Aarushhh/wikipedia-simple-splitted huggingface dataset:
After the crash
Iran ordered that the reason the plane crashed be found out. A day after the crash, people at the location had found both the flight's cockpit voice recorder, which records sounds in the cockpit, and the flight data recorder, which records what the plane does. Iran's Transport Ministry said that the investigation will be made up of several groups of people that study different parts of. The Iran Civil Aviation Organization will be in charge. The flight data recorder and cockpit voice recorder were both taken to Tehran as part of the investigation.

References

Other websites
 Photo of aircraft involved
 Photos from crash

2011 disasters in Asia
Aviation accidents and incidents in the 2010s
2010s in Iran
Aviation accidents and incidents in Asia
Disasters in Iran
Airliner accidents and incidents caused by ice
January 2011 events
Space colony may mean:

 any place where humans live outside of the planet Earth; see space colonization.
 a large object in space built by humans to live in; see space habitat.
 Space colony (Gundam), fictional space colonies in the Gundam anime series.
 Space Colony (video game), a real-time strategy video game.
 Colony in Space, a season 8 serial from Doctor Who
The North American Ford Focus was a compact vehicle made by the Ford Motor Company. The North American version was introduced in 1999 for the 2000 model year, although the Escort was sold alongside it until 2002. It was then facelifted in April 2004 for the 2005 model year, a new version came in late 2007 for the 2008 model year and was then redesigned in early 2011 for the 2012 model year, that generation was the same that was sold worldwide. The North American Ford Focus was discontinued after the 2018 model year.  

2000s automobiles
2010s automobiles
Focus (North America)
The NESFA gives the Edward E. Smith Memorial Award for Imaginative Fiction award each year to a science fiction writer. The award is for their work and for acting like "Doc" Smith. Many people who knew Smith loved him. The award is also called the Skylark.

The award is a trophy with a large lens in it. Regular members of the New England Science Fiction Association, Inc. vote for the winner. It is presented at Boskone, NESFA's annual convention.
1966  Frederik Pohl
 1967  Isaac Asimov
 1968  John W. Campbell
 1969  Hal Clement
 1970  Judy-Lynn Benjamin del Rey
 1971  No Award Given
 1972  Lester del Rey
 1973  Larry Niven
 1974  Ben Bova
 1975  Gordon R. Dickson
 1976  Anne McCaffrey
 1977  Jack Gaughan
 1978  Spider Robinson
 1979  David Gerrold
 1980  Jack L. Chalker
 1981  Frank Kelly Freas
 1982  Poul Anderson
 1983  Andre Norton
 1984  Robert Silverberg
 1985  Jack Williamson
 1986  Wilson (Bob) Tucker
 1987  Vincent Di Fate
 1988  C. J. Cherryh
 1989  Gene Wolfe
 1990  Jane Yolen
 1991  David Cherry
 1992  Orson Scott Card
 1993  Tom Doherty
 1994  Esther M. Friesner
 1995  Mike Resnick
 1996  Joe and Gay Haldeman
 1997  Hal Clement
 1998  James White
 1999  Bob Eggleton 
 2000  Bruce Coville
 2001  Ellen Asher
 2002  Dave Langford 
 2003  Patrick and Teresa Nielsen Hayden
 2004  George R.R. Martin
 2005  Tamora Pierce
 2006  David G. Hartwell
 2007  Beth Meacham
 2008  Charles Stross
 2009  Terry Pratchett

Related pages
Related pages

 Science fiction
 List of science fiction awards

Other websites
 NESFA
 Skylark Award 
 Boskone

Literary awards
Science fiction awards
Sinornithoides (meaning "Chinese bird form") is a genus of troodontid theropod dinosaur. It lived during the Early Cretaceous (Barremian stage, around 130 125 million years ago). It measured approximately 1 meter long (3 ft). It lived in Inner Mongolia, China, and probably ate invertebrates and other small prey.

