Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical Properties
The evolution of atmospheric and Earth surface physical properties over a period of 15 years (based on data from the longer period from 2004 to 2022) is analyzed through the radiance fluxes measured by the Meteosat second generation (MSG) satellite series. The results show significant changes in the...
Main Authors: | , |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2023-08-01
|
Series: | Atmosphere |
Subjects: | |
Online Access: | https://www.mdpi.com/2073-4433/14/9/1354 |
_version_ | 1797581280095764480 |
---|---|
author | José I. Prieto Fernández Christo G. Georgiev |
author_facet | José I. Prieto Fernández Christo G. Georgiev |
author_sort | José I. Prieto Fernández |
collection | DOAJ |
description | The evolution of atmospheric and Earth surface physical properties over a period of 15 years (based on data from the longer period from 2004 to 2022) is analyzed through the radiance fluxes measured by the Meteosat second generation (MSG) satellite series. The results show significant changes in the solar (−2.6% to −1.2%) and infrared (+0.4% to +1.0%) domains, with −3.9% for the CO<sub>2</sub> absorption band (near 13.4 µm), all variations consistent with results from similar studies of radiation fluxes. Whereas the variation at 13.4 μm radiation is explained by the increase in the CO<sub>2</sub> concentration in the atmosphere, the flux increase towards the satellite in the remainder of the infrared spectra measured by MSG corresponds to surface warming (as documented in external sources like the IPCC, the Intergovernmental Panel on Climate Change). The solar outgoing flux decrease exposes a recent reduction in the Earth’s cloud cover under the nominal field of view of Meteosat at 0 degrees longitude (MFOV). Radiance evolution at 6.2 µm and 7.3 µm, a spectral region of intense absorption by water vapor, is interpreted in terms of sensitivity to the humidity content in the middle and upper troposphere by means of a simple radiation transfer model. |
first_indexed | 2024-03-10T23:03:13Z |
format | Article |
id | doaj.art-1e3a3787266c4817aa66dc101b591c7e |
institution | Directory Open Access Journal |
issn | 2073-4433 |
language | English |
last_indexed | 2024-03-10T23:03:13Z |
publishDate | 2023-08-01 |
publisher | MDPI AG |
record_format | Article |
series | Atmosphere |
spelling | doaj.art-1e3a3787266c4817aa66dc101b591c7e2023-11-19T09:30:08ZengMDPI AGAtmosphere2073-44332023-08-01149135410.3390/atmos14091354Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical PropertiesJosé I. Prieto Fernández0Christo G. Georgiev1PraproSL, 06420 Castuera, SpainForecasts and Information Service Department, National Institute of Meteorology and Hydrology, 1784 Sofia, BulgariaThe evolution of atmospheric and Earth surface physical properties over a period of 15 years (based on data from the longer period from 2004 to 2022) is analyzed through the radiance fluxes measured by the Meteosat second generation (MSG) satellite series. The results show significant changes in the solar (−2.6% to −1.2%) and infrared (+0.4% to +1.0%) domains, with −3.9% for the CO<sub>2</sub> absorption band (near 13.4 µm), all variations consistent with results from similar studies of radiation fluxes. Whereas the variation at 13.4 μm radiation is explained by the increase in the CO<sub>2</sub> concentration in the atmosphere, the flux increase towards the satellite in the remainder of the infrared spectra measured by MSG corresponds to surface warming (as documented in external sources like the IPCC, the Intergovernmental Panel on Climate Change). The solar outgoing flux decrease exposes a recent reduction in the Earth’s cloud cover under the nominal field of view of Meteosat at 0 degrees longitude (MFOV). Radiance evolution at 6.2 µm and 7.3 µm, a spectral region of intense absorption by water vapor, is interpreted in terms of sensitivity to the humidity content in the middle and upper troposphere by means of a simple radiation transfer model.https://www.mdpi.com/2073-4433/14/9/1354satellite observationsradianceabsorption of thermal radiationradiation fluxlong-term series |
spellingShingle | José I. Prieto Fernández Christo G. Georgiev Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical Properties Atmosphere satellite observations radiance absorption of thermal radiation radiation flux long-term series |
title | Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical Properties |
title_full | Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical Properties |
title_fullStr | Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical Properties |
title_full_unstemmed | Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical Properties |
title_short | Evolution of Meteosat Solar and Infrared Spectra (2004–2022) and Related Atmospheric and Earth Surface Physical Properties |
title_sort | evolution of meteosat solar and infrared spectra 2004 2022 and related atmospheric and earth surface physical properties |
topic | satellite observations radiance absorption of thermal radiation radiation flux long-term series |
url | https://www.mdpi.com/2073-4433/14/9/1354 |
work_keys_str_mv | AT joseiprietofernandez evolutionofmeteosatsolarandinfraredspectra20042022andrelatedatmosphericandearthsurfacephysicalproperties AT christoggeorgiev evolutionofmeteosatsolarandinfraredspectra20042022andrelatedatmosphericandearthsurfacephysicalproperties |