Revision as of 23:22, 30 May 2006 editVerrai (talk | contribs)Administrators8,748 editsm →Impact: Rearrange words← Previous edit | Latest revision as of 18:24, 23 December 2024 edit undoZzzs (talk | contribs)Extended confirmed users6,377 edits →Impact: better image | ||
(524 intermediate revisions by more than 100 users not shown) | |||
Line 1: | Line 1: | ||
{{Short description|Category 5 Pacific hurricane and typhoon}} | |||
{{dablink|This article is about the Pacific hurricane/typhoon of 1994; for other storms of the same name, see ].}} | |||
{{Featured article}} | |||
{{infobox hurricane | name=Hurricane John | |||
{{Use mdy dates|date=December 2021}} | |||
| category=cat5 | |||
{{Infobox weather event | |||
| type=hurricane | |||
| |
| name = Hurricane John | ||
| image |
| image = John 1994-08-23 0200Z.png | ||
| caption = John near peak intensity to the south of Hawaii on August 23 | |||
| formed=], ] | |||
| |
| formed = August 11, 1994 | ||
| extratropical = September 10, 1994 | |||
| highest winds=175 ] (280 km/h) sustained | |||
| dissipated = September 13, 1994 | |||
| lowest pressure=≤929 ] (]) <!-- Pressure taken before peak strength --> | |||
| duration = {{Age in months, weeks and days|year1=1994|month1=08|day1=11|year2=1994|month2=09|day2=10}} | |||
| total damages=$15 million (1994 USD)<br> $19 million (2005 USD) | |||
}}{{Infobox weather event/NWS | |||
| total fatalities=0 | |||
| winds = 150 | |||
| areas affected=], ] | |||
| pressure = 929 | |||
| hurricane season=]<br>] | |||
}}{{Infobox weather event/Effects | |||
| year = 1994 | |||
| fatalities = None | |||
| damage = 15000000 | |||
| areas = ], ], ], ] | |||
| refs = | |||
}}{{Infobox weather event/Footer | |||
| season = ]''' and '''] seasons | |||
}} | }} | ||
'''Hurricane John''', also known as '''Typhoon John''', was the farthest-traveling ] ever observed worldwide. It was also the longest-lasting tropical cyclone on record globally at the time, until it was surpassed by ] in 2023.<ref name=wmopr /> John formed during the ], which had above-average activity due to the ] of 1994–1995,<ref>{{cite web|url=http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ensoyears.shtml|title=Cold and Warm Episodes by Season|date=August 4, 2014|access-date=August 11, 2014}}</ref> and peaked as a Category 5 hurricane on the ], the highest categorization for hurricanes. | |||
Over the course of its existence, John followed a {{convert|13,180|km|mi|abbr=on|round=5}} path from the eastern Pacific to the western Pacific and back to the central Pacific, lasting 31 days in total.<ref name="report1">{{cite web | author=Lawrence, Miles| year=1995| title=Hurricane John Preliminary Report (page 1) | publisher=] | url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994-prelim/john/prelim01.gif | access-date=May 22, 2006}}</ref><ref name=noaafaq2>{{cite web|author=Dorst, Neal |year=2004 |title=What is the farthest a tropical cyclone has traveled? |publisher=] |work=NOAA Tropical cyclone FAQ |url=http://www.aoml.noaa.gov/hrd/tcfaq/E7.html |access-date=May 22, 2006 |url-status=dead |archive-url=https://web.archive.org/web/20090506175506/http://www.aoml.noaa.gov/hrd/tcfaq/E7.html |archive-date=May 6, 2009 }}</ref><ref>{{cite web|url=https://wmo.asu.edu/content/tropical-cyclone-longest-distance-traveled-tropical-cyclone|title=Tropical Cyclone: Longest Distance Traveled by Tropical Cyclone|publisher=]|access-date=9 March 2023}}</ref> Because it existed in both the eastern and western Pacific, John was one of a small number of tropical cyclones to be designated as both a hurricane and a typhoon. Despite lasting for a full month, John barely affected land at all, bringing only minimal effects to the ] and the United States ] on ]. Its remnants later affected ]. | |||
'''Hurricane John''' (also '''Typhoon John''') formed during the ] and became both the longest-lasting and second-farthest-traveling ] ever observed. John formed during the strong ] of 1991 to 1994 and peaked as a Category 5 hurricane on the ], the highest categorization for hurricanes. | |||
== Meteorological history == | |||
Over the course of its existence, it followed an 8,000 ] (13,000 ]) path from the eastern Pacific to the western Pacific and back to the central Pacific, lasting 31 days total.<ref name="report1"> | |||
{{Storm path|John 1994 path.png|colors=new}} | |||
{{cite web | author=Lawrence, Miles| year=1995| title=Hurricane John Preliminary Report (page 1) | publisher=] | url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994-prelim/john/prelim01.gif | accessdate=2006-05-22}}</ref> Because it existed in both the eastern and western Pacific, John was one of a small number of tropical cyclones to be designated as both a hurricane and a typhoon. Despite lasting for a full month, John barely affected land at all, bringing only minimal effects to the ] and a ] ] on ]. | |||
