Question: Hurricane Dora was one of few tropical cyclones to track across all three north Pacific basins, after weakening to a tropical depression on August 22, the storm dissipated on August 23 while centered several hundred miles north of which coral atoll in the western Pacific Ocean in the northeastern area of the Micronesia subregion, 1,501 mi east of Guam, 2,298 mi west of Honolulu and 1,991 mi southeast of Tokyo?

Context articles: Wake Island
List of retired Philippine typhoon names
1949 Pacific typhoon season
1948 Pacific typhoon season
Hurricane Gil (1983)
2005 Pacific hurricane season
Hurricane Norman (1978)
Hurricane Genevieve (2014)
History of tropical cyclone naming
Hurricane Dora (1999)

Wake Island (also known as Wake Atoll) is a coral atoll in the western Pacific Ocean in the northeastern area of the Micronesia subregion, 1,501 mi east of Guam, 2,298 mi west of Honolulu and 1,991 mi southeast of Tokyo.
 The island is an unorganized, unincorporated territory of the United States Minor Outlying Islands that is also claimed by the Republic of the Marshall Islands.
 Wake Island is one of the most isolated islands in the world and the nearest inhabited island is Utirik Atoll in the Marshall Islands, 592 mi to the southeast.
Since 1963, there have been three agencies who have named tropical cyclones within the north western Pacific Ocean which has often resulted in a cyclone having two names.
 From 1945 to 2000 the US Navy's Joint Typhoon Warning Center assigned names to tropical cyclones before the Japan Meteorological Agency (JMA), took over the naming of tropical cyclones in 2000.
 Both agencies assigned names to tropical cyclones when they intensified into a tropical storm.
 Since 1963 the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) has assigned local names to a tropical cyclone should it move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N-25°N even if the cyclone has had an international name assigned to it.
 All three agencies that have assigned names to tropical cyclones within the Western Pacific have retired the names of significant tropical cyclones, with PAGASA retiring names if a cyclone has caused at least ₱ in damage and or have caused at least 300 deaths within the Philippines.
 Since 1963 the naming lists have been revised in 1979, 1985, 2001 and 2005 for various reasons including to help minimize confusion in the historical records and to remove the names that might have negative associations with real persons.
 Within this list all information with regards to intensity is taken from while the system was in the Philippine area of responsibility and is thus taken from PAGASA's archives, rather than the JTWC or JMA's archives.
The 1949 Pacific typhoon season is an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean.
 The season runs throughout 1949, though most tropical cyclones typically develop between May and October.
 The scope of this article is limited to the Pacific Ocean to the north of the equator between 100°E and 180th meridian.
 Within the northwestern Pacific Ocean, there are two separate agencies that assign names to tropical cyclones which can often result in a cyclone having two names.
 The Japan Meteorological Agency  will name a tropical cyclone should it be judged to have 10-minute sustained wind speeds of at least 65 km/h (40 mph) anywhere in the basin, whilst the Philippine Atmospheric, Geophysical and Astronomical Services Administration  assigns names to tropical cyclones which move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N–25°N regardless of whether or not a tropical cyclone has already been given a name by the JMA.
 Tropical depressions that are monitored by the United States' Joint Typhoon Warning Center  are given a number with a "W" suffix.
The 1948 Pacific typhoon season is an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean.
 The season runs throughout 1948, though most tropical cyclones typically develop between May and October.
 The scope of this article is limited to the Pacific Ocean to the north of the equator between 100°E and 180th meridian.
 Within the northwestern Pacific Ocean, there are two separate agencies that assign names to tropical cyclones which can often result in a cyclone having two names.
 The Japan Meteorological Agency  will name a tropical cyclone should it be judged to have 10-minute sustained wind speeds of at least 65 km/h (40 mph) anywhere in the basin, whilst the Philippine Atmospheric, Geophysical and Astronomical Services Administration  assigns names to tropical cyclones which move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N–25°N regardless of whether or not a tropical cyclone has already been given a name by the JMA.
 Tropical depressions that are monitored by the United States' Joint Typhoon Warning Center  are given a number with a "W" suffix.
Hurricane Gil was the first of several tropical cyclones to affect Hawaii during the 1983 Pacific hurricane season.
 Gil originated from a tropical depression that developed near Clipperton Island on July 23.
 Steadily intensifying, it attained tropical storm status six hours later and was upgraded to a hurricane on July 26.
 After attaining peak intensity on July 27, Gil encountered cooler sea surface temperatures and began to weaken.
 Moving west-northwest, the weakening system also accelerated and on July 31, was downgraded to a tropical depression.
 However, Gil began to re-intensify on August 1, becoming a tropical storm again later that day.
 Initially expected to veer north of Hawaii, it continued west-northwest and began to approach the Hawaiian group on August 3.
 While passing through the island group, Gil reached its secondary peak intensity.
 Subsequently, Gil began to weaken once again as it threatened the Northwestern Hawaiian Islands.
 After passing through the islands, Gil was downgraded to a tropical depression on August 5.
 Several hours later, the storm dissipated.
 The remnants of the storm moved into the West Pacific late on August 6 and were last noted the next morning while passing south of Midway Island.