Dinosaurs of Asia
Cretaceous dinosaurs
Shuvuuia is a genus of bird-like theropod dinosaur from the later Cretaceous of Mongolia. 

It is a member of the family Alvarezsauridae, small coelurosaurian dinosaurs which have short but powerful forelimbs specialized for digging. 

The name Shuvuuia is derived from the Mongolian word shuvuu meaning "bird".

Dinosaurs of Asia
Cretaceous dinosaurs
Feathered dinosaurs
WWE SmackDown vs. Raw 2011 is a wrestling video game that's published by THQ, It is available for the PlayStation 2, PlayStation 3, PlayStation Portable, Wii and Xbox 360 systems.

The game featured new physics system which can allow the player to use weapons more realistically for example tables can now break differently depending on the impact of them. Inside and outside the ring, ladders can now be rested onto the ring ropes and be broken into pieces and chairs can be thrown at the player's opponents. 

It is part of the WWE SmackDown vs. Raw video game series.

Other websites
 Official game website 

2010 video games
PlayStation 2 games
PlayStation 3 games
PlayStation Portable games
Wii games
Xbox 360 games
SmackDown vs. Raw 2011
THQ games
[[File:Juan Gris 001.jpg|thumb|right|250px|'Juan Gris, The Sunblind, 1914, Tate Gallery]]Collage''' is an art term. It is a work of art like a painting but with pieces of paper and fabric ('found objects') stuck on a surface such as a piece of paper, wood or canvas. 

Collage is a popular technique in modern art. Types of collage are 'decoupage', photomontage and digital collage. When actual painting is included, or any other medium, the technique is called 'mixed media'. Work in three dimensions may be called 'assemblage'.

Works of art
Chevrolet Van-simply called Chevy Van-refers to passenger or cargo vans which were full size. The vans went by the names of Sport Van, Beauville and Chevrolet G-Series. GMC's version of the vans were called Vandura and Rally Wagon. The vehicles were first made around 1964 under Chevrolet and GMC divisions of General Motors. They were discontinued after 1996. The post 1996 replacements were the Chevrolet Express and GMC Savana.

Vans
Pro-choice is the view that a woman should have the right to decide whether or not to have an abortion and that there should not be laws that stop people from getting abortions. 

People who are pro-choice believe that people should be able to use abortion to end a pregnancy. The view that abortion should be against the law is called pro-life.

The pro-choice movement is sometimes called the abortion rights movement. It is largely based on the belief, that woman should be able to decide what they want to do with their bodies. Having a baby would be a huge invasion to the body and should be a choice. They believe that an unborn embryo should not be valued over the pregnant woman. Pro-choice believes in a woman's right to choose.

Related pages
Abortion debate
Anti-abortion movement
Social movements related to abortion
Clinical psychology is the study in psychology of mental disorders. It is about learning, understanding, diagnosing, treating or preventing these types of illnesses. Clinical psychologists examine the mental functioning of a person and use psychotherapy to treat the disorder. Psychotherapy uses talking instead of medical or physical treatments.

The first psychological clinic opened in 1896 at the University of Pennsylvania by Lightner Witmer.In the first half of the 20th century, clinical psychology mainly was about psychological assessment, and not treatment. After World War II, there was a big increase in the numbers of trained clinical psychologists. There are two main educational models - the Ph.D. scientist-practitioner model which looks at research, and the Psy.D. practitioner-scholar model which looks at the treatments. Clinical psychologists are now regarded as experts in psychotherapy.
Four main schools 
Clinical psychologists generally train in one of the four primary academic areas – psychodynamic, humanistic, behavior therapy/cognitive behavioral, and systems or family therapy.

Psychodynamic 
Sigmund Freud's ideas led to the development of psychodynamic psychotherapy. Its goal is to help the patient, or client, to understand the meaning of the unconscious desires and conflicts that have caused their problems.

