Typhoon Dolphin (2008)

Last updated
Map key
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
Disc Plain black.svg Tropical cyclone
Solid black.svg Subtropical cyclone
ArrowUp.svg Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

On December 2, the Japan Meteorological Agency (JMA) began to issue gale warnings on a new-born extratropical cyclone around the Ogasawara Islands, and JMA started to issue storm warnings when the system accelerated eastward on the next day. [1] [2] The storm reached storm-force and attained its extratropical peak intensity with 10-minute maximum sustained winds of 60 knots (110 km/h, 70 mph) on December 4, when it was located far east of Japan; however, the low became developed late on the same day. [3]

The storm north of Wake Island started to track east-southeastward on December 5, as well as it tracked southeastward then southward on December 6. [4] At noon, it became a developing low again and reached its extratropical peak intensity for the second time, before it moved into the tropics. [5] On December 7, the storm started to track southwestward and weakened into a gale-force system; eventually, the system transformed into a tropical depression southeast of Wake Island early on December 8. [6] [7]

However, early the next day, the JMA downgraded the depression to a low pressure area, as the depression's low level circulation center was partially exposed, and was in an area of moderate to high vertical wind shear. However the JMA re-upgraded the disturbance to a weak tropical depression 24 hours later. At 0600 UTC that morning, the Joint Typhoon Warning Center (JTWC), released a significant tropical weather advisory and rated the chances of the disturbance becoming a significant tropical cyclone within 24 hours as poor, due to a quikscat pass had shown that the low level circulation center had broken down into a wave. However, after the advisory was released the low level circulation center started to rapidly consolidate, and thus the JTWC initiated issuing warnings at 1200 UTC, December 10, and designated it as Tropical Depression 27W, while it was about 640 km (400 mi) to the east of Guam and moving towards the west. Early the next day the depression's centre passed about 100 km (62 mi) to the south of Guam and made its closest approach.

Track map of the precursor to Typhoon Dolphin Tropical Storm Dolphin Track Map.jpeg
Track map of the precursor to Typhoon Dolphin

The JTWC upgraded the depression to a Tropical Storm late the next day and then early on December 12 the JMA designated the depression as a full tropical depression. [8] [9] The Tropical Depression was then upgraded to a Tropical Storm and named Dolphin later that morning as it moved westwards towards the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) area of responsibility. [10] [11] The next day as Tropical Storm Dolphin moved into PAGASA's area of responsibility, PAGASA assigned the local name of Ulysses to Dolphin. [12] The JMA upgraded Tropical Storm Dolphin to a Severe Tropical Storm late on December 14. [13] Whilst Dolphin was upgraded to a Typhoon by the JTWC early the next day as Dolphin recurved towards the North. [14] Later that day the JTWC reported that Typhoon Dolphin had reached its peak winds of 90 kts (105 mph; 165 km/h 1-minute winds) which made Typhoon Dolphin a category two Typhoon on the Saffir–Simpson hurricane scale. [15] At the same time the JMA reported that Severe Tropical Storm Dolphin had intensified into a Typhoon and had also reached its peak wind speeds of 65 kts (75 mph; 120 km/h 10-minute winds). [16]

Early in the afternoon of December 16, the JMA downgraded Typhoon Dolphin from a Typhoon to a Severe Tropical Storm, as it moved towards the northwest. [17] This came as the JTWC reported that Dolphin had weakened into a Category One Typhoon. [15] Early the next day the JTWC downgraded Typhoon Dolphin to a Tropical Storm, whilst later that day the JMA also downgraded Dolphin to a Tropical Storm. [15] [18] This came as Tropical Storm Dolphin moved out of PAGASA's Area of responsibility. [19] Early in the afternoon of December 18, both the JMA and the JTWC released their final advisories on Tropical Storm Dolphin as they downgraded Dolphin to an extratropical low. [20] [21] The extratropical low dissipated two days later. [15]

Preparations, impact and aftermath

Micronesia

From December 8 to December 12, large sea swells up to 3 m (9.8 ft), generated by the extratropical cyclone that was to become Typhoon Dolphin and Tropical Disturbance 03F, affected many islands throughout Micronesia including Papua New Guinea and Hawaii. [22] [23] The most affected areas included New Ireland, Bougainville, Manus, East Sepik, Morobe, and West Sepik. The waves affected over 50,000 to 80,000 people with over 400 people left homeless after their homes were destroyed.

