Tag Archives: Madagascar

Tropical Cyclone Elvis Spins Near Southwest Madagascar

Tropical Cyclone Elvis continued to spin near southwestern Madagascar on Wednesday.  At 4:00 p.m. EST on Wednesday the center of Tropical Cyclone Elvis was located at latitude 26.0°S and longitude 43.3°E which put the center about 115 miles (185 km) southwest of Beloha, Madagascar.  Elvis was moving toward the south-southeast at 13 m.p.h. (21 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.

Although Tropical Cyclone Elvis strengthened on Wednesday, drier air appeared to be getting pulled into Elvis’ circulation.  Many of the thunderstorms near the center of Tropical Cyclone Elvis dissipated. Thunderstorms were still occurring in bands in the southeastern part of Elvis’ circulation.  Bands in the other parts of Tropical Cyclone Elvis consisted primarily of showers and lower clouds.  The few remaining thunderstorms near the center of Elvis were not generating much upper level divergence

The distribution of wind speeds in Tropical Cyclone Elvis was asymmetrical.  Winds to tropical storm force extended out 140 miles (220 km) in the southeastern part of Elvis’s circulation.  Winds to tropical storm force only extended out 50 miles in the northern side of Tropical Cyclone Elvis.

Tropical Cyclone Elvis will move through an environment marginally favorable for intensification during the next 24 hours.  Elvis will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the eastern side of an upper level trough near southern Africa.  The upper level trough will produce northwesterly winds that will blow toward the top of Elvis’ circulation.  Those winds will cause moderate to strong vertical wind shear. The vertical wind shear will inhibit intensification of Tropical Cyclone Elvis.  Drier air will also inhibit the intensification of Elvis.  The vertical wind shear and the drier air are likely to cause Tropical Cyclone Elvis to weaken during the next 24 hours.

The upper level trough near southern Africa will steer Tropical Cyclone Elvis toward the southeast during the next 24 hours.  On its anticipated track, the center of Tropical of Cyclone Elvis will pass south of southern Madagascar.  Elvis will move away from Madagascar on Friday.

Tropical Cyclone Elvis Forms Near Southwest Madagascar

Tropical Cyclone Elvis formed near southwestern Madagascar on Tuesday night.  At 10:00 p.m. EST on Tuesday the center of Tropical Cyclone Elvis was located at latitude 25.1°S and longitude 42.8°E which put the center about 75 miles (120 km) southwest of Toliara, Madagascar.  Elvis was moving toward the southeast at 5 m.p.h. (8 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 995 mb.

A low pressure system over the Southwest Indian Ocean near southwestern Madagascar strengthened on Tuesday evening and Meteo France La Reunion designated the system as Tropical Cyclone Elvis.  The distribution of thunderstorms in Tropical Cyclone Elvis was asymmetrical.  Thunderstorms were occurring in bands in the eastern and southern parts of Elvis’ circulation.  Bands in the northern and western parts of Tropical Cyclone Elvis consisted primarily of showers and lower clouds.  Storms near the center of Elvis generated upper level divergence that pumped mass away to the southeast of the tropical cyclone.

Tropical Cyclone Elvis will move through an environment marginally favorable for intensification during the next 24 hours.  Elvis will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the eastern side of an upper level trough over southern Africa.  The upper level trough will produce northwesterly winds that will blow toward the top of Elvis’ circulation.  Those winds will cause moderate to strong vertical wind shear.  The vertical wind shear will inhibit intensification of Tropical Cyclone Elvis.  Elvis could intensify a little if the vertical wind shear does not increase.  However, if the wind shear does increase then Elvis is likely to weaken.

Tropical Cyclone Elvis will move around the southwestern part of a high pressure system over the South Indian Ocean.  The high pressure system will steer Elvis slowly toward the southeast during the next 24 hours.  On its anticipated track, the center of Tropical of Cyclone Elvis will pass just to the south of southern Madagascar.