Humanistic 
Humanistic psychology was developed in the 1950s in reaction to both behaviourism (the belief that conditioning is the main cause of human behavior) and psychoanalysis (the belief that the unconscious is the main cause of human behavior).
The major principles of humanistic psychology are:
 A person's present is more important than his past or future
 People must take responsibility for their actions to be mentally healthy
 Every person deserves basic human dignity
 Self-improvement and self-understanding is the key to happiness.

References

Branches of psychology
Lapu-Lapu City is a first class highly urbanized city in the Philippine province of Cebu. The city occupies most of Mactan Island, a few kilometers off the main island of Cebu and also covers the area of Olango Island further to the southeast region, plus a few other islands. According to the 2007 census, it has a population of about 292,530 people.

The city is linked to Mandaue on mainland Cebu by the Mactan-Mandaue Bridge and Marcelo Fernan Bridge. Mactan-Cebu International Airport, the second busiest airport in the Philippines, is in Lapu-Lapu City. The only aquarium attraction in the Visayas is also in Lapu-lapu City. It is known as "Opon'.It is also home to the Mactan Shrine.

Location
Lapu-Lapu City borders Mandaue to the west, Cebu Strait to the east, Consolacion to the north, and Cordova to the south.
History
In the 16th century, Mactan Island was colonized by Spain. Augustinian friars founded the town of Opon in 1730. It became a city in 1961 and was renamed after Native Royalty the Datu Lapu-Lapu, the Island's chieftain who defeated Portuguese explorer Ferdinand Magellan in 1521. This battle is commemorated at the Lapu-Lapu shrine in Punta Engaño.

Politician Manuel A. Zosa, the representative of the Sixth District of Cebu, sponsored the Bill converting the former municipality of Opon into the present day City of Lapu-Lapu. This was the Republic Act 3134, known as the City Charter of Lapu-Lapu which was signed on June 17, 1961 by former Philippine President Carlos P. Garcia.

Barangays
Lapu-Lapu City is politically subdivided into 30 barangays.

Gallery

References

Other websites
 Official Lapu-Lapu City government website 

Cities in the Philippines
1730 establishments
Establishments in the Philippines
1730s establishments in Asia
Lee Hoi-chang (Korean:이회창, hanja:李會昌, June 2 1935 - ) is South Korean politician and judge. Chairman of Comptroller's and 26th prime minister of South Korea. His nicknames were 'Kyungsa' (경사), 'TaeZZeok' (대쪽).

After 1960, he was served 30 years as a judge, 1993 13th Chairman of Comptroller's of South Korea, prime minister of South Korea December 17 1993 to June 2 1994.

Books 
 『Beautiful's Principles』(아름다운 원칙)

Related pages
 Park Chung-hee
 Kim Young-sam
 Roh Tae-u
 Roh Moo-hyun
 Chun Doo-hwan

Other websites 
 Republic of Korea National Assembly:Lee Hoi-chang 
 ChangSarang  - Lee Hoi-chang's Fan Club
 Lee Hoi-chang 

1935 births
Living people
Prime Ministers of South Korea
Anti-communists
Xangsane made landfall in the Philippines, battering the northern islands with torrential rains and strong winds, and causing widespread flooding and landslides. After passing over Manila and emerging over the South China Sea, the typhoon made a second landfall in central Vietnam, also causing flooding and landslides there and in Thailand. The storm was responsible for at least 279 deaths, mostly in the Philippines and Vietnam, and at least $747 million (2006 USD) in damage.

