Retrieval of water vapor in the atmosphere and its spectral content: From OLCI to GPS

Publikation: Beitrag in Buch/Bericht/Sammelwerk/KonferenzbandAufsatz in KonferenzbandForschungPeer-Review

Autoren

Externe Organisationen

  • Agencia Estatal de Meteorología (AEMET)
  • Helmholtz-Zentrum Potsdam Deutsches GeoForschungsZentrum (GFZ)
  • Freie Universität Berlin (FU Berlin)
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Details

OriginalspracheEnglisch
Titel des SammelwerksRemote Sensing of Clouds and the Atmosphere XXVIII
Herausgeber/-innenAdolfo Comeron, Evgueni I. Kassianov, Klaus Schafer, Richard H. Picard, Konradin Weber
Herausgeber (Verlag)SPIE
ISBN (elektronisch)9781510666894
PublikationsstatusVeröffentlicht - 2023
VeranstaltungRemote Sensing of Clouds and the Atmosphere XXVIII 2023 - Amsterdam, Niederlande
Dauer: 5 Sept. 20236 Sept. 2023

Publikationsreihe

NameProceedings of SPIE - The International Society for Optical Engineering
Band12730
ISSN (Print)0277-786X
ISSN (elektronisch)1996-756X

Abstract

Understanding the tropospheric diabatic heating is essential for predicting Earth’s weather and climate. To reach that goal, information on water vapor (WV) in the atmosphere is mandatory. Unfortunately, monitoring WV is challenging, because of its high variability in both space and time. Particularly, advanced knowledge and modeling of its fine scale behavior would be beneficial to improve forecasting applications. In this contribution, we propose to compare and discuss the spectral content of dataset from two instruments recording WV content of the atmosphere, focusing on small scales: Ocean Land Color Instrument (OLCI) on board of Copernicus Sentinel-3 and Zenith wet delay (ZWD) retrieved from Global Navigation Satellite System (GNSS) observations. Kolmogorov’s theory states that the structure function of passive scalar, or equivalently the temporal power spectrum (assuming taylor frozen turbulence), should follow a given power law within the inertial range. Using the von Karman modelling, it is possible to assess the outer scale length of turbulence defined as the frequency where the spectrum saturates. For our analysis on WV small scales, we have selected a region around Lindenberg in Germany. We will discuss the spectral content of the retrieved observations and their specificity. We will highlight the potential of ZWD from GNSS observations to study daily variations of turbulence parameters.

ASJC Scopus Sachgebiete

Ziele für nachhaltige Entwicklung

Zitieren

Retrieval of water vapor in the atmosphere and its spectral content: From OLCI to GPS. / Kermarrec, G.; Calbet, X.; Deng, Z. et al.
Remote Sensing of Clouds and the Atmosphere XXVIII. Hrsg. / Adolfo Comeron; Evgueni I. Kassianov; Klaus Schafer; Richard H. Picard; Konradin Weber. SPIE, 2023. 127300F (Proceedings of SPIE - The International Society for Optical Engineering; Band 12730).

Publikation: Beitrag in Buch/Bericht/Sammelwerk/KonferenzbandAufsatz in KonferenzbandForschungPeer-Review

