Processing


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  • ESR is a Skynet Regional sub-network providing for some selected sites the following new products:

    • 1. SUNRAD MOON: Night-time Aerosol Optical depth from Moon irradiance
    • 4 levels are given:
    • L2 Cloud Screened available at the end of each month after the calculation of the last solar calibration constants; Cloud screning is performed
    • L2A Cloud Screened dailiy available using the last available solar calibration constants; Cloud screning is performed
    • L2 Not Cloud Screened available at the end of each month after the calculation of the last solar calibration constants; Cloud screning is NOT performed
    • L2A Not Cloud Screened dailiy available using the last available solar calibration constants; Cloud screning is NOT performed

    • 2. WATER VAPOUR: Columnar Water vapour
    • this part is under development

    • 3. SUNRAD: Aerosol Optical depth as in ISDC
    • (same products of ISDC)
    • It will be available only for some AERONET-SKYNET co-located sites

    • 4. SKYRAD_MRI: Aerosol products as in ISDC
    • (same products of ISDC)
    • It will be available only for some AERONET-SKYNET co-located sites

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  • For Scientic pourpose and for some SKYNET-AERONET co-located sites, ESR provides the official AERONET products:

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  • Downloading:
    • Datacan be monthly downloaded from the ARCHIVE link in the folders:
    • L2CC, L2ACC (Cloud screned)
    • L2NC, L2ANC (not Cloud screened)

    In the solar aureole technique, two different calibrations are needed:

    ->

    The solar calibration constant (F0):
    it is the signal corresponding to the solar irradiance incident at the top of the atmosphere. All the instruments in ESR and SKYNET are calibrated using an in situ procedure called Improved Langley (Campanelli et al 2004; Campanelli et al. 2007), a modified version of the standard Langley plot technique.
    In the Improved Langley, F0 is retrieved by fitting the natural logarithm of the direct solar irradiance versus the product of the relative optical air mass and the total extinction optical thickness (retrieved by the inversion) instead of the air mass alone, as done with the standard Langley plot. This in situ calibration procedure allows the operators to track and evaluate the calibration status on a continuous basis, keeping the revision of the instrument mostly for maintenance reasons and offering the advantage of reducing the number of instrument expeditions. In this way, the data gaps incurred by the periodical shipments are considerably reduced, and the likelihood of instrumental damages attributable to transport also decreases.
    ESR calibrates its instruments on a monthly base.

    In order to observe the requirements from WMO, ESR and SKYNET instruments are periodically calibrated at the WRCC in Davos and at the MAUNA LOA laboratory, respectively. Some ESR instruments attended the QUATRAM campaign for in 2017-2019 treacebility studies and validation of the Improved Langley technique.

    The Solid view angle:
    it corresponds to the field of view of the instrument. Its value can be approached by the geometric solid viewing angle of the telescope. However, several factors contribute to this value: color aberration of the lens, diffraction at the edges, misalignment of the optical axis, and surface nonuniformity of filters and sensor. As a consequence, an in situ method is made available for determining the actual solid view angle (only for PREDE sun-sky radiometers) from optical data. This in situ method consists on performing a scanning of the irradiance field around the Sun, centered at the origin of a local system of rectangular coordinates (Boi et al. 1999).
    ESR mostly assumes this value as privided by the company using the above method.

    References

      About Skyrad.pack:

    • T. Nakajima, M. Tanaka and T. Yamauchi, Retrieval of the optical properties of aerosols from the aureole and extinction data. App. Opt. No.22, pp.2951-2959, 1983.

    • T. Nakajima, G. Tonna, R. Rao, P. Boi, Y. Kaufman and B. Holben, Use of sky brightness measurements from ground for remote sensing of particulate polydispersions. App. Opt. vol.35,No.15, pp.2672-2686, 1996.

    • M. Hashimoto, T. Nakajima, O.Dubovik, M. Campanelli, H. Che, P. Khatri, T. Takamura, G. Pandithurai, Development of a new data-processing method for SKYNET sky radiometer observations, Atmos. Meas. Tech., 5 (11), pp. 2723-2737, 2012.

    • Kudo, R., Nishizawa, T., and Aoyagi, T.: Vertical profiles of aerosol optical properties and the solar heating rate estimated by combining sky radiometer and lidar measurements, Atmos. Meas. Tech., 9, 3223–3243, https://doi.org/10.5194/amt-9-3223-2016, 2016.

    • Kudo, R., 2019.2.13, Developement of aerosol and cloud retrieval methods using the sky radiometer, 5th International SKYNET workshop, New Delhi, India


    • About ESR.pack:

    • V. Estellés, M. Campanelli, T. J. Smyth, M. P. Utrillas, and J. A. Martínez-Lozano. "AERONET and ESR sun direct products comparison performed on Cimel CE318 and Prede POM01 solar radiometers". Atmos. Chem. Physics Discuss. 12, 4341-4371, 2012, doi:10.5194/acpd-12-4341-2012.

    • V. Estellés, M. Campanelli, T.J. Smyth, M.P. Utrillas and J.A. Martinez-Lozano, Comparison of AERONET and SKYRAD4.2 inversion products retrieved from a Cimel CE318 sunphotometer, Atmos. Meas. Tech., 5, 1-11, 2012.


    • About Calibration:

    • M. Campanelli, T. Nakajima, B.Olivieri, "Determination of the solar calibration constant for a sun sky radiometer. Proposal of an in situ procedure". Applied Optics, Vol 43 n. 3, 20 January 2004

    • M. Campanelli, V. Estellés, C. Tomasi, T. Nakajima, V. Malvestuto and J. A. Martínez-Lozano. "Application of the SKYRAD improved Langley plot method for the in situ calibration of CIMEL sun-skphotometers" Vol. 46, No. 14 May, 2007, Applied Optics.

    • Paolo Boi, Glauco Tonna, Giuseppe Dalu, Teruyuki Nakajima, Bruno Olivieri, Alberto Pompei, Monica Campanelli, and R. Rao, "Calibration and data elaboration procedure for sky irradiance measurements," Appl. Opt. 38, 896-907 (1999).


    • About Cloud Screening:

    • Khatri, P. and T. Takamura. "An algorithm to screen cloud-affected data for sky radiometer data anlaysis". J. Meteorol Soc. Jpn., 87, 189-204,2009.


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    Webmasters: Flavio Marcozzi - email: flavio.marcozzi@gmail.com