The origins of Hurricane John were thought by the United States ] (NHC) to be from a ] that moved off the coast of Africa on July 25, 1994.<ref name="John NHC TCR">{{cite report|author=Lawrence, Miles B |date=January 3, 1995 |publisher=United States National Hurricane Center |url-status=live |access-date=August 11, 2014 |title=Preliminary Report: Hurricane John: August 11 – September 10, 1994 |url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994-prelim/john/prelim01.gif |format=gif |page=1 |archive-url=https://web.archive.org/web/20131029204352/http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994-prelim/john/prelim01.gif |archive-date=October 29, 2013 }}</ref><ref name="MWR">{{cite journal|author=Mayfield, Britt Max|author2=Pasch, Richard J|year=1996|journal=Monthly Weather Review|volume=124|title=Eastern North Pacific Hurricane Season of 1994|issue=7|pages=1585–1586|publisher=American Meteorological Society|doi=10.1175/1520-0493(1996)124<1579:ENPHSO>2.0.CO;2|bibcode = 1996MWRv..124.1579P |doi-access=free}}</ref> The wave subsequently moved across the Atlantic Ocean and Caribbean without distinction, before it crossed Central America and moved into the Eastern Pacific Ocean on or around August 8.<ref name="John NHC TCR"/><ref name="MWR"/> Upon entering the Eastern Pacific the wave gradually developed, before the NHC initiated advisories on the system and designated it as Tropical Depression Ten-E on August 11.<ref name="John Dis 1">{{cite report|author=Lawrence, Miles B |date=August 11, 1994 |publisher=United States National Hurricane Center |url-status=live |access-date=August 11, 2014 |title=Tropical Depression Ten-E Discussion Number 1: August 11, 1994 09z |url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994/john/tropdisc/nep1094.001 |archive-url=https://web.archive.org/web/20140812214758/http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994/john/tropdisc/nep1094.001 |archive-date=August 12, 2014 }}</ref> The system was at this time moving westwards and located around {{convert|345|mi|km|round=5}} to the south-southeast of ], Mexico.<ref name="John NHC TCR"/><ref name="MWR"/> Quickly developing banding features and well-defined outflow, it was upgraded to a tropical storm and named ''John'' later that day.<ref name="report1" /> | |||
A strong ridge of high pressure over the northeastern Pacific Ocean forced John westward, where upper level ] kept John a tropical storm. Intensity fluctuated considerably, however, as shear levels varied. More than once, shear cleared away most of the clouds above John and nearly caused it to weaken to a tropical depression.<ref name="report1" /> However, after eight days of slow westward movement across the Pacific Ocean, shear lessened greatly on August 19, and John intensified significantly and was designated as a hurricane at 17:00 ]<!--PDT is UTC -7.-->. During an eighteen-hour period between August 19 and 20, John further strengthened from a weak Category 1 hurricane to a Category 3 major hurricane. Around 11:00 PDT on August 20, John crossed into the central Pacific, the first of three basin crosses John would make.<ref name="report1" /> | |||
==Storm history== | |||
{{storm path|John 1994 track.png}} | |||
The ]' ] (NHC) later identified the precursor to Hurricane John as a ] that moved off the coast of ] on ], ].<ref name="report1" /> The environment in the ] was hostile to tropical development, so the wave continued without developing until reaching the Eastern Pacific on ]. It slowly organized, and on ] was recognized as Tropical Depression Ten-E 300 ]s south-southeast of ].<ref name="report1" /> Conditions were not ideal for development, but it quickly developed banding features and well-defined outflow, and was upgraded to a tropical storm and named Tropical Storm John later that day.<ref name="report1" /> | |||
After entering the central Pacific, John left the area monitored by the NHC and was instead monitored by the ] (CPHC). As the storm moved slowly westward, Hurricane John continued to strengthen considerably in an increasingly favorable environment well south of the ]; on August 22, John was designated a Category 5 hurricane on the ] (the highest classification for hurricanes) and later that day (by ]) reached its peak intensity, with 1-minute sustained winds of {{convert|175|mph|km/h|round=5}} and a minimum central ] of {{convert|929|mbar|inHg}}.<ref name="report2">{{cite web | author=Lawrence, Miles| year=1995| title=Hurricane John Preliminary Report (page 2) | publisher=] | url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994-prelim/john/prelim02.gif | access-date=May 23, 2006}}</ref> Also, on August 22 (by Hawaii Standard Time), John made its closest approach to the Hawaiian Islands, {{convert|345|mi|km}} to the south. John had threatened to turn north and affect the islands days before, but the ridge of high pressure that typically shields the islands from hurricanes kept John on its southerly path. Nonetheless, heavy rains and wind from the outer bands of John affected the islands.<ref name="report2" /> | |||
A strong ridge of high pressure over the Northeastern Pacific Ocean forced John westward, where upper level ] kept John a tropical storm. Intensity fluctuated considerably, however, as shear levels varied. More than once, shear cleared away most of the clouds above John and nearly caused it to weaken to a tropical depression.<ref name="report1" /> However, after eight days of slow westward movement across the ], shear lessened greatly on ], and John intensified significantly and was designated as a hurricane at 1700 ]<!--PDT is UTC -7.-->. During an eighteen-hour period between ] and ], John further strengthened from a weak Category 1 hurricane to a major Category 3 hurricane. Around 1100 PDT on ], it crossed into the central Pacific, the first of three basin crosses John would make.<ref name="report1" /> | |||