Bands in the northern part of Tropical Cyclone Elvis could bring gusty winds and locally heavy rain to southern Madagascar.  Heavy rain could cause flash floods in some locations.

Tropical Cyclone Dikeledi Passes Southwest of Madagascar

Tropical Cyclone Dikeledi passed southwest of Madagascar on Wednesday.  At 4:00 p.m. EST on Wednesday the center of Tropical Cyclone Dikeledi was located at latitude 26.4°S and longitude 42.9°E which put the center about 150 miles (240 km) southwest of Beloha, Madagascar.  Dikeledi was moving toward the south-southeast at 22 m.p.h. (35 km/h).  The maximum sustained wind speed was 100 m.p.h. (160 km/h) and there were wind gusts to 120 m.p.h. (195 km/h).  The minimum surface pressure was 963 mb.

Tropical Cyclone Dikeledi intensified on Wednesday as it moved southwest of Madagascar.  A circular eye with a diameter of 25 miles (40 km) formed at the center of Dikeledi’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Dikeledi.  Storms near the core of Dikeledi generated upper level divergence that pumped mass away from the tropical cyclone.  The removal of mass caused the surface pressure to decrease.

The size of the circulation around Tropical Cyclone Dikeledi increased on Wednesday.  Winds to hurricane/typhoon force extended out 25 miles (40 km) from the center of Dikeledi’s circulation.  Winds to tropical storm force extended out 150 miles (240 km) in the eastern side of Tropical Cyclone Dikeledi.  Winds to tropical storm force only extended out 60 miles (95 km) in the western side of Dikeledi.

The Hurricane Intensity Index (HII) for Tropical Cyclone Dikeledi was 16.5.  The Hurricane Size Index (HSI) was 11.8 and the Hurricane Wind intensity Size INdex (HWISI) was 28.3.  Tropical Cyclone Dikeledi was similar in size and intensity to Hurricane Idalia when Idalia hit Florida in 2023.

Bands in the eastern side of Tropical Cyclone Dikeledi were bring gusty winds and heavy rain to southern Madagascar.  Heavy rain could cause flash floods in some locations.

Tropical Cyclone Dikeledi will move through an environment that will become unfavorable for intensification during the next 24 hours.  Dikeledi will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the eastern side of an upper level trough over southern Africa.  The upper level trough will produce northwesterly winds that will blow toward the top of Dikeledi’s circulation.  Those winds will cause the vertical wind shear to increase.  Tropical Cyclone Dikeledi will weaken when the wind shear increases.

The upper level trough over southern Africa will steer Tropical Cyclone Dikeledi toward the southeast during the next 24 hours.  On its anticipated track, Tropical Cyclone Dikeldi will pass south of Madagascar.  Dikeledi will move southeast of Madagascar on Thursday.

Tropical Cyclone Dikeledi Moves Back Over the Mozambique Channel

Tropical Cyclone Dikeledi moved back over the Mozambique Channel on Tuesday.  At 4:00 p.m. EST on Tuesday the center of Tropical Cyclone Dikeledi was located at latitude 19.6°S and longitude 40.0°E which put the center about 225 miles (365 km) southeast of Quelimane, Mozambique.  Dikeledi was moving toward the south at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 70 m.p.h. (110 km/h) and there were wind gusts to 85 m.p.h. (135 km/h).  The minimum surface pressure was 985 mb.

Tropical Cyclone Dikeledi moved back over the Mozambique Channel on Tuesday.  Dikeledi began to strengthen again after the center of circulation moved back over water.  More thunderstorms formed near the center of Dikeledi’s circulation.  More thunderstorms also formed in bands revolving around the center of Tropical Cyclone Dikeledi.  Storms near the center of Dikeledi generated upper level divergence that pumped mass away from the tropical cyclone.

The distribution of winds speeds in Tropical Cyclone Dikeledi after its passage over northeastern Mozambique on Monday.  Winds to tropical storm force extended out 140 miles (225 km) in the eastern side of Dikeledi’s circulation.  Winds to tropical storm force extended out 90 miles (145 km) in the western side of Tropical Cyclone Dikeledi.

