Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica)

Selected case studies of precipitating ice clouds at Dome C (Antarctic Plateau) were used to test a new approach for the estimation of ice cloud reflectivity at 24 GHz (12.37 mm wavelength) using ground-based far infrared spectral measurements from the REFIR-PAD Fourier transform spectroradiometer a...

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Published in:Atmospheric Measurement Techniques
Main Authors: Natale, Gianluca, Turner, David D., Bianchini, Giovanni, Guasta, Massimo, Palchetti, Luca, Bracci, Alessandro, Baldini, Luca, Maestri, Tiziano, Cossich, William, Martinazzo, Michele, Facheris, Luca
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Language:English
Published: 2022
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Online Access:https://doi.org/10.5194/amt-15-7235-2022
https://amt.copernicus.org/articles/15/7235/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:amt105251 2023-05-15T13:38:41+02:00 Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica) Natale, Gianluca Turner, David D. Bianchini, Giovanni Guasta, Massimo Palchetti, Luca Bracci, Alessandro Baldini, Luca Maestri, Tiziano Cossich, William Martinazzo, Michele Facheris, Luca 2022-12-16 application/pdf https://doi.org/10.5194/amt-15-7235-2022 https://amt.copernicus.org/articles/15/7235/2022/ eng eng doi:10.5194/amt-15-7235-2022 https://amt.copernicus.org/articles/15/7235/2022/ eISSN: 1867-8548 Text 2022 ftcopernicus https://doi.org/10.5194/amt-15-7235-2022 2022-12-19T17:22:42Z Selected case studies of precipitating ice clouds at Dome C (Antarctic Plateau) were used to test a new approach for the estimation of ice cloud reflectivity at 24 GHz (12.37 mm wavelength) using ground-based far infrared spectral measurements from the REFIR-PAD Fourier transform spectroradiometer and backscattering/depolarization lidar profiles. The resulting reflectivity was evaluated with the direct reflectivity measurements provided by a co-located micro rain radar (MRR) operating at 24 GHz, that was able to detect falling crystals with large particle size, typically above 600 µ m. To obtain the 24 GHz reflectivity, we used the particle effective diameter and the cloud optical depth retrieved from the far infrared spectral radiances provided by REFIR-PAD and the tropospheric co-located backscattering lidar to calculate the modal radius and the intercept of the particle size distribution. These parameters spanned in the wide ranges between 570–2400 µ m and 10 −2 – 10 4 cm −5 , respectively. The retrieved effective sizes and optical depths mostly varied in the ranges 70–250 µ m and 0.1–5, respectively. From these parameters, the theoretical reflectivity at 24 GHz was obtained by integrating the size distribution over different cross sections for various habit crystals provided by Eriksson et al. ( 2018 ) databases. From the comparison with the radar reflectivity measurements, we found that the hexagonal column-like habits, the columnar crystal aggregates, and the <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">5</mn><mo>/</mo><mn mathvariant="normal">6</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="023af0f8880475ce1a583f0c7c2ff620"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-15-7235-2022-ie00001.svg" width="20pt" height="14pt" ... Text Antarc* Antarctic Antarctica Copernicus Publications: E-Journals Antarctic Atmospheric Measurement Techniques 15 24 7235 7258
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description Selected case studies of precipitating ice clouds at Dome C (Antarctic Plateau) were used to test a new approach for the estimation of ice cloud reflectivity at 24 GHz (12.37 mm wavelength) using ground-based far infrared spectral measurements from the REFIR-PAD Fourier transform spectroradiometer and backscattering/depolarization lidar profiles. The resulting reflectivity was evaluated with the direct reflectivity measurements provided by a co-located micro rain radar (MRR) operating at 24 GHz, that was able to detect falling crystals with large particle size, typically above 600 µ m. To obtain the 24 GHz reflectivity, we used the particle effective diameter and the cloud optical depth retrieved from the far infrared spectral radiances provided by REFIR-PAD and the tropospheric co-located backscattering lidar to calculate the modal radius and the intercept of the particle size distribution. These parameters spanned in the wide ranges between 570–2400 µ m and 10 −2 – 10 4 cm −5 , respectively. The retrieved effective sizes and optical depths mostly varied in the ranges 70–250 µ m and 0.1–5, respectively. From these parameters, the theoretical reflectivity at 24 GHz was obtained by integrating the size distribution over different cross sections for various habit crystals provided by Eriksson et al. ( 2018 ) databases. From the comparison with the radar reflectivity measurements, we found that the hexagonal column-like habits, the columnar crystal aggregates, and the <math xmlns="http://www.w3.org/1998/Math/MathML" id="M7" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">5</mn><mo>/</mo><mn mathvariant="normal">6</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="023af0f8880475ce1a583f0c7c2ff620"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-15-7235-2022-ie00001.svg" width="20pt" height="14pt" ...
format Text
author Natale, Gianluca
Turner, David D.
Bianchini, Giovanni
Guasta, Massimo
Palchetti, Luca
Bracci, Alessandro
Baldini, Luca
Maestri, Tiziano
Cossich, William
Martinazzo, Michele
Facheris, Luca
spellingShingle Natale, Gianluca
Turner, David D.
Bianchini, Giovanni
Guasta, Massimo
Palchetti, Luca
Bracci, Alessandro
Baldini, Luca
Maestri, Tiziano
Cossich, William
Martinazzo, Michele
Facheris, Luca
Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica)
author_facet Natale, Gianluca
Turner, David D.
Bianchini, Giovanni
Guasta, Massimo
Palchetti, Luca
Bracci, Alessandro
Baldini, Luca
Maestri, Tiziano
Cossich, William
Martinazzo, Michele
Facheris, Luca
author_sort Natale, Gianluca
title Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica)
title_short Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica)
title_full Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica)
title_fullStr Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica)
title_full_unstemmed Consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at Dome C (Antarctica)
title_sort consistency test of precipitating ice cloud retrieval properties obtained from the observations of different instruments operating at dome c (antarctica)
publishDate 2022
url https://doi.org/10.5194/amt-15-7235-2022
https://amt.copernicus.org/articles/15/7235/2022/
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genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
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op_relation doi:10.5194/amt-15-7235-2022
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container_title Atmospheric Measurement Techniques
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