Category Archives: Indian Ocean

Tropical Cyclone Fani Strengthens to Equivalent of Major Hurricane

Tropical Cyclone Fani strengthened to the equivalent of a major hurricane on Tuesday.  At 11:00 p.m. EDT on Tuesday the center of Tropical Cyclone Fani was located at latitude 14.1°N and longitude 83.9°E which put it about 670 miles (1080 km) south-southwest of Kolkata (Calcutta), India.  Fani was moving toward the northwest at 7 m.p.h. (11 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 946 mb.

Tropical Cyclone Fani strengthened on Tuesday.  A small eye emerged at the center of circulation.  The eye was surround by a ring of thunderstorms.  The storms were stronger in the western half of the ring and that was where the strongest winds were.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Fani.  The stronger bands were south and west of the center of Fani.  It appeared that a little drier air may have been pulled into the northern half of the circulation and the bands were weaker in that part of the circulation.  Storms near the core were generating upper level divergence which was pumping mass away from the tropical cyclone.

Tropical Cyclone Fani had a moderately sized circulation.  Winds to hurricane/typhoon force extended out about 40 miles (65 km) from the center of circulation.  Winds to tropical storm force extended out about 150 miles (240 km) from the center.  The Hurricane Intensity Index (HII) for Tropical Cyclone Fani was 22.1.  The Hurricane Size Index (HSI) was 14.7 and the Hurricane Wind Intensity Size Index (HWISI) was 36.8.

Tropical Cyclone Fani will remain in an environment favorable for strong tropical cyclones during the next 24 to 36 hours.  Fani will move over water where the Sea Surface Temperature is near 30°C.  It will move near the western end of an upper level ridge and the upper level winds will not be too strong.  The major inhibiting factor will be the drier air over the northern half of the circulation.  Tropical Cyclone Fani could maintain its intensity and even strengthen during the next 24 hours if the drier air moistens over the warm water of the Bay of Bengal.

Tropical Cyclone Fani will move around the western end of a subtropical ridge on Wednesday.  Fani will move more toward the north when it rounds the end of the ridge.  An upper level trough approaching India from the west will turn Tropical Cyclone Fani toward the northeast in about 18 to 24 hours.  On its anticipated track Fani could approach the coast of Orissa state southwest of Kolkata in about 48 hours.  Tropical Cyclone Fani could bring strong winds to parts of Orissa and West Bengal.  Fani could also cause a significant storm surge along portions of the coast around the northern Bay of Bengal.  Locally heavy rain could also cause floods in Orissa and West Bengal.

Tropical Cyclone Fani Strengthens to Equivalent of Hurricane/Typhoon

Tropical Cyclone Fani strengthened to the equivalent of a hurricane/typhoon over the Bay of Bengal on Monday.  At 5:00 p.m. EDT on Monday the center of Tropical Cyclone Fani was located at latitude 11.4°N and longitude 86.9°E which put it about 800 miles (1290 km) south of Kolkata (Calcutta), India.  Fani was moving toward the north at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 75 m.p.h. (120 km/h) and there were wind gusts to 90 m.p.h. (145 km/h).  The minimum surface pressure was 974 mb.

The circulation around Tropical Cyclone Fani exhibited greater organization on Monday.  The inner end of a rainband wrapped most of the way around the eastern and northern sides of the center of circulation.  Although there was still a break on the southwestern side of the center, an eye may have been forming at the center of circulation.  Bands of showers and thunderstorms were revolving around the core of Tropical Cyclone Fani and the circulation was much more symmetrical.  Storm around the core were generating upper level divergence which was pumping mass away from the tropical cyclone.  Winds to tropical storm force extended out about 140 miles (225 km) from the center of circulation.

Tropical Cyclone Fani will move through an environment favorable for intensification during the next several days.  Fani will move over water where the Sea Surface Temperature is near 31°C.  It will move under the axis of an upper level ridge where the winds are weak.  Very warm water and little vertical wind shear will allow Tropical Cyclone Fani to intensify during the next 48 hours.  It could intensify rapidly once the inner core is fully developed.  Fani is likely to strengthen into the equivalent of a major hurricane during the next  2 to 3 days.

