{"id":66500,"date":"2026-01-02T10:10:22","date_gmt":"2026-01-02T04:40:22","guid":{"rendered":"https:\/\/vajiramandravi.com\/current-affairs\/?p=66500"},"modified":"2026-01-02T16:05:17","modified_gmt":"2026-01-02T10:35:17","slug":"cyclone-shakti-maharashtra","status":"publish","type":"post","link":"https:\/\/vajiramandravi.com\/current-affairs\/cyclone-shakti-maharashtra\/","title":{"rendered":"Cyclone Shakti, Naming, Formation, Location, Classification"},"content":{"rendered":"

Cyclone Shakti is a recent example of a tropical cyclone that formed over the Arabian Sea in 2025. It provides an important case study for understanding cyclone formation, movement, and classification in India. The event highlights the increasing trend of severe cyclones over the Arabian Sea as reported by the Indian Meteorological Department (IMD) and Indian Institute of Tropical Meteorology (IITM) due to warming ocean temperatures.<\/span><\/p>\n

Cyclone Shakti<\/b><\/h2>\n

Cyclone Shakti was classified as a <\/span>Severe Cyclonic Storm (SCS)<\/b> by the IMD. It formed over the east-central Arabian Sea<\/strong><\/a> with wind speeds expected reaching 130-145 km\/h. The cyclone serves as a representative example for studying the physical processes of tropical cyclone development, including oceanic heat content, Coriolis force, and atmospheric instability. Such cyclones are part of the tropical storm system in the North Indian Ocean Basin.<\/span><\/p>\n

Cyclone Shakti 2025 Naming<\/b><\/h2>\n

The naming of Cyclone Shakti 2025 follows the guidelines of the World Meteorological Organization<\/strong><\/a> (WMO) and the ESCAP Panel on Tropical Cyclones. The name \u201cShakti,\u201d proposed by Sri Lanka, symbolizes power and resilience. Names are selected from lists contributed by 13 member countries, including India, Bangladesh, Oman, and Myanmar. The purpose of naming cyclones is to facilitate better communication and public awareness during weather forecasting and disaster management.<\/span><\/p>\n

\u00a0Cyclone Shakti Formation<\/b><\/h2>\n

Cyclone Shakti formed through a process typical of tropical cyclone development. Warm ocean waters above 27\u00b0C provided latent heat, fueling convection. Rising moist air created low pressure at the surface, while the Coriolis effect caused rotation, forming a cyclonic system. In the upper troposphere, outflow maintained the system\u2019s structure. The low vertical wind shear over the Arabian Sea in October 2025 allowed the cyclone to intensify into a Severe Cyclonic Storm.<\/span><\/p>\n

Factors Affecting Cyclone Formation in Arabian Sea<\/b><\/h2>\n

The Arabian Sea has become increasingly favorable for cyclones due to changing climatic and oceanic conditions. According to a 2017 study by the Centre for Science and Environment (CSE) the annual mean temperature of India has increased by about 1.2\u2103 since 1901. This warming has enhanced the frequency of intense cyclones. Additionally, reduced vertical wind shear and increased moisture transport from the equatorial region have supported cyclone formation near India\u2019s west coast.<\/span><\/p>\n

Cyclone Shakti Geographical Location and Path<\/b><\/h2>\n

Cyclone Shakti developed over the east-central Arabian Sea, roughly near 21\u00b0N latitude and 66.8\u00b0E longitude. Located about 270 km southwest to Naliya, 300km east to Porbandar and 360 km south of Karachi, as of Oct 03, 2025 morning. Its path followed a typical northwestward movement under the influence of subtropical westerly winds. The Arabian Sea\u2019s unique geography- enclosed by landmasses on three sides and open toward the southwest- helps trap heat and moisture, providing ideal conditions for cyclone formation. This path also reflects the regional wind circulation patterns during the post-monsoon season.<\/span><\/p>\n

Classification of Cyclones in India<\/b><\/h2>\n

The IMD classifies cyclones based on their wind speeds and pressure levels. Cyclone Shakti falls under the \u201cSevere Cyclonic Storm\u201d category with sustained wind speeds between 118 and 165 km\/h. The classification of cyclones<\/strong><\/a> helps in understanding cyclone intensity and potential damage levels. Such categorization also aligns with the international Saffir-Simpson Scale, though the Indian scale has region-specific terminology for the North Indian Ocean basin.<\/span><\/p>\n\n\n\n\n\n\n\n\n\n
Classification of Cyclones in India<\/b><\/td>\n<\/tr>\n
\n

IMD Category<\/b><\/p>\n<\/td>\n

\n

Wind Speed (km\/h)<\/b><\/p>\n<\/td>\n

\n

Example<\/b><\/p>\n<\/td>\n<\/tr>\n

\n

Cyclonic Storm<\/span><\/p>\n<\/td>\n

\n

62-88<\/span><\/p>\n<\/td>\n

\n

Cyclone Nilam (2012)<\/span><\/p>\n<\/td>\n<\/tr>\n

\n

Severe Cyclonic Storm<\/span><\/p>\n<\/td>\n

\n

89-117<\/span><\/p>\n<\/td>\n

\n

Cyclone Ockhi (2017)<\/span><\/p>\n<\/td>\n<\/tr>\n

\n

Very Severe Cyclonic Storm<\/span><\/p>\n<\/td>\n

\n

118-165<\/span><\/p>\n<\/td>\n

\n

Cyclone Hudhud (2014)<\/span><\/p>\n<\/td>\n<\/tr>\n

\n

Extremely Severe Cyclonic Storm<\/span><\/p>\n<\/td>\n

\n

166-220<\/span><\/p>\n<\/td>\n

\n

Cyclone Tauktae (2021)<\/span><\/p>\n<\/td>\n<\/tr>\n

\n

Super Cyclone<\/span><\/p>\n<\/td>\n

\n

>221<\/span><\/p>\n<\/td>\n

\n

Odisha Super Cyclone (1999)<\/span><\/p>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

Cyclone Trends in the Arabian Sea<\/b><\/h2>\n

The Arabian Sea, traditionally less active than the Bay of Bengal, has witnessed a rise in intense cyclones over the past two decades. The IITM and Union Ministry of Earth Sciences\u2019 2021 Annual Climate Report noted a 52% increase in Severe Cyclonic Storms in the Arabian Sea between 2001 and 2019. Cyclone Shakti exemplifies this growing pattern, showing how climatic warming and Indian Ocean Dipole events influence cyclone frequency and intensity.<\/span><\/p>\n

Cyclone Shakti Challenges<\/b><\/h2>\n

Cyclone Shakti poses multi-dimensional challenges affecting ecology, economy, and human settlements along the western coast of India.<\/span><\/p>\n