Guam and Rota

Late on December 10, as the JTWC reported that Tropical Depression 27W had formed, the National Weather Service forecast office in Guam issued a tropical storm warning for Guam as tropical storm conditions were anticipated to impact the island within 24 hours. [24] A tropical storm watch was also declared for Rota at this time as tropical storm-force winds were possibly going to affect Rota within 24 hours. Early the next day the tropical storm watch for Rota was cancelled followed by the tropical storm warning for Guam later that day as the depression was accelerating away from the Islands. [25] [26] The Guam Emergency Operations Center was partially activated and Guam Homeland Security and Office of Civil Defense personnel were on call in case they were needed. Residents were advised to bring in all holiday decorations that may become airborne and prepare their emergency disaster kits. [27] Within Guam, flights in and out of Guam International Airport were not cancelled as winds did not exceed 90 km/h, (55 mph). [28] The maximum reported rainfall amount was at Inarajan Handar which reported 2.05 inches of rainfall in the 48 hours starting on December 10 at 0100 UTC. [29] Guam government officials reported that there was not much significant damage, with power outages around the island being sporadic which were primarily caused by falling trees and debris. [29] There was also some minor flooding and beach erosion caused by storm tides. [29]

M/Bca Mae Jan

The M/Bca Mae Jan was a cargo passenger ship which sank on December 14 due to rough seas caused by Typhoon Dolphin. [30] The M/Bca Mae Jan was only licensed to carry 40 passengers and 10 members of crew; however, at the time of its sinking the M/Bca Mae Jan was carrying 97 people. [31] Of the 98 people, 47 died and 7 were missing. [32] Vessels operating in the area were asked to help in the search and rescue operation, whilst the Philippine coastguard directed three ships to perform aerial and surface searches. [30]

The Philippine National Disaster Coordinating Council reported on December 17 that the local Government unit of Ballesteros, Cagayan had provided assistance worth 16,500  PHP ($352 2008  USD). [32] Whilst the Department of Health-Center for Health Development had provided 27,203 PHP ($582 2008 USD) worth of assistance, in the form of drugs, fluids and medicines for the injured victims that were confined at the Ballesteros District Hospital. [32] The Department of Social Welfare and Development provided cash and relief goods totalling up to 128,000 PHP ($2,740 2008 USD), The Department of Social Welfare and Development also propositioned standby funds of 255,000 PHP ($5,453 2008 USD). [32]

See also

Related Research Articles

<span class="mw-page-title-main">2007 Pacific typhoon season</span>

The 2007 Pacific typhoon season was a near average season which featured 24 named storms, fourteen typhoons, and five super typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2007, though most tropical cyclones typically develop between May and November. The season's first named storm, Kong-rey, developed on March 30, while the season's last named storm, Mitag, dissipated on November 27. The season's first typhoon, Yutu, reached typhoon status on May 18, and became the first super typhoon of the year on the next day.

<span class="mw-page-title-main">2008 Pacific typhoon season</span>

The 2008 Pacific typhoon season was a below average season which featured 22 named storms, eleven typhoons, and two super typhoons. The season had no official bounds; it ran year-round in 2008, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.

<span class="mw-page-title-main">Timeline of the 2008 Pacific typhoon season</span>

This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation during the 2008 Pacific typhoon season. The 2008 Pacific typhoon season officially started on January 1, 2008 and ended on January 1, 2009. The first tropical cyclone of the season formed on January 13. The timeline also includes information which was not operationally released, meaning that information from post-storm reviews by the various warning agencies, such as information on a storm that was not operationally warned on, has been included.