Meteorological history
Late on September 24, 2006, the Joint Typhoon Warning Center, noted that an area of convection, had persisted about 460 NM to the southeast of Manila, in the Philippines. The JTWC assessed the development of a significant Tropical cyclone, as fair. This was because convection was beginning to flare up near a developing Low Level Circulation Center, the JTWC also noted that the disturbance had a broad circulation. Early the next day both the Japan Meteorological Agency and the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) designated the Tropical disturbance as a Tropical Depression with PAGASA assigning the local name of Tropical Depression Milenyo, to the depression. Later that morning the JTWC reassessed the potential of the disturbance forming into a significant tropical Cyclone within 24 hours as good, and issued a Tropical Cyclone Formation Alert on the developing disturbance
. Early that afternoon the JTWC started to issue advisories on the disturbance and designated it as Tropical Depression 18W. Later that day the JTWC upgraded as the depression moved towards the west it was upgraded to a Tropical Storm by the JTWC. Early on September 26 the JMA also upgraded the depression to a tropical storm, and assigned the international name of Xangsane.
Xangsane then passed through the Philippine islands, wreaking havoc and becoming the strongest typhoon to directly impact Metro Manila in eleven years. As it entered the South China Sea as a weak typhoon, it began to re-intensify, reaching its secondary peak strength shortly before landfall at Danang, Vietnam on October 1. The JTWC ceased advisories after landfall, while the JMA carried the storm inland until it was over Thailand as a tropical depression. It remained as a low pressure area over central Indochina on the JMA's weather charts for several days, while the U.S. Navy's Automated Tropical Cyclone Forecasting system carried the remnants of Xangsane into the Bay of Bengal.

Preparations

Philippines
Philippines

On September 27, PAGASA issued Storm Signal Number 3, a warning for winds of 100– 185 km/h (62– 115 mph), for areas of southern Luzon. Storm Signal Number 2, for winds of 60– 100 km/h (37– 62 mph), was raised for northern Samar Island and central Luzon. Storm Signal Number 1 (30– 60 km/h, 20– 37 mph) was issued for northwestern Luzon, including Metro Manila, and northern Visayas, including the rest of Samar Island. Schools in the warned area were suspended, and airports and seaports were closed. Philippine Airlines cancelled over half of its flights to and from Ninoy Aquino International Airport for September 28, and various transit services also suspended service. Metro Manila and the Tagalog provinces were warned of possible flooding and strong winds.

When it became clear that Xangsane would approach the Capital, PAGASA upgraded the warning for Manila and central Luzon to Storm Signal Number 3 on September 28. All the storm signals were discontinued later that day.

References
References

Other websites

 Digital Typhoon page on Xangsane

Typhoon Xangsane
Pacific typhoons
2000s in the Philippines
2000s in China
History of Vietnam
21st century in Cambodia
2000s in Thailand
Retired tropical cyclone names
William David Trimble, Baron Trimble, PC (15 October 1944 – 25 July 2022), was a politician from Northern Ireland. He was Leader of the Ulster Unionist Party (UUP; 1995–2005), the first First Minister of Northern Ireland (1998–2002), and was a Member of the House of Commons (1990–2005).

He was a life peer for the Conservative Party. Trimble was awarded the 1998 Nobel Peace Prize, along with John Hume because of effort toward Belfast Agreement.

Trimble died on 25 July 2022, aged 77.

References

1944 births
2022 deaths
British lawyers
British Nobel Prize winners
Conservative Party (UK) people
Leaders of political parties in the United Kingdom
Members of the House of Lords
Nobel Peace Prize winners
Ulster Unionist members of the Northern Ireland Assembly
Northern Irish Protestants
Presbyterians
Members of the Privy Council of the United Kingdom
UK MPs 1987–1992
UK MPs 1992–1997
UK MPs 1997–2001
UK MPs 2001–2005
First Ministers of Northern Ireland
Ulster Unionist Party MPs
The stamen is a male reproductive organ of a flower. It produces the pollen. The stamen has two parts: anther and stalk. The stalk is also called a filament.

The anther contains microsporangia. Each microsporangium contains pollen mother cells. These undergo meiosis, and produce pollen grains, which contain the male gametes (sperm).

The pollen grains are actually haploid male gametophytes.

The pollen is released by the opening of the anther. The pollen is carried by some agent (wind, or some animal) to the receptive surface of the stigma of the same or another flower. This process is known as pollination. After successful pollination, the pollen grain (immature microgametophyte) completes its development by growing a pollen tube and the two male gametes move through the pollen tube to the ovule.

