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🔆 Cyclone Shakti: Severe Cyclonic Storm over Arabian Sea (2025)

📍 Classification:
Cyclone Shakti was classified as a Severe Cyclonic Storm (SCS) by the India Meteorological Department (IMD) with wind speeds of 130–145 km/h.
It formed over the east-central Arabian Sea, serving as a key case for studying tropical cyclone dynamics — oceanic heat, Coriolis force, and atmospheric instability.

📍 Naming:
The name “Shakti”, meaning power and resilience, was proposed by Sri Lanka under the WMO–ESCAP Panel on Tropical Cyclones.
Cyclone names are drawn from lists submitted by 13 member countries (including India, Bangladesh, Oman, Myanmar, etc.) to enhance clarity in communication and disaster management.

📍 Formation Mechanism:
Warm sea surface temperatures (>27°C) provided latent heat for convection.
Low pressure formed at the surface; Coriolis effect induced rotation.
Upper-level outflow maintained structure, while low wind shear over the Arabian Sea (Oct 2025) aided intensification into a Severe Cyclonic Storm.

📍 Climatic Background:
Arabian Sea cyclones are rising in frequency and intensity due to warming trends — India’s mean temperature has risen by ~1.2°C since 1901 (CSE, 2017).
Reduced vertical wind shear and higher moisture transport from the equatorial zone support cyclone formation along India’s west coast.

📍 Geographical Path:
Formed near 21°N, 66.8°E, around 270 km southwest of Naliya, 300 km east of Porbandar, and 360 km south of Karachi (as of Oct 3, 2025).
Moved northwestward under subtropical westerly influence, a typical post-monsoon trajectory.
The Arabian Sea’s semi-enclosed basin traps heat and moisture, making it increasingly cyclone-prone.


#CycloneShakti #environment #Geography



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🔆 Cyclone Shakti: Severe Cyclonic Storm over Arabian Sea (2025)

📍 Classification:
Cyclone Shakti was classified as a Severe Cyclonic Storm (SCS) by the India Meteorological Department (IMD) with wind speeds of 130–145 km/h.
It formed over the east-central Arabian Sea, serving as a key case for studying tropical cyclone dynamics — oceanic heat, Coriolis force, and atmospheric instability.

📍 Naming:
The name “Shakti”, meaning power and resilience, was proposed by Sri Lanka under the WMO–ESCAP Panel on Tropical Cyclones.
Cyclone names are drawn from lists submitted by 13 member countries (including India, Bangladesh, Oman, Myanmar, etc.) to enhance clarity in communication and disaster management.

📍 Formation Mechanism:
Warm sea surface temperatures (>27°C) provided latent heat for convection.
Low pressure formed at the surface; Coriolis effect induced rotation.
Upper-level outflow maintained structure, while low wind shear over the Arabian Sea (Oct 2025) aided intensification into a Severe Cyclonic Storm.

📍 Climatic Background:
Arabian Sea cyclones are rising in frequency and intensity due to warming trends — India’s mean temperature has risen by ~1.2°C since 1901 (CSE, 2017).
Reduced vertical wind shear and higher moisture transport from the equatorial zone support cyclone formation along India’s west coast.

📍 Geographical Path:
Formed near 21°N, 66.8°E, around 270 km southwest of Naliya, 300 km east of Porbandar, and 360 km south of Karachi (as of Oct 3, 2025).
Moved northwestward under subtropical westerly influence, a typical post-monsoon trajectory.
The Arabian Sea’s semi-enclosed basin traps heat and moisture, making it increasingly cyclone-prone.


#CycloneShakti #environment #Geography

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