{{Category 5 Pacific hurricanes|align=left}} | |||
After entering the central Pacific, John left the area monitored by the NHC and was instead monitored by the ] (CPHC). As it moved slowly westward, Hurricane John continued to strengthen considerably in an increasingly favorable environment well south of the ]; on ] John was designated a Category 5 hurricane on the ] (the highest classification for hurricanes) and later that day (by ]) reached its peak winds of 175 ] (280 km/h).<ref name="report2"> | |||
{{cite web | author=Lawrence, Miles| year=1995| title=Hurricane John Preliminary Report (page 2) | publisher=] | url=http://www.nhc.noaa.gov/archive/storm_wallets/epacific/ep1994-prelim/john/prelim02.gif | accessdate=2006-05-23}}</ref> Also on ] (by ]), John made its closest approach to the ], 345 miles (500 km) to the south. John had posed a threat to the islands days before, but the ridge of high pressure that typically shields the islands from hurricanes kept John on its southerly path. Nonetheless, heavy rains and wind from the outer bands of John impacted the islands.<ref name="report2" /> | |||
With the Hawaiian |
With the Hawaiian Islands behind it, John began a slow turn to the north, taking near-direct aim at ], a small group of islands populated only by a United States military base. The storm slowly weakened from its peak as a Category 5 hurricane in the face of increasing shear, dropping down to a Category 1 hurricane with maximum winds of 90 mph (150 km/h). On August 25 local time, John made its closest approach to the Johnston Atoll only {{convert|15|mi|km}} to the north. On Johnston Atoll, sustained winds were reported up to {{convert|60|mph|km/h}}, the equivalent of a strong tropical storm, and gusts up to {{convert|75|mph|km/h}} were recorded.<ref name="Centralreport">{{cite web | author=Central Pacific Hurricane Center| year=2004| title=Hurricane John Preliminary Report | publisher=] | url={{NHC TCR url|id=CP1994_Seasonal_TCR}}| access-date=May 24, 2006}} (Note that this report does not reflect changes made in post-season analysis.)</ref> | ||
] | |||
Clearing Johnston Atoll, John turned to the northwest and began strengthening again as shear decreased. On ] local time, John reached a secondary peak strength of 135 miles per hour (210 km/h), and shortly thereafter it crossed the ] at approximately 22° ] and came under the surveillance of the ] branch of the ] (JTWC). By crossing into the western Pacific, John also became a typhoon and was referred to as Typhoon John during its time in the western Pacific.<ref name="Centralreport" /> Immediately after crossing the Date Line, John again weakened and its forward motion stalled. By ], John had weakened to a tropical storm and was nearly motionless just west of the Date Line. There, John lingered for six days while performing a multi-day ] loop. On ], a trough moved into the area and quickly moved John to the northwest. John crossed the Date Line again on ] and reentered the central Pacific, becoming only the third tropical cyclone to enter the central Pacific from the western Pacific (Tropical Storms Carmen and Skip in 1980 and 1985, respectively, had done so previously).<ref name="Centralreport" /> | |||
Clearing Johnston Atoll, John turned to the northwest and began strengthening again as shear decreased. On August 27 local time, John reached a secondary peak strength of 130 mph (215 km/h), and shortly thereafter it crossed the ] at approximately 22° ] and came under the surveillance of the ] branch of the ] (JTWC). By crossing into the western Pacific, John also became a typhoon and was referred to as Typhoon John during its time in the western Pacific.<ref name="Centralreport" /> Immediately after crossing the Date Line, John again weakened and its forward motion stalled. By September 1, John had weakened to a tropical storm and was nearly motionless just west of the Date Line. There, John lingered for six days while performing a multi-day ] loop. On September 7, a trough moved into the area and quickly moved John to the northeast. John crossed the Date Line again on September 8 and reentered the central Pacific.<ref name="Centralreport" /> | |||
After reentering the central Pacific, John briefly reached a tertiary peak strength of 90 miles per hour (145 km/h), a strong Category 1 hurricane, well to the north of ]. However, the trough was rapidly pulling apart John's structure, and the cold waters of the northern central Pacific were not conducive to a tropical cyclone. On ], the 120th advisory was released on the system, finally declaring John to have become extratropical approximately one thousand miles south of ].<ref name="Centralreport" /> | |||
After reentering the central Pacific, John briefly reached a tertiary peak strength of 90 mph (150 km/h), a strong Category 1 hurricane, well to the north of ]. However, the trough was rapidly pulling apart John's structure, and the cold waters of the northern central Pacific were not conducive to a tropical cyclone. On September 10, the 120th advisory was released on the system, finally declaring John to have become ] approximately {{convert|1,000|mi|km}} south of ].<ref name="Centralreport" /> | |||
