquire non correlated data Sampling distance: 100 km ALT and ACT 15 IWGGMS-12. Kyoto. June 7-9, 2016

Spectrometer Spectral performances MICROCARB: Spectral bands B1 B1 (=B5) B2 B3 Range (nm) 758-769 1264-1282 1596-1619 2023-2051 Detection O2. Surface pressure + properties of aerosol Idem B1. Aerosols properties at l close to B2-B3 CO 2 CO 2 Cloud imager Cloud detection 0,625 µm Ground sampling distance: 100 m

Standard Sounding geometry Ground footprint: 13 km (ACT) x 9 km (ALT) Data combined on ground => 3 simultaneous samples with size 4,5 km x 9km Improved resolution or «City «mode (exploratory) MICROCARB: scanning modes Goal: experiment capacity to characterize local emissions + Support for vicarious validation locally improvement of the spatial resolution 9 km Area covered during integration time 13,5 km Around 100 pixels Normal mode 3 macropixels 4,5x9 km Obtained by slowing down the satellite scrolling + scan + binning tuning Typical footprint: 2x2 km Typical area surface: 40 x 40 km² 2 km Exploratory mode 6 macropixels 2x2 km

Sat. chimie/climat & contexte EU Copernicus services : Intégration des différentes composantes : Mesures sol, + Satellites, + modèles Composante satellite Atmosphère S4 et S5 Climat S6-S7 http://www.esa.int/spaceinimages/images/2014/02/the_sentinel_family

Sat. chimie/climat & contexte EU CAMS C3S