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2014–15 South-West Indian Ocean cyclone season
The 2014–15 South-West Indian Ocean cyclone season was an above average event in tropical cyclone formation. It began on November 15, 2014, and ended on April 30, 2015, with the exception for Mauritius and the Seychelles, for which it ended on May 15, 2015. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion.
During October 2014, the Mauritius Meteorological Services issued its seasonal outlook for the summer of 2014–15 and predicted that between ten and twelve named storms would develop during the season. The first tropical disturbance of the season developed on November 16, and quickly developed into the first named storm of the season and was named Adjali by Mauritius. The last tropical storm of this season, Tropical Depression 14, later known as Ikola, strengthened to a Category 1 tropical cyclone before it crossed on the Australian basin the next day. 2 storms, Bansi and Eunice, became Very Intense Tropical Cyclones.
An area of low pressure developed close to Diego Garcia on November 14. It slowly organized as it made a northwest–south-southeast loop over the next two days. By the evening of November 16, the center of the storm became more well defined with convective rainbands wrapped tightly into it. Around that time, RSMC La Réunion started tracking the system as a tropical disturbance, and subsequently upgraded it to a Tropical Depression. Later that day, the JTWC issued a Tropical Cyclone Formation Alert on the system. The depression strengthened further and became the first named tropical storm of the year. On the same day, Mauritius Meteorological Service, which usually names storms in the region, named the system Adjali. The JTWC also initiated advisories on Adjali. On November 17, MFR upgraded it to a Severe Tropical Storm. On November 20, Adjali turned west until reached the northern tip of Madagascar on November 23 and rapidly dissipated. It stayed well from land.
During November 25, RSMC La Réunion reported that Tropical Disturbance 2, had developed within a marginal environment for further development to the northeast of the Mascarene islands. During that day despite having a low-level circulation centre that was located to the east of the deepest atmospheric convection, the system developed into a tropical depression. The depression continued to intensified as it was classified as a tropical storm by the JTWC early on November 28. The next day, the system moved in a southwestward direction and cooler waters. With this, the MFR downgraded it to a tropical disturbance again on November 29, with the JTWC downgrading it to a tropical depression.[citation needed]
During December 30, Severe Tropical Cyclone Kate moved into the basin from the Australian region, where it was immediately classified as an intense tropical cyclone with 10-minute sustained wind speeds of 175 km/h (110 mph) by RSMC La Réunion. Over the next day the system rapidly weakened into a tropical storm as it moved into an unfavourable environment for development, before RSMC La Réunion and the JTWC issued their final advisories on the system during December 31.[citation needed]
On January 9, the MFR upgraded a low-pressure system east of Madagascar to a zone of disturbed weather, and the system became a tropical disturbance late on the next day. On January 11, the MFR upgraded the system to a tropical depression. Later that day, it intensified into a moderate tropical storm, receiving the name Bansi, whilst the JTWC upgraded it to a tropical storm. In the next day, the MFR upgraded Bansi to a tropical cyclone, as the system formed a ragged eye. On January 13, Bansi explosively intensified into a Category 5 cyclone. However, it soon weakened to a Category 2 on the SSHWS (intense tropical cyclone for MFR) due to an eyewall replacement cycle.
It re-intensified slowly to a Category 4 on the SSHWS as it moved East-Southeast until January 13. Then it slowly curved Southeast and impacted Rodrigues on January 14.[citation needed] Approximately 90 percent of the island was left without power as a result of the storm. Some flooding occurred and 115 people sought refuge in shelters. From this moment onwards it started weakening gradually at first, but then deteriorated quickly. On January 16, Bansi began to undergo an extratropical transition. Consequently, the MFR and JTWC issued Bansi's final warning, as Bansi was absorbed by an extratropical cyclone to the northeast.[citation needed]
On January 11, the JTWC started to monitor a weak tropical disturbance inland over Mozambique. On January 14, the MFR upgraded a low-pressure system east of Mozambique to a zone of disturbed weather, and the system became a tropical disturbance late on the same day. On January 15, the MFR upgraded the system to a tropical depression. Later next day, it intensified into a moderate tropical storm, receiving the name Chedza, whilst the JTWC upgraded it to a tropical storm. On the same day, MFR upgraded it to a Severe Tropical Storm. Later that day, it made landfall over Madagascar. On January 17, it left Madagascar and went to the South-West Indian Ocean. On the next day, it re-intensified to a Severe Tropical Storm. On January 19, Chedza began to undergo an extratropical transition. Consequently, the MFR issued Chedza's final warning.[citation needed]
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2014–15 South-West Indian Ocean cyclone season AI simulator
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2014–15 South-West Indian Ocean cyclone season
The 2014–15 South-West Indian Ocean cyclone season was an above average event in tropical cyclone formation. It began on November 15, 2014, and ended on April 30, 2015, with the exception for Mauritius and the Seychelles, for which it ended on May 15, 2015. These dates conventionally delimit the period of each year when most tropical and subtropical cyclones form in the basin, which is west of 90°E and south of the Equator. Tropical and subtropical cyclones in this basin are monitored by the Regional Specialised Meteorological Centre in Réunion.