<span class="mw-page-title-main">Typhoon Rammasun (2008)</span> Pacific typhoon in 2008

Typhoon Rammasun, known in the Philippines as Typhoon Butchoy, was recognized as the second typhoon of the 2008 Pacific typhoon season by the Japan Meteorological Agency (JMA) and the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA). Rammasun was also recognised as the third tropical storm, the second typhoon and the first super typhoon of the 2008 Pacific typhoon season by the Joint Typhoon Warning Center (JTWC).

<span class="mw-page-title-main">Typhoon Jangmi (2008)</span> Pacific typhoon in 2008

Typhoon Jangmi, known in the Philippines as Super Typhoon Ofel, was the most intense tropical cyclone in the Northwest Pacific Ocean during the 2000s, tied with Nida in 2009, and the most intense tropical cyclone worldwide in 2008. Jangmi, which means rose in Korean, formed in a low pressure area south of Guam on September 22. After undergoing serious consolidating with convective banding, the low pressure area was upgraded to a Joint Typhoon Warning Center late the same data. Undergoing the same process, the storm developed into a tropical storm on September 24. Undergoing rapid deepening on September 26–27, the storm, now a Super Typhoon entered the Philippine Area of Responsibility, and was named Ofel. The next day, Jangmi made impact in Taiwan, thousands were evacuated, rainfall, up to 994mm were recorded, and thousands of acres of farmland were destroyed. Jangmi was significantly weakened as it interacted with Taiwan, as being downgraded to tropical storm status after leaving Taiwan on September 29. After undergoing an extratropical transition, Jangmi became a remnant low on October 1. After slowly moving eastward, until finally dissipating near Iwo Jima on October 5.

<span class="mw-page-title-main">2012 Pacific typhoon season</span>

The 2012 Pacific typhoon season was a slightly above average season that produced 25 named storms, fourteen typhoons, and four intense typhoons. It was a destructive and the second consecutive year to be the deadliest season, primarily due to Typhoon Bopha which killed 1,901 people in the Philippines. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2012, though most tropical cyclones typically develop between May and October. The season's first named storm, Pakhar, developed on March 28, while the season's last named storm, Wukong, dissipated on December 29. The season's first typhoon, Guchol, reached typhoon status on June 15, and became the first super typhoon of the year on June 17.

<span class="mw-page-title-main">2009 Pacific typhoon season</span>

The 2009 Pacific typhoon season was a below average season that spawned only 22 named storms, 13 typhoons, and five super typhoons. It was also recognized as the deadliest season in the Philippines for decades. The first half of the season was very quiet whereas the second half of the season was extremely active. The season's first named storm, Kujira, developed on May 3 while the season's last named storm, Nida, dissipated on December 3.

<span class="mw-page-title-main">Timeline of the 2009 Pacific typhoon season</span>

This timeline documents all of the events of the 2009 Pacific typhoon season which was the period that tropical cyclones formed in the Western Pacific Ocean during 2009, with most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.

<span class="mw-page-title-main">Typhoon Choi-wan (2009)</span> Pacific typhoon in 2009

Typhoon Choi-wan was a powerful typhoon that became the first Category 5-equivalent super typhoon to form during the 2009 Pacific typhoon season. Forming on September 11, 2009, about 1,100 km (700 mi) to the east of Guam, the initial disturbance rapidly organized into a tropical depression. By September 12, the depression intensified into a tropical storm, at which time it was given the name Choi-wan. The following day, rapid intensification took place through September 14. Choi-wan attained its peak intensity on September 15, as it moved through the Northern Mariana Islands with the Japan Meteorological Agency reporting peak 10-minute sustained winds of 195 km/h (121 mph). Additionally, the Joint Typhoon Warning Center reported the storm to have attained 1-minute sustained winds of 260 km/h (160 mph). The typhoon remained very powerful until September 17 when the storm's outflow weakened. The typhoon underwent an eyewall replacement cycle, leading to intensity fluctuations. By September 19, Choi-wan rapidly weakened as strong wind shear caused convection to diminish. The following day, the system transitioned into an extratropical cyclone and dissipated several hours later over open waters.

