1369:
to its south closer to Réunion. The structure resembled a monsoon depression, but as the two low-pressure areas consolidated, they became more distinct. On March 2, the system that would become Diwa originated out of the southern low, and both systems continued to interact until Diwa absorbed the other disturbance. The wind field was large and asymmetrical, ranging 2,000 km (1,200 mi) in diameter, and there was little convection near the centers. Despite the lack of organization, the
Meteorological Service of Mauritius named the system Tropical Storm Diwa on March 3 due to the threat to the Mascarene Islands, as well as the presence of gale-force winds. The structure slowly evolved into that of a tropical cyclone as the convection concentrated. On March 4, Diwa passed northwest of Réunion, still disorganized with much of the convection to the south. That day, the JTWC initiated advisories on the system as Tropical Cyclone 16S. The storm continued slowly to the southwest at first, until it turned to the southeast on March 6 while rounding the ridge. Despite accelerating into an area of cooler waters, Diwa's structure became much more like a tropical cyclone on March 8. The MFR estimated peak 10 minute winds of 110 km/h (68 mph), making it a severe tropical storm, and the JTWC estimated peak 1 minute winds of 100 km/h (62 mph). Diwa quickly transitioned into an extratropical cyclone as it interacted with a cold front to the south, completing the transition by March 9. The circulation gradually lost its definition, dissipating on March 11.
285:, killing six people when it brushed the island's southwest coast. In February, there was a small, short-lived unnamed tropical storm that presented difficulties to warning agencies in determining its structure. Intense Tropical Cyclone Carina was the strongest system of the season, attaining peak 10 minute winds of 205 km/h (127 mph) in the open waters of the eastern portion of the basin. Sprawling Tropical Storm Diwa brought six months' worth of rainfall to the drought-ridden island of Réunion, reaching 2,943 mm (115.9 in) in the mountainous peaks. The rains led to flooding and landslides that killed 10 people directly or indirectly. Two of the deaths occurred when a saturated cliff collapsed onto a coastal road. The final storm, Elia, dissipated on April 17 after previously entering from the Australian basin.
881:
Tropical
Depression 6. At the time, the circulation was partially exposed from the convection, although it organized over the next day. This spurred the JTWC to designate it as Tropical Cyclone 04S on December 24 with winds of 65 km/h (40 mph). As with other systems in the season, strong shear caused the system to weaken; the JTWC discontinued advisories on December 25, and the MFR followed suit the next day. However, the system continued to the southwest, reorganizing enough on December 27 for the MFR to reissue advisories. Shear again weakened the convection, and the MFR discontinued advisories again on December 29 while the system was a short distance west-northwest of Rodrigues.
1458:
The low meandered for several days, unable to intensify much due to insufficient moisture in the region. On April 6, the MFR designated the system as
Tropical Disturbance 13, although the agency discontinued advisories on the next day. On April 7, the low crossed back into the Australian basin, only to turn to the southwest on April 10, steered by a ridge to the southeast. During this time, the system passed about 185 km (115 mi) northwest of the Cocos Islands. On April 12, the JTWC designated the system as Tropical Cyclone 12S. On the same day, the system intensified into a tropical depression, after the convective structure improved amid favoring conditions.
31:
530:
rainbands, the MFR upgraded the system to a 55 km/h (34 mph) tropical depression on
October 14. This period of organization occurred during a brief decrease in wind shear. At 12:00 UTC on October 14, the JTWC classified the system as Tropical Cyclone 01S, estimating peak 1 minute winds of 75 km/h (47 mph). Increasingly unfavorable conditions caused the convection to diminish. Late on October 15, both the JTWC and MFR discontinued advisories due to the increasing disorganization of the disturbance. The circulation remained well-organized but devoid of convection, and the MFR last monitored the center on October 21.
1378:
power outages on the island, and three people died due to using a generator inside their home during the storm. One person drowned during the floods, and four people drowned in residual flooding accidents on the island in the weeks after the storm. The floods wrecked several homes during river flooding and caused several landslides, some of which occurred two weeks after the storm due to saturated grounds. On March 24, a cliff collapsed onto a coastal road, killing two people and severely injuring two others; the road was reopened three months later. In addition to the damaging effects, the rainfall also alleviated drought conditions.
1290:(43 mi). Based on the storm's presentation on satellite imagery, the MFR estimated peak 10 minute winds of 205 km/h (127 mph) on February 28. On the same day, the JTWC estimated peak 1 minute winds of 240 km/h (150 mph). Unfavorable conditions – cooler waters and stronger wind shear – caused Carina's structure to rapidly degrade after the peak intensity. By March 2, the storm weakened below tropical cyclone status, and soon after the circulation became exposed from the convection, prompting the JTWC to discontinue advisories. Carina stalled that day when it reached a
1708:
997:
714:
901:
1462:
assessing peak 10 minute winds of 75 km/h (47 mph). The JTWC meanwhile estimated 1 minute winds of 95 km/h (59 mph). Increasing wind shear and cooler waters resulted in diminished intensity of the convection, causing Elia to weaken. The MFR downgraded the storm to tropical depression status on April 15 after the circulation became exposed. On the same day, the JTWC discontinued advisories. The circulation dissipated on April 17, signaling the end of the season.
828:
1228:
722:
1403:
550:
475:
401:
1005:
630:
1199:, which is a small and short-lived system, and there was also uncertainty whether the winds were at the surface. As a result, there was a disagreement between the MFR, which estimated peak 10 minute winds of 95 km/h (59 mph), and the Meteorological Service of Mauritius, which assessed a much weaker storm. The latter agency is responsible for officially naming systems, and as a result, the severe tropical storm was unnamed.
450:
waters fueled an increase in convection, and the MFR classified the system as
Tropical Disturbance 1 on September 5. That day, the JTWC issued a TCFA, but continued shear caused weakening as the disturbance tracked southeastward. By September 8, the MFR had discontinued advisories on the system, after the circulation had become exposed. After turning to the west-northwest, the circulation began dissipating on September 12.
1236:
1057:. After a brief period of strengthening, the storm weakened due to increased shear and diurnal cooling. The track shifted to the south-southwest, paralleling Madagascar to the east. Steered between ridges to the east and west, Boloetse stalled and turned to the west-northwest. Late on January 27, the MFR downgraded the storm to a tropical depression, and late the next day, the circulation struck eastern Madagascar just north of
1328:
1411:
1133:
836:
638:
558:
483:
409:
782:. The storm moved southwestward and intensified due to favorable water temperatures and atmospheric conditions, reaching winds of 185 km/h (115 mph) on November 22 while just east of 90º E. The track shifted nearly due south, and the eye moved along the dividing line between the Australian and south-west Indian Ocean basins. Early on November 24, the cyclone crossed 90º E and was renamed
1320:
1125:
1373:
rainfall at a station in the southeastern portion of the island. Gale-force winds affected Réunion for nearly three days, due to the storm's lopsided structure, and gusts peaked at 194 km/h (121 mph) along the coast. Diwa dropped the equivalent of six months' worth of rainfall, peaking at 2,943 mm (115.9 in) at Grand-Îlet over four days, which approached the record totals set by
1053:. With light wind shear, the system developed a small area of convection over a well-defined circulation. Early on January 25, the MFR upgraded the disturbance to a tropical depression, and the JTWC classified it as Tropical Cyclone 09S. Later that day, the MFR upgraded it to a moderate tropical storm, giving it the name
1203:
was exposed and the intensity had dropped to tropical depression status. It turned back to the northwest, steered by the low-level trade winds and following its previous path. Late on
February 20, the JTWC discontinued advisories, and three days later, the circulation dissipated off the east coast of Madagascar.