References 

Flowers
Plant anatomy
The 2011 Pacific typhoon season was an event in which tropical cyclones formed in the Western Pacific Ocean. The season ran throughout 2011 with most tropical cycle agency storming between May and November. The scope of this article is limited to the Pacific Ocean to the north of the equator between 100th meridian east and the 180th meridian.

Within the Northwestern Pacific Ocean, there are two separate agencies who assign names to tropical cyclones. This can often result in a cyclone having two names. The Japan Meteorological Agency named a tropical cyclone if it was judged to have 10-minute sustained wind speeds of at least 65 km/h (40 mph) anywhere in the basin.
While the Philippine Atmospheric, Geophysical and Astronomical Services Administration assigned names to tropical cyclones which moved into or form as a tropical depression in their area of responsibility between 135°E and 115°E and between 5°N and 25°N even if the cyclone has had a name assigned to it by the Japan Meteorological Agency. Tropical depressions that were monitored by the United States' Joint Typhoon Warning Center were given a number with a "W" suffix. On average, 27 storms form in this basin every year.



Seasonal forecasts

During each season several national meteorological services and scientific agencies forecast how many tropical cyclones, tropical storms, and typhoons will form during a season and/or how many tropical cyclones will affect a particular country.
City University of Hong Kong
Since the 2000 Pacific typhoon season, the Guy Carpenter Asia-Pacific Climate Impact Centre (GCACIC), of the City University of Hong Kong (CityUHK), have issued forecasts of activity for each upcoming typhoon season. On May 4 and July 5, 2011, the GCACIC issued forecasts which predicted the amount of tropical cyclones, tropical storms and typhoons there would be during 2011 as well as for how many tropical cyclones will make landfall on China or pass within 100 km (60 mi) of the Korean Peninsula or Japan.
This season the GCACIC predicted in May that 31 tropical cyclones, 27 tropical storms, and 17 typhoons would either form or move into the northwestern Pacific this year. In their July forecast, the GCACIC lowered their prediction for the number of tropical storms developing into a typhoon by one which they blamed on the strength of the India-Burma trough. For Southern China the GCACIC predicted in May that seven tropical cyclones would make landfall, during the year compared to an average of five. They further predicted that five of the cyclones would make landfall on Southern China between May and August, while the other two would landfall between September and December. After two tropical cyclones had made landfall on Southern China during June, the July GCACIC forecast predicted that seven tropical cyclones would make landfall, during the main season between July and December
. For the Korean Peninsular and Japan, the GCACIC predicted in May that six tropical cyclones would affect either Japan or the peninsular during the year compared to an average of four, and predicted that there would be an above average amount of landfalls on Japan. After three tropical cyclones affected the region in May and June, the GCACIC predicted that seven tropical cyclones would affect either the Korean Peninsular or Japan during the main part of the season.
Tropical Storm Risk Consortium
Since the 2000 Pacific typhoon season, the Tropical Storm Risk Consortium (TSR) of University College London have issued forecasts of activity for each upcoming typhoon season. Forecasts on the number of tropical storms, typhoons and intense typhoons there would be during 2011 in the Western Pacific were released in March, May, July and August. In all of their forecasts this year, TSR predicted that the season would see activity close to the average with 28 tropical storms, 18 typhoons and 8 intense typhoons developing during the season.
National meteorological service predictions
On January 17, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) reported that they were expecting between 20 and 22 tropical cyclones to pass through the Philippine area of responsibility during 2011. On March 23 the Hong Kong Observatory (HKO), reported that they had predicted that 6-9 tropical cyclones would affect Hong Kong during the season. On April 26, the Thai Meteorological Department predicted that 2 tropical storms would affect Thailand during 2011. They predicted that 1 would move through Vietnam and affect Upper Thailand, during August or September. While the second tropical storm was expected to move through Southern Thailand during October or November. On June 30, Taiwan's Central Weather Bureau predicted that the 2011 season would be near its normal climatic average of 25.7, and predicted that 22-26 tropical storms, would occur over the Western Pacific during 2011, with 3 to 5 of them affecting Taiwan.
Seasonal summary

