Draft:1982 Burma cyclone
Draft article not currently submitted for review.
This is a draft Articles for creation (AfC) submission. It is not currently pending review. While there are no deadlines, abandoned drafts may be deleted after six months. To edit the draft click on the "Edit" tab at the top of the window. To be accepted, a draft should:
It is strongly discouraged to write about yourself, your business or employer. If you do so, you must declare it. Where to get help
How to improve a draft
You can also browse Wikipedia:Featured articles and Wikipedia:Good articles to find examples of Wikipedia's best writing on topics similar to your proposed article. Improving your odds of a speedy review To improve your odds of a faster review, tag your draft with relevant WikiProject tags using the button below. This will let reviewers know a new draft has been submitted in their area of interest. For instance, if you wrote about a female astronomer, you would want to add the Biography, Astronomy, and Women scientists tags. Editor resources
Last edited by WereSpielChequers (talk | contribs) 4 months ago. (Update) |
Meteorological history | |
---|---|
Formed | 30 April 1982 |
Dissipated | 4 May 1982 |
Extremely severe cyclonic storm | |
3-minute sustained (IMD) | |
Highest winds | 215 km/h (130 mph) |
Category 4-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 230 km/h (145 mph) |
Overall effects | |
Areas affected | Myanmar |
IBTrACS | |
Part of the 1982 North Indian Ocean cyclone season |
The 1982 Burma cyclone, also known as the 1982 Gwa cyclone,[1][2] was a powerful and destructive tropical cyclone which affected Myanmar during May 1982. The first tropical cyclone of the 1982 North Indian Ocean cyclone season, BOB 01 developed from a low-pressure area [to be determined].
Meteorological history[edit]
In later April, the monsoon trough was active south of Sri Lanka, extending eastward into the central portion of the Bay of Bengal. On 26 April, an area of convection associated with this trough was first monitored by the Joint Typhoon Warning Center (JTWC). On 1 May, a Tropical Cyclone Formation Alert was issued as a central dense overcast (CDO) formed over the system. The next day, the JTWC issued the first warning for the system.
The tropical cyclone tracked northeastward, remaining approximately 120 nm (222 km) east of India. While crossing the Bay of Bengal, the cyclone continued to intensify, peaking with 1-minute sustained winds of 125 kt prior to landfall. After landfall, the system rapidly weakened, dissipating on 4 May.[3]
Preparations and impacts[edit]
References[edit]
- ^ "Simulation of Storm Surges Along Myanmar Coast". IIT Delhi.
- ^ Brill, Dominik; Seeger, Katharina; Pint, Anna; Reize, Felix; Hlaing, Kay Thwe; Seeliger, Martin; Opitz, Stephan; Win, Khin Mi Mi; Nyunt, Win Thuzar; Aye, Nilar; Aung, Aung; Kyaw, Kyaw; Kraas, Frauke; Brückner, Helmut (April 2020). Costa, Pedro (ed.). "Modern and historical tropical cyclone and tsunami deposits at the coast of Myanmar: Implications for their identification and preservation in the geological record". Sedimentology. 67 (3): 1431–1459. doi:10.1111/sed.12586. ISSN 0037-0746.
- ^ "1982 Tropical Cyclone Report" (PDF). Joint Typhoon Warning Center. Archived from the original (PDF) on 2020-10-20. Retrieved 2024-01-22.