1202:
Moving southeastward in the flow of the trough, the small storm began weakening on
February 20 due to strong northwesterly wind shear, which caused the convection to dwindle over the circulation. That day, the storm passed just 80 km (50 mi) north of Mauritius, by which time the center
1194:
that spurred development. The structure rapidly organized, and by
February 19, there was an eye-like feature in the center of the thunderstorms. At 18:00 UTC that day, the JTWC classified it as Tropical Cyclone 12S, and the MFR upgraded it to a moderate tropical storm. Forecasters initially
1189:
recorded 376 mm (14.8 in) in just three hours, and over 48 hours, Le Brûlé recorded 1,274 mm (50.2 in) of precipitation. A weak low-pressure area began organizing within the trough on
February 17, organizing enough to be classified as Tropical Disturbance 09 the next day
1095:
over 18 hours. The storm deluged coastal
Mozambique with over 100 mm (3.9 in) of rainfall, causing river levels to increase in Inhambane Province. Europa Island recorded 136 mm (5.4 in) of rainfall over just six hours. The cyclone still maintained much of its intensity during
1074:
in the center of the organizing convection. An approaching trough caused the storm to accelerate southeastward, bringing it northeast of Europa Island. Late on February 3, the JTWC estimated peak 1 minute winds of 185 km/h (115 mph), while the MFR estimated 10 minute winds of
529:
The second disturbance was first classified by the MFR on October 12 about 1,575 km (979 mi) east of Diego Garcia. The system had enough of a circulation and associated convection, and proceeded southwestward for its duration. After the convection consolidated more and developed curved
449:
At the beginning of September 2005, the ITCZ was active in the northeastern portion of the basin, accompanied by a small circulation and scattered convection. Located in the presence of strong wind shear, the circulation was exposed from the convection, a sign of unfavorable conditions. However, warm
1368:
In the beginning of March, the monsoon was active to the northeast of Madagascar, the first time during the season that such active convection persisted northeast of the island. The broad system had two foci of low pressure; one was located northeast of Madagascar near St. Brandon, and the other was
1294:
between two ridges; as a result, the track shifted to the northeast and later northwest due to the building influence of the ridge to the southeast. Environmental conditions prevented significant convection to regenerate, and the circulation of Carina turned westward across the Indian Ocean without
880:
On December 21, the BoM began monitoring a tropical low in the western portion of the Australian basin, which had moved eastward from the south-west Indian Ocean basin. The system moved southwestward and later to the southwest, once again crossing 90º E and causing the MFR to designate it
688:
Simultaneous to Tropical Depression Three was Tropical Depression Four, which entered the basin on November 7 from the Australian region, and was also classified by the JTWC as Tropical Cyclone 02S with winds of 65 km/h (40 mph). The depression was weakening at the time, and both the
1457:
At the end of March, an active phase of the Madden–Julian oscillation caused an increase in convection over the northeastern portion of the basin. A low-pressure area formed on April 1 in the neighboring Australian basin, although the system soon after moved northwestward to cross 90º E.
1285:
while it was still an intensifying system. Also on February 23, the JTWC initiated warnings on the storm as Tropical Cyclone 14S. On the next day, the MFR upgraded Carina to a moderate tropical storm. The storm stalled on February 25 due to weakness in the ridge, and on the same day, the
1280:
increased convection across the northeastern periphery of the basin, and the ITCZ produced a distinct low-pressure area on February 21 to the east of Diego Garcia. The convective structure organized, aided by good outflow and moderate but lessening wind shear. A ridge to its southeast steered
1069:
allowed for restrengthening. By late on January 31, the system had reorganized into a moderate tropical storm. On the next day, the JTWC reissued advisories on Boloetse as the storm was just 170 km (110 mi) east of the Mozambique coast. Weak steering from the ridge to the southeast
336:
of at least 65 km/h (40 mph), below the average of nine. There were 30 days in which a moderate tropical storm was active, less than the average of 48. Three tropical storms attained tropical cyclone status, or 10 minute winds of at least 120 km/h (75 mph), and there
1377:
in 1980, making it the 6th wettest tropical system in history. The volcanic peak Commerson's Crater recorded 1,474 mm (58.0 in) over 24 hours, while coastal areas just 15 km (9.3 mi) away recorded 188 mm (7.4 in) of rainfall over the same time. The storm caused
1372:
The formative stages of Diwa brought heavy rainfall, reaching 193 mm (7.6 in) over 48 hours, to St. Brandon, as well as gale-force winds, with gusts to 120 km/h (75 mph). Along Mauritius, winds reached 126 km/h (78 mph), along with 495 mm (19.5 in) of
798:
to the south turned the storm to the west-northwest. By November 25, the increased wind shear had exposed the circulation from the convection, indicative of rapid weakening, and on that day Alvin was downgraded below tropical cyclone status. On the next day, the storm weakened to tropical
1461:
Early on April 13, the depression crossed 90º E into the south-west Indian Ocean. By that time, the system had good outflow to the south, although lack of moisture prevented significant development. Late on April 13, the MFR upgraded the system to Moderate Tropical Storm Elia,
793:
The MFR estimated peak 10 minute winds of 175 km/h (109 mph) within the basin, making it an intense tropical cyclone; it was the third consecutive year in which there was a November storm of such intensity. The JTWC, which designated Alvin as Tropical Cyclone 03S, estimated
1289:
Continued favorable conditions, including minimal wind shear and powerful outflow, allowed Carina to intensify further while progressing slowly southwestward. Late on February 27, the MFR upgraded the storm to an intense tropical cyclone, and the eye reached a diameter of 70 km
948:(ITCZ) produced an area of convection northeast of Madagascar on December 29, which had an association circulation. On January 1, the system moved across northern Madagascar and subsequently entered the Mozambique Channel. It continued quickly to the southwest, passing north of
972:. The rains resulted in flooding but also alleviated drought conditions in Mozambique. The rains also caused the Mutamba River to exceed its banks in Inhambane, flooding roads up to a meter (3.3 ft) deep and halting traffic. Across Mozambique, 26 people died due to the floods.
799:
depression status after nearly all of the convection was gone, prompting the JTWC to cease issuing advisories. The residual circulation remained well-defined with only temporary increases in convection. The MFR stopped issuing warnings on December 3, after Alvin had passed south of
1286:
JTWC upgraded the storm to the equivalent of hurricane status with 1 minute winds of 120 km/h (75 mph). By that time, an eye had developed within the center of increasingly organized convection, and the MFR upgraded Carina to tropical cyclone status on February 26.
1470:
Tropical Disturbance 12 briefly was classified by the MFR on March 4, located 620 km (390 mi) north of the developing Tropical Storm Diwa. The disturbance moved quickly to the southeast around Diwa's circulation, and was ultimately absorbed by the larger storm.
341:; both had late starts for the first named storm, drought conditions over much of the basin, and low activity. The third named storm, Carina, did not occur until late February, which at the time was the latest such date since naming began in 1960.
