Hurricane Fausto (2002)

Map plotting the track and the intensity of the storm, according to the Saffir–Simpson scale

The origins of Hurricane Fausto were from a tropical wave that emerged into the eastern Atlantic Ocean from the west coast of Africa on August 11. It crossed the Atlantic and Caribbean uneventfully. The tropical wave ultimately entered the Eastern Pacific Basin on August 17. Rapidly organizing, the system was classified using the Dvorak technique at 1800 UTC on August 18. Although a broad closed circulation was present on August 19, the system became less organized and thus was not immediately classified as a tropical depression.[1]

Over the next two days, however, the system became much more organized. Early on August 21, the National Hurricane Center had initiated advisories on Tropical Depression Eight-E.[2] After the existence of banding features was noted, the intensity was increased to 40 mph (65 km/h), indicating that the system had intensified into a tropical storm, which was named Fausto by the National Hurricane Center (NHC).[3] Although no further strengthening initially occurred, Fausto began to intensify after a burst in convection early on August 22.[4] Rapid deepening began to occur thereafter, and the NHC noted that Fausto exhibited a classic-type banding feature and also noted that the outflow was increasing. The large size and widespread convection closely resembled a system that would become a major hurricane, Category 3 or higher on the Saffir–Simpson hurricane scale.[5] The associated banding features began to wrap completely around the system, and evidence of a developing eye was seen via weather satellite. Simultaneously, satellite estimates made via the Dvorak technique indicated that intensity of Fausto was 75 mph (120 km/h), and as a result, the NHC upgraded it to a hurricane.[6]

Hurricane Fausto weakening on August 25

Although the eye feature became obscured and banding features appeared to be dissipating six hours after becoming a hurricane, the NHC predicted rapid intensification.[7] As the eye became visible on satellite imagery early on August 23, winds increased to 100 mph (155 km/h), and Fausto became a Category 2 hurricane.[8] Although the convective cloud tops had warmed slightly late that day, wind speeds continued to increase, and intensity estimates made at the University of Wisconsin were as high as 145 mph (230 km/h), though the National Hurricane Center was in agreement with estimates from all three Dvorak Technique agencies (the Tropical Analysis and Forecast Branch (TAFB), the Satellite Analysis Branch (SAB), and the Air Force Weather Agency (AFWA)), which estimated winds at 115 mph (185 km/h). Based on this, Hurricane Fausto had intensified into a Category 3 on the Saffir–Simpson hurricane scale.[9]

The hurricane continued to intensify, although the NHC anticipated strengthening to cease, because the hurricane was expected to move into areas of colder sea surface temperatures.[10] During this period, the winds of the system increased and Fausto became a Category 4 hurricane.[11] Becoming a Category 4 hurricane, Fausto attained its peak intensity, with winds of 145 mph (230 km/h) and a minimum barometric pressure of 936 mbar (hPa; 27.64 inHg).[1] After attaining peak intensity, the NHC again noted that it was very likely that Fausto attained its peak intensity, as it was nearing a region of sea surface temperatures less than 78 °F (26 °C).[12]

Tropical Storm Fausto shortly after regeneration on September 2

Deep convection around the eyewall began to diminish, and Fausto then weakened to a Category 3 hurricane.[13] After quickly dropping in strength to a Category 2 hurricane, Fausto weakened at nearly the same rate as it had intensified.[14] Although Fausto held steady as a Category 2 hurricane for 18 hours, it then began to rapidly weaken back into a Category 1 hurricane,[15] then a tropical storm six hours later early on August 26. Upon weakening into a tropical storm, Forecaster Miles Lawrence at NHC noted "...there is no longer any deep convection associated with its circulation...", although Fausto still remained a tropical cyclone.[16] On August 27, the NHC issued its final advisory on Fausto, although not for dissipation, but rather that the storm crossed 140˚W, and had entered the area of responsibility for the Central Pacific Hurricane Center (CPHC).[17] While post-storm analysis from the CPHC indicated that Fausto was a tropical storm upon emerging into the CPHC's area of responsibility (AOR),[1][18] the storm was operationally classified as a tropical depression upon entering the AOR.[17] With no deep convection remaining, the CPHC downgraded Fausto into a tropical depression at 0000 UTC August 28. Fausto degenerated into a remnant low while located over 800 mi (1287 km) north of Hilo, Hawaii on August 28 at 1200 UTC.[18]

Although Fausto headed generally northwest while a tropical cyclone, it curved west-northwest after degenerating into a remnant low. Passing several hundred miles north of Hawaii, deep convection began to re-develop as the remnants of Fausto interacted with a tropical upper tropospheric trough. By 1800 UTC on August 28, the low had enough deep convection to be reclassified as a tropical depression while located roughly 635 mi (1020 km) north of Oahu. No further re-intensification occurred for almost 48 hours, and then Fausto became a tropical storm again at 1800 UTC September 1. This regeneration at high latitude was attributed to a temperature anomaly with waters 3.4 °F (2 °C) above normal and a favorable upper-level atmospheric pattern. Although sea surface temperature anomalies are usually attributed to the development of an El Niño, the El Niño had no effect with atmospheric conditions.[19] A mid-latitude cyclone approached Tropical Storm Fausto and caused the system to accelerate northward. The mid-latitude cyclone eventually absorbed Fausto, and the combined system reached the Aleutian Islands of Alaska shortly thereafter.[18]

Hurricane Fausto's regeneration north of Hawaii was unusual but not unprecedented. The other time this happened since 1966 was in the 1975 season. That time, another TUTT absorbed the remnant of Hurricane Ilsa, which led to the formation of an unnamed hurricane at high latitude. Other tropical cyclones have strengthened north of Hawaii, but the actual formation of one is rare.[18]

Fausto did not have any effect on land, and only one ship named Jo Lonn reported minimal gales on August 24, and again the next day. No reports of damage or casualties were attributed to Fausto.[1] The mid-latitude cyclone that absorbed Fausto passed over the Aleutian Islands.[19] Impact from the remnants of Fausto in the Aleutian Islands or mainland Alaska is unknown.

• Other tropical cyclones named Fausto
• List of Category 4 Pacific hurricanes