Tropical Cyclone Fani will move around the western end of a subtropical ridge during the next few days.  The ridge will steer Fani in a generally northward direction.  On its anticipated track Tropical Cyclone Fani could approach the coast of India southwest of Kolkata in three or four days.  Fani could be the equivalent of a major hurricane when it approaches the coast.  Tropical Cyclone Fani has the potential to cause major wind damage.  It will also generate a dangerous storm surge along the coast.  Heavy rain will create the potential for fresh water flooding in inland locations.  The greatest risks at this time are for the Indian states of Orissa and West Bengal.

Tropical Cyclone Fani Develops East of Sri Lanka

Tropical Cyclone Fani developed over the southern Bay of Bengal east of Sri Lanka on Saturday.  At 5:00 p.m. EDT on Saturday the center of Tropical Cyclone Fani was located at latitude 7.8°N and longitude 88.6°E which put it about 635 miles (1020 km) east-southeast of Chennai, India.  Fani was moving toward the north-northwest at 15 m.p.h. (24 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.

A distinct low level center of circulation formed on the eastern side of a cluster of thunderstorms over the southern Bay of Bengal on Saturday and the India Meteorological Department designated the system as Tropical Cyclone Fani.  The circulation around Fani was still organizing.  Bands of showers and thunderstorms were developing.  Many of the stronger thunderstorms were developing in two clusters which were east and northwest of the center of circulation.  Bands in other parts of the circulation consisted primarily of showers and lower clouds.  Winds to tropical storm force extended out about 100 miles (160 km) from the center of circulation.

Tropical Cyclone Fani will move into an environment that is more favorable for intensification.  Fani is currently under the southern part of an upper level ridge.  The ridge is producing easterly winds which are causing moderate vertical wind shear.  The wind shear is the primary factor slowing the intensification of Tropical Cyclone Fani.  Fani is forecast to move under the axis of the ridge where the upper level winds are weaker.  There will be less vertical wind shear when that happens.  Tropical Cyclone Fani will move over water where the Sea Surface Temperature is near 31°C.  So, intensification is very likely when the wind shear decreases.  Fani is likely to strengthen into the equivalent of a hurricane/typhoon.  Rapid intensification could occur if the inner core of the circulation becomes more well developed.

Tropical Cyclone Fani will move around the western end of a subtropical ridge over southeast Asia.  The ridge will steer Fani toward the north-northwest during the next several days.  It will move more toward the north when it moves around the western end of the ridge.  On its anticipated track Tropical Cyclone Fani will move toward the northern Bay of Bengal.

Powerful Tropical Cyclone Kenneth Makes Landfall in Northern Mozambique

Powerful Tropical Cyclone Kenneth made landfall in northern Mozambique on Thursday.  At 11:00 a.m. EDT on Thursday the center of Tropical Cyclone Kenneth was located at latitude 12.1°S and longitude 40.5°E which put it about 60 miles (95 km) north of Pemba, Mozambique.  Kenneth was moving toward the west-southwest at 13 m.p.h. (20 km/h).  The maximum sustained wind speed was 140 m.p.h. (225 km/h) and there were wind gusts to 165 m.p.h. (270 km/h).  The minimum surface pressure was 937 mb.

Tropical Cyclone Kenneth continued to intensify until it made landfall near Quissanga, Mozambique.  Winds to hurricane/typhoon force extended out about 45 miles (75 km) from the center of circulation.  Winds to tropical storm force extended out about 160 miles (260 km) from the center.  The Hurricane Intensity Index (HII) for Tropical Cyclone Kenneth was 28.2.  The Hurricane Size Index (HSI) was 16.3 and the Hurricane Wind Intensity Size Index (HWISI) was 44.5.  Those indices mean that Tropical Cyclone Kenneth was capable of causing significant regional damage.  In addition to wind damage Kenneth will cause a significant storm surge at the coast.  Locally heavy rain will produce flooding over parts of northern Mozambique.

