Tag Archives: Mauritius

Tropical Cyclone Carlos Stronger As It Meanders North of Mauritius

Tropical Cyclone Carlos strengthened on Sunday as it meandered slowly north of Mauritius.  At 10:00 p.m. EST on Sunday the center of Tropical Cyclone Carlos was located at latitude 18.0°S and longitude 57.9°E which put it about 160 miles (260 km) north-northeast of Port Louis, Mauritius.  Carlos was moving toward the east-southeast at 3 m.p.h. (5 km/h).  The maximum sustained wind speed was 65 m.p.h. (105 km/h) and there were wind gusts to 80 m.p.h. (130 km/h).  The minimum surface pressure was 987.

Although Tropical Cyclone Carlos strengthened on Sunday, the circulation is exhibiting some effects of vertical wind shear.  Thunderstorms dissipated north of the center of circulation and the strongest thunderstorms are currently forming south of the center.  A primary band of storms extends southeast of the center of circulation.  A new broken band of showers and thunderstorms is beginning to develop around the northern periphery of the circulation.  The thunderstorms south of the center are generating upper level divergence which is pumping out mass to the southeast of the tropical cyclone.

The environment around Tropical Cyclone Carlos has both favorable and unfavorable factors.  Carlos will be moving over water where the Sea Surface Temperature is near 28°C which means there is sufficient energy in the upper ocean.  However, an upper level ridge east of Tropical Cyclone Carlos is generating northwesterly winds which are blowing across the top of the circulation.  The upper level winds are generating moderate vertical wind shear which is inhibiting the development of thunderstorms northwest of the center.  The wind shear is contributing to the asymmetrical distribution of the storms around the tropical cyclone and it is inhibiting divergence to the west of Carlos.  If the wind shear continues, it will continue to inhibit intensification.  Tropical Cyclone Carlos does have a very well organized low level circulation and it could intensify if the wind shear decreases.

The steering currents around Tropical Cyclone Carlos are weak, which is why it has not moved much during the past 24 hours.  A subtropical ridge east of Carlos is forecast to strengthen and the ridge is likely to steer the tropical cyclone more toward the southwest during the next day or two.  On its anticipated track the center of Tropical Cyclone Carlos could be near Mauritius in about 24 hours.  Carlos could be approaching La Reunion in 36 hours.  Tropical Cyclone Carlos could be the equivalent of a strong tropical storm or a hurricane when it approaches Mauritius and La Reunion.  Carlos could bring gusty winds and locally heavy rain to those locations.

Tropical Cyclone Carlos Strengthens North of Mauritius

Tropical Cyclone Carlos strengthened on Saturday as it moved north of Mauritius and La Reunion.  At 10:00 p.m. EST on Saturday the center of Tropical Cyclone Carlos was located at latitude 17.5°S and longitude 56.7°E which put it about 190 miles (310 km) north-northwest of Port Louis, Mauritius.  Carlos was moving toward the south at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 50 m.p.h. (80 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 995 mb.

The circulation of Tropical Cyclone Carlos was asymmetrical for much of Saturday, but more thunderstorms formed close to the center of circulation during the past few hours.  There is a small circular clear area at the center of circulation which could indicate the formation of an eye.  Strong thunderstorms are building in a circular ring around the clear area.  The strongest winds are occurring in those thunderstorms.  There are additional showers and thunderstorms developing in bands in the eastern half of the circulation.  Few thunderstorms are forming in the western half of the circulation.  The thunderstorms around core of the circulation are generating upper level divergence which is pumping out mass.

Tropical Cyclone Carlos is moving through an environment that is favorable for intensification.  It is moving over water where the Sea Surface Temperature is near 28.5°C.  The upper level winds are weak and there is little vertical wind shear.  Carlos is likely to strengthen and there could be a period of rapid intensification if the inner core consolidates around and eye.  Tropical Cyclone Carlos is likely to intensify into the equivalent of a hurricane during the next several days.