Storms

Tropical Depression (01W)
On April 1, the Japan Meteorological Agency (JMA) and Joint Typhoon Warning Center (JTWC) began monitoring an area of low pressure associated with intermittent convection over the South China Sea, roughly 535 km (335 mi) east-southeast of Ho Chi Minh City, Vietnam. The former of these two agencies immediately declared the system a tropical depression, the first of the 2011 season. Following further development of the system, most notably convective banding around the low-level circulation center, the JTWC issued a Tropical Cyclone Formation Alert on the storm. Early on April 2, the agency followed through with this alert and designated the low as Tropical Depression 01W. However, within hours of this, the depression became devoid of convection as wind shear buffeted the system. This prevented the cyclone from intensifying beyond depression status as it remained nearly stationary
. Failing to regain convection by April 3, the depression degenerated into a remnant low and the final advisory from the JTWC was issued. The JMA continued to monitor the system as a tropical depression for another day before issuing their last warning on the system.
On March 30, the JMA began monitoring an area of low pressure southwest of Yap. By April 2, the system developed a low-level circulation, though convection appeared disorganized. Exhibiting good outflow within a region of weak wind shear, the low was anticipated to develop further over the following several days as it drifted west-northwestward. After briefly stalling early on April 3, the storm turned towards the east. Additionally, the JMA considered the system sufficiently organized to be declared a tropical depression. As the system was to the west of 135°E, PAGASA began issuing advisories on the depression as well, assigning it the name "Amang". Tracking northeastward, the depression eventually developed enough convection to be declared Tropical Depression 02W by the JTWC on April 4. However, this was expected to be brief as a decaying frontal boundary approached from the west and prompted the system to undergo an extratropical transition
. This intensification prompted the National Weather Service (NWS) in Tiyan, Guam to issue a tropical storm warning for the islands of Agrihan, Pagan and Alamagan. Interacting with the front and high wind shear, the system became partially exposed and elongated as it moved over cooler waters. Early on April 6, the JTWC issued their final advisory on the depression as it began to dissipate over open waters. Following degradation of the storm's structure, the NWS discontinued warnings for the Mariana Islands on April 6. The JMA continued to monitor the system for several more hours before ceasing advisories on it as well.
Early on May 4, an area of low pressure formed about 140 km (85 mi) to the west of Palau Island. On that same day, the low pressure starts to strengthen rapidly with improved LLCC, tightly–wrapped shallow convective banding and a well–defined center. On the next day the low pressure starts to move northwest in general direction to the seas east of Philippine Islands. However it remained almost stationary by afternoon due to the influence of high pressure in the northeast of the system. By that time, its LLCC starts to become elongated and the system was also in favorable sea surface temperatures with low vertical wind shear. Later of that day, its LLCC starts to consolidate again and the system starts to move northwest slowly, whilst the Japan Meteorological Agency upgraded the system into a tropical depression In the afternoon of May 6, Joint Typhoon Warning Center upgraded the low pressure into a tropical depression
. In the same evening, PAGASA upgraded the low pressure into a tropical depression and assigned its local name 'Bebeng'. In the afternoon of May 7, JMA upgraded the tropical depression to a tropical storm, and assigned the name 'Aere'. During the early morning of May 12, the JMA downgraded Aere to a tropical depression while south of Kyushu Island.
Throughout the Philippines, multiple agencies activated their emergency plans as the storm approached. The Armed Forces of the Philippines, the Philippine National Police, and the Philippine Coast Guard were all placed on standby to deploy to areas struck by Aere once the storm passed. Several ports were affected by the storm, stranding 1,379 passengers by the afternoon of May 7. According to the National Disaster Risk Reduction and Management Council, at least 35 people have been killed and two more are missing as a result of Aere. Agricultural losses are estimated at PHP1.37 billion (US$31.7 million). Widespread flooding and landslides damaged homes, blocked off roads and severed communications. In Catarman, Northern Samar,  of rain fell in just 24 hours, resulted in significant flash flooding.