1281:
the nascent system slowly to the southwest into an area of increasingly favorable conditions. On February 22, the system was classified as Tropical Disturbance 10. The next day, the Mauritius Meteorological Service named the disturbance
1064:
The circulation became difficult to locate over land, and the JTWC briefly halted issuing advisories on January 29. On the next day, the circulation emerged westward into the Mozambique Channel, where low wind shear and good
295:
323:
There were 13 tropical disturbances in the season that were monitored by the MFR. Since the agency began operations in the early 1990s, this season had the second-fewest disturbances that received warning, only behind the
1295:
redevelopment. It turned back to the southwest, passing near St. Brandon on March 10. The MFR stopped tracking Carina on the next day, and the circulation dissipated on March 13 to the southeast of Madagascar.
368:– was rarely active. Conditions became generally more favorable in February and March, when four of the six tropical storms occurred. The general lack of thunderstorms over the basin caused drought-like conditions.
1079:
and increased wind shear caused Boloetse to weaken, and on February 4, the cyclone passed within 20 km (12 mi) of southwestern Madagascar. The storm accelerated and weakened, transitioning into an
604:
Tropical Depression Three formed on November 6 while east-southeast of Diego Garcia; it moved generally southward, reaching peak winds of 55 km/h (34 mph) before dissipating on November 8.
276:
in late November. After another short-lived disturbance in late December, there was a tropical disturbance in the Mozambique Channel in January that killed 26 people when it brought heavy rainfall to
337:
were 10 days in which these systems were active; this is half the average of 20 days, continuing the trend since the 2000–01 season of fewer stronger systems. The season was very similar to the
1100:
recorded wind gusts of 145 km/h (90 mph). In addition, heavy rainfall flooded two villages. Boloetse killed six people across southern Madagascar, while leaving 6,500 people homeless.
328:. Since the advent of satellite imagery in 1967, this season was the fifth least-active in terms of storm days and the number of cyclones. There were six systems that attained the intensity of a
320:(JTWC), which is a joint United States Navy – United States Air Force task force that issues tropical cyclone warnings for the region, also issued advisories for storms during the season.
1049:
from the trade winds prevented any initial organization as the system tracked southeastward. A ridge steered the disturbance to the southwest on January 23, bringing it just southeast of
1483:, then the Sub-regional Tropical Cyclone Advisory Centre in Madagascar assigns the appropriate name to the storm. If a tropical disturbance reaches moderate tropical storm status between
1045:
A pulse in the monsoon spawned an area of convection from the Seychelles westward. A circulation was evident by January 20, signalling its formation as a tropical disturbance. Poor
735:
273:
1190:
just off the eastern coast of Madagascar. A small system, it developed a concentrated area of convection just 200 km (120 mi) in diameter, which followed a powerful
1181:
on Mauritius recorded 177 mm (7.0 in) of rainfall in 48 hours. The heaviest precipitation occurred on Réunion in a short amount of time, with 1-in-50 year
2667:
2604:
2337:
683:
599:
524:
3060:
1426:
1173:
On February 15, a broad low-pressure area developed east of Madagascar. Over the next few days, the system dropped heavy rainfall to the Mascarene Islands.
297:
372:
on Réunion recorded just 18 mm (0.71 in) of rainfall from November to January, a record minimum. The island also recorded its third-highest average
849:
651:
1721:
1479:
A tropical disturbance is named when it reaches moderate tropical storm strength. If a tropical disturbance reaches moderate tropical storm status west of
2490:
2439:
2395:
2239:
2217:
2195:
2173:
2151:
2102:
2080:
2058:
2014:
1992:
1970:
1941:
3038:
3031:
3026:
3021:
3016:
3006:
3001:
2996:
2991:
2986:
2980:
338:
325:
217:
213:
205:
201:
2818:
261:, but suppressed activity in the western Indian Ocean. As a result, most of the storms developed near or entered from the Australian basin, crossing
1070:
caused the storm to meander in the area of favorable conditions. By late on February 2, Boloetse attain tropical cyclone status, developing an
952:, and was classified as Tropical Disturbance 7 late on January 3. It continued intensifying and organizing until moving ashore Mozambique near
774:, which spawned a circulation at 2º S on November 16. Two days later, the BoM classified the system as a tropical low to the north of the
268:
A series of four short-lived systems occurred from September to November in the northeastern portion of the basin. These were followed by the first
3065:
2342:
1178:
1826:
956:, and the system nearly attained tropical depression stage. The system followed the country's coastline, bending southward toward the capital
2849:
258:
182:
1091:
recorded 175 mm (6.9 in) of rainfall over 24 hours. In eastern Madagascar, the storm dropped 133 mm (5.2 in) in
1061:. The circulation had been weak during the approach to land, although there was a large increase in convection at the time of landfall.
309:
2871:
197:
187:
2675:
2612:
2351:
960:. On January 7, the disturbance moved offshore, but the system soon moved back overland and dissipated later that day over
2967:
2860:
2855:
1771:
1767:
1087:
Along much of its path, the storm dropped heavy rainfall. The formative stages of Boloetse spread rainfall to Mauritius, where
2811:
2346:(Report). The International Best Track Archive for Climate Stewardship (IBTrACS): Unifying tropical cyclone best track data.
1096:
its final approach to southwestern Madagascar, bringing estimated wind gusts of 200 km/h (120 mph) to the coast.
2785:
2945:
329:
238:
3075:
3070:
2804:
2950:
2672:
The International Best Track Archive for Climate Stewardship (IBTrACS): Unifying tropical cyclone best track data
2609:
The International Best Track Archive for Climate Stewardship (IBTrACS): Unifying tropical cyclone best track data
2347:
2893:
2888:
1741:
1737:
945:
361:
2791:
360:, which increased convection over the Australian region, but suppressed convection over the Indian Ocean. The
2905:
2900:
1791:
1751:
1747:
1277:
803:, although the circulation continued westward and was still visible north of Madagascar on December 10.
2745:
2775:
317:
312:
for the South-West Indian Ocean – tracked and named all tropical cyclones from the east coast of Africa to
246:
30:
2928:
2923:
1761:
1757:
1495:
assigns the appropriate name to the storm. A new annual list is used every year so no names are retired.
1196:
2835:
2831:
1731:
1727:
1076:
2961:
1833:
1713:
254:
1058:
775:
333:
269:
242:
1186:
2724:
2640:
2582:
2491:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2469:
2440:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2418:
2396:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2374:
2287:
2265:
2240:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2218:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2196:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2174:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2152:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2130:
2103:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2081:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2059:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
2037:
2015:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
1993:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
1971:"Bulletin for Cyclonic Activity and Significant Tropical Weather in the Southwest Indian Ocean"
241:. Three of these systems proceeded to attain tropical cyclone status – reaching 10 minute
1084:
on February 5. The remnant system was absorbed by the approaching trough two days later.
