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2013–14 South-West Indian Ocean cyclone season

2013–14 South-West Indian Ocean cyclone season
2013-2014 South-West Indian Ocean cyclone season summary.png
Season summary map
Seasonal boundaries
First system formed October 23, 2013
Last system dissipated April 6, 2014
Strongest storm
Name Hellen
 • Maximum winds 230 km/h (145 mph)
(10-minute sustained)
 • Lowest pressure 915 hPa (mbar)
Seasonal statistics
Total disturbances 15
Total depressions 13
Total storms 11
Tropical cyclones 5
Intense tropical cyclones 5
Very intense tropical cyclones 2
Total fatalities 11 total
Total damage At least $89.2 million (2014 USD)
Related articles
South-West Indian Ocean tropical cyclone seasons
2011–12, 2012–13, 2013–14, 2014–15, 2015–16
Moderate tropical storm (MFR)
Tropical storm (SSHWS)
01R Oct 26 2013 0555Z.jpg 01R 2013 track.png
Duration October 23 – October 27
Peak intensity 65 km/h (40 mph) (10-min)  997 hPa (mbar)
Intense tropical cyclone (MFR)
Category 4 tropical cyclone (SSHWS)
Amara Dec 21 2013 0935z.jpg Amara 2013 track.png
Duration December 14 – December 27
Peak intensity 205 km/h (125 mph) (10-min)  935 hPa (mbar)
Very intense tropical cyclone (MFR)
Category 5 tropical cyclone (SSHWS)
Bruce Dec 21 2013 0755Z.jpg Bruce 2013 track.png
Duration December 20 (Entered basin) – December 23
Peak intensity 220 km/h (140 mph) (10-min)  920 hPa (mbar)
Intense tropical cyclone (MFR)
Category 4 tropical cyclone (SSHWS)
Bejisa Dec 31 2013 1010Z.jpg Bejisa 2013 track.png
Duration December 27 – January 4
Peak intensity 175 km/h (110 mph) (10-min)  950 hPa (mbar)
Tropical depression (MFR)
05R Jan 9 2014 0720Z.jpg 05R 2014 track.png
Duration January 7 – January 10
Peak intensity 55 km/h (35 mph) (10-min)  997 hPa (mbar)
Intense tropical cyclone (MFR)
Category 4 tropical cyclone (SSHWS)
Cyclone Colin Jan 11 2014 0815Z.jpg Colin 2014 track.png
Duration January 9 (Entered basin) – January 14
Peak intensity 205 km/h (125 mph) (10-min)  915 hPa (mbar)
Moderate tropical storm (MFR)
Tropical storm (SSHWS)
Deliwe Jan 17 2014 1055Z.jpg Deliwe 2014 track.png
Duration January 14 – January 22
Peak intensity 85 km/h (50 mph) (10-min)  990 hPa (mbar)
Zone of Disturbed Weather (MFR)
08R 18 January 2014.jpg 08R 2014 track.png
Duration January 16 – January 20
Peak intensity 35 km/h (25 mph) (10-min)  1004 hPa (mbar)
Tropical disturbance (MFR)
09R 28 January 2014.jpg 09R 2014 track.png
Duration January 24 – January 31
Peak intensity 45 km/h (30 mph) (10-min)  1002 hPa (mbar)

The 2013–14 South-West Indian Ocean cyclone season is an event in the annual cycle of tropical cyclone formation that ended on June 30, 2014. The season officially began on July 1, 2013, though the first tropical system designated by Météo-France was a short-lived tropical disturbance that developed on July 8. However, the first named storm was Cyclone Amara in December. Bruce was the first very intense tropical cyclone since Edzani in 2010, which originated from the Australian region. The strongest system of the cyclone season was Hellen, also one of the most intense tropical cyclones over the Mozambique Channel.

Within this basin, tropical and subtropical disturbances are officially monitored by the Regional Specialised Meteorological Centre on Réunion island, while the Mauritius and Madagascar weather services assign names to significant tropical and subtropical disturbances.

The predecessor to the season's first designated tropical depression began as an area of persistent convection well removed from any landmasses. The JTWC began issuing products on the storm complex on October 21, noting recent consolidation patterns and its association with an ill-defined low-level circulation center. Over subsequent hours, the system developed a central region of convection with incipient rainbands. Despite these signs of potential tropical cyclogenesis in the very near future, the storm remained unclassified for several days as it tracked generally towards the west. At 1200 UTC on October 25, however, Météo-France classified the system as a tropical disturbance. Though upper-level atmospheric conditions were rather conducive for continued strengthening, factors including decreasing convergence and marginally sustainable sea surface temperatures were expected to inhibit tropical development, and as such initial forecasts only anticipated minimal and gradual strengthening.


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