Typhoon Songda (Chedeng)
On May 19, the JTWC reported that an area of low pressure had persisted about 510 km (320 mi) to the southeast of Yap. As the system moved towards the northwest under the influence of a subtropical ridge of high pressure, it rapidly consolidated in an area of light to moderate vertical windshear. The JMA then started to monitor the system as a tropical depression later that day, before the JTWC designated it as Tropical Depression 04W early on May 20. The JTWC then reported later that day that the depression had intensified into a tropical storm with windspeeds of 65 km/h (40 mph), however it later reported that it had overestimated the windspeeds and consequently lowered the storm's status to a tropical depression, based on observations from Yap island. Late on May 21, both the JMA and the JTWC reported that the depression had now become a tropical storm with the JMA naming it as Songda
. Over the next couple of days, the system gradually intensified further while moving northwest into PAGASA's area of responsibility. PAGASA named it as Chedeng. At 1200  UTC on May 24, the JTWC reported that Songda had intensified into a typhoon. 12 hours later the JMA followed suit while the system was about 800 km (500 mi) to the southeast of Manila in the Philippines. It rapidly intensified into a Category 5 typhoon. In the afternoon of May 29, Songda became extratropical south of Shikoku Island.
Although Songda remained offshore, heavy rains within the typhoon's outer bands impacted the Philippines, causing significant flash flooding and landslides. Four fatalities are attributed to the system there. Further north, Okinawa experience intense wind gusts, measured up to 198 km/h (123 mph), along with torrential rain. Extensive damage took place across the area with losses reaching ¥23.2 billion ($287 million); however, there were no fatalities. As it became extratropical, Songda brought heavy rains from Kyushu to eastern Honshu, causing significant flooding. At least 13 people were killed in the country and an estimated 400,000 had to be evacuated around Tokyo alone.

Tropical Depression

During the evening of May 31, the JMA upgraded an area of low pressure to a tropical depression. Initially, the tropical depression was about 400 km (250 miles) southwest of Hong Kong. The system did not develop further and was downgraded to an area of low pressure by the JMA on June 2.
Tropical Storm Sarika (Dodong)

On early June 8, an area of low pressure formed about 10 km west of Cebu City, Philippines. As it moved towards the Mindoro Strait the JMA and JTWC began to monitor the system. In the early morning hours of June 9, the Philippines' PAGASA upgraded the system to a tropical depression and reported the storm center to be about 450 km west of Dagupan City in the Philippines. The next day, the JMA and JTWC upgraded the tropical depression into a tropical storm, with the JMA naming it Sarika. During the morning of June 11 the JTWC downgraded Sarika to a tropical depression after making landfall in Shantou, China. The JTWC soon issued their final advisory on Sarika. Sarika made landfall on mainland China with winds of 75 km/h (45 mph). As a result of the storm, 23 people were killed in Xianning, and ten more were declared missing. Damages from Sarika are estimated at $248 million.

Tropical Depression
Early June 15 an area of low pressure area embedded along the Intertropical Convergence Zone about 250 km west of Puerto Princesa, Palawan. As is moved towards the South China Sea, both the JMA and the JTWC started monitoring it. During the morning of June 15, the JMA upgraded it into a tropical depression. Due to an anticyclone, the system dissipated during the early morning of June 16,as it made landfall in Hong Kong.As it drifted over Hong Kong, the Hong Kong observatory's radar captured the center of the system.

Tropical Storm Haima (Egay)
During the evening of June 23, the JTWC downgraded Haima to a tropical depression after making landfall in Zhanjiang, Guangdong, China but upgraded it to a tropical storm again on June 24. Early on June 25, Haima became a tropical depression after moving inland in Vietnam. As it made landfall over Hanoi, Vietnam, the JTWC and the Hong Kong Observatory downgraded Haima to a low pressure area.