1081:
1066:
365:
1291:
1046:
373:
8:
795:
767:
369:
2308:
1488:
1484:
1480:
965:
353:
349:
313:
262:
250:
2796:
2746:"Tropical Cyclone Operational Plan for the South Pacific and South-East Indian Ocean"
1374:
345:
301:
230:
249:
also tracked eight storms in the basin. Activity was below normal due to a powerful
2827:
778:. The low moved southwestward, quickly intensifying, prompting the BoM to name it
2779:
2531:
1050:
344:
In general, storms in the season formed in the basin's periphery or north of the
2665:
2602:
2335:
996:
713:
1088:
900:
2666:
K. R. Knapp; M. C. Kruk; D. H. Levinson; H. J. Diamond; C. J. Neumann (2012).
2603:
K. R. Knapp; M. C. Kruk; D. H. Levinson; H. J. Diamond; C. J. Neumann (2012).
2336:
K. R. Knapp; M. C. Kruk; D. H. Levinson; H. J. Diamond; C. J. Neumann (2012).
3054:
1444:
1355:
1263:
1182:
1160:
1071:
1032:
949:
931:
867:
753:
669:
585:
510:
436:
281:. Later in the month, Tropical Cyclone Boloetse took an erratic track across
97:
827:
786:; at the time, the system was beginning to weaken due to cooler waters from
800:
272:– Alvin – which was renamed after it crossed from the Australian region as
1227:
721:
352:, an unusual occurrence. The overall lack of activity was due to a strong
2674:(Report). Bulletin of the American Meteorological Society. Archived from
2611:(Report). Bulletin of the American Meteorological Society. Archived from
1174:
1402:
1448:
1359:
1267:
1177:
recorded 229 mm (9.0 in) of rainfall over 24 hours, and
1164:
1036:
935:
871:
757:
673:
589:
549:
514:
474:
440:
400:
282:
278:
237:
tracked 13 tropical disturbances, of which six intensified into a
101:
1004:
629:
305:
234:
2966:
1492:
1191:
969:
961:
953:
787:
357:
1235:
1092:
1792:
Operational procedures of TC satellite analysis at RSMC La Réunion
1410:
1327:
1132:
2697:
Steve Newman (March 13, 2006). "EarthWeek; Diary of the planet".
1097:
835:
771:
637:
557:
482:
408:
2772:
1319:
794:
1 minute winds of 195 km/h (121 mph). A building
1124:
957:
294:
1824:
1491:, then the Sub-regional Tropical Cyclone Advisory Centre in
684:
List of off-season South-West Indian Ocean tropical cyclones
600:
List of off-season South-West Indian Ocean tropical cyclones
525:
List of off-season South-West Indian Ocean tropical cyclones
245:
of at least 120 km/h (75 mph). The American-based
2512:"Mozambique; Inhambane Isolated, Limpopo Line Suspended".
689:
JTWC and MFR discontinued advisories on November 8.
2038:"Monthly Global Tropical Cyclone Summary September 2005"
692:
2583:"Monthly Global Tropical Cyclone Summary February 2006"
2375:"Monthly Global Tropical Cyclone Summary December 2005"
2266:"Monthly Global Tropical Cyclone Summary November 2005"
2826:
2553:"Mozambique; Cyclone Brings Heavy Rain to Inhambane".
2470:"Monthly Global Tropical Cyclone Summary January 2006"
2288:"Monthly Global Tropical Cyclone Tracks November 2005"
2131:"Monthly Global Tropical Cyclone Summary October 2005"
2534:. New Zealand: AllAfrica. The Herald. January 6, 2006
2532:"Zimbabwe: Heavy Rains Pound Chipinge As Floods Loom"
2419:"Monthly Global Tropical Cyclone Tracks January 2006"
2725:"Monthly Global Tropical Cyclone Summary April 2006"
2641:"Monthly Global Tropical Cyclone Summary March 2006"
1722:
List of Southern Hemisphere tropical cyclone seasons
1703:
1206:
2968:2000–2009 South-West Indian Ocean cyclone seasons
3052:
198:South-West Indian Ocean tropical cyclone seasons
2343:Bulletin of the American Meteorological Society
1789:
1381:
3061:2005–06 South-West Indian Ocean cyclone season
227:2005–06 South-West Indian Ocean cyclone season
24:2005–06 South-West Indian Ocean cyclone season
2812:
1298:
1219:Category 4 tropical cyclone (SSHWS)
988:Category 3 tropical cyclone (SSHWS)
705:Category 3 tropical cyclone (SSHWS)
2722:
2696:
2638:
2580:
2467:
2416:
2372:
2285:
2263:
2128:
2035:
975:
770:produced an area of convection southwest of
16:Cyclone season in the Southwest Indian Ocean
1797:(Report). World Meteorological Organization
1103:
2819:
2805:
1790:Philippe Caroff; et al. (June 2011).
884:
384:
310:Regional Specialized Meteorological Center
229:was the fifth least-active on record. The
2751:. World Meteorological Organization. 2005
806:
608:
533:
453:
2738:
968:, reaching 162 mm (6.4 in) in
183:2005–06 Australian region cyclone season
3066:South-West Indian Ocean cyclone seasons
964:. The system brought heavy rainfall to
3053:
2718:
2716:
2714:
2712:
2661:
2659:
2657:
2634:
2632:
2630:
2576:
2574:
2572:
2570:
2568:
2463:
2461:
2459:
2457:
2331:
2329:
2259:
2257:
2124:
2122:
2120:
1936:
1934:
1932:
1930:
1928:
1926:
1924:
1922:
1920:
1918:
1916:
1914:
1912:
1910:
1908:
1906:
1904:
1902:
1900:
1898:
1896:
1894:
1892:
1890:
1888:
1886:
1884:
1882:
1880:
1878:
1876:
1874:
1820:
1818:
1816:
1814:
1812:
265:to enter the South-West Indian Ocean.
2965:
2800:
1872:
1870:
1868:
1866:
1864:
1862:
1860:
1858:
1856:
1854:
1825:Joint Typhoon Warning Center (2006).
693:Intense Tropical Cyclone Bertie–Alvin
1832:(Report). p. 71. Archived from
1766:North Indian Ocean cyclone seasons:
1195:assessed the structure as akin to a
188:2005–06 South Pacific cyclone season
2773:Joint Typhoon Warning Center (JTWC)
2709:
2654:
2627:
2596:
2565:
2454:
2326:
2254:
2117:
1827:2006 Annual Tropical Cyclone Report
1809:
1214:Intense tropical cyclone (MFR)
700:Intense tropical cyclone (MFR)
364:– typically a major contributor to
288:
13:
2703: – via Lexis Nexis
2559: – via Lexis Nexis
2518: – via Lexis Nexis
2286:Gary Padgett (December 11, 2005).
2105:. Météo-France. September 12, 2005
2036:Gary Padgett (February 12, 2006).
1851:
1389:Moderate tropical storm (MFR)
14:
3087:
2792:World Meteorological Organization
2766:
2417:Gary Padgett (February 7, 2006).
2398:. Météo-France. December 29, 2005
2338:2006 Alvin:Bertie (2005322S04095)
2083:. Météo-France. September 8, 2005
2061:. Météo-France. September 6, 2005
2017:. Météo-France. September 5, 2005
1995:. Météo-France. September 4, 2005
1973:. Météo-France. September 1, 2005
2242:. Météo-France. October 21, 2005
2220:. Météo-France. October 17, 2005
2198:. Météo-France. October 15, 2005
2176:. Météo-France. October 14, 2005
2154:. Météo-France. October 13, 2005
1706:
1465:
1409:
1401:
1326:
1318:
1306:Severe tropical storm (MFR)
1234:
1226:
1131:
1123:
1111:Severe tropical storm (MFR)
1075:155 km/h (96 mph). An
1003:
995:
899:
834:
826:
720:
712:
636:
628:
621:Tropical depression (SSHWS)
556:
548:
481:
473:
407:
399:
316:, and south of the equator. The
29:
2723:Gary Padgett (August 6, 2006).
2690:
2605:2006 0920052006 (2006049S16051)
2581:Gary Padgett (April 28, 2006).
