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Measurement of dust optical depth using the solar...

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Libros Measurement of dust optical depth using the solar irradiance sensor (SIS) onboard the ExoMars 2016 EDM (2023-03-07T10:43:01Z) - Toledo, D. ‌

Número de control: XXX20230197028

Autor: Toledo, D.

Título: Measurement of dust optical depth using the solar irradiance sensor (SIS) onboard the ExoMars 2016 EDM

Publicación: Elsevier, 2023-03-07T10:43:01Z, 2023-03-07T10:43:01Z, 2017-01-20

Notas: "The solar irradiance sensor (SIS) was included in the DREAMS package onboard the ExoMars 2016 Entry Descent and Landing Demonstrator Module, and has been selected in the METED meteorological station onboard the ExoMars 2020 Lander. This instrument is designed to measure at different time intervals the scattered flux or the sum of direct flux and scattered flux in UVA (315-400 nm) and NIR (700-1100 nm) bands. For SIS'16, these measurements are performed by a total of 3 sensors per band placed at the faces of a truncated tetrahedron with face inclination angles of 60. The principal goal of SIS'16 design is to perform measurements of the dust opacity in UVA and NIR wavelengths ranges, crucial parameters in the understanding of the Martian dust cycle. The retrieval procedure is based on the use of radiative transfer simulations to reproduce SIS observations acquired during daytime as a function of dust opacity. Based on different sensitivity analysis, the retrieval procedure also requires to include as free parameters (1) the, dust effective radius; (2) the dust effective variance; and (3) the imaginary part of the refractive index of dust particles in UVA band. We found that the imaginary part of the refractive index of dust particles does not have a big impact on NIR signal, and hence we can kept constant this parameter in the retrieval of dust opacity at this channel.
In addition to dust opacity measurements, this instrument is also capable to detect and characterize clouds by looking at the time variation of the color index (CI), defined as the ratio between the observations in NIR and UVA channels, during daytime or twilight. By simulating CI signals with a radiative transfer model, the cloud opacity and cloud altitude (only during twilight) can be retrieved. Here the different retrieval procedures that are used to analyze SIS measurements, as well as the results obtained in different sensitivity analysis, are presented and discussed."

Part of this work has been funded with the help of the Spanish National Research, Development and Innovation Program, through the grant ESP2014-54256-C4-3-R.
Peerreview
Documento relacionado: . - info:eu-repo/grantAgreement/MINECO//ESP2014-54256-C4-3-R/ES/INSTRUMENTACION PARA LA INVESTIGACION Y CIENCIA ATMOSFERICA EN MARTE/
© 2017 Elsevier Ltd. All rights reserved.
info:eu-repo/semantics/restrictedAccess

Registros relacionados: Documento relacionado: . - info:eu-repo/grantAgreement/MINECO//ESP2014-54256-C4-3-R/ES/INSTRUMENTACION PARA LA INVESTIGACION Y CIENCIA ATMOSFERICA EN MARTE/

Tipo de impreso: info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501

Otros autores: Instituto Nacional de Técnica Aeroespacial (INTA)
Ministerio de Economía y Competitividad (MINECO)
Arruego, I.
Apéstigue, V.
Jiménez, J. J.
Gómez, L.
Yela González, M.
Rannou, P.
Pommereau, J. P.

Números normalizados: Planetary and Space Science 138: 33-43(2017)
0032-0633
https://www.sciencedirect.com/science/article/abs/pii/S0032063316301866
0.1016/j.pss.2017.01.015

Procedencia: Digital.INTA - Repositorio institucional del INTA

Tipo de publicación: Libros Libros

Derechos: In Copyright (InC)

‌ http://hdl.handle.net/20.500.12666/851

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