Cloud and building shadows frequently appear in high spatial resolution satellite images in the visible channels. During a solar eclipse, the shadow of the Moon can be identified in satellite imagery. Typically, shadows are removed or ignored when deriving satellite products, such as cloud properties, aerosol optical thickness, atmospheric composition. We have analyzed the impacts of shadows on the satellite products and utilised the shadows to derive new satellite products. In our analyses the shadows include cloud shadows, building shadows, and the shadow of the Moon.
We have developed an automated cloud shadow detection algorithm for TROPOMI, called DARCLOS (Trees et al., 2022). This algorithm has been used in deriving the TROPOMI surface directional Lambertian Equivalent reflection (DLER) product (Tilstra et al., 2023). We analysed TROPOMI absorbing aerosol product (AAI) and NO2 products for pixels inside and outside the cloud shadows. However, we did not find significant bias in the AAI (Trees et al., 2024b) and NO2 products in the cloud shadows.
We restored the TROPOMI and GOME-2 satellite measurements during solar eclipses, consequently the artefact of high AAI values in TROPOMI and GOME-2 AAI products disappeared (Trees et al., 2021). We analysed TROPOMI NO2 products during solar eclipse and found the increasing NO2 column densities with increasing obscuration fractions during the solar eclipse (Schrijver, 2024).
Solar eclipse can be detected in multiple time slots of geostationary satellite images. We found shallow cumulus clouds over land disappeared rapidly during solar eclipses and simulated this process using a LES mdoel (Trees et al., 2024a).
Cloud shadows and building shadows in satellite images have also been used to derive cloud optical thickness. We derived aerosol optical thickness at selected locations using building shadows in GF-2 images (Qiao et al., 2024). The cloud shadows in Sentinel-2 images were used to derive aerosol optical thickness and compared with MODIS measurements.
In the presentation, we will show some highlights of the papers and provide a summary of the project.
References
Qiao Congcong,Zhou ying,Zong Xuemei, Huo Juan, Sun Bin, Duan Minzheng, 2024a,A Novel Algorithm for Deriving Aerosol Optical Depth over Cities using the Building Shadows of High-resolution Satellite Imagery paper, Submitted to TGRS, 2024
Schrijver, Impact of solar eclipses on NO2 in the Earth's atmosphere as measured from space by TROPOMI, master thesis, TU Delft, 2024.
Tilstra, L. G., de Graaf, M., Trees, V., Litvinov, P., Dubovik, O., and Stammes, P.: A directional surface reflectance climatology determined from TROPOMI observations, Atmos. Meas. Tech. Discuss. [preprint], https://doi.org/10.5194/amt-2023-222, accepted, 2023.
Trees, V., Wang, P. & Stammes, P. Restoring the top-of-atmosphere reflectance during solar eclipses: a proof of concept with the UV absorbing aerosol index measured by TROPOMI. Atmos. Chem. Phys. 21, 8593–8614 (2021).
Trees, V. J. H., Wang, P., Stammes, P., Tilstra, L. G., Donovan, D. P., and Siebesma, A. P.: DARCLOS: a cloud shadow detection algorithm for TROPOMI, Atmos. Meas. Tech., 15, 3121–3140, https://doi.org/10.5194/amt-15-3121-2022, 2022.
Trees, V.J.H., Stephan R. de Roode, Job I. Wiltink, Jan Fokke Meirink, Ping Wang, Piet Stammes and A. Pier Siebesma. Clouds dissipate quickly during solar eclipses as the land surface cools. Nature Communications Earth & Environment. 12 February 2024a.
Trees, V. J. H. et al., Cancellation of cloud shadow effects in the absorbing aerosol index retrieval algorithm of TROPOMI, submitted to AMTD, 2024b.