User:Tavantius/1952 North Indian Ocean cyclone season
| Tavantius/1952 North Indian Ocean cyclone season | |
|---|---|
 Season summary map | |
| Seasonal boundaries | |
| First system formed | Unknown |
| Last system dissipated | Unknown |
| Strongest storm | |
| Name | Unknown |
| Seasonal statistics | |
| Depressions | Unknown official, Unknown unofficial |
| Deep depressions | Unknown official, Unknown unofficial |
| Cyclonic storms | Unknown official, Unknown unofficial |
| Severe cyclonic storms | Unknown official, Unknown unofficial |
| Very severe cyclonic storms | Unknown official, Unknown unofficial |
| Extremely severe cyclonic storms | Unknown official, Unknown unofficial |
| Super cyclonic storms | Unknown official, Unknown unofficial |
| Total fatalities | Unknown |
| Total damage | $0,000 (1952 USD) |
| Related articles | |
The 1952 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The scope of this article is limited to the Indian Ocean in the Northern Hemisphere, east of the Horn of Africa and west of the Malay Peninsula. There are two main seas in the North Indian Ocean – the Arabian Sea to the west of the Indian subcontinent and the Bay of Bengal to the east. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the Joint Typhoon Warning Center releases unofficial advisories.
Systems
[edit]Depression One
[edit]| Depression (IMD) | |
| Duration | May 16 – May 17 |
|---|---|
| Peak intensity | Winds not specified; |
On May 14, an unsettled area of weather was identified over the southeastern Bay of Bengal. Developing into a well-marked low-pressure area the next day over Car Nicobar, on May 16, the disturbance developed into a depression around 70 mi (110 km) south-southwest of Port Blair. Tracking north soon after, the depression steadily weakened, degenerating into a trough of low-pressure on the evening of the next day.[1]
Port Blair received east-southeasterly winds of 35 mph (55 km/h) as the depression passed near it.[1]
Severe Cyclonic Storm Two
[edit]Bibliographies
[edit]- India Meteorological Department (1952). "Annual Summary — Storms & Depressions" (PDF). India Weather Review. National Oceanic and Atmospheric Administration. Retrieved September 2, 2024.
References
[edit]- ^ a b Indian Weather Review 1952, p. 3.