2546:
2524:
2505:
2493:. Météo-France. January 7, 2006
2483:
2468:Gary Padgett (April 18, 2006).
2442:. Météo-France. January 4, 2006
2432:
2410:
2388:
2373:Gary Padgett (March 26, 2006).
2366:
2348:American Meteorological Society
2314:(Report). Bureau of Meteorology
2301:
2279:
2264:Gary Padgett (March 19, 2006).
2232:
2210:
2188:
2166:
2144:
2129:Gary Padgett (March 13, 2006).
2095:
1207:Intense Tropical Cyclone Carina
892:Tropical disturbance (MFR)
392:Tropical disturbance (MFR)
2786:Météo France (RSMC La Réunion)
2309:Severe Tropical Cyclone Bertie
2073:
2051:
2029:
2007:
1985:
1963:
1783:
1474:
1145:February 18 – February 23
946:Intertropical Convergence Zone
814:Tropical depression (MFR)
616:Tropical depression (MFR)
541:Tropical depression (MFR)
461:Tropical depression (MFR)
421:September 5 – September 8
362:Intertropical Convergence Zone
348:. No systems developed in the
1:
2639:Gary Padgett (July 9, 2006).
1777:
1256:205 km/h (125 mph)
1025:155 km/h (100 mph)
766:In the middle of November, a
746:175 km/h (110 mph)
1736:Atlantic hurricane seasons:
1497:
1382:Moderate Tropical Storm Elia
1348:110 km/h (70 mph)
1017:January 20 – February 5
570:November 6 – November 8
495:October 12 – October 15
318:Joint Typhoon Warning Center
304:'s meteorological office in
247:Joint Typhoon Warning Center
93: • Lowest pressure
7:
1746:Pacific hurricane seasons:
1699:
1437:75 km/h (45 mph)
1394:Tropical storm (SSHWS)
1311:Tropical storm (SSHWS)
1248:February 22 – March 11
1197:mesoscale convective vortex
1185:. A station in the capital
1153:95 km/h (60 mph)
1116:Tropical storm (SSHWS)
983:Tropical cyclone (MFR)
924:45 km/h (30 mph)
860:55 km/h (35 mph)
819:Tropical storm (SSHWS)
662:55 km/h (35 mph)
578:55 km/h (35 mph)
503:55 km/h (35 mph)
466:Tropical storm (SSHWS)
429:45 km/h (30 mph)
332:, which has 10 minute
10:
3092:
1299:Severe Tropical Storm Diwa
916:January 3 – January 7
790:and increased wind shear.
681:
597:
522:
379:
79: • Maximum winds
3076:Tropical cyclones in 2006
3071:Tropical cyclones in 2005
2974:
2938:
2915:
2880:
2842:
2668:2006 Diwa (2006060S13058)
1756:Pacific typhoon seasons:
1433:
1419:
1398:
1393:
1388:
1344:
1336:
1315:
1310:
1305:
1278:Madden–Julian oscillation
1252:
1244:
1223:
1218:
1213:
1149:
1141:
1120:
1115:
1110:
1077:eyewall replacement cycle
1021:
1013:
992:
987:
982:
976:Tropical Cyclone Boloetse
920:
912:
896:
891:
856:
844:
823:
818:
813:
742:
730:
709:
704:
699:
658:
646:
625:
620:
615:
574:
566:
545:
540:
499:
491:
470:
465:
460:
425:
417:
396:
391:
196:
178:
173:
165:
157:
150:Intense tropical cyclones
149:
141:
133:
125:
117:
112:
108:
92:
78:
70:
66:
61:
53:
45:
40:
28:
23:
1942:Cyclone Season 2005–2006
1714:Tropical cyclones portal
1104:Severe Tropical Storm 09
376:from November to April.
233:office on the island of
2867:South-West Indian Ocean
2705:(subscription required)
2561:(subscription required)
2520:(subscription required)
1427:out of basin April 7–13
1423:April 6 – April 17
1276:An active phase of the
885:Tropical Disturbance 07
385:Tropical Disturbance 01
330:moderate tropical storm
274:Tropical Cyclone Bertie
243:maximum sustained winds
239:moderate tropical storm
1951:(Report). Météo-France
1340:March 2 – March 8
807:Tropical Depression 06
609:Tropical Depression 04
534:Tropical Depression 03
454:Tropical Depression 02
54:Last system dissipated
1726:Tropical cyclones in
1082:extratropical cyclone
682:Further information:
598:Further information:
523:Further information:
366:tropical cyclogenesis
308:(MFR) – the official
257:over the neighboring
2854:North Indian Ocean (
1839:on February 21, 2013
374:atmospheric pressure
2557:. February 2, 2006.
852: – December 29
768:westerly wind burst
738:) – December 3
370:Pierrefonds Airport
113:Seasonal statistics
86:10-minute sustained
46:First system formed
41:Seasonal boundaries
2939:Non-seasonal lists
2778:2010-03-01 at the
2516:. January 9, 2006.
966:Inhambane Province
654: – November 8
354:Walker circulation
350:Mozambique Channel
253:, which increased
251:Walker circulation
118:Total disturbances
82:205 km/h (125 mph)
35:Season summary map
3048:
3047:
3041:
2983:
2959:
2958:
2850:Australian region
2828:Tropical cyclones
2678:on March 27, 2016
2615:on March 27, 2016
2354:on March 26, 2016
1697:
1696:
1455:
1454:
1440:
1375:Cyclone Hyacinthe
1366:
1365:
1351:
1274:
1273:
1259:
1179:Plaisance Airport
1171:
1170:
1156:
1043:
1042:
1028:
942:
941:
927:
878:
877:
863:
764:
763:
749:
680:
679:
665:
596:
595:
581:
521:
520:
506:
447:
446:
432:
346:Mascarene Islands
223:
222:
161:At least 42 total
142:Tropical cyclones
126:Total depressions
49:September 5, 2005
3083:
3036:
2978:
2963:
2962:
2821:
2814:
2807:
2798:
2797:
2761:
2760:
2758:
2756:
2750:
2742:
2736:
2735:
2733:
2731:
2720:
2707:
2706:
2702:
2694:
2688:
2687:
2685:
2683:
2663:
2652:
2651:
2649:
2647:
2636:
2625:
2624:
2622:
2620:
2600:
2594:
2593:
2591:
2589:
2578:
2563:
2562:
2558:
2550:
2544:
2543:
2541:
2539:
2528:
2522:
2521:
2517:
2509:
2503:
