Further validation of the estimates of the downwelling solar radiation at ground level in cloud-free conditions provided by the McClear service: the case of Sub-Saharan Africa and the Maldives Archipelago
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Published:2023-04-17
Issue:7
Volume:16
Page:2001-2036
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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:
Wandji Nyamsi WilliamORCID, Saint-Drenan Yves-MarieORCID, Arola AnttiORCID, Wald LucienORCID
Abstract
Abstract. Being part of the Copernicus Atmosphere Monitoring
Service (CAMS), the McClear service provides estimates of the downwelling
shortwave irradiance and its direct and diffuse components received at
ground level in cloud-free conditions, with inputs on ozone, water vapor and
aerosol properties from CAMS. McClear estimates have been validated over
several parts of the world by various authors. This article makes a step
forward by comparing McClear estimates to measurements performed at 44
ground-based stations located in Sub-Saharan Africa and the Maldives
Archipelago in the Indian Ocean. The global irradiance received on a
horizontal surface (G) and its direct component received at normal incidence
(BN) provided by the McClear-v3 service were compared to 1 min measurements made in cloud-free conditions at the stations. The correlation
coefficient is greater than 0.96 for G, whereas it is greater than 0.70 at all
stations but five for BN. The mean of G is accurately estimated at
stations located in arid climates (BSh, BWh, BSk, BWk) and temperate
climates without a dry season and a hot or warm summer (Cfa, Cfb) or with a dry
and hot summer (Csa) with a relative bias in the range [−1.5, 1.5] %
with respect to the means of the measurements at each station. It is
underestimated in tropical climates of monsoon type (Am) and overestimated in
tropical climates of savannah type (Aw) and temperate climates with a dry
winter and hot (Cwa) or warm (Cwb) summer. The McClear service tends to
overestimate the mean of BN. The standard deviation of errors for G
ranges between 13 W m−2 (1.3 %) and 31 W m−2 (3.7 %) and
that for BN ranges between 31 W m−2 (3.0 %), and 70 W m−2
(7.9 %). Both offer small variations in time and space. A review of
previous works reveals no significant difference between their results and
ours. This work establishes a general overview of the performances of the
McClear service.
Funder
European Centre for Medium-Range Weather Forecasts
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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