Abstract
Precipitable water vapor retrievals are of major importance for assessing and understanding atmospheric radiative balance and solar radiation resources. On that basis, this study presents the first PWV values measured with a novel EKO MS-711 grating spectroradiometer from direct normal irradiance in the spectral range between 930 and 960 nm at the Izaña Observatory (IZO, Spain) between April and December 2019. The expanded uncertainty of PWV (UPWV) was theoretically evaluated using the Monte-Carlo method, obtaining an averaged value of 0.37 ± 0.11 mm. The estimated uncertainty presents a clear dependence on PWV. For PWV ≤ 5 mm (62% of the data), the mean UPWV is 0.31 ± 0.07 mm, while for PWV > 5 mm (38% of the data) is 0.47 ± 0.08 mm. In addition, the EKO PWV retrievals were comprehensively compared against the PWV measurements from several reference techniques available at IZO, including meteorological radiosondes, Global Navigation Satellite System (GNSS), CIMEL-AERONET sun photometer and Fourier Transform Infrared spectrometry (FTIR). The EKO PWV values closely align with the above mentioned different techniques, providing a mean bias and standard deviation of −0.30 ± 0.89 mm, 0.02 ± 0.68 mm, −0.57 ± 0.68 mm, and 0.33 ± 0.59 mm, with respect to the RS92, GNSS, FTIR and CIMEL-AERONET, respectively. According to the theoretical analysis, MB decreases when comparing values for PWV > 5 mm, leading to a PWV MB between −0.45 mm (EKO vs. FTIR), and 0.11 mm (EKO vs. CIMEL-AERONET). These results confirm that the EKO MS-711 spectroradiometer is precise enough to provide reliable PWV data on a routine basis and, as a result, can complement existing ground-based PWV observations. The implementation of PWV measurements in a spectroradiometer increases the capabilities of these types of instruments to simultaneously obtain key parameters used in certain applications such as monitoring solar power plants performance.
Highlights
In recent decades, greenhouse gases (GHG) have become of major interest as main drivers of climate change [1]
We present the comparison between the EKO PWV retrievals determined in the spectral range between 930 and 960 nm and other techniques available (RS92, Global Navigation Satellite System (GNSS), CIMEL-AErosol RObotic NETwork (AERONET) and Fourier Transform Infrared spectrometry (FTIR)) at Izaña Observatory between April and
For FTIR and CIMEL-AERONET the temporal window was reduced to 2 min around each EKO measurement
Summary
Greenhouse gases (GHG) have become of major interest as main drivers of climate change [1]. 2021, 13, 350 is driven by temperature, with a strong positive feedback in the Earth’s climate system [1]. It has been defined as an “essential climate variable” by the World Meteorological. Water vapor is one of the greatest sources of error in space-based remote sensing and communications, leading to errors in satellite pointing and attenuation on their signals [6]. In this context, precise measurements atmospheric water vapor content measurements with high temporal frequency and spatial resolution are mandatory
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