2502:
2500:
2498:
2487:
2481:
2480:
2478:
2476:
2465:
2452:
2451:
2449:
2447:
2436:
2430:
2429:
2427:
2425:
2414:
2408:
2407:
2405:
2403:
2392:
2386:
2385:
2383:
2381:
2370:
2364:
2363:
2361:
2359:
2350:. Archived from
2333:
2324:
2323:
2321:
2319:
2313:
2305:
2299:
2298:
2296:
2294:
2283:
2277:
2276:
2274:
2272:
2261:
2252:
2251:
2249:
2247:
2236:
2230:
2229:
2227:
2225:
2214:
2208:
2207:
2205:
2203:
2192:
2186:
2185:
2183:
2181:
2170:
2164:
2163:
2161:
2159:
2148:
2142:
2141:
2139:
2137:
2126:
2115:
2114:
2112:
2110:
2099:
2093:
2092:
2090:
2088:
2077:
2071:
2070:
2068:
2066:
2055:
2049:
2048:
2046:
2044:
2033:
2027:
2026:
2024:
2022:
2011:
2005:
2004:
2002:
2000:
1989:
1983:
1982:
1980:
1978:
1967:
1961:
1960:
1958:
1956:
1946:
1938:
1849:
1848:
1846:
1844:
1838:
1831:
1822:
1807:
1806:
1804:
1802:
1796:
1787:
1716:
1711:
1710:
1709:
1691:
1683:
1675:
1667:
1659:
1651:
1643:
1635:
1623:
1615:
1607:
1599:
1591:
1583:
1575:
1567:
1559:
1547:
1539:
1531:
1523:
1498:
1438:
1414:
1413:
1408:
1405:
1386:
1385:
1349:
1331:
1330:
1325:
1322:
1303:
1302:
1257:
1239:
1238:
1233:
1230:
1211:
1210:
1154:
1136:
1135:
1130:
1127:
1108:
1107:
1026:
1008:
1007:
1002:
999:
980:
979:
925:
907:
906:
903:
889:
888:
861:
839:
838:
833:
830:
811:
810:
747:
725:
724:
719:
716:
697:
696:
663:
641:
640:
635:
632:
613:
612:
579:
561:
560:
555:
552:
538:
537:
504:
486:
485:
480:
477:
458:
457:
430:
412:
411:
406:
403:
389:
388:
289:Seasonal summary
259:Australian basin
174:Related articles
158:Total fatalities
33:
21:
20:
3091:
3090:
3086:
3085:
3084:
3082:
3081:
3080:
3051:
3050:
3049:
3044:
2970:
2960:
2955:
2934:
2911:
2876:
2838:
2825:
2780:Wayback Machine
2769:
2764:
2754:
2752:
2748:
2744:
2743:
2739:
2729:
2727:
2721:
2710:
2704:
2695:
2691:
2681:
2679:
2664:
2655:
2645:
2643:
2637:
2628:
2618:
2616:
2601:
2597:
2587:
2585:
2579:
2566:
2560:
2552:
2551:
2547:
2537:
2535:
2530:
2529:
2525:
2519:
2511:
2510:
2506:
2496:
2494:
2489:
2488:
2484:
2474:
2472:
2466:
2455:
2445:
2443:
2438:
2437:
2433:
2423:
2421:
2415:
2411:
2401:
2399:
2394:
2393:
2389:
2379:
2377:
2371:
2367:
2357:
2355:
2334:
2327:
2317:
2315:
2311:
2307:
2306:
2302:
2292:
2290:
2284:
2280:
2270:
2268:
2262:
2255:
2245:
2243:
2238:
2237:
2233:
2223:
2221:
2216:
2215:
2211:
2201:
2199:
2194:
2193:
2189:
2179:
2177:
2172:
2171:
2167:
2157:
2155:
2150:
2149:
2145:
2135:
2133:
2127:
2118:
2108:
2106:
2101:
2100:
2096:
2086:
2084:
2079:
2078:
2074:
2064:
2062:
2057:
2056:
2052:
2042:
2040:
2034:
2030:
2020:
2018:
2013:
2012:
2008:
1998:
1996:
1991:
1990:
1986:
1976:
1974:
1969:
1968:
1964:
1954:
1952:
1949:RSMC La Réunion
1944:
1940:
1939:
1852:
1842:
1840:
1836:
1829:
1823:
1810:
1800:
1798:
1794:
1788:
1784:
1780:
1712:
1707:
1705:
1702:
1686:
1678:
1670:
1662:
1654:
1646:
1638:
1630:
1618:
1610:
1602:
1594:
1586:
1578:
1570:
1562:
1554:
1542:
1534:
1526:
1518:
1477:
1468:
1442:
1424:
1415:
1406:
1400:
1384:
1353:
1332:
1323:
1317:
1301:
1261:
1240:
1231:
1225:
1209:
1158:
1137:
1128:
1122:
1106:
1051:Tromelin Island
1030:
1009:
1000:
994:
978:
929:
908:
904:
898:
887:
865:
850:(Entered basin)
840:
831:
825:
809:
751:
726:
717:
711:
695:
686:
667:
652:(Entered basin)
642:
633:
627:
611:
602:
583:
562:
553:
547:
536:
527:
508:
487:
478:
472:
456:
434:
413:
404:
398:
387:
382:
334:sustained winds
299:
298:
296:
291:
200:
192:
83:
62:Strongest storm
36:
17:
12:
11:
5:
3089:
3079:
3078:
3073:
3068:
3063:
3046:
3045:
3043:
3042:
3034:
3029:
3024:
3019:
3014:
3009:
3004:
2999:
2994:
2989:
2984:
2975:
2972:
2971:
2957:
2956:
2954:
2953:
2951:South Atlantic
2948:
2942:
2940:
2936:
2935:
2933:
2932:
2926:
2919:
2917:
2913:
2912:
2910:
2909:
2903:
2897:
2891:
2884:
2882:
2878:
2877:
2875:
2874:
2872:South Pacific
2869:
2864:
2858:
2852:
2846:
2844:
2840:
2839:
2824:
2823:
2816:
2809:
2801:
2795:
2794:
2789:
2783:
2768:
2767:External links
2765:
2763:
2762:
2737:
2708:
2699:Hobart Mercury
2689:
2653:
2626:
2595:
2564:
2545:
2523:
2504:
2482:
2453:
2431:
2409:
2387:
2365:
2325:
2300:
2278:
2253:
2231:
2209:
2187:
2165:
2143:
2116:
2094:
2072:
2050:
2028:
2006:
1984:
1962:
1850:
1808:
1781:
1779:
1776:
1775:
1774:
1764:
1754:
1744:
1734:
1724:
1718:
1717:
1701:
1698:
1695:
1694:
1693:
1692:
1684:
1676:
1668:
1660:
1652:
1644:
1636:
1626:
1625:
1624:
1616:
1608:
1600:
1592:
1584:
1576:
1568:
1560:
1550:
1549:
1548:
1543:Isabella
1540:
1532:
1524:
1516:
1513:
1510:
1507:
1504:
1476:
1473:
1467:
1464:
1453:
1452:
1435:
1434:Peak intensity
1431:
1430:
1421:
1417:
1416:
1399:
1396:
1395:
1391:
1390:
1383:
1380:
1364:
1363:
1346:
1345:Peak intensity
1342:
1341:
1338:
1334:
1333:
1316:
1313:
1312:
1308:
1307:
1300:
1297:
1272:
1271:
1254:
1253:Peak intensity
1250:
1249:
1246:
1242:
1241:
1224:
1221:
1220:
1216:
1215:
1208:
1205:
1183:rainfall rates
1169:
1168:
1151:
1150:Peak intensity
1147:
1146:
1143:
1139:
1138:
1121:
1118:
1117:
1113:
1112:
1105:
1102:
1041:
1040:
1023:
1022:Peak intensity
1019:
1018:
1015:
1011:
1010:
993:
990:
989:
985:
984:
977:
974:
940:
939:
922:
921:Peak intensity
918:
917:
914:
910:
909:
897:
894:
893:
886:
883:
876:
875:
858:
857:Peak intensity
854:
853:
846:
842:
841:
824:
821:
820:
816:
815:
808:
805:
762:
761:
744:
743:Peak intensity
740:
739:
732:
728:
727:
710:
707:
706:
702:
701:
694:
691:
678:
677:
660:
659:Peak intensity
656:
655:
648:
644:
643:
626:
623:
622:
618:
617:
610:
607:
594:
593:
576:
575:Peak intensity
572:
571:
568:
564:
563:
546:
543:
542:
535:
532:
519:
518:
501:
500:Peak intensity
497:
496:
493:
489:
488:
471:
468:
467:
463:
462:
455:
452:
445:
444:
427:
426:Peak intensity
423:
422:
419:
415:
414:
397:
394:
393:
386:
383:
381:
378:
339:1998–99 season
326:2000–01 season
293:
292:
290:
287:
221:
220:
194:
193:
191:
190:
185:
179:
176:
175:
171:
170:
167:
163:
162:
159:
155:
154:
151:
147:
146:
143:
139:
138:
135:
131:
130:
127:
123:
122:
119:
115:
114:
110:
109:
106:
105:
94:
90:
89:
80:
76:
75:
72:
68:
67:
64:
63:
59:
58:
57:April 17, 2006
55:
51:
50:
47:
43:
42:
38:
37:
34:
26:
25:
15:
9:
6:
4:
3:
2:
3088:
3077:
3074:
3072:
3069:
3067:
3064:
3062:
3059:
3058:
3056:
3040:
3035:
3033:
3030:
3028:
3025:
3023:
3020:
3018:
3015:
3013:
3010:
3008:
3005:
3003:
3000:
2998:
2995:
2993:
2990:
2988:
2985:
2982:
2977:
2976:
2973:
2969:
2964:
2952:
2949:
2947:
2946:Mediterranean
2944:
2943:
2941:
2937:
2930:
2927:
2925:
2921:
2920:
2918:
2914:
2907:
2904:
2902:
2898:
2895:
2892:
2890:
2886:
2885:
2883:
2879:
2873:
2870:
2868:
2865:
2862:
2859:
2857:
2853:
2851:
2848:
2847:
2845:
2841:
2837:
2833:
2829:
2822:
2817:
2815:
2810:
2808:
2803:
2802:
2799:
2793:
2790:
2787:
2784:
2781:
2777:
2774:
2771:
2770:
2747:
2741:
2726:
2719:
2717:
2715:
2713:
2700:
2693:
2677:
2673:
2669:
2662:
2660:
2658:
2642:
2635:
2633:
2631:
2614:
2610:
2606:
2599:
2584:
2577:
2575:
2573:
2571:
2569:
2556:
2549:
2533:
2527:
2515:
2508:
2492:
2486:
2471:
2464:
2462:
2460:
2458:
2441:
2435:
2420:
2413:
2397:
2391:
2376:
2369:
2353:
2349:
2345:
2344:
2339:
2332:
2330:
2310:
2304:
2289:
2282:
2267:
2260:
2258:
2241:
2235:
2219:
2213:
2197:
2191:
2175:
2169:
2153:
2147:
2132:
2125:
2123:
2121:
2104:
2098:
2082:
2076:
2060:
2054:
2039:
2032:
2016:
2010:
1994:
1988:
1972:
1966:
1950:
1943:
1937:
1935:
1933:
1931:
1929:
1927:
1925:
1923:
1921:
1919:
1917:
1915:
1913:
1911:
1909:
1907:
1905:
1903:
1901:
1899:
1897:
1895:
1893:
1891:
1889:
1887:
1885:
1883:
1881:
1879:
1877:
1875:
1873:
1871:
1869:
1867:
1865:
1863:
1861:
1859:
1857:
1855:
1835:
1828:
1821:
1819:
1817:
1815:
1813:
1793:
1786:
1782:
1773:
1769:
1765:
1763:
1759:
1755:
1753:
1749:
1745:
1743:
1739:
1735:
1733:
1729:
1725:
1723:
1720:
1719:
1715:
1704:
1690:
1685:
1682:
1677:
1674:
1669:
1666:
1661:
1658:
1653:
1650:
1645:
1642:
1637:
1634:
1629:
1628:
1627:
1622:
1617:
1614:
1609:
1606:
1603:Pindile
1601:
1598:
1593:
1590:
1585:
1582:
1579:Marinda
1577:
1574:
1571:Lindsay
1569:
1566:
1561:
1558:
1553:
1552:
1551:
1546:
1541:
1538:
1533:
1530:
1525:
1522:
1517:
1514:
1511:
1508:
1505:
1502:
1501:
1500:
1499:
1496:
1494:
1490:
1486:
1482:
1472:
1466:Other systems
1463:
1459:
1450:
1446:
1436:
1432:
1428:
1422:
1418:
1412:
1404:
1397:
1392:
1387:
1379:
1376:
1370:
1361:
1357:
1347:
1343:
1339:
1335:
1329:
1321:
1314:
1309:
1304:
1296:
1293:
1287:
1284:
1279:
1269:
1265:
1255:
1251:
1247:
1243:
1237:
1229:
1222:
1217:
1212:
1204:
1200:
1198:
1193:
1188:
1184:
1180:
1176:
1166:
1162:
1152:
1148:
1144:
1140:
1134:
1126:
1119:
1114:
1109:
1101:
1099:
1094:
1090:
1085:
1083:
1078:
1073:
1068:
1062:
1060:
1056:
1052:
1048:
1038:
1034:
1024:
1020:
1016:
1012:
1006:
998:
991:
986:
981:
973:
971:
967:
963:
959:
955:
951:
950:Europa Island
947:
937:
933:
923:
919:
915:
911:
902:
895:
890:
882:
873:
869:
859:
855:
851:
847:
843:
837:
829:
822:
817:
812:
804:
802:
797:
791:
789:
785:
781:
777:
776:Cocos Islands
773:
769:
759:
755:
745:
741:
737:
736:entered basin
734:November 24 (
733:
729:
723:
715:
708:
703:
698:
690:
685:
675:
671:
661:
657:
653:
649:
645:
639:
631:
624:
619:
614:
606:
601:
591:
587:
577:
573:
569:
565:
559:
551:
544:
539:
531:
526:
516:
512:
502:
498:
494:
490:
484:
476:
469:
464:
459:
451:
442:
438:
428:
424:
420:
416:
410:
402:
395:
390:
377:
375:
371:
367:
363:
359:
355:
351:
347:
342:
340:
335:
331:
327:
321:
319:
315:
311:
307:
303:
286:
284:
280:
275:
271:
266:
264:
260:
256:
252:
248:
244:
240:
236:
232:
228:
219:
215:
211:
207:
203:
199:
195:
189:
186:
184:
181:
180:
177:
172:
168:
164:
160:
156:
152:
148:
144:
140:
136:
132:
128:
124:
120:
116:
111:
107:
103:
99:
95:
91:
87:
81:
77:
73:
69:
65:
60:
56:
52:
48:
44:
39:
32:
27:
22:
19:
3011:
2866:
2753:. Retrieved
2740:
2728:. Retrieved
2698:
2692:
2680:. Retrieved
2676:the original
2671:
2644:. Retrieved
2617:. Retrieved
2613:the original
2608:
2598:
2586:. Retrieved
2554:
2548:
2536:. Retrieved
2526:
2513:
2507:
2495:. Retrieved
2485:
2473:. Retrieved
2444:. Retrieved
2434:
2422:. Retrieved
2412:
2400:. Retrieved
2390:
2378:. Retrieved
2368:
2356:. Retrieved
2352:the original
2341:
2316:. Retrieved
2303:
2291:. Retrieved
2281:
2269:. Retrieved
2244:. Retrieved
2234:
2222:. Retrieved
2212:
2200:. Retrieved
2190:
2178:. Retrieved
2168:
2156:. Retrieved
2146:
2134:. Retrieved
2107:. Retrieved
2097:
2085:. Retrieved
2075:
2063:. Retrieved
2053:
2041:. Retrieved
2031:
2019:. Retrieved
2009:
1997:. Retrieved
1987:
1975:. Retrieved
1965:
1953:. Retrieved
1948:
1841:. Retrieved
1834:the original
1799:. Retrieved
1785:
1688:
1687:Zoelle
1680:
1672:
1664:
1656:
1648:
1640:
1632:
1631:Sebina
1620:
1619:Rugare
1612:
1611:Quincy
1604:
1596:
1588:
1587:Nadety
1580:
1572:
1564:
1563:Kundai
1556:
1544:
1536:
1528:
1527:Guduza
1520:
1478:
1469:
1460:
1456:
1371:
1367:
1288:
1282:
1275:
1201:
1172:
1086:
1063:
1054:
1044:
943:
879:
848:December 23
801:Diego Garcia
792:
783:
779:
765:
687:
603:
528:
448:
343:
322:
302:Météo-France
300:
267:
231:Météo-France
226:
224:
209:
166:Total damage
134:Total storms
85:
18:
2555:Africa News
2514:Africa News
1671:Xanda
1663:Wilby
1639:Timba
1595:Otile
1555:Jaone
1535:Helio
1519:Farda
1475:Storm names
1187:Saint-Denis
1175:St. Brandon
650:November 6
270:named storm
3055:Categories
2979:Previous:
2887:Atlantic (
2881:Hurricanes
1778:References
1679:Yuri
1655:Velo
1647:Usta
930:1002
435:1001
283:Madagascar
279:Mozambique
255:convection
2922:Pacific (
2899:Pacific (
2646:March 31,
2619:March 31,
2588:March 31,
2538:March 30,
2497:March 30,
2475:March 30,
2446:March 30,
2424:March 30,
2402:March 30,
2380:March 30,
2358:March 30,
2318:March 30,
2293:March 29,
2271:March 29,
2246:March 29,
2224:March 29,
2202:March 29,
2180:March 29,
2158:March 29,
2136:March 29,
2109:March 29,
2087:March 29,
2065:March 29,
2043:March 29,
2021:March 29,
1999:March 29,
1977:March 29,
1955:March 29,
1843:March 29,
1801:April 22,
1493:Mauritius
1443:990
1354:980
1262:915
1192:hot tower
1159:992
1059:Mananjary
1031:950
970:Inhambane
962:Swaziland
954:Vilankulo
866:998
788:upwelling
752:930
668:995
584:998
509:997
358:Indonesia
2916:Typhoons
2843:Cyclones
2776:Archived
2730:April 1,
2682:April 1,
1700:See also
1689:(unused)
1681:(unused)
1673:(unused)
1665:(unused)
1657:(unused)
1649:(unused)
1641:(unused)
1633:(unused)
1621:(unused)
1613:(unused)
1605:(unused)
1597:(unused)
1589:(unused)
1581:(unused)
1573:(unused)
1565:(unused)
1557:(unused)
1545:(unused)
1537:(unused)
1529:(unused)
1521:(unused)
1506:Boloetse
1439:(10-min)
1420:Duration
1350:(10-min)
1337:Duration
1258:(10-min)
1245:Duration
1155:(10-min)
1142:Duration
1093:Mahanoro
1055:Boloetse
1027:(10-min)
1014:Duration
926:(10-min)
913:Duration
862:(10-min)
845:Duration
748:(10-min)
731:Duration
664:(10-min)
647:Duration
580:(10-min)
567:Duration
505:(10-min)
492:Duration
431:(10-min)
418:Duration
3039:2010–11
3032:2009–10
3027:2008–09
3022:2007–08
3017:2006–07
3012:2005–06
3007:2004–05
3002:2003–04
2997:2002–03
2992:2001–02
2987:2000–01
2981:1999–00
2755:May 20,
1447: (
1358: (
1266: (
1163: (
1098:Toliara
1067:outflow
1035: (
934: (
870: (
772:Sumatra
756: (
672: (
588: (
513: (
439: (
380:Systems
306:Réunion
235:Réunion
218:2007–08
214:2006–07
210:2005–06
206:2004–05
202:2003–04
169:Unknown
3037:Next:
1509:Carina
1407:
1324:
1283:Carina
1232:
1129:
1089:Vacoas
1047:inflow
1001:
958:Maputo
905:
832:
780:Bertie
718:
634:
554:
479:
405:
74:Carina
2749:(PDF)
2312:(PDF)
1945:(PDF)
1837:(PDF)
1830:(PDF)
1795:(PDF)
1503:Alvin
796:ridge
784:Alvin
356:over
314:90° E
2929:2006
2924:2005
2906:2006
2901:2005
2894:2006
2889:2005
2861:2006
2856:2005
2836:2006
2834:and
2832:2005
2757:2016
2732:2016
2684:2016
2648:2016
2621:2016
2590:2016
2540:2016
2499:2016
2477:2016
2448:2016
2426:2016
2404:2016
2382:2016
2360:2016
2320:2016
2295:2016
2273:2016
2248:2016
2226:2016
2204:2016
2182:2016
2160:2016
2138:2016
2111:2016
2089:2016
2067:2016
2045:2016
2023:2016
2001:2016
1979:2016
1957:2016
1845:2016
1803:2013
1772:2006
1768:2005
1762:2006
1758:2005
1752:2006
1748:2005
1742:2006
1738:2005
1732:2006
1730:and
1728:2005
1515:Elia
1512:Diwa
1489:90°E
1487:and
1485:55°E
1481:55°E
1449:mbar
1360:mbar
1268:mbar
1165:mbar
1037:mbar
944:The
936:mbar
872:mbar
758:mbar
674:mbar
590:mbar
515:mbar
441:mbar
263:90°E
225:The
102:mbar
96:915
71:Name
2830:in
1445:hPa
1356:hPa
1292:col
1264:hPa
1161:hPa
1072:eye
1033:hPa
932:hPa
868:hPa
754:hPa
670:hPa
586:hPa
511:hPa
437:hPa
98:hPa
3057::
2711:^
2670:.
2656:^
2629:^
2607:.
2567:^
2456:^
2340:.
2328:^
2256:^
2119:^
1947:.
1853:^
1811:^
1770:,
1760:,
1750:,
1740:,
216:,
212:,
208:,
204:,
129:10
121:13
2931:)
2908:)
2896:)
2863:)
2820:e
2813:t
2806:v
2788:.
2782:.
2759:.
2734:.
2701:.
2686:.
2650:.
2623:.
2592:.
2542:.
2501:.
2479:.
2450:.
2428:.
2406:.
2384:.
2362:.
2322:.
2297:.
2275:.
2250:.
2228:.
2206:.
2184:.
2162:.
2140:.
2113:.
2091:.
2069:.
2047:.
2025:.
2003:.
1981:.
1959:.
1847:.
1805:.
1451:)
1441:;
1429:)
1425:(
1362:)
1352:;
1270:)
1260:;
1167:)
1157:;
1039:)
1029:;
938:)
928:;
874:)
864:;
760:)
750:;
676:)
666:;
592:)
582:;
517:)
507:;
443:)
433:;
153:2
145:3
137:6
104:)
100:(
88:)
84:(
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