Kermarrec, G, Calbet, X, Deng, Z, Carbajal Henken, C & Preusker, R 2023, Retrieval of water vapor in the atmosphere and its spectral content: From OLCI to GPS. in A Comeron, EI Kassianov, K Schafer, RH Picard & K Weber (Hrsg.), Remote Sensing of Clouds and the Atmosphere XXVIII., 127300F, Proceedings of SPIE - The International Society for Optical Engineering, Bd. 12730, SPIE, Remote Sensing of Clouds and the Atmosphere XXVIII 2023, Amsterdam, Niederlande, 5 Sept. 2023. https://doi.org/10.1117/12.2678381
Kermarrec, G., Calbet, X., Deng, Z., Carbajal Henken, C., & Preusker, R. (2023). Retrieval of water vapor in the atmosphere and its spectral content: From OLCI to GPS. In A. Comeron, E. I. Kassianov, K. Schafer, R. H. Picard, & K. Weber (Hrsg.), Remote Sensing of Clouds and the Atmosphere XXVIII Artikel 127300F (Proceedings of SPIE - The International Society for Optical Engineering; Band 12730). SPIE. https://doi.org/10.1117/12.2678381
Kermarrec G, Calbet X, Deng Z, Carbajal Henken C, Preusker R. Retrieval of water vapor in the atmosphere and its spectral content: From OLCI to GPS. in Comeron A, Kassianov EI, Schafer K, Picard RH, Weber K, Hrsg., Remote Sensing of Clouds and the Atmosphere XXVIII. SPIE. 2023. 127300F. (Proceedings of SPIE - The International Society for Optical Engineering). Epub 2023 Okt 19. doi: 10.1117/12.2678381
Kermarrec, G. ; Calbet, X. ; Deng, Z. et al. / Retrieval of water vapor in the atmosphere and its spectral content : From OLCI to GPS. Remote Sensing of Clouds and the Atmosphere XXVIII. Hrsg. / Adolfo Comeron ; Evgueni I. Kassianov ; Klaus Schafer ; Richard H. Picard ; Konradin Weber. SPIE, 2023. (Proceedings of SPIE - The International Society for Optical Engineering).
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title = "Retrieval of water vapor in the atmosphere and its spectral content: From OLCI to GPS",
abstract = "Understanding the tropospheric diabatic heating is essential for predicting Earth{\textquoteright}s weather and climate. To reach that goal, information on water vapor (WV) in the atmosphere is mandatory. Unfortunately, monitoring WV is challenging, because of its high variability in both space and time. Particularly, advanced knowledge and modeling of its fine scale behavior would be beneficial to improve forecasting applications. In this contribution, we propose to compare and discuss the spectral content of dataset from two instruments recording WV content of the atmosphere, focusing on small scales: Ocean Land Color Instrument (OLCI) on board of Copernicus Sentinel-3 and Zenith wet delay (ZWD) retrieved from Global Navigation Satellite System (GNSS) observations. Kolmogorov{\textquoteright}s theory states that the structure function of passive scalar, or equivalently the temporal power spectrum (assuming taylor frozen turbulence), should follow a given power law within the inertial range. Using the von Karman modelling, it is possible to assess the outer scale length of turbulence defined as the frequency where the spectrum saturates. For our analysis on WV small scales, we have selected a region around Lindenberg in Germany. We will discuss the spectral content of the retrieved observations and their specificity. We will highlight the potential of ZWD from GNSS observations to study daily variations of turbulence parameters.",
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T1 - Retrieval of water vapor in the atmosphere and its spectral content

T2 - Remote Sensing of Clouds and the Atmosphere XXVIII 2023

AU - Kermarrec, G.

AU - Calbet, X.

AU - Deng, Z.

AU - Carbajal Henken, C.

AU - Preusker, R.

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AB - Understanding the tropospheric diabatic heating is essential for predicting Earth’s weather and climate. To reach that goal, information on water vapor (WV) in the atmosphere is mandatory. Unfortunately, monitoring WV is challenging, because of its high variability in both space and time. Particularly, advanced knowledge and modeling of its fine scale behavior would be beneficial to improve forecasting applications. In this contribution, we propose to compare and discuss the spectral content of dataset from two instruments recording WV content of the atmosphere, focusing on small scales: Ocean Land Color Instrument (OLCI) on board of Copernicus Sentinel-3 and Zenith wet delay (ZWD) retrieved from Global Navigation Satellite System (GNSS) observations. Kolmogorov’s theory states that the structure function of passive scalar, or equivalently the temporal power spectrum (assuming taylor frozen turbulence), should follow a given power law within the inertial range. Using the von Karman modelling, it is possible to assess the outer scale length of turbulence defined as the frequency where the spectrum saturates. For our analysis on WV small scales, we have selected a region around Lindenberg in Germany. We will discuss the spectral content of the retrieved observations and their specificity. We will highlight the potential of ZWD from GNSS observations to study daily variations of turbulence parameters.

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KW - GNSS

KW - OLCI

KW - outer scale length

KW - Remote sensing water vapor

KW - von Karman power spectrum

KW - Zenith wet delay

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PB - SPIE

Y2 - 5 September 2023 through 6 September 2023

ER -

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