== Records == | |||
Its 31-day existence made John the longest-lasting tropical cyclone recorded in both the ] and worldwide, surpassing both ]'s previous record in the Pacific of 24 days in the ] and ]'s previous world record of 28 days in the ].<ref name=noaafaq1>{{cite web | author=Dorst, Neal| year=2004| title=Which tropical cyclone lasted the longest? | publisher =] | work=NOAA Tropical cyclone FAQ | url=http://www.aoml.noaa.gov/hrd/tcfaq/E6.html | accessdate=2006-05-22}}</ref> In addition, despite its slow movement throughout much of its path, John was the second-farthest-traveling tropical cyclone worldwide and the farthest-traveling in the eastern Pacific, out-distancing previous record holder ]. John's travel distance of 8,000 miles (13,000 km) was farther than that of any tropical cyclone save ] of the ].<ref name=noaafaq2> | |||
{{cite web | author=Dorst, Neal| year=2004| title=What is the farthest a tropical cyclone has traveled? | publisher =] | work=NOAA Tropical cyclone FAQ | url=http://www.aoml.noaa.gov/hrd/tcfaq/E7.html | accessdate=2006-05-22}}</ref> | |||
=== Records === | |||
Pressure readings from John's peak are not consistently available as the CPHC did not monitor pressures at the time, but ] aircraft did measure a surface pressure of 929 ] (]), making John one of the most intense hurricanes recorded in the central Pacific; ] recorded a lower pressure in the central Pacific earlier in the 1994 season, but with lower wind speeds. (Intensity is measured by minimum central pressure, which correlates with but is not directly linked to wind speeds.) John was also only the third Category 5 hurricane recorded in the central Pacific (the first was ] in 1959 and the second, ] earlier in 1994), and possessed the highest recorded wind speed in a central Pacific hurricane, 175 miles per hour (280 km/h).<ref name="report2" /> | |||
] on August 28]] | |||
John's 31-day existence made it the longest-lasting tropical cyclone recorded in the Pacific Ocean, surpassing ]'s previous record of 24 days in the ], and the longest-lived globally on record, surpassing the ] duration of 28 days in the ].<ref name=noaafaq1>{{cite web|author=Dorst, Neal |year=2004 |title=Which tropical cyclone lasted the longest? |publisher=] |work=NOAA Tropical cyclone FAQ |url=http://www.aoml.noaa.gov/hrd/tcfaq/E6.html |access-date=May 22, 2006 |url-status=dead |archive-url=https://web.archive.org/web/20080924074803/http://www.aoml.noaa.gov/hrd/tcfaq/E6.html |archive-date=September 24, 2008 }}</ref> John's global record stood until 2023, when it was broken by ], which traversed the Indian Ocean in the Southern Hemisphere for 36 days.<ref name=wmopr>{{Cite web |date=2024-07-01 |title=Tropical Cyclone Freddy is the longest tropical cyclone on record at 36 days: WMO |url=https://wmo.int/news/media-centre/tropical-cyclone-freddy-longest-tropical-cyclone-record-36-days-wmo |access-date=2024-07-02 |website=World Meteorological Organization |language=en}}</ref> | |||
Additionally, despite its slow movement throughout much of its path, John was also the farthest-traveling tropical cyclone in both the Pacific Ocean and globally, with a distance traveled of {{convert|13,180|km|mi|abbr=on|round=5}}, ahead of 2023's Cyclone Freddy, with a distance traveled of 12,785 km (7,945 mi), or about 33% of the Earth's circumference,<ref name=wmopr /> outdistancing the previous record of {{convert|7,600|km|mi}} set by ] in the ].<ref name="noaafaq2" /> In addition, John was the first tropical cyclone on record to become a hurricane in the Eastern Pacific (east of ]), traverse the entire Central Pacific at hurricane strength, and then cross into the Western Pacific at the International Date Line (]) and become a typhoon, a feat matched only by ] in 2023.<ref>{{cite news|title=Dora to become 2nd hurricane-strength storm to be in Eastern, Central and Western Pacific Ocean|last1=Barker|first1=Aaron|last2=Oberholtz|first2=Chris|date=August 11, 2023|url=https://www.foxweather.com/weather-news/hurricane-dora-wildfires-high-surf-hawaii|publisher=FOX Weather|access-date=August 11, 2023}}</ref> | |||
Pressure readings from John's peak are not consistently available as the CPHC did not monitor pressures at the time, but ] aircraft did measure a surface pressure of 929 ] (]), making John one of the most intense hurricanes recorded in the central Pacific; both hurricanes ] and ] of 1994, as well as hurricanes ] of 2006 and ] and ] of 2018 all recorded lower pressures in the central Pacific. However, all five had lower wind speeds than John. (Intensity is measured by minimum central pressure, which correlates with but is not directly linked to wind speeds.) John was also only the fourth Category 5 hurricane recorded in the central Pacific (the first was ] in ], the second was Hurricane Emilia and the third one was Hurricane Gilma, both earlier in 1994). John also possessed the highest recorded wind speed in a central Pacific hurricane, {{convert|175|mph|km/h|abbr=on|round=5}}, a record shared with the aforementioned Patsy of 1959.<ref name="report2" /> Since 1994, only three Category 5 hurricanes, ] in 2006, and hurricanes ] and ] in 2018 have formed in or entered into the Central Pacific. Despite this however, John's pressure record is incomplete; the {{convert|929|mbar|inHg|sigfig=4}} reading was only measured when the winds were {{convert|160|mph|km/h|round=10|abbr=on}}; there is no pressure estimate for when it had winds of {{convert|175|mph|km/h|round=5|abbr=on}}, so it could have been more intense than Emilia, Gilma, Ioke, Lane, or Walaka.{{EPAC hurricane best track}} | |||