The 2005 Pacific hurricane season continued the trend of generally below-average activity that began a decade prior.
 The season officially began on May 15 in the eastern Pacific, and on June 1 in the central Pacific; it lasted until November 30 in both basins.
 These dates conventionally delimit the period during each year when most tropical cyclones form in the northeastern Pacific Ocean.
 Activity began with the formation of Hurricane Adrian, the fourth-earliest-forming tropical storm on record in the basin at the time.
 Adrian led to flash flooding and several landslides across Central America, resulting in five deaths and $12 million (2005 USD) in damage.
 Tropical storms Calvin and Dora caused minor damage along the coastline, while Tropical Storm Eugene led to one death in Acapulco.
 In early October, Otis produced tropical storm-force winds and minor flooding across the Baja California peninsula.
 The remnants of Tropical Depression One-C in the central Pacific, meanwhile, caused minor impacts in Hawaii.
 The strongest storm of the period was Hurricane Kenneth, which attained peak winds of 130 mph (215 km/h) over the open Pacific.
 Cooler than average ocean temperatures throughout the year aided in below-average activity through the course of the season, which ended with 15 named storms, 7 hurricanes, 2 major hurricanes, and an Accumulated cyclone energy index of 75 units.
Hurricane Norman was the most recent tropical system to make landfall in California.
 The 14th named storm, 11th hurricane, and 6th major hurricane of the 1978 Pacific hurricane season, Norman evolved from a tropical disturbance noted 400 mi southeast of Acapulco on the afternoon of August 29, 1978.
 The system moved westward and developed into a tropical depression on August 30.
 Modest strengthening ensued, and the cyclone became a tropical storm that evening and a hurricane on the evening of August 31 as it turned to the west-northwest.
 Late on the night of September 1, Norman became a major hurricane with an eye 40 mi wide, and a nearby ship reported seas of 41 ft .
 The center grazed the northeast side of Socorro Island on the afternoon of September 2.
 Moving over cooler waters west of Baja California, the cyclone slowly weakened.
 By early on September 4, moisture from the hurricane spread north into California initiating rains in the Golden State.
 A developing trough to its west caused the initial influx of moisture and Norman's turn to the north as a weakening tropical storm.
 Eventually turning north-northeast towards southern California, the cyclone did eventually turn north-northeast towards southern California, and the cyclone weakened to a tropical depression as it passed the 30th parallel.
 Hurricane Norman made landfall in California on September 5, as a minimal tropical depression.
 The tropical cyclone became a remnant low shortly after California landfall, and the final advisory was issued at 00:00 GMT, on September 6.
 Over 7.01 in of rain occurred in the Sierra Nevada range.
 Rare snowfall was also reported.
Hurricane Genevieve, also referred to as Typhoon Genevieve, was the fourth-most intense tropical cyclone of the North Pacific Ocean in 2014.
 A long-lasting system, Genevieve was the first one to track across all three northern Pacific basins since Hurricane Dora in 1999.
 Genevieve developed from a tropical wave into the eighth tropical storm of the 2014 Pacific hurricane season well east-southeast of Hawaii on July 25.
 However, increased vertical wind shear caused it to weaken into a tropical depression by the following day and degenerate into a remnant low on July 28.
 Late on July 29, the system regenerated into a tropical depression, but it weakened into a remnant low again on July 31, owing to vertical wind shear and dry air.
The practice of using names to identify tropical cyclones goes back several centuries, with storms named after places, saints or things they hit before the formal start of naming in each basin.
 Examples of such names are the 1911 Ship Cyclone, the 1928 Okeechobee hurricane and the 1938 New England hurricane.
 The system currently in place provides identification of tropical cyclones in a brief form that is easily understood and recognized by the public.
 The credit for the first usage of personal names for weather systems is given to the Queensland Government Meteorologist Clement Wragge, who named tropical cyclones and anticyclones between 1887 and 1907.
 This system of naming fell into disuse for several years after Wragge retired, until it was revived in the latter part of World War II for the Western Pacific.
 Over the following decades formal naming schemes were introduced for several tropical cyclone basins, including the North and South Atlantic, Eastern, Central, Western and Southern Pacific basins as well as the Australian region and Indian Ocean.
Hurricane Dora was one of few tropical cyclones to track across all three north Pacific basins.
 The fourth named storm, third hurricane, and second major hurricane of the 1999 Pacific hurricane season, Dora developed on August 6 from a tropical wave to the south of Mexico.
 Forming as a tropical depression, it gradually strengthened and was upgraded to Tropical Storm Dora later that day.
 Thereafter, Dora began heading in a steadily westward, before becoming a hurricane on August 8.
 Under warm sea surface temperatures (SST's) and low wind shear, the storm continued to intensify, eventually peaking as a 140 mph (220 km/h) Category 4 hurricane on August 12.
 While passing south of Hawaii, Dora significantly fluctuated in intensity, ranging from winds of 140 mph (220 km/h) to a low-end Category 1 hurricane.
 While crossing the International Dateline on August 20, Dora weakened to a tropical storm.
 After weakening to a tropical depression on August 22, the storm dissipated on August 23 while centered several hundred miles north of Wake Island.