Carlos is moving around the western end of a subtropical ridge which is steering the tropical cyclone slowly southward.  A general southward motion is expected to continue for another day or two.  After that time the subtropical ridge is expected to strengthen and steer Tropical Cyclone Carlos more toward the southwest.  On its anticipated track the center of Tropical Cyclone Carlos could be approaching Mauritius and La Reunion in 36 to 48 hours.  Even if the center passes northwest of those locations, Tropical Cyclone Carlos could come close enough to bring gusty winds and locally heavy rainfall.

Tropical Cyclone Organizing Over Southwest Indian Ocean

A tropical cyclone organized north of La Reunion and east of Madagascar over the Southwest Indian Ocean on Friday.  At 1:00 p.m. EST on Friday the center of the tropical cyclone was located at latitude 14.5°N and longitude 56.1°E, which put it about 435 miles (700 km) north of La Reunion.  The tropical cyclone was moving toward the south at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 35 m.p.h. (55 km/h) and there were wind gusts to 45 m.p.h. (75 km/h).  The minimum surface pressure was 1002 mb.

An area of showers and thunderstorms persisted north of La Reunion for much of the past week.  Curved bands of showers and thunderstorms began to develop on Friday and the circulation took on more of a circular shape.  Thunderstorms near the center of the circulation began to generate upper level divergence which was pumping out mass and the surface pressure started to decrease.  There is a distinct center in the low level circulation and the tropical cyclone would be the equivalent of a tropical depression if it were over the Atlantic or Pacific Oceans.

The environment surrounding the tropical cyclone is favorable for further intensification.  The tropical cyclone is over water where the Sea Surface temperature is around 28.5°C.  So, there is plenty of energy in the upper ocean.  The upper level winds over the tropical cyclone are light and there is little vertical wind shear.  The absence of vertical wind shear is allowing the upper level divergence to pump out mass in all directions.  The tropical cyclone is expected to strengthen during the next 24 hours and it could intensify quickly if the inner core continues to develop.

The winds at the steering level are weak, which is why the system did not move much during the past few days.  Weak northerly winds could push the tropical cyclone slowly toward the south toward Mauritius and La Reunion.  The tropical cyclone could be near those islands in about three or four days.

Tropical Cyclone Abela Forms over the South Indian Ocean in the Middle of Winter

Tropical Cyclone Abela formed over the South Indian Ocean in the middle of winter on Sunday.  At 5:00 p.m. EDT on Sunday the center of Tropical Cyclone Abela was located at latitude 12.9°S and longitude 62.4°E which put it about 640 miles (1030 km) northeast of Port Louis, Mauritius.  Abela was moving toward the west-southwest at 18 m.p.h. (29 km/h).  The maximum sustained wind speed was 50 m.p.h. (80 km/h) and there were wind gusts to 65 m.p.h. (105 km/h).  The minimum surface pressure was 989 mb.

Enough spiral banding developed in a low pressure system over the South Indian Ocean to allow the system to be classified as Tropical Cyclone Abela.  The circulation is not well organized.  Most of the thunderstorms were located in a thin primary rainband that wrapped around the western side of the center of circulation.  The other rainbands contained shallower clouds.  There was enough convection to produce some upper level divergence.  Winds to tropical storm force extend out about 150 miles (240 km) from the center of circulation.

The environment around Tropical Cyclone Abela is only marginal for further intensification.  It is moving over water where the Sea Surface Temperature (SST) is near 26°C.  Northeasterly winds in the upper levels are creating a moderate amount of vertical wind shear.  The wind shear will limit the potential for intensification during the short term.  In about a day or so Abela will move over cooler SSTs and it should start to weaken.

A ridge of high pressure located east of Abela is steering the tropical cyclone toward the west-southwest and that general motion is expected to continue for another day or two.  On its anticipated track Tropical Cyclone Abela will pass north of Mauritius and La Reunion.  Abela is expected to reach the western end of the ridge and recurve toward the south as it nears the east coast of Madagascar.

Tropical Cyclone Fantala Weakens Northeast of Madagascar

Thunderstorms near the center of Tropical Cyclone Fantala dissipated and it weakened as moved northeast of Madagascar.  At 5:00 p.m. EDT  on Saturday the center of Tropical Cyclone Fantala was located at latitude 11.5°S and longitude 54.5°E which put it about 350 miles (565 km) east of Antsirañana, Madagascar.  Fantala was moving west-northwest at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 60 m.p.h. (95 km/h) and there were wind gusts to 75 m.p.h. (120 km/h).  The minimum surface pressure was 988 mb.

Tropical Cyclone Fantala reversed course again on Saturday and it is moving over the same part of the South Indian Ocean that it already crossed twice during the past few days.  The winds produced by Fantala mixed cooler water up to to the surface of the ocean during its previous passages over the same region.  The cooler water means that there is less energy available to power the circulation of Tropical Cyclone.  Although the winds continue to rotate around the center of circulation, there are no thunderstorms near the core of Fantala.  There are still several thunderstorms in rainbands farther to the east of the center of circulation.

If new thunderstorms do not develop around the core of the circulation, the winds will gradually spin down and the tropical cyclone will dissipate within a few days.  Upper level winds blowing from the west-northwest are also generating some vertical wind shear, which will make it more difficult for new thunderstorms to form.

A subtropical ridge southwest of Fantala is steering the tropical cyclone toward the west-northwest and that general motion is expected to continue for the next several days.  On its anticipated track Tropical Cyclone Fantala is forecast to pass north of Madagascar and move over the Seychelles.  It could be even weaker by the time it gets to the Seychelles.

Tropical Cyclone Fantala Stalls East of Madagascar

Tropical Cyclone Fantala moved into an area of weaker steering currents on Thursday and it stalled about 500 miles (800 km) east of northern Madagascar.  At 5:00 p.m. EDT on Thursday the center of Tropical Cyclone Fantala was located at latitude 13.0°S and longitude 56.7°E which put it about 515 miles (830 km) east of Antsirañana, Madagascar.  Fantala was moving toward the southeast at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 95 m.p.h. (155 km/h) and there were wind gusts to 115 m.p.h. (185 km/h).  The minimum surface pressure was 963 mb.

Although Fantala weakened slightly on Thursday, the structure of the inner core of the circulation remained fairly intact.  A thin ring of thunderstorms was wrapped around an that was obscured on conventional satellite imagery.  Other bands of thunderstorms spiraled around the eyewall.  The thunderstorms in the core of Fantala were generating upper level divergence to the north and east of the center of circulation.  It appears that drier air may be getting pulled into the eastern portion of the circulation outside the core of Fantala.  There only only isolated thunderstorms in the rainbands in that part of the circulation.

The environment is marginally favorable for intensification.  The upper level winds are light enough so there is only a moderate amount of vertical wind shear.  Fantala is over water where the Sea Surface Temperature is near 29°C.  However, because Fantala is moving so slowly, it could mix cooler water to the surface which would reduce the energy available to the tropical cyclone.  In addition the drier air will also limit the supply of energy being transported into the core of the circulation.

Tropical Cyclone Fantala has moved into an area where the steering currents are weak.  It may not move much during the next 24 hours.  A subtropical ridge is forecast to develop southwest of Fantala in a day or two.  When the subtropical ridge develops, it is expected to steer Fantala back toward the west again.  On its anticipated track Tropical Cyclone Fantala could be approaching the northern part of Madagascar in 60 to 72 hours.

Tropical Cyclone Fantala Reorganizes Northeast of Madagascar

Tropical Cyclone Fantala reorganized northeast of Madagascar on Tuesday.  At 8:00 p.m. EDT on Tuesday the center of Tropical Cyclone Fantala was located at latitude 10.0°S and longitude 52.0°E which put it about 240 miles (385 km) northeast of Antsirañana, Madagascar.  Fantala was moving toward the east-southeast at 8 m.p.h. (13 km/h).  The maximum sustained wind speed was 110 m.p.h. (175 km/h) and there were wind gusts to 135 m.p.h. (220 km/h).  The minimum surface pressure was 952 mb.

The core of the circulation of Tropical Cyclone Fantala became more organized on Tuesday.  A ring of strong thunderstorms surrounded a circular eye that was visible on satellite imagery.  It did still appear that some drier air was wrapping around the eastern and southern sides of the circulation, but the drier air did not appear to be spiraling into the center of the circulation.  Upper level divergence appeared to increase throughout the day.

The environment around Tropical Cyclone Fantala is favorable for intensification.  It is moving over water where the Sea Surface Temperature is near 29°C.  The upper level winds are weak and there is not much vertical wind shear.  The only inhibiting factor is the presence of a band of drier air on the eastern and southern sides of the circulation.  Given the improved organization of the core of the circulation, Tropical Cyclone Fantala could intensify further on Wednesday.

A ridge north of Fantala is steering the Tropical Cyclone toward the east-southeast and that general motion is expected to continue for another day or two.  A new subtropical ridge could develop southwest of Fantala and turn it back toward the west later this week.  Tropical Cyclone Fantala could still have an impact on northern Madagascar in a few days.

Tropical Cyclone Fantala Stalls and Weakens North of Madagascar

Tropical Cyclone Fantala stalled north of Madagascar on Monday and it weakened below Category 5 on the Saffir-Simpson Scale.  At 8:00 p.m. EDT on Monday the center of Tropical Cyclone Fantala was located at latitude 9.2°S and longitude 49.6°E which put it about 200 miles (320 km) north of Antsirañana, Madagascar.  Fantala was nearly stationary.  The maximum sustained wind speed was 140 m.p.h. (220 km/h) and there were wind gusts to 165 m.p.h. (265 km/h).  The minimum surface pressure was 933 mb.

The structure of the circulation of Tropical Cyclone Fantala deteriorated on Monday.  An eye was no longer visible in satellite imagery and the ring of thunderstorms that was around the eye appeared to have a gap on the east side.  There were still bands of thunderstorms spiraling around the outer portion of the circulation.  However, it appeared that some drier air may have been pulled into the northeastern part of Fantala.  Thunderstorms were still generating upper level divergence, but it was mainly to the south of the tropical cyclone.  The upper level divergence pumped out less mass than the amount of mass that converged in the lower levels and the surface pressure rose about 20 mb on Monday.

The environment around Tropical Cyclone Fantala contains a mixture of favorable and unfavorable features.  Fantala is over water where the Sea Surface Temperatures are near 29°C.  Upper level winds are blowing a little more strongly from the northeast, but the vertical wind shear is still not too significant.  Fantala does seem to be pulling in some drier air into its circulation.  The tropical cyclone is nearly stationary and its strong winds may be mixing some cooler water to the surface.  Drier air and cooler water would reduce the energy available to drive the circulation of Fantala and it is likely to weaken further on Tuesday.

Fantala is in an area where the steering currents are weak and it may not move much during the next 12 to 24 hours.  Eventually, a ridge is expected to develop northeast of Fantala and start to steer the tropical cyclone toward the southeast.  On its anticipated track the core of strongest winds would pass north of Madagascar.  However, there is still uncertainty about the future track of Fantala and it could still have an impact on northern Madagascar.

 

Tropical Cyclone Fantala Reaches Cat. 5 North of Madagascar

Tropical Cyclone Fantala continued to intensify on Sunday and it reached the equivalent of a Category 5 hurricane on the Saffir-Simpson Scale.  At 5:00 p.m. EDT on Sunday the center of Tropical Cyclone Fantala was located at latitude 9.7°S and longitude 50.5°E which put it about 190 miles (305 km) north-northeast of Antsirañana, Madagascar.  Fantala was moving toward the west-northwest at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 175 m.p.h. (280 km/h) and there were wind gusts to 205 m.p.h. (335 km/h).  The minimum surface pressure was 911 mb.