Tropical Cyclone Dikeledi will move through an environment favorable for intensification during the next 24 hours.  Dikeledi will move over water where where the Sea Surface Temperatures are near 29°C.  It will move under the middle of an upper level ridge over southern Africa and the Mozambique Channel.  The upper level winds are weak near the middle of the ridge and there will be little vertical wind shear.  Tropical Cyclone Dikeledi will intensify back to the equivalent of a hurricane/typhoon during the next 24 hours.

Tropical Cyclone Dikeledi will move around the western end of a high pressure system over the South Indian Ocean.  The high pressure system will steer Dikeledi toward the south-southeast during the next 24 hours.  On its anticipated track, Tropical Cyclone Dikeledi will approach Europa Island in 12 hours.  Dikeledi will be southwest of Madagascar in 24 hours.

Tropical Cyclone Dikeledi Brings Wind and Rain to Northern Madagascar

Tropical Cyclone Dikeledi brought wind and rain to northern Madagascar on Saturday.  At 4:00 p.m. EST on Saturday the center of Tropical Cyclone Dikeledi was located at latitude 13.1°S and longitude 48.4°E which put the center about 60 miles (95 km) south of Antsiranana, Madagascar.  Dikeledi was moving toward the west-southwest at 15 m.p.h. (24 km/h).  The maximum sustained wind speed was 85 m.p.h. (135 km/h) and there were wind gusts to 100 m.p.h. (160 km/h).  The minimum surface pressure was 980 mb.

Tropical Cyclone Dikeledi intensified to the equivalent of a hurricane/typhoon before it reached northern Madagascar on Saturday.  The inner end of a rainband wrapped around the center of Dikeledi’s circulation.  An eye appeared intermittently on microwave satellite images.  The intermittent eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core to Tropical Cyclone Dikeledi.  Storms near the core generated upper level divergence that pumped mass away from the tropical cyclone.  The removal of mass caused the surface pressure to decrease.

The circulation around Tropical Cyclone Dikeledi was symmetrical.  Winds to hurricane/typhoon force extended out 25 miles (40 km) from the center of Dikeledi’s circulation.  Winds to tropical storm force extended out 100 miles (160 km) from the center of Tropical Cyclone Dikeledi.

The Hurricane Intensity Index (HII) for Tropical Cyclone Dikeledi is 12.7.  The Hurricane Size Index (HSI) is 9.5 and the Hurricane Wind Intensity Size Index (HWISI) is 22.2  Tropical Cyclone Dikeledi is similar in size and intensity to Hurricane Isaias when Isaias hit North Carolina in 2020.

Tropical Cyclone Dikeledi will move across northern Madagascar during the next few hours.  Dikeledi is capable of causing localized minor wind damage.  Tropical Cyclone Dikeledi will also drop heavy rain over parts of northern Madagascar.  Heavy rain is likely to cause flash floods in some locations.

Tropical Cyclone Dikeledi will move around the northern side of a high pressure system over the South Indian Ocean.  The high pressure system will steer Dikeledi toward the west-southwest during the next 24 hours.  On its anticipated track, Tropical Cyclone Dikeledi will move across northern Madagascar during the next few hours.  The center of Dikeledi’s circulation will pass near Mayotte on Sunday.

Tropical Cyclone Dikeledi will weaken while it moves across northern Madagascar.  Dikeledi will will move through an environment favorable for intensification when it reaches the northern Mozambique Channel on Sunday.  Dikeledi will move over water where where the Sea Surface Temperatures are near 30°C. It will move under the northern part of an upper level ridge over the South Indian Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Dikeledi’s circulation.  Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification.  Tropical Cyclone Dikeledi is likely to intensify on Sunday when it gets to the northern Mozambique Channel.