<span class="mw-page-title-main">Typhoon Melor (2009)</span> Pacific typhoon in 2009

Typhoon Melor, known in the Philippines as Super Typhoon Quedan, was the second category 5 super typhoon in 2009. It interacted with Typhoon Parma in the first week of October southeast of Taiwan.

<span class="mw-page-title-main">2011 Pacific typhoon season</span>

The 2011 Pacific typhoon season was a below average season that produced a total of 21 named storms, 8 typhoons, and four super typhoons. This season was much more active than the previous season, although both seasons were below the Pacific typhoon average of 26. The season ran throughout 2011, though most tropical cyclone tend to develop between May and October. The season's first named storm, Aere, developed on May 7 while the season's last named storm, Washi dissipated on December 19.

<span class="mw-page-title-main">2014 Pacific typhoon season</span>

The 2014 Pacific typhoon season was a slightly below average season in terms of named storms, but featured the highest amount of Category 5 typhoons since 1997. This was mainly due to a developing El Niño that favors multiple powerful storms to form in the basin. The season formed twenty-three tropical storms, eleven typhoons, eight super typhoons, and seven Category 5 typhoons. The season's peak months August and September saw minimal activity caused by an unusually strong and a persistent suppressing phase of the Madden–Julian oscillation (MJO). The season ran throughout 2014, though most tropical cyclones typically develop between May and October. The season began with the development of Tropical Storm Lingling on January 18, and ended after Tropical Storm Jangmi which dissipated on January 1 of the next year.

<span class="mw-page-title-main">2015 Pacific typhoon season</span>

The 2015 Pacific typhoon season was a slightly above average season that produced twenty-seven tropical storms, eighteen typhoons, and nine super typhoons. The season ran throughout 2015, though most tropical cyclones typically develop between May and November. The season's first named storm, Mekkhala, developed on January 15, while the season's last named storm, Melor, dissipated on December 17. The season saw at least one named tropical system forming in each of every month, the first time since 1965. Similar to the previous season, this season saw a high number of super typhoons. Accumulated cyclone energy (ACE) during 2015 was extremely high, the third highest since 1970, and the 2015 ACE has been attributed in part to anthropogenic warming, and also the 2014-16 El Niño event, that led to similarly high ACE values in the East Pacific.

<span class="mw-page-title-main">2016 Pacific typhoon season</span>

The 2016 Pacific typhoon season is considered to have been the fourth-latest start for a Pacific typhoon season since reliable records began. It was an average season, with a total of 26 named storms, 13 typhoons, and six super typhoons. The season ran throughout 2016, though typically most tropical cyclones develop between May and October. The season's first named storm, Nepartak, developed on July 3, while the season's last named storm, Nock-ten, dissipated on December 28.

<span class="mw-page-title-main">Timeline of the 2013 Pacific typhoon season</span>

Most of the tropical cyclones of the 2013 Pacific typhoon season formed between May and November of that year. The scope of this article is the Pacific Ocean north of the equator, between 100°E and the International Date Line. Tropical storms which form in the Western Pacific basin are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions forming in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center (JTWC). The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility, but these names are not in common use outside the Philippines.

<span class="mw-page-title-main">Timeline of the 2011 Pacific typhoon season</span>

This timeline documents all of the events of the 2011 Pacific typhoon season, the period that tropical cyclones formed in the Western Pacific Ocean in 2011. Most of the tropical cyclones formed between May and November 2011. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center (JTWC). In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.

<span class="mw-page-title-main">Timeline of the 2014 Pacific typhoon season</span>

This timeline documents all of the events of the 2014 Pacific typhoon season. Most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.