Severe Tropical Storm Meari (Falcon)
On June 26, Meari rapidly moved to the Yellow Sea but slowly passed Weihai, Shandong, China, and then the JMA downgraded Meari to a tropical storm on the same day. On June 27, the JTWC downgraded Meari to a tropical depression before it made landfall in North Korea, and the JMA reported that Meari became a low pressure area later.

Heavy rains from the storm's outer bands triggered significant flooding and landslides in South Korea. At least nine people were killed and three others were reported missing across the country. In North Korea, heavy rains from the storm caused widespread flooding and damage. At least 160 homes were destroyed and 50,000 hectares of crops submerged. Several reports of confirmed fatalities arose but no details on how many were given to news agencies.

Tropical Depression Goring
Late July 9, 2011, an area of low pressure area formed about 300 km (186 mi) east of Aurora. The center was  north of Basco, Batanes. On the morning of July 9, JMA upgraded the low pressure area into a tropical depression and it was 450 km northeast of Cagayan. In the afternoon, PAGASA upgraded the low pressure area into a tropical depression and named it Goring. After moving to Fujian, China, it weakened into an overland low pressure area on the evening on July 10.The remnant low of Goring appears to have redeveloped into a Tropical Depression on July 16

Typhoon Ma-on (Ineng)
On July 11, both the JMA and JTWC upgraded a tropical disturbance to a tropical depression which was near Minamitorishima. On July 12, both the JMA and JTWC upgraded the system to a tropical storm and named it Ma-on. Early on July 13, the JMA upgraded Ma-on to a severe tropical storm. Late on July 13, both the JMA and the JTWC upgraded Ma-on to a typhoon. After absorbing Tokage, Ma-on reached its peak strength on July 16. The PAGASA named it Ineng on July 17.

As Ma-on was affecting Japan, the JTWC downgraded it to a tropical storm in the evening on July 19. Ma-on made landfall in Tokushima later. The JMA downgraded Ma-on to a severe tropical storm after it made landfall in Wakayama early on July 20. The JTWC downgraded Ma-on to a tropical depression on July 21 and discontinued advisories the following day. The JMA downgraded Ma-on to a tropical storm early on July 23. On July 24, Ma-on weakened into an extratropical cyclone east of the Tōhoku region.

Tropical Storm Tokage (Hanna)
A low pressure area has formed about 740 km north-northwest of Palau. Early on July 14, the JMA upgraded it into a tropical depression, and the JTWC issued a Tropical Cyclone Formation Alert. On July 15, the JMA upgraded the system to a tropical storm and named it Tokage, and the JTWC upgraded it to a tropical depression later. PAGASA also upgraded it to a tropical depression and named it Hanna. Due to the Fujiwhara effect, Typhoon Ma-on, the powerful storm just northeast of Tokage, later weakened Tokage to a tropical depression and completely absorbed it early on July 16.

Tropical Depression
It can be traced back to a Tropical Depression on July 10, which made landfall over Fujian, China.The remnant low of the weak depression drifted back south, and entered the South China Sea on July 13, and later started to reintensify as it drift back inland, the JMA reported that a low has strengthen into tropical depression as it drifted over Guangdong, China on July 16. On July 17, the depression dissipated completely.

Tropical Depression

Originally a low pressure area, the JMA reported that a tropical depression formed from it in the Gulf of Tonkin near Guangdong, China on July 16. However, it quickly dissipated after only six hours.

Severe Tropical Storm Nock-ten (Juaning)
Early on July 22, an area of low pressure formed to the east of Philippines. The system gradually drifted west over the next few days and late on July 24, the Joint Typhoon Warning Center Started Monitoring the system as a Tropical Depression. Early the next day, the Japan Meteorological Agency (JMA) upgraded the area of low pressure into a Tropical Depression. A few hours later, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) started monitoring the system as a Tropical Depression and named it 'Juaning'. The system continued to drift westwards and strengthened rapidly, that on midnight, