Water vapour retrieval using the Precision Solar Spectroradiometer
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Published:2018-02-27
Issue:2
Volume:11
Page:1143-1157
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ISSN:1867-8548
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Container-title:Atmospheric Measurement Techniques
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language:en
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Short-container-title:Atmos. Meas. Tech.
Author:
Raptis Panagiotis-IoannisORCID, Kazadzis Stelios, Gröbner Julian, Kouremeti Natalia, Doppler LionelORCID, Becker Ralf, Helmis Constantinos
Abstract
Abstract. The Precision Solar Spectroradiometer (PSR) is a new spectroradiometer
developed at Physikalisch-Meteorologisches Observatorium Davos – World
Radiation Center (PMOD–WRC), Davos, measuring direct solar irradiance at the
surface, in the 300–1020 nm spectral range and at high temporal resolution. The
purpose of this work is to investigate the instrument's potential to
retrieve integrated water vapour (IWV) using its spectral measurements. Two
different approaches were developed in order to retrieve IWV: the first one
uses single-channel and wavelength measurements, following a theoretical water
vapour high absorption wavelength, and the second one uses direct sun
irradiance integrated at a certain spectral region. IWV results have been
validated using a 2-year data set, consisting of an AERONET sun-photometer
Cimel CE318, a Global Positioning System (GPS), a microwave radiometer profiler (MWP) and radiosonde retrievals recorded at Meteorological
Observatorium Lindenberg, Germany. For the monochromatic approach, better
agreement with retrievals from other methods and instruments was achieved using
the 946 nm channel, while for the spectral approach the 934–948 nm
window was used. Compared to other instruments' retrievals, the monochromatic approach
leads to mean relative differences up to 3.3 % with the coefficient of
determination (R2) being in the region of 0.87–0.95, while for the
spectral approach mean relative differences up to 0.7 % were recorded
with R2 in the region of 0.96–0.98. Uncertainties related to IWV
retrieval methods were investigated and found to be less than 0.28 cm for
both methods. Absolute IWV deviations of differences between PSR and other
instruments were determined the range of 0.08–0.30 cm and only in extreme
cases would reach up to 15 %.
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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