<span class="mw-page-title-main">Timeline of the 2015 Pacific typhoon season</span>

This timeline documents all of the events of the 2015 Pacific typhoon season. Most of the tropical cyclones formed between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. This area, called the Western Pacific basin, is the responsibility of the Japanese Meteorological Agency (JMA). They host and operate the Regional Specialized Meteorological Center (RSMC), located in Tokyo. The Japanese Meteorological Agency (JMA) is also responsible for assigning names to all tropical storms that are formed within the basin. However, any storm that enters or forms in the Philippine Area of Responsibility (PAR) will be named by the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) using a local name. Also of note - the Western Pacific basin is monitored by the United States' Joint Typhoon Warning Center (JTWC), which gives all Tropical depressions a number with a "W" suffix.

<span class="mw-page-title-main">2021 Pacific typhoon season</span>

The 2021 Pacific typhoon season was the second consecutive to have below average tropical cyclone activity, with twenty-two named storms, and was the least active since 2011. Nine became typhoons, and five of those intensified into super typhoons. This low activity was caused by a strong La Niña that had persisted from the previous year. The season's first named storm, Dujuan, developed on February 16, while the last named storm, Rai, dissipated on December 21. The season's first typhoon, Surigae, reached typhoon status on April 16. It became the first super typhoon of the year on the next day, also becoming the strongest tropical cyclone in 2021. Surigae was also the most powerful tropical cyclone on record in the Northern Hemisphere for the month of April. Typhoons In-fa and Rai are responsible for more than half of the total damage this season, adding up to a combined total of $2.02 billion.

<span class="mw-page-title-main">Tropical Storm Barijat</span> Pacific tropical storm in 2018

Tropical Storm Barijat, known in the Philippines as Tropical Storm Neneng, was a weak tropical storm that caused flooding in the far northern regions of the Philippines and Southern China. Barijat, a replacement name for Utor which is a Marshallese word for coastal areas impacted by waves or winds, the thirty-third tropical depression and twenty-third tropical storm of the 2018 Pacific typhoon season, it was first noted as an area of convection in the South China Sea on September 6. On September 8, it was upgraded to a tropical depression, and by September 11, it intensified into a tropical storm, with the Japan Meteorological Agency (JMA) giving it the name Barijat. Barijat peaked in intensity 6 hours later, with 10-min winds of 40 knots and 1-min winds of 45 knots. Barijat continued westward, and on November 12 at 00:30 UTC, it made landfall over Zhanjiang, quickly dissipating afterwards.

