2020
DOI: 10.3390/rs12091424
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Column Integrated Water Vapor and Aerosol Load Characterization with the New ZEN-R52 Radiometer

Abstract: The study shows the first results of the column-integrated water vapor retrieved by the new ZEN-R52 radiometer. This new radiometer has been specifically designed to monitor aerosols and atmospheric water vapor with a high degree of autonomy and robustness in order to allow the expansion of the observations of these parameters to remote desert areas from ground-based platforms. The ZEN-R52 device shows substantial improvements compared to the previous ZEN-R41 prototype: a smaller field of view, an increased si… Show more

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Cited by 12 publications
(14 citation statements)
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“…Recently, at IZO, Ref. [35] further studies corroborated these results, obtaining a mean bias of −0.006 mm (−1.3%) when comparing TCCON FTIR PWV values to those obtained from meteorological radiosondes launched on Tenerife island and processed according to the GRUAN scheme (http://www.gruan.org, last access: 28 November 2020). The Almansa's study also found a relative difference of +3.4% respect to collocated CIMEL-AERONET data (FTIR-CIMEL).…”
Section: • Ftirmentioning
confidence: 74%
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“…Recently, at IZO, Ref. [35] further studies corroborated these results, obtaining a mean bias of −0.006 mm (−1.3%) when comparing TCCON FTIR PWV values to those obtained from meteorological radiosondes launched on Tenerife island and processed according to the GRUAN scheme (http://www.gruan.org, last access: 28 November 2020). The Almansa's study also found a relative difference of +3.4% respect to collocated CIMEL-AERONET data (FTIR-CIMEL).…”
Section: • Ftirmentioning
confidence: 74%
“…On the other hand, when analyzing the bias among techniques, the least differences are found respect to GNSS PWV with MB of 0.02 (3.3%), while the largest differences are respect to CIMEL-AERONET and FTIR PWV with MB of 0.33 mm (9.5%) and −0.57 mm (14.5%), respectively. These systematic differences can be attributed the possible calibration inaccuracy of the AERONET PWV product [35], while the differences found respect to FTIR PWV are likely due to spectroscopy inconsistences between the different spectral ranges in which the PWV is determined (930-960 nm for EKO PWV and 1500-2200 nm for FTIR PWV). The bias found respect to different techniques are within the uncertainty determined with the Monte-Carlo method (Section 5) with values ranging between 0.13 and 0.81 mm.…”
Section: Results: Comparison To Pwv Observationsmentioning
confidence: 96%
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“…It should be noted that these two high PWV amounts are extreme values at IZO given the predominantly dry atmospheric conditions of the observatory. Considering the TCCON FTIR PWV time series in the 2007-2019 period, the annual average of PWV is only 4.8 mm (standard deviation, σ, of 2.8 mm), with maximum PWV amounts reached in summer (mean and σ of 7.1 and 3.3 mm, respectively) [77]. All remaining inputs for the simulations have been kept identical.…”
Section: Ftir Micro-windows Selectionmentioning
confidence: 99%