Nitrous oxide observations from GOSAT-2/TANSO-FTS-2: Evaluation and potential
Jean-Luc
Attié
LAERO-Laboratoire d'Aérologie, Université de Toulouse, UMR CNRS 5560, France
Philippe Ricaud, CNRM, Météo-France, CNRS, Université de Toulouse, UMR CNRS 3589, France
Naoko Saito, Center for Environmental Remote Sensing, Chiba University, Japan
Prabir Patra, Center for Environmental Remote Sensing, Chiba University, Japan; Research Institute for Global Change, JAMSTEC, Yokohama, 236-0001, Japan
Isabelle Pison, Laboratoire des Sciences du Climat et de l’Environnement, CNRS UMR 1572, Gif-sur-Yvette, France
Adrien Martinez, Laboratoire des Sciences du Climat et de l’Environnement, CNRS UMR 1572, Gif-sur-Yvette, France
Rémi Chalinel, WaltR-Parc Technologique du Canal, Ramonville Saint Agne, France
Béatrice Josse, CNRM, Météo-France, CNRS, Université de Toulouse, UMR CNRS 3589, France
Didier Hauglustaine, Laboratoire des Sciences du Climat et de l’Environnement, CNRS UMR 1572, Gif-sur-Yvette, France

Poster
Nitrous oxide (N2O), with a lifetime of ~120 years, is the third most important greenhouse gas after carbon dioxide (CO2) and methane (CH4) contributing to global warming. It has a global warming potential 300 times greater than CO2 on the 100-year horizon. N2O emissions are not regulated by the Montreal Protocol and, although subject to the Kyoto Protocol, the ~0.25%/year increase in N2O observed over the last 10 years is expected to continue until 2100. N2O emissions involve both biotic (living organisms) and abiotic (environmentally induced e.g. water, soil, air) processes and are: 1) 60% natural, and 2) 40% anthropogenic. The annual average of N2O in the atmosphere is about 332 ppb (for the year 2019).

Despite its importance, tropospheric N2O measurements and surface emissions/sources remain understudied globally, with limited surface observations. However, sparse FTIR/NDACC instruments monitor N2O profiles and satellite observations performed in the thermal infrared (TIR) from IASI (Ricaud et al., 2009; Chalinel et al., 2022), AIRS and GOSAT (Kangah et al. 2017) provide valuable global data. GOSAT-2/TANSO-FTS-2, with some sensitivity to lower tropospheric N2O, offers potential studies on surface emissions using inversion methods.

This study evaluates the quality of GOSAT-2/TANSO-FTS-2 N2O observations for 2019. Comparisons with ground-based observations, IASI (Chalinel et al., 2022), NDACC N2O profiles and chemical transport models will assess the reliability of GOSAT-2 measurements at different atmospheric levels. The study includes discussion of measurement sensitivities, evaluation results, and potential for inverting N2O surface fluxes.

References:

Chalinel, R., et al., Global-scale observation and evaluation of nitrous oxide from IASI on MetOp-A, Remote Sens., 2022, doi : 10.3390/rs14061403
Kangah, Y., et al., Summertime upper tropospheric nitrous oxide over the Mediterranean as a footprint of Asian emissions, J. Geophys. Res. Atmos., 122, doi:10.1002/2016JD026119, 2017.
Ricaud, P., et al., Equatorial total column of nitrous oxide as measured by IASI on MetOp-A: Implications for transport processes, Atmos. Chem. Phys., 9, 3947-3956, 2009.
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