== Impact == | == Impact == | ||
John impacted both the ] and ], but only lightly. While John passed over 345 miles (550 km) to the south of ], the islands did experience strengthened trade winds and rough surf along the southeast- and south-facing shores, and, as John moved westward, on west-facing shores as well. <ref name="Centralreport" /> The waves, ranging from 6 to 10 feet in height, flooded beach parks in ]. <ref name="ncdc">{{cite web|author=National Climatic Data Center|year=1994|title=Event Report for Hawaii|accessdate=2006-05-28|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~203411}}</ref> Additionally, heavy rains on the ] caused minor, localized flooding and some short-term road closings. No deaths, injuries or significant damages were reported in Hawaii.<ref name="Centralreport" /> | |||
] on August 23]] | |||
Although John passed within 15 miles (25 km) of ], it had weakened greatly to a Category 2 system by closest approach. Additionally, in the ], the strongest winds and heaviest rain lie to the north of a tropical cyclone, so the atoll, which lay to the south of the storm's path, was spared the brunt of the storm. Nonetheless, the 1,100-man personnel for the ] military base on ] had been evacuated to ] as a precaution while John approached. Damages to structures were considerable, but the size of the island and relative functionality of the base led to low damages; damages were estimated at close to $15 million (1994 ]).<ref name="Centralreport" /> | |||
John affected both the ] and ], but only lightly. While John passed over {{convert|345|mi|km}} to the south of Hawaii, the islands did experience strengthened trade winds and rough surf along the southeast- and south-facing shores, and, while moving westward, on west-facing shores as well.<ref name="Centralreport" /> The waves, ranging from {{convert|6|to|10|ft|m|abbr=on}} in height, flooded beach parks in ].<ref name="ncdc">{{cite web|author=National Climatic Data Center |year=1994 |title=Event Report for Hawaii |access-date=May 28, 2006 |url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~197724 |archive-url=https://web.archive.org/web/20120112022335/http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~197724 |archive-date=January 12, 2012 |url-status=dead }}</ref> Additionally, heavy rains on the ] caused minor, localized flooding and some short-term road closures. No deaths, injuries or significant damages were reported in Hawai{{okina}}i.<ref name="Centralreport" /> | |||
Although John passed within {{convert|25|km|mi|abbr=on}} of ], it had weakened to a ] by closest approach.<ref name="Centralreport" /> Prior to the storm's arrival, waves between {{convert|20|and|30|ft|m|abbr=on}} were reported on the island.<ref>{{cite news|work=Gainesville Sun|author=Staff Writer|date=August 26, 1994|access-date=December 12, 2009|title=Island braces for Hurricane John|url=https://news.google.com/newspapers?id=VTcTAAAAIBAJ&sjid=hOoDAAAAIBAJ&pg=4899,7188940&dq=hurricane+john&hl=en|page=4}}</ref> Additionally, in the Northern Hemisphere, the strongest winds and heaviest rain lie to the north of a tropical cyclone, so the atoll, which lay to the south of the storm's path, was spared the brunt of the storm. Nonetheless, the 1,100-man personnel for the United States military base on Johnston Atoll had been evacuated to ] as a precaution while John approached. Damage to structures was considerable, but the size of the island and relative functionality of the base led to low damage; monetary losses were estimated at close to $15 million (1994 US$).<ref name="Centralreport" /> | |||
In Alaska, the remnants of John moved through the ], producing a wind gust of {{convert|46|mph|km/h|abbr=on}} in ]. The storm brought a plume of warm air, and two stations recorded a high temperature of {{convert|66|°F|°C|abbr=on}}.<ref>{{cite journal|volume=36 |number=9 |journal=Storm Data|title=A Composite of Outstanding Storms |date=September 1994 |access-date=April 22, 2012 |archive-url=https://web.archive.org/web/20140814052307/http://www1.ncdc.noaa.gov/pub/orders/IPS/IPS-53E370C8-CDF6-4B89-9E1F-6A310071F216.pdf |archive-date=August 14, 2014 |url=http://www1.ncdc.noaa.gov/pub/orders/IPS/IPS-53E370C8-CDF6-4B89-9E1F-6A310071F216.pdf |page=60 |url-status=dead }}</ref> | |||
==See also== | |||
Despite John's record-setting endurance, the name John was not retired following the storm due to low damages. It was used again in the ] and is on the list for the ]. | |||
{{Portal|Tropical cyclones}} | |||
* ] | |||
* ] – The longest-lived tropical cyclone recorded in the Atlantic Ocean | |||
* ] (2000) – The second longest-lived tropical cyclone recorded in the Indian Ocean | |||
* ] (2023) – The longest-lived tropical cyclone recorded worldwide | |||
Other powerful hurricanes that crossed the ]: | |||
* ] | |||
* ] | |||
* ] | |||
* ] | |||
* ] | |||
== |
==References== | ||
{{ |
{{Reflist|30em}} | ||
*] | |||
*] | |||
== |
==External links== | ||
{{Commons category|Hurricane John (1994)}} | |||
<div style=font-size:90%> | |||
* | |||
<references /> | |||
* | |||
</div> | |||
* {{Webarchive|url=https://web.archive.org/web/20130221092023/http://www.usno.navy.mil/NOOC/nmfc-ph/RSS/jtwc/atcr/1994atcr.pdf |date=February 21, 2013 }} | |||
{{Category 5 Pacific hurricanes}} | |||
== External links == | |||
{{1994 Pacific hurricane season buttons}} | |||
* | |||
* | |||
{{DEFAULTSORT:John (1994)}} | |||
] | ] | ||
] | ] | ||
] | ] | ||
] | ] | ||
] | ] | ||
] | |||
] | |||
] | |||
] |
Latest revision as of 18:24, 23 December 2024
Category 5 Pacific hurricane and typhoon
John near peak intensity to the south of Hawaii on August 23 | |
Meteorological history | |
---|---|
Formed | August 11, 1994 |
Extratropical | September 10, 1994 |
Dissipated | September 13, 1994 |
Duration | 4 weeks and 2 days |
Category 5 major hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 175 mph (280 km/h) |
Lowest pressure | 929 mbar (hPa); 27.43 inHg |
Overall effects | |
Fatalities | None |
Damage | $15 million (1994 USD) |
Areas affected | Hawaiian Islands, Johnston Atoll, Aleutian Islands, Alaska |
IBTrACS | |
Part of the 1994 Pacific hurricane and typhoon seasons |
Hurricane John, also known as Typhoon John, was the farthest-traveling tropical cyclone ever observed worldwide. It was also the longest-lasting tropical cyclone on record globally at the time, until it was surpassed by Cyclone Freddy in 2023. John formed during the 1994 Pacific hurricane season, which had above-average activity due to the El Niño of 1994–1995, and peaked as a Category 5 hurricane on the Saffir–Simpson scale, the highest categorization for hurricanes.
Over the course of its existence, John followed a 13,180 km (8,190 mi) path from the eastern Pacific to the western Pacific and back to the central Pacific, lasting 31 days in total. Because it existed in both the eastern and western Pacific, John was one of a small number of tropical cyclones to be designated as both a hurricane and a typhoon. Despite lasting for a full month, John barely affected land at all, bringing only minimal effects to the Hawaiian Islands and the United States military base on Johnston Atoll. Its remnants later affected Alaska.
Meteorological history
The origins of Hurricane John were thought by the United States National Hurricane Center (NHC) to be from a tropical wave that moved off the coast of Africa on July 25, 1994. The wave subsequently moved across the Atlantic Ocean and Caribbean without distinction, before it crossed Central America and moved into the Eastern Pacific Ocean on or around August 8. Upon entering the Eastern Pacific the wave gradually developed, before the NHC initiated advisories on the system and designated it as Tropical Depression Ten-E on August 11. The system was at this time moving westwards and located around 345 miles (555 km) to the south-southeast of Acapulco, Mexico. Quickly developing banding features and well-defined outflow, it was upgraded to a tropical storm and named John later that day.
A strong ridge of high pressure over the northeastern Pacific Ocean forced John westward, where upper level wind shear kept John a tropical storm. Intensity fluctuated considerably, however, as shear levels varied. More than once, shear cleared away most of the clouds above John and nearly caused it to weaken to a tropical depression. However, after eight days of slow westward movement across the Pacific Ocean, shear lessened greatly on August 19, and John intensified significantly and was designated as a hurricane at 17:00 PDT. During an eighteen-hour period between August 19 and 20, John further strengthened from a weak Category 1 hurricane to a Category 3 major hurricane. Around 11:00 PDT on August 20, John crossed into the central Pacific, the first of three basin crosses John would make.
After entering the central Pacific, John left the area monitored by the NHC and was instead monitored by the Central Pacific Hurricane Center (CPHC). As the storm moved slowly westward, Hurricane John continued to strengthen considerably in an increasingly favorable environment well south of the Hawaiian Islands; on August 22, John was designated a Category 5 hurricane on the Saffir–Simpson hurricane scale (the highest classification for hurricanes) and later that day (by Hawaii Standard Time) reached its peak intensity, with 1-minute sustained winds of 175 miles per hour (280 km/h) and a minimum central pressure of 929 millibars (27.4 inHg). Also, on August 22 (by Hawaii Standard Time), John made its closest approach to the Hawaiian Islands, 345 miles (555 km) to the south. John had threatened to turn north and affect the islands days before, but the ridge of high pressure that typically shields the islands from hurricanes kept John on its southerly path. Nonetheless, heavy rains and wind from the outer bands of John affected the islands.
With the Hawaiian Islands behind it, John began a slow turn to the north, taking near-direct aim at Johnston Atoll, a small group of islands populated only by a United States military base. The storm slowly weakened from its peak as a Category 5 hurricane in the face of increasing shear, dropping down to a Category 1 hurricane with maximum winds of 90 mph (150 km/h). On August 25 local time, John made its closest approach to the Johnston Atoll only 15 miles (24 km) to the north. On Johnston Atoll, sustained winds were reported up to 60 miles per hour (97 km/h), the equivalent of a strong tropical storm, and gusts up to 75 miles per hour (121 km/h) were recorded.
Clearing Johnston Atoll, John turned to the northwest and began strengthening again as shear decreased. On August 27 local time, John reached a secondary peak strength of 130 mph (215 km/h), and shortly thereafter it crossed the International Date Line at approximately 22° N and came under the surveillance of the Guam branch of the Joint Typhoon Warning Center (JTWC). By crossing into the western Pacific, John also became a typhoon and was referred to as Typhoon John during its time in the western Pacific. Immediately after crossing the Date Line, John again weakened and its forward motion stalled. By September 1, John had weakened to a tropical storm and was nearly motionless just west of the Date Line. There, John lingered for six days while performing a multi-day counterclockwise loop. On September 7, a trough moved into the area and quickly moved John to the northeast. John crossed the Date Line again on September 8 and reentered the central Pacific.
After reentering the central Pacific, John briefly reached a tertiary peak strength of 90 mph (150 km/h), a strong Category 1 hurricane, well to the north of Midway Island. However, the trough was rapidly pulling apart John's structure, and the cold waters of the northern central Pacific were not conducive to a tropical cyclone. On September 10, the 120th advisory was released on the system, finally declaring John to have become extratropical approximately 1,000 miles (1,600 km) south of Unalaska Island.
Records
John's 31-day existence made it the longest-lasting tropical cyclone recorded in the Pacific Ocean, surpassing Hurricane Tina's previous record of 24 days in the 1992 season, and the longest-lived globally on record, surpassing the San Ciriaco hurricane's duration of 28 days in the 1899 Atlantic season. John's global record stood until 2023, when it was broken by Cyclone Freddy, which traversed the Indian Ocean in the Southern Hemisphere for 36 days.
Additionally, despite its slow movement throughout much of its path, John was also the farthest-traveling tropical cyclone in both the Pacific Ocean and globally, with a distance traveled of 13,180 km (8,190 mi), ahead of 2023's Cyclone Freddy, with a distance traveled of 12,785 km (7,945 mi), or about 33% of the Earth's circumference, outdistancing the previous record of 7,600 kilometres (4,700 mi) set by Hurricane Fico in the 1978 season. In addition, John was the first tropical cyclone on record to become a hurricane in the Eastern Pacific (east of 140°W), traverse the entire Central Pacific at hurricane strength, and then cross into the Western Pacific at the International Date Line (180°W) and become a typhoon, a feat matched only by Hurricane Dora in 2023.
Pressure readings from John's peak are not consistently available as the CPHC did not monitor pressures at the time, but Air Force Reserve aircraft did measure a surface pressure of 929 mbar (hPa), making John one of the most intense hurricanes recorded in the central Pacific; both hurricanes Emilia and Gilma of 1994, as well as hurricanes Ioke of 2006 and Lane and Walaka of 2018 all recorded lower pressures in the central Pacific. However, all five had lower wind speeds than John. (Intensity is measured by minimum central pressure, which correlates with but is not directly linked to wind speeds.) John was also only the fourth Category 5 hurricane recorded in the central Pacific (the first was Hurricane Patsy in 1959, the second was Hurricane Emilia and the third one was Hurricane Gilma, both earlier in 1994). John also possessed the highest recorded wind speed in a central Pacific hurricane, 175 mph (280 km/h), a record shared with the aforementioned Patsy of 1959. Since 1994, only three Category 5 hurricanes, Ioke in 2006, and hurricanes Lane and Walaka in 2018 have formed in or entered into the Central Pacific. Despite this however, John's pressure record is incomplete; the 929 millibars (27.43 inHg) reading was only measured when the winds were 160 mph (260 km/h); there is no pressure estimate for when it had winds of 175 mph (280 km/h), so it could have been more intense than Emilia, Gilma, Ioke, Lane, or Walaka.
Impact
John affected both the Hawaiian Islands and Johnston Atoll, but only lightly. While John passed over 345 miles (555 km) to the south of Hawaii, the islands did experience strengthened trade winds and rough surf along the southeast- and south-facing shores, and, while moving westward, on west-facing shores as well. The waves, ranging from 6 to 10 ft (1.8 to 3.0 m) in height, flooded beach parks in Kailua-Kona. Additionally, heavy rains on the Big Island of Hawaiʻi caused minor, localized flooding and some short-term road closures. No deaths, injuries or significant damages were reported in Hawaiʻi.
Although John passed within 25 km (16 mi) of Johnston Atoll, it had weakened to a Category 1 hurricane by closest approach. Prior to the storm's arrival, waves between 20 and 30 ft (6.1 and 9.1 m) were reported on the island. Additionally, in the Northern Hemisphere, the strongest winds and heaviest rain lie to the north of a tropical cyclone, so the atoll, which lay to the south of the storm's path, was spared the brunt of the storm. Nonetheless, the 1,100-man personnel for the United States military base on Johnston Atoll had been evacuated to Honolulu as a precaution while John approached. Damage to structures was considerable, but the size of the island and relative functionality of the base led to low damage; monetary losses were estimated at close to $15 million (1994 US$).