Tropical Cyclone Dikeledi Approaches Northern Madagascar

Tropical Cyclone Dikeledi was approaching northern Madagascar on Friday afternoon.  At 4:00 p.m. EST on Friday the center of Tropical Cyclone Dikeledi was located at latitude 13.1°S and longitude 53.5°E which put the center about 285 miles (460 km) east of Antsiranana, Madagascar.  Dikeledi was moving toward the west at 16 m.p.h. (26 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 991 mb.

Tropical Cyclone Dikeledi intensified on Friday as it approached northern Madagascar.  The inner end of a rainband wrapped around the western and northern sides of the center of Dikeledi’s circulation.  An eye appeared to be forming at the center of Tropical Cyclone Dikeledi.  Bands of showers and thunderstorms were revolving around the core of Dikeledi’s circulation.  Storms near the core generated upper level divergence that pumped mass away from the tropical cyclone.  The removal of mass caused the surface pressure to decrease.

The circulation around Tropical Cyclone Dikeledi became more symmetrical on Friday.  Winds to tropical storm force extended out 70 miles (110 km) from the center of Dikeledi’s circulation.

Tropical Cyclone Dikeledi will move through an environment favorable for intensification during the next 12 hours.  Dikeledi will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the northern part of an upper level ridge over the South Indian Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Dikeledi’s circulation.  Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification.  Tropical Cyclone Dikeledi will intensify during the next 12 hours.  Dikeledi could strengthen to the equivalent of a hurricane/typhoon.

Tropical Cyclone Dikeledi will move around the northern side of a high pressure system over the South Indian Ocean.  The high pressure system will steer DIkeledi toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Dikeledi will reach northern Madagascar in 12 hours.

Tropical Cyclone Dikeledi will bring strong winds and locally heavy rain to northern Madagascar.  Heavy rain is likely to cause flash floods in some locations.

Tropical Cyclone Dikeledi Passes North of Mauritius

Tropical Cyclone Dikeledi was passing north of Mauritius on Thursday.  At 4:00 p.m. EST on Thussday the center of Tropical Cyclone Dikeledi was located at latitude 13.5°S and longitude 59.4°E which put the center about 485 miles (785 km) north-northeast of Port Louis, Mauritius.  Dikeledi was moving toward the west at 17 m.p.h. (28 km/h).  The maximum sustained wind speed was 45 m.p.h. (75 km/h) and there were wind gusts to 60 m.p.h. (95 km/h).  The minimum surface pressure was 999 mb.

Tropical Cyclone Dikeledi strengthened gradually as it moved over the South Indian Ocean north-northeast of Mauritius on Thursday.  More thunderstorms formed near the center of Dikeledi’s circulation.  The inner end of a rainband wrapped around the southern and western sides of the center of Tropical Cyclone Dikeledi.  Bands of showers and thunderstorms were revolving around the center of Dikeledi.  Storms near the center of Dikeledi generated upper level divergence that pumped mass away from the tropical cyclone.

The distribution of wind speeds in Tropical Cyclone Dikeledi was asymmetrical.  Winds to tropical storm force extended out 70 miles (110 km) in the southern half of Dikeledi’s circulation.  The winds in the northern half of Tropical Cyclone Dikeledi were blowing at less than tropical storm force.

Tropical Cyclone Dikeledi will move through an environment favorable for intensification during the next 24 hours.  Dikeledi will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the northern part of an upper level ridge over the South Indian Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Dikeledi’s circulation.  Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification.  Tropical Cyclone Dikeledi will intensify during the next 24 hours.  Dikeledi could strengthen to the equivalent of a hurricane/typhoon within 36 hours.

Tropical Cyclone Dikeledi will move around the northern side of a high pressure system over the South Indian Ocean.  The high pressure system will steer DIkeledi toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Dikeledi will approach northern Madagascar in 36 hours.