Tropical Cyclone Kenneth will weaken when it moves inland over northern Mozambique.  However, It will take several days for the circulation around Kenneth to spin down.  The circulation could linger in that area for several days.  If that happens, persistent rainfall will exacerbate flooding of rivers and streams, which would hinder rescue and recovery efforts.

Elsewhere over the southern Indian Ocean, Tropical Cyclone Lorna was swirling well to the east-southeast of Diego Garcia.  At 11:00 a.m. EDT on Thursday the center of Tropical Cyclone Lorna was located at latitude 11.0°S and longitude 86.1°E which put it about 950 miles (1530 km) east-southeast of Diego Garcia.  Lorna was moving toward the east-southeast at 6 m.p.h. (10 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.

Major Tropical Cyclone Kenneth Brings Strong Wind, Rain to Comoros

Major Tropical Cyclone Kenneth brought strong wind and rain to the Comoros on Wednesday.  At 5:00 p.m. EDT on Wednesday the center of Tropical Cyclone Kenneth was located at latitude 11.3°S and longitude 42.8°E which put it about 35 miles (55 km) north of the Comoros.  Kenneth was moving toward the west at 13 m.p.h. (20 km/h).  The maximum sustained wind speed was 115 m.p.h. (185 km/h) and there were wind gusts to 145 m.p.h. (235 km/h).  The minimum surface pressure was 954 mb.

Tropical Cyclone Kenneth intensified rapidly on Tuesday into the equivalent of a major hurricane.  A small circular eye appeared at the center of circulation on infrared satellite images.  The eye was surrounded by a ring of strong thunderstorms and the strongest winds were occurring in that ring of storms.  Bands of showers and thunderstorms were revolving around the core of the circulation.  Storms near the core were generating strong upper level divergence which was pumping mass away from the tropical cyclone in all directions.

Winds to hurricane/typhoon force extended out about 35 miles (55 km) from the center of Tropical Cyclone Kenneth.  Winds to tropical storm force extended out about 130 miles (215 km) from the center of circulation.  The Hurricane Intensity Index (HII) for Kenneth was 20.1.  The Hurricane Size Index (HSI) was 11.0 and the Hurricane Wind Intensity Size Index (HWISI) was 31.1.  Tropical Cyclone Kenneth was capable of causing major damage.

The southern half of the eyewall of Tropical Cyclone Kenneth passed over northern Grande Comore (Njazidja).  Mitsamiouli and Mbeni were likely to have experienced winds to hurricane/typhoon force.  Strong winds may have also affected the capital, Moroni.  Major wind damage may have occurred in those areas.  Heavy rain falling on steep slopes may cause flash flooding.  Easterly winds blowing up the slopes would have enhanced rainfall and the greatest risks for flooding were on the eastern sides of the mountains.  Those easterly winds may have also generated a significant storms surge along the northeast coast of Grande Comore (Njazidja).

Tropical Cyclone Kenneth will move through an environment very favorable for intensification during the next 12 to 18 hours.  Kenneth will move over water where the Sea Surface Temperature is near 29°C.  It will move under the axis of an upper level ridge where the winds are weak and there will be little vertical wind shear.  Tropical Cyclone Kenneth is likely to intensify more while it moves across the Mozambique Channel.

Tropical Cyclone Kenneth will move north of a subtropical ridge.  The ridge will steer Kenneth a little to the south of due west.  On its anticipated track Tropical Cyclone Kenneth will make landfall on the north coast of Mozambique between Ibo and Mocimboa da Praia in about 18 hours.  Kenneth is likely to be a strong tropical cyclone at the time of landfall.  It will be capable of causing major wind damage and a storm surge at the coast.  Tropical Cyclone Kenneth will also drop heavy rain when it moves inland over northern Mozambique and it could cause additional flooding in that region.