During October 2014, the Mauritius Meteorological Services issued its seasonal outlook for the summer of 2014–15 and predicted that between ten and twelve named storms would develop during the season. The first tropical disturbance of the season developed on November 16, and quickly developed into the first named storm of the season and was named Adjali by Mauritius. The last tropical storm of this season, Tropical Depression 14, later known as Ikola, strengthened to a Category 1 tropical cyclone before it crossed on the Australian basin the next day. 2 storms, Bansi and Eunice, became Very Intense Tropical Cyclones.
An area of low pressure developed close to Diego Garcia on November 14. It slowly organized as it made a northwest–south-southeast loop over the next two days. By the evening of November 16, the center of the storm became more well defined with convective rainbands wrapped tightly into it. Around that time, RSMC La Réunion started tracking the system as a tropical disturbance, and subsequently upgraded it to a Tropical Depression. Later that day, the JTWC issued a Tropical Cyclone Formation Alert on the system. The depression strengthened further and became the first named tropical storm of the year. On the same day, Mauritius Meteorological Service, which usually names storms in the region, named the system Adjali. The JTWC also initiated advisories on Adjali. On November 17, MFR upgraded it to a Severe Tropical Storm. On November 20, Adjali turned west until reached the northern tip of Madagascar on November 23 and rapidly dissipated. It stayed well from land.
During November 25, RSMC La Réunion reported that Tropical Disturbance 2, had developed within a marginal environment for further development to the northeast of the Mascarene islands. During that day despite having a low-level circulation centre that was located to the east of the deepest atmospheric convection, the system developed into a tropical depression. The depression continued to intensified as it was classified as a tropical storm by the JTWC early on November 28. The next day, the system moved in a southwestward direction and cooler waters. With this, the MFR downgraded it to a tropical disturbance again on November 29, with the JTWC downgrading it to a tropical depression.[citation needed]
During December 30, Severe Tropical Cyclone Kate moved into the basin from the Australian region, where it was immediately classified as an intense tropical cyclone with 10-minute sustained wind speeds of 175 km/h (110 mph) by RSMC La Réunion. Over the next day the system rapidly weakened into a tropical storm as it moved into an unfavourable environment for development, before RSMC La Réunion and the JTWC issued their final advisories on the system during December 31.[citation needed]
On January 9, the MFR upgraded a low-pressure system east of Madagascar to a zone of disturbed weather, and the system became a tropical disturbance late on the next day. On January 11, the MFR upgraded the system to a tropical depression. Later that day, it intensified into a moderate tropical storm, receiving the name Bansi, whilst the JTWC upgraded it to a tropical storm. In the next day, the MFR upgraded Bansi to a tropical cyclone, as the system formed a ragged eye. On January 13, Bansi explosively intensified into a Category 5 cyclone. However, it soon weakened to a Category 2 on the SSHWS (intense tropical cyclone for MFR) due to an eyewall replacement cycle.
It re-intensified slowly to a Category 4 on the SSHWS as it moved East-Southeast until January 13. Then it slowly curved Southeast and impacted Rodrigues on January 14.[citation needed] Approximately 90 percent of the island was left without power as a result of the storm. Some flooding occurred and 115 people sought refuge in shelters. From this moment onwards it started weakening gradually at first, but then deteriorated quickly. On January 16, Bansi began to undergo an extratropical transition. Consequently, the MFR and JTWC issued Bansi's final warning, as Bansi was absorbed by an extratropical cyclone to the northeast.[citation needed]
On January 11, the JTWC started to monitor a weak tropical disturbance inland over Mozambique. On January 14, the MFR upgraded a low-pressure system east of Mozambique to a zone of disturbed weather, and the system became a tropical disturbance late on the same day. On January 15, the MFR upgraded the system to a tropical depression. Later next day, it intensified into a moderate tropical storm, receiving the name Chedza, whilst the JTWC upgraded it to a tropical storm. On the same day, MFR upgraded it to a Severe Tropical Storm. Later that day, it made landfall over Madagascar. On January 17, it left Madagascar and went to the South-West Indian Ocean. On the next day, it re-intensified to a Severe Tropical Storm. On January 19, Chedza began to undergo an extratropical transition. Consequently, the MFR issued Chedza's final warning.[citation needed]