Tropical Cyclone Dikeledi Forms Northeast of Mauritius

Tropical Cyclone Dikeledi formed over the South Indian Ocean northeast of Mauritius on Wednesday evening.  At 7:00 p.m. EST on Wednesday the center of Tropical Cyclone Dikeledi was located at latitude 15.0°S and longitude 66.4°E which put the center about 685 miles (1110 km) northeast of Port Louis, Mauritius.  Dikeledi was moving toward the west at 22 m.p.h. (33 km/h).  The maximum sustained wind speed was 40 m.p.h. (65 km/h) and there were wind gusts to 50 m.p.h. (80 km/h).  The minimum surface pressure was 1001 mb.

A low pressure system over the South Indian Ocean northeast of Mauritius strengthened on Wednesday evening and Meteo France la Reunion designated the system as Tropical Cyclone Dikeledi.  More thunderstorms formed near the center of Tropical Cyclone Dikeledi.  The inner end of a rainband wrapped around the northern and eastern sides of the center of Dikeledi’s circulation.  Other bands of showers and thunderstorms were revolving around the center of Tropical Cyclone Dikeledi.  Storms near the center of Dikeledi generated upper level divergence that pumped mass away to the south and west of the tropical cyclone.

Tropical Cyclone Dikeledi will move through an environment favorable for intensification during the next 24 hours.  Dikeledi will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the northern part of an upper level ridge over the South Indian Ocean.  The upper level ridge will produce easterly winds that will blow toward the top of Dikeledi’s circulation.  Those winds will cause some vertical wind shear, but the wind shear will not be enough to prevent intensification.  Tropical Cyclone Dikeledi will intensify during the next 24 hours.  Dikeledi could strengthen to the equivalent of a hurricane/typhoon later this week.

Tropical Cyclone Dikeledi will move around the northern side of a high pressure system over the South Indian Ocean.  The high pressure system will steer DIkeledi toward the west during the next 24 hours.  On its anticipated track, Tropical Cyclone Dikeledi will pass north of Mauritius and La Reunion.  Dikeledi is likely to approach northern Madagascar later this week.

Tropical Cyclone Chido Passes North of Madagascar

The center of Tropical Cyclone Chido passed just to the north of Madagascar on Friday morning.  At 4:00 a.m. EST on Friday the center of Tropical Cyclone Chido was located at latitude 12.0°S and longitude 49.4°E which put the center about 75 miles (120 km) north of Antsiranana, Madascar.  Chido was moving toward the west at 13 m.p.h. (20 km/h).  The maximum sustained wind speed was 120 m.p.h. (195 km/h) and there were wind gusts to 150 m.p.h. (240 km/h).  The minimum surface pressure was 960 mb.

Tropical Cyclone Chido was weakening slowly as it passed just to the north of Madagascar on Friday morning.  A circular eye with a diameter of 25 miles (40 km) was at the center of Chido’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Chido.  Storms near the core of Chido generated upper level divergence that pumped mass away from the tropical cyclone.  The removal of mass in the upper levels was not quite able to balance the stronger inflow of mass in the lower levels of the atmosphere.  The greater inflow of mass in the lower levels caused the surface pressure to increase.

The circulation around Tropical Cyclone Chodi was very symmetrical.  Winds to hurricane/typhoon force extended out 45 miles (75 km) from the center of Chido’s circulation.  Winds to tropical storm force extended out 105 miles (165 km) from the center of Tropical Cyclone Chido.

The Hurricane Intensity Index (HII) for Tropical Cyclone Chido is 22.1.  The Hurricane Size Index (HSI) is 15.0 and the Hurricane Wind Intensity Size Index (HWISI) is 37.1.  Tropical Cyclone Chido is similar in size and intensity to Hurricane Delta when Delta made landfall in southwest Louisiana in 2020.

Tropical Cyclone Chido will move through an environment favorable for a powerful tropical cyclone during the next 24 hours.  Chido will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the axis of an upper level ridge over the South Indian Ocean.  The upper level winds are weak near the axis of the ridge and there will be little vertical wind shear.  Tropical Cyclone Chido could maintain its intensity during the next 24 hours if the inflow of mass in the lower levels is balanced by the divergence of mass in the upper levels of the atmosphere.