Elsewhere over the South Indian Ocean, Tropical Cyclone Lorna moved gradually farther away from Diego Garcia.  At 5:00 p.m. EDT on Wednesday the center of Tropical Cyclone Lorna was located at latitude 10.3°S and longitude 84.8°E which put it about 855 miles (1380 km) east-southeast of Diego Garcia.  Lorna was moving toward the east at 4 m.p.h. (6 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 997 mb.

Tropical Cyclone Kenneth Develops North of Madagascar

Tropical Cyclone Kenneth developed north of Madagascar on Tuesday.  At 5:00 p.m. EDT on Tuesday the center of Tropical Cyclone Kenneth was located at latitude 10.7°S and longitude 47.2°E which put it about 310 miles (500 km) east-northeast of the Comoros.  Kenneth was moving toward the west at 12 m.p.h. (19 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 981 mb.

The circulation around Tropical Cyclone Kenneth organized rapidly on Tuesday.  A band of showers and thunderstorms wrapped around the eastern side of the center of circulation.  Microwave satellite imagery indicated that an eye might be forming at the center of Kenneth.  Other bands of showers and thunderstorms were developing outside the core of the circulation.  Storms around the core were generating upper level divergence which was pumping mass away from the tropical cyclone in all directions.  Winds to tropical storm force extended out about 130 miles (210 km) from the center of circulation.

Tropical Cyclone Kenneth will move through an environment favorable for intensification during the next day or two.  Kenneth will move over water where the Sea Surface Temperature is near 29°C.  It will move under an upper level ridge.  The winds are weak near the core of the ridge and vertical wind shear will be limited as long as Tropical Cyclone Kenneth stays under the central part of the ridge.  Kenneth is likely to intensify into the equivalent of a hurricane/typhoon during the next 12 to 24 hours.  Once an eye forms, Tropical Cyclone Kenneth could intensify rapidly and it could strengthen into the equivalent of a major hurricane.

Tropical Cyclone Kenneth will move north of a subtropical ridge during the next several days.  The ridge will steer Kenneth a little to the south of due west during that time period.  On its anticipated track the core of Tropical Cyclone Kenneth could pass near the Comoros in about 24 hours.  Kenneth could be the equivalent of a major hurricane by that time.  It could cause major wind damage and a significant storm surge at the coast.  Kenneth could also drop heavy rain, which could cause flash flooding along the steeper slopes.   Tropical Cyclone Kenneth could make landfall on the coast of northern Mozambique within 48 hours.

Elsewhere over the South Indian Ocean, Tropical Cyclone Lorna developed east of Diego Garcia on Tuesday.  At 5:00 p.m. EDT on Tuesday the center of Tropical Cyclone Lorna was located at latitude 9.7°S and longitude 82.9°E which put it about 715 miles (1155 km) east-southeast of Diego Garcia.  Lorna was moving toward the southeast at 13 m.p.h. (20 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 997 mb.

Tropical Cyclone Wallace Churns Northwest of Australia

Tropical Cyclone Wallace continued to churn northwest of Australia on Sunday.  At 11:00 p.m. EDT on Sunday the center of Tropical Cyclone Wallace was located at latitude 15.3°S and longitude 116.4°E which put it about 435 miles (700 km) north of Karratha, Australia.  Wallace was moving toward the southwest at 11 m.p.h. (17 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 mb.

The circulation around Tropical Cyclone Wallace exhibited signs of greater organization on Sunday.  The inner end of a band of showers and thunderstorms wrapped around the southern and western sides of the center of circulation.  More thunderstorms formed in other bands that were revolving around the core of Tropical Cyclone Wallace.  Storms near the core were generating upper level divergence which was pumping mass away to the west and south of the tropical cyclone.  Winds to tropical storm force extended out about 140 miles (220 km) from the center of circulation.

Tropical Cyclone Wallace will move through an environment somewhat favorable for intensification during the next 24 hours.  Wallace will move over water where Sea Surface Temperature is near 28°C.  It will move near the western end of an upper level ridge over northern Australia.  The ridge will produce easterly winds which will cause moderate vertical wind shear.  The shear will limit intensification, but it may not be great enough to prevent Tropical Cyclone Wallace from getting stronger.  Wallace could strengthen into the equivalent of a hurricane/typhoon during the next 24 hours.

The ridge over northern Australia will steer Tropical Cyclone Wallace toward the west-southwest during the next few days.  On its anticipated track Wallace is forecast to remain north of Western Australia.

Tropical Cyclone Wallace Develops North of Western Australia

Tropical Cyclone Wallace developed over the Timor Sea north of Western Australia on Friday.  At 2:00 p.m. EDT on Friday the center of Tropical Cyclone Wallace was located at latitude 11.7°S and longitude 125.7°E which put it about 280 miles (440 km) north-northeast of Kuri Bay, Australia.  Wallace was moving toward the west at 6 m.p.h. (9 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 997 mb.

The Australian Bureau of Meteorology posted a Tropical Cyclone Warning from Kalumburu to Beagle Bay.

More thunderstorms developed near the center of a Tropical Low over the Timor Sea on Friday and the Australian Bureau of Meteorology designated the system as Tropical Cyclone Wallace.  The distribution of thunderstorms in the circulation around Wallace was asymmetrical.  Most of the thunderstorms were occurring west of the center of circulation and in bands in the western half of the tropical cyclone.  Bands in the eastern half of of Tropical Cyclone Wallace consisted primarily of showers and lower clouds.  Winds to tropical storm force extended out about 150 miles (240 km) from the center of circulation.

Tropical Cyclone Wallace was moving north of an upper level ridge.  The ridge was producing strong easterly winds which were causing significant vertical wind shear.  Those winds and the shear were probably the cause of the asymmetrical distribution of thunderstorms.  Storms west of the center of circulation were generating upper level divergence which was pumping mass away to the west of Tropical Cyclone Wallace.

Tropical Cyclone Wallace may move into an area more favorable for intensification during the next day or two.  Wallace could move into an area where the upper level winds are not quite as strong.  Tropical Cyclone Wallace will move over water where the Sea Surface Temperature is near 29°C.  So, if it moves into an area where the shear is less, then Tropical Cyclone Wallace is likely to strengthen.  There is a chance Wallace could intensify into the equivalent of a hurricane/typhoon during the next two or three days.

Tropical Cyclone Wallace will move around the northwestern end of a subtropical ridge over Australia.  The ridge will steer Wallace toward the west-southwest during the next several days.  On its anticipated track the core of Tropical Cyclone Wallace is forecast to stay north of the coast of Western Australia during the next few days.

Major Tropical Cyclone Joaninha Brings Wind and Rain to Rodrigues

Major Tropical Cyclone Joaninha brought wind and rain to Rodrigues on Monday night.  At 11:00 p.m. EDT on Monday the center of Tropical Cyclone Joaninha was located at latitude 19.3°S and longitude 63.9°E which put it about 45 miles (75 km) from Rodrigues, Mauritius.  Joaninha was moving toward the southeast at 10 m.p.h. (16 km/h).  The maximum sustained wind speed was 125 m.p.h. (200 km/h) and there were wind gusts to 155 m.p.h. (250 km/h).  The minimum surface pressure was 946 mb.

Tropical Cyclone Joaninha was the equivalent of a major hurricane.  Winds to hurricane/typhoon force extended out about 50 miles (80 km) from the center of circulation.  Winds to tropical storm force extended out about 180 miles (290 km) from the center.  The Hurricane Intensity Index (HII) for Tropical Cyclone Joaninha was 23.6.  The Hurricane Size Index (HSI) was 18.7 and the Hurricane Wind Intensity Size Index (HWISI) was 42.3.  Joaninha was capable of causing major damage.

The southwestern portion of the eyewall of Tropical Cyclone Joaninha was very near Rodrigues.  Winds to hurricane typhoon force were occurring in that part of the eyewall.  Winds to tropical storm force are likely to affect all of Rodrigues.  The circulation around Joaninha was somewhat asymmetrical.  Most of the stronger rainbands were occurring in the eastern half of the circulation and the heaviest rain is likely to fall east of Rodrigues.  However, heavy rain in the eyewall could cause flooding in some locations.

Tropical Cyclone Joaninha will move through an environment favorable for intensification during the next 24 hours.  Joaninha will move over water where the Sea Surface Temperature is near 28°C.  It will move through a region where there will be little vertical wind shear.  Tropical Cyclone Joaninha could strengthen slightly while it passes by Rodrigues.

An upper level trough near Madagascar will produce northwesterly winds which will steer Tropical Cyclone Joaninha toward the southeast.  On its anticipated track Joaninha will move away from Rodrigues on Tuesday.  Conditions in Rodrigues should improve gradually as Tropical Cyclone Joaninha moves away.

Elsewhere over the South Indian Ocean, weakening Tropical Cyclone Veronica was skirting the coast of Western Australia.  At 11:00 p.m. EDT on Monday the center of Tropical Cyclone Veronica was located at latitude 21.1°S and longitude 115.4°E which put it about 140 miles (230 km) northeast of Learmonth, Australia.  Veronica was moving toward the southwest at 10 m.p.h. (16 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 992 mb.  Tropical Cyclone Veronica dropped heavy rain over parts of Western Australia and flooding was occurring in some locations.

Tropical Cyclone Veronica Stalls, Weakens Near Western Australia Coast

Tropical Cyclone Veronica stalled and weakened near the coast of Western Australia west of Port Hedand.  At 5:00 p.m. EDT on Sunday the center of Tropical Cyclone Veronica was located at latitude 20.5°S and longitude 117.5°E which put it about 70 miles (110 km) west of Port Hedland.  Veronica was moving toward the southwest at 2 m.p.h. (3 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 974 mb.  A Tropical Cyclone Warning remained in effect from Port Hedland to Mardie including Karratha and Barrow Island.

The southern eyewall of Tropical Cyclone Veronica moved over the coast of Western Australia west of Port Hedland on Saturday night.  Veronica was the equivalent of a major hurricane and there would have been a period of strong winds near the coast.  It likely caused some wind damage and generated a storm surge at the coast.  An upper level trough west of Australia produced strong northwesterly winds that reached the top of Tropical Cyclone Veronica as it neared the coast.  Those winds produced very strong vertical wind shear and they blew the upper half of the circulation southeast of the lower half of the tropical cyclone.  The decoupling of the upper and lower parts of the circulation caused Tropical Cyclone Veronica to weaken very quickly during the past 12 hours.  Veronica weakened from the equivalent of a major hurricane to a tropical storm.

The strong wind shear also generated an asymmetrical distribution of rainfall.  Most of the rain was falling in the southeastern half of the circulation which was over Western Australia.  Bands in the northwestern half of the circulation consisted primarily of showers and lower clouds.  Locally heavy rain could produce flooding in a few locations, but the rapid weakening of Tropical Cyclone Veronica will reduce the risk of flooding.

Tropical Cyclone Veronica will continue to weaken quickly because of the strong vertical wind shear.  The decoupling of the upper and lower halves of the circulation has resulted in little motion during the past few hours.  However, the lower half of Veronica will be steered more by the winds in the lower troposphere.  Those winds will steer Tropical Cyclone Veronica toward the west-southwest during the next day or two.  On its anticipated track the lower half of Veronica will move near the coast of Western Australia.  On its anticipated track Tropical Cyclone Veronica will pass near Wickham, Karratha, Dampier, Onslow and Exmouth.  Veronica will bring some gusty winds, but it should pose a limited risk.

Elsewhere over the South Indian Ocean, Tropical Cyclone Joaninha was strengthening northwest of Rodrigues.  At 5:00 p.m. EDT on Sunday the center of Tropical Cyclone Joaninha was located at latitude 17.4°S and longitude 62.0°E which put it about 180 miles (290 km) northwest of Rodrigues, Mauritius.  Joaninha was moving toward the southeast at 2 m.p.h. (3 km/h).  The maximum sustained wind speed was 110 m.p.h. (175 km/h) and there were wind gusts to 130 m.p.h. (210 km/h).  The minimum surface pressure was 956 mb.