In Alaska, the remnants of John moved through the Aleutian Islands, producing a wind gust of 46 mph (74 km/h) in Unalaska. The storm brought a plume of warm air, and two stations recorded a high temperature of 66 °F (19 °C).
See also
- Other storms of the same name
- 1899 San Ciriaco hurricane – The longest-lived tropical cyclone recorded in the Atlantic Ocean
- Cyclone Leon–Eline (2000) – The second longest-lived tropical cyclone recorded in the Indian Ocean
- Cyclone Freddy (2023) – The longest-lived tropical cyclone recorded worldwide
Other powerful hurricanes that crossed the International Date Line:
- Hurricane Dora (1999)
- Hurricane Ioke (2006)
- Hurricane Genevieve (2014)
- Hurricane Hector (2018)
- Hurricane Dora (2023)
References
- ^ "Tropical Cyclone Freddy is the longest tropical cyclone on record at 36 days: WMO". World Meteorological Organization. July 1, 2024. Retrieved July 2, 2024.
- "Cold and Warm Episodes by Season". August 4, 2014. Retrieved August 11, 2014.
- ^ Lawrence, Miles (1995). "Hurricane John Preliminary Report (page 1)". NOAA. Retrieved May 22, 2006.
- ^ Dorst, Neal (2004). "What is the farthest a tropical cyclone has traveled?". NOAA Tropical cyclone FAQ. NOAA. Archived from the original on May 6, 2009. Retrieved May 22, 2006.
- "Tropical Cyclone: Longest Distance Traveled by Tropical Cyclone". World Meteorological Organization. Retrieved March 9, 2023.
- ^ Lawrence, Miles B (January 3, 1995). Preliminary Report: Hurricane John: August 11 – September 10, 1994 (gif) (Report). United States National Hurricane Center. p. 1. Archived from the original on October 29, 2013. Retrieved August 11, 2014.
- ^ Mayfield, Britt Max; Pasch, Richard J (1996). "Eastern North Pacific Hurricane Season of 1994". Monthly Weather Review. 124 (7). American Meteorological Society: 1585–1586. Bibcode:1996MWRv..124.1579P. doi:10.1175/1520-0493(1996)124<1579:ENPHSO>2.0.CO;2.
- Lawrence, Miles B (August 11, 1994). Tropical Depression Ten-E Discussion Number 1: August 11, 1994 09z (Report). United States National Hurricane Center. Archived from the original on August 12, 2014. Retrieved August 11, 2014.
- ^ Lawrence, Miles (1995). "Hurricane John Preliminary Report (page 2)". NOAA. Retrieved May 23, 2006.
- ^ Central Pacific Hurricane Center (2004). "Hurricane John Preliminary Report" (PDF). NOAA. Retrieved May 24, 2006. (Note that this report does not reflect changes made in post-season analysis.)
- Dorst, Neal (2004). "Which tropical cyclone lasted the longest?". NOAA Tropical cyclone FAQ. NOAA. Archived from the original on September 24, 2008. Retrieved May 22, 2006.
- Barker, Aaron; Oberholtz, Chris (August 11, 2023). "Dora to become 2nd hurricane-strength storm to be in Eastern, Central and Western Pacific Ocean". FOX Weather. Retrieved August 11, 2023.
- National Hurricane Center; Hurricane Research Division; Central Pacific Hurricane Center (April 26, 2024). "The Northeast and North Central Pacific hurricane database 1949–2023". United States National Oceanic and Atmospheric Administration's National Weather Service. Archived from the original on May 29, 2024. A guide on how to read the database is available here. This article incorporates text from this source, which is in the public domain.
- National Climatic Data Center (1994). "Event Report for Hawaii". Archived from the original on January 12, 2012. Retrieved May 28, 2006.
- Staff Writer (August 26, 1994). "Island braces for Hurricane John". Gainesville Sun. p. 4. Retrieved December 12, 2009.
- "A Composite of Outstanding Storms" (PDF). Storm Data. 36 (9): 60. September 1994. Archived from the original (PDF) on August 14, 2014. Retrieved April 22, 2012.
External links
- The National Hurricane Center's report on Hurricane John
- The Central Pacific Hurricane Center's report on Hurricane John
- The Joint Typhoon Warning Center's 1994 Annual Tropical Cyclone Report Archived February 21, 2013, at the Wayback Machine
Category 5 Pacific hurricanes | |
---|---|
1950s | |
1970s | |
1990s | |
2000s | |
2010s | |
2020s | |
Tropical cyclones of the 1994 Pacific hurricane season | ||
---|---|---|
TSAletta TSBud 2Carlotta TSDaniel 5Emilia TSFabio 5Gilma 1Li TSHector TDOne-C 1Ileana 5John TDTwelve-E 2Kristy 4Lane TSMele TSMiriam TSNorman 4Olivia TSPaul 2Rosa TSNona | ||