References

  1. "Advisories on December 2, 2008" (TXT). Mtarchive Data Server. Iowa State University of Science and Technology.
  2. "Advisories on December 3, 2008" (TXT). Mtarchive Data Server. Iowa State University of Science and Technology.
  3. "Advisories on December 4, 2008" (TXT). Mtarchive Data Server. Iowa State University of Science and Technology.
  4. "Advisories on December 5, 2008" (TXT). Mtarchive Data Server. Iowa State University of Science and Technology.
  5. "Advisories on December 6, 2008" (TXT). Mtarchive Data Server. Iowa State University of Science and Technology.
  6. "Advisories on December 7, 2008" (TXT). Mtarchive Data Server. Iowa State University of Science and Technology.
  7. "Advisories on December 8, 2008" (TXT). Mtarchive Data Server. Iowa State University of Science and Technology.
  8. "JTWC Advisory 11-12-08 21z". Joint Typhoon Warning Center. Archived from the original on October 14, 2008. Retrieved 2008-12-17.{{cite web}}: CS1 maint: unfit URL (link)
  9. "JMA Advisory 12-12-08 00z". Japan Meteorological Agency. Archived from the original on 2024-05-23. Retrieved 2008-12-17.
  10. "JMA Advisory 12-12-08 06z". Japan Meteorological Agency. Archived from the original on 2024-05-23. Retrieved 2008-12-17.
  11. "PAGASA Weather Advisory 12-12-08 09z". PAGASA. Archived from the original on October 4, 2016. Retrieved 2008-12-17.{{cite web}}: CS1 maint: unfit URL (link)
  12. "PAGASA Advisory 13-12-08 09z". PAGASA. Archived from the original on 2008-05-07. Retrieved 2008-12-18.
  13. "JMA Advisory 14-12-08 18z". Japan Meteorological Agency. Archived from the original on 2024-05-23. Retrieved 2008-12-20.
  14. "JTWC Advisory 15-12-08 03z". Joint Typhoon Warning Center. Archived from the original on October 14, 2008. Retrieved 2008-12-20.{{cite web}}: CS1 maint: unfit URL (link)
  15. 1 2 3 4 "JTWC Best Track:Dolphin". Joint Typhoon Warning Center . Retrieved 2008-12-17.
  16. "JMA Advisory 15-12-08 12z". Japan Meteorological Agency. Archived from the original on 2024-05-23. Retrieved 2008-12-20.
  17. "JMA Advisory 16-12-08 12z". Japan Meteorological Agency. Archived from the original on 2024-05-23. Retrieved 2008-12-20.
  18. "JMA Advisory 17-12-08 18z". Japan Meteorological Agency. Archived from the original on 2024-05-23. Retrieved 2008-12-20.
  19. "PAGASA Advisory 17-12-08 15z". PAGASA. Archived from the original on 2008-05-07. Retrieved 2008-12-20.
  20. "JMA Advisory 18-12-08 12z". Japan Meteorological Agency. Archived from the original on 2024-05-23. Retrieved 2008-12-20.
  21. "JTWC Advisory 18-12-08 15z". Joint Typhoon Warning Center. Archived from the original on October 14, 2008. Retrieved 2008-12-20.{{cite web}}: CS1 maint: unfit URL (link)
  22. Gary Padgett (2009-02-11). "Monthly Tropical Cyclone Summary for December 2008". Australian Severe Weather. Retrieved 2009-02-11.
  23. Bill Ward. "An Unusual Low in the Northwest Pacific Ocean" (PDF). National Weather Service Weather Forecast Office Honolulu, Hawaii . National Oceanic and Atmospheric Administration . Retrieved 2008-01-28.
  24. "Tropical Depression 27W Advisory 10-12-2008 16z". National Weather Service Weather Forecast Office Tiyan, Guam . National Oceanic and Atmospheric Administration. 2008-12-10. Archived from the original on 2024-05-23. Retrieved 2009-07-26.
  25. "Tropical Depression 27W Advisory 11-12-2008 12z". National Weather Service, Weather Forecast Office Tiyan, Guam . National Oceanic and Atmospheric Administration. 2008-12-11. Archived from the original on 2024-05-23. Retrieved 2009-07-26.
  26. "Tropical Depression 27W Advisory 11-12-2008 09z". National Weather Service Weather Forecast Office Tiyan, Guam . National Oceanic and Atmospheric Administration. 2008-12-11. Archived from the original on 2024-05-23. Retrieved 2009-07-26.
  27. "TD 27W Begins Closest Point of Approach". Guam Homeland Security. 2008-12-10. Retrieved 2009-01-28.
  28. "Tropical Depression 27W moves closer to Guam". Kuam.com. 2008-12-11. Archived from the original on December 15, 2008. Retrieved 2009-07-27.
  29. 1 2 3 "Post Storm Report Tropical Depression 27W (Dolphin)". National Weather Service Weather Forecast Office Tiyan, Guam . National Oceanic and Atmospheric Administration. 2008-12-12. Archived from the original on July 3, 2010. Retrieved 2009-07-27.{{cite web}}: CS1 maint: unfit URL (link)
  30. 1 2 "NDCC Update - M/Bca Mae Jan" (PDF). National Disaster Coordinating Council. Retrieved 2008-12-18.
  31. "Sitrep No 2. Re Capsized M/Bca Mae Jan" (PDF). National Disaster Coordinating Council. 2008-12-17. Retrieved 2008-12-18.
  32. 1 2 3 4 "Sitrep No 3. Re Capsized M/Bca Mae Jan" (PDF). National Disaster Coordinating Council. 2008-12-18. Retrieved 2008-12-20.[ dead link ]
Typhoon Dolphin (Ulysses)
Dolphin 2008-12-16 0445Z.jpg
Typhoon Dolphin at peak intensity on December 16