Fantala is an extremely well organized tropical cyclone.  There is a solid ring of thunderstorms surrounding a clear eye.  Other bands of thunderstorms spiral into the core of the circulation.  Hurricane force winds extend out about 30 miles (50 km) south of the center.  The thunderstorms are generating enough upper level divergence to cause the surface pressure to decrease to 911 mb.

Fantala is a very powerful tropical cyclone.  The Hurricane Intensity Index (HII) is 40.4, the Hurricane Size (HSI) is 10.5, and the Hurricane Wind Intensity Size Index (HWISI) is 50.9.

The environment around Tropical Cyclone Fantala is very favorable.  It is over water where the Sea Surface Temperature is near 29°C.  The upper level winds are weak and there is little vertical wind shear.  Fantala could intensify a little more, but it is likely near its maximum intensity.  Any increase in the speed of the upper level winds would generate more vertical wind shear and start to weaken Fantala.

A subtropical ridge southwest of the tropical cyclone is steering Fantala toward the west-northwest.  That general motion is expected to continue for another 12 to 24 hours.  Guidance from numerical models predicts that in a day or so a second ridge located northeast of Fantala will begin to steer the tropical cyclone back to the southeast.  There is variability in the location and sharpness of the turn to the southeast.  If there is a sharp turn to the southeast, the core of Fantala could remain north of Madagascar.  If the turn occurs later and/or is more gradual the core of Fantala could come closer to the northern end of Madagascar.

Tropical Cyclone Fantala is a very dangerous storm.  It would be capable of causing catastrophic damage if it were to make landfall.

Tropical Cyclone Fantala Almost Equal to Cat. 5 Hurricane

Tropical Cyclone Fantala intensified further on Saturday and it is almost the equivalent of a Category 5 hurricane on the Saffir-Simpson Scale.  At 8:00 p.m. EDT on Saturday the center of Tropical Cyclone Fantala was located at latitude 11.1°S and longitude 53.4°E which put it about 620 miles north of St. Denis, La Reunion.  Fantala was moving toward the west-northwest at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 155 m.p.h. (250 km/h) and there were wind gusts to 190 m.p.h. (305 km/h).  The minimum surface pressure was 922 mb.

Tropical Cyclone Fantala increased in both intensity and size again on Saturday.  Hurricane force winds now extend out about 60 miles (95 km) south of the center of circulation.  The Hurricane Intensity Index (HII) for Fantala is 33.3.  The Hurricane Size Index (HSI) is 18.7 and the Hurricane Wind Intensity Size Index (HWISI) is 52.0.

The circulation of Tropical Cyclone Fantala is very well organized.  It has a clearly visible eye on satellite imagery.  The eye is surrounded by a ring of strong thunderstorms.  Additional bands of thunderstorms are rotating around the core of the circulation.  The thunderstorms are generating strong upper level divergence which is pumping out mass in all directions.

The environment around Tropical Cyclone Fantala is favorable.  It is over water where the Sea Surface Temperature is near 29°C.  The upper level winds are weak and there is little vertical wind shear.  Tropical Cyclone Fantala could intensify a little more during the next 24 hours.  If one of the rainbands wraps around the existing eye, and eyewall replacement cycle could cause fluctuations of intensity.

A subtropical ridge southwest of Fantala is steering the tropical cyclone toward the west-northwest.  That general motion is expected to continue for another 24 to 36 hours.  In a day or so Fantala will move into an area where the steering currents are weaker and it could slow down or stall.  Eventually a northwesterly flow is forecast turn Tropical Cyclone Fantala back toward the southeast.  However, guidance from numerical models differs on when and where the southeasterly turn will occur.

On its anticipated track Tropical Cyclone Fantala could be near the northern end of Madagascar in a day or two.  The current size and intensity of Fantala means that it could produce regional significant damage if it were to hit land.  The future track of Fantala will determine if the tropical cyclone has an impact on Madagascar.