Investigation of the Synoptic and Dynamical Characteristics of Cyclone Shaheen (2021) and Its Influence on the Omani Coastal Region

Author:

Katsafados Petros1ORCID,Saviolakis Pantelis-Manolis1,Varlas George2ORCID,Ben-Romdhane Haifa34ORCID,Pavlopoulos Kosmas3ORCID,Spyrou Christos5ORCID,Farrah Sufian6

Affiliation:

1. Department of Geography, Harokopio University of Athens, HUA, 17671 Athens, Greece

2. Hellenic Centre for Marine Research, Institute of Marine Biological Resources and Inland Waters, 46.7 km of Athens-Sounio Ave., 19013 Anavissos, Greece

3. Department of Geography and Planning, Sorbonne University Abu Dhabi, Abu Dhabi P.O. Box 38044, United Arab Emirates

4. Department of Environmental Health and Safety, College of Health Sciences, Abu Dhabi University, Abu Dhabi P.O. Box 59911, United Arab Emirates

5. Research Centre for Atmospheric Physics and Climatology, Academy of Athens, 10679 Athens, Greece

6. Department of Meteorology, National Centre of Meteorology, Abu Dhabi P.O. Box 4815, United Arab Emirates

Abstract

Tropical Cyclone Shaheen (TCS), originating in the Arabian Sea on 30 September 2021, followed an east-to-west trajectory and made landfall as a category-1 cyclone in northern Oman on 3 October 2021, causing severe floods and damages before dissipating in the United Arab Emirates. This study aims to analyze the synoptic and dynamical conditions influencing Shaheen’s genesis and evolution. Utilizing ERA5 reanalysis data, SEVIRI-EUMETSAT imagery, and Sorbonne University Atmospheric Forecasting System (SUAFS) outputs, it was found that Shaheen manifested as a warm-core cyclone with moderate vertical wind shear within the eyewall. Distinctive features included a trajectory aligned with rising sea surface temperatures and increased specific humidity levels at 700 hPa in the Arabian Sea. As Shaheen approached the Gulf of Oman, a significant increase in rainfall rates occurred, correlated with variations in sea surface temperatures and vertical wind shear. Comparative analysis between SUAFS and ERA5 data revealed a slight northward shift in the SUAFS track and landfall. Advance warnings highlighted heavy rainfall, rough seas, and strong winds. This study provides valuable insights into the meteorological factors contributing to Shaheen’s formation and impact.

Publisher

MDPI AG

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