- 1ERATOSTHENES Centre of Excellence, Limassol, Cyprus
- 2Cyprus University of Technology, Department of Civil Engineering and Geomatics, Limassol, Cyprus
- 3Leibniz Institute for Tropospheric Research, Leipzig, Germany
This study utilizes the results of the Cyprus Cloud Aerosol and Radiation Experiment (CyCARE) campaign that took place in Limassol, Cyprus, during the period October 2016 - March 2018. The cloudnet target classification scheme was followed for the retrieval of cloud geometrical and microphysical properties and a climatological statistical analysis was applied for the investigation of cloud seasonal variability and characteristics. Of the total number of 1,338,785 available vertical profiles 440,377 (33%) were found to contain hydrometeors. The applied statistical analysis revealed that, in the presence of clouds, ice phase has appeared in 86% of the cases, mixed phase was identified in 43% of the cases, and liquid phase was observed in 42% of the cases. Precipitation (drizzle or rain) occurred in 28% of the cases. The seasonal analysis showed that clouds over Limassol during the study period are more frequent during the winter season (60%) followed by spring (22%) and autumn (17%). The most frequent cloud type is mixed phased clouds (354,440 profiles), followed by pure ice clouds (251,402) and liquid phase clouds (125,838). Concerning the cloud geometrical characteristics, cloud base height ranged from a median value of 1478 m for liquid precipitable clouds during winter to 9803 m for ice clouds during summer. Cloud top height varied from a median value of 1977 m for liquid precipitable clouds during winter to 10271 m for ice clouds during summer. Cloud vertical thickness ranged from a median of 249 m for liquid clouds during spring to 5519 m for mixed phase precipitable clouds during spring. Since June 2024 a new permanent ground-based remote sensing station, namely Cyprus Aerosol Remote sensing Observatory (CARO), has been established in Limassol and the continuous observations will be used in future aerosol-cloud interaction relevant studies in the region of eastern Mediterranean.
Acknowledgements
The authors acknowledge the ‘EXCELSIOR’: ERATOSTHENES: EΧcellence Research Centre for Earth Surveillance and Space-Based Monitoring of the Environment H2020 Widespread Teaming project (www.excelsior2020.eu). The ‘EXCELSIOR’ project has received funding from he European Union’s Horizon 2020 research and innovation programme under Grant Agreement No 857510, from the Government of the Republic of Cyprus through the Directorate General for the European Programmes, Coordination and Development and the Cyprus University of Technology. This study was supported by the ATARRI Horizon Europe Widespread Twinning Project. ATARRI receives funding from the European Union’s Horizon Europe Twinning Call (HORIZON-WIDERA-2023-ACCESS-02) under the grant agreement No 101160258.
How to cite: Kotsias, G., Mamouri, R.-E., Nisantzi, A., and Seifert, P.: Cloud observations over Limassol, Cyprus using CLOUDNET facilities, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-18461, https://doi.org/10.5194/egusphere-egu25-18461, 2025.