Tropical Cyclone Chido will move around the northern side of a high pressure system over the South Indian Ocean.  The high pressure system will steer Chido toward the west-southwest during the next 24 hours.  On its anticipated track, the center of Tropical Cyclone Chido will reach Mayotte and the Comoros in 24 hours.  Chido could approach the coast of northern Mozambique in 48 hours.

Tropical Cyclone Chido could be the equivalent of a major hurricane when it reaches Mayotte and the Comoros.  Chido will bring strong winds and locally heavy rain to Mayotte and the Comoros.  Heavy rain is likely to cause flash floods in some locations.  Tropical Cyclone Chido could also cause a storm surge of up to 10 feet (3 meters) along the coast of Mayotte and the Comoros.

Powerful Tropical Cyclone Chido Nears Northern Madagascar

Powerful Tropical Cyclone Chido was nearing northern end of Madagascar on Thursday evening.  At 4:00 p.m. EST on Thursday the center of Tropical Cyclone Chido was located at latitude 11.0°S and longitude 51.7°E which put the center about 185 miles (295 km) east-northeast of Antsiranana, Madascar.  Chido was moving toward the west-southwest at 12 m.p.h. (19 km/h).  The maximum sustained wind speed was 145 m.p.h. (235 km/h) and there were wind gusts to 175 m.p.h. (280 km/h).  The minimum surface pressure was 939 mb.

Powerful Tropical Cyclone Chido was maintaining its intensity as it approached northern Madagascar on Thursday evening.  A small circular eye with a diameter of 14 miles (22 km) was at the center of Chido’s circulation.  The eye was surrounded by a ring of thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Chido.  Storms near the core of Chido generated strong upper level divergence that pumped large quantities of mass away from the tropical cyclone.  The removal of mass in the upper levels was not quite able to  balance the stronger inflow of mass in the lower levels of the atmosphere.  The greater inflow of mass in the lower levels caused the surface pressure to start to increase.

The circulation around Tropical Cyclone Chodi was very symmetrical.  Winds to hurricane/typhoon force extended out 35 miles (55 km) from the center of Chido’s circulation.  Winds to tropical storm force extended out 105 miles (165 km) from the center of Tropical Cyclone Chido.

The Hurricane Intensity Index (HII) for Tropical Cyclone Chido is 29.9.  The Hurricane Size Index (HSI) is 12.2 and the Hurricane Wind Intensity Size Index (HWISI) is 42.1.  Tropical Cyclone Chido is similar in intensity to Hurricane Charley when Charley made landfall in southwest Florida in 2004.  Chido is larger than Charley was.

Tropical Cyclone Chido will move through an environment favorable for a powerful tropical cyclone during the next 24 hours.  Chido will move over water where where the Sea Surface Temperatures are near 28°C.  It will move under the axis of an upper level ridge over the South Indian Ocean.  The upper level winds are weak near the axis of the ridge and there will be little vertical wind shear.  Tropical Cyclone Chido could weaken slowly during the next 24 hours if the inflow of mass in the lower levels continues to exceed the divergence of mass in the upper levels of the atmosphere.  Chido will also weaken of the core of its circulation moves over northern Madagacar.

Tropical Cyclone Chido will move around the northern side of a high pressure system over the South Indian Ocean.  The high pressure system will steer Chido toward the west-southwest during the next 24 hours.  On its anticipated track, the center of Tropical Cyclone Chido will pass near the northern end of Madagascar in 12 hours.

Tropical Cyclone Chido will bring strong winds and heavy rain to northern Madagascar.  Chido is likely to be the equivalent of a major hurricane when it hits Madagascar.  Heavy rain is likely to cause flash floods in some locations.  Tropical Cyclone Chido could also cause a storm surge of up to 13 feet (4 meters ) along parts of the coast of northern Madagascar.  Chido could cause major damage if the eyewall moves over the northern end of Madagascar.