4.7 Article

Global Cloudiness and Cloud Top Information from AVHRR in the 42-Year CLARA-A3 Climate Data Record Covering the Period 1979-2020

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REMOTE SENSING
卷 15, 期 12, 页码 -

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MDPI
DOI: 10.3390/rs15123044

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climate monitoring; global cloudiness; cloud trends; cloud detection

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This paper examines the quality of global cloud fraction and cloud-top height products provided by the CM SAF cLoud, Albedo and surface RAdiation dataset from the AVHRR data (CLARA-A3) climate data record produced by the EUMETSAT CM SAF. Compared to other cloud CDRs and CALIPSO-CALIOP cloud lidar data, CLARA-A3 shows improved cloud detection, especially over ocean surfaces, and better accuracy in global cloud-top height measurements. The study attempts to estimate trends in observable low-level clouds and finds inconclusive results in the tropics, with small negative trends over oceanic surfaces outside the core tropical region.
This paper investigates the quality of global cloud fraction and cloud-top height products provided by the third edition of the CM SAF cLoud, Albedo and surface RAdiation dataset from the AVHRR data (CLARA-A3) climate data record (CDR) produced by the EUMETSAT Climate Monitoring Satellite Application Facility (CM SAF). Compared with with CALIPSO-CALIOP cloud lidar data and six other cloud CDRs, including the predecessor CLARA-A2, CLARA-A3 has improved cloud detection, especially over ocean surfaces, and improved geographical variation and cloud detection efficiency. In addition, CLARA-A3 exhibits remarkable improvements in the accuracy of its global cloud-top height measurements. For example, in tropical regions, previous underestimations for high-level clouds are reduced by more than 2 km. By taking advantage of more realistic descriptions of global cloudiness, this study attempted to estimate trends in the observable fraction of low-level clouds, acknowledging their importance in producing a net climate cooling effect. The results were generally inconclusive in the tropics, mainly due to the interference of El Nino modes during the period under study. However, the analysis found small negative trends over oceanic surfaces outside the core tropical region. Further studies are needed to verify the significance of these results.

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