Aerosol properties derived from ground-based Fourier transform spectra within the COllaborative Carbon Column Observing Network

Fourier transform infrared (FTIR) spectroscopy is particularly relevant for climate studies due to its ability to provide information on both fine absorption structures (i.e. trace gases) and broadband continuum signatures (i.e. aerosols or water continuum) across the entire infrared (IR) domain. In...

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Bibliographic Details
Published in:Atmospheric Measurement Techniques
Main Authors: Álvarez, Óscar, Barreto Velasco, África, García Rodríguez, Omaira Elena, Hase, Frank, García Cabrera, Rosa Delia, Gröbner, Julian, León-Luis, Sergio Fabián, Sepúlveda Hernández, Eliezer, Carreño Corbella, Virgilio, Alcántara, Antonio, Ramos López, Ramón, Almansa Rodríguez, Antonio Fernando, Kazadzis, Stelios, Taquet, Noémie, Toledano, Carlos, Cuevas Agulló, Emilio
Format: Article in Journal/Newspaper
Language:English
Published: European Geosciences Union 2023
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Online Access:https://hdl.handle.net/20.500.11765/15307
Description
Summary:Fourier transform infrared (FTIR) spectroscopy is particularly relevant for climate studies due to its ability to provide information on both fine absorption structures (i.e. trace gases) and broadband continuum signatures (i.e. aerosols or water continuum) across the entire infrared (IR) domain. In this context, this study assesses the capability of the portable and compact EM27/SUN spectrometer, used within the research infrastructure COCCON (COllaborative Carbon Column Observing Network), to retrieve spectral aerosol properties from low-resolution FTIR solar absorption spectra (0.5 cm−1 ). The study focuses on the retrieval of aerosol optical depth (AOD) and its spectral dependence in the 873–2314 nm spectral range from COCCON measurements at the subtropical high-mountain Izaña Observatory (IZO, Tenerife, Spain), which were coincidentally carried out with standard sun photometry within the Aerosol Robotic Network (AERONET) in the 3-year period from December 2019 to September 2022. This research has been supported by the European Community Research Infrastructure Action under the ACTRIS grant (grant no. 871115), the Ministerio de Economía y Competitividad of Spain through the project SYNERA (grant no. PID2020-521-118793GA-I00), and the European Metrology Programme for Innovation and Research (EMPIR) within the joint research project EMPIR 19ENV04 MAPP. The EMPIR is jointly funded by the EMPIR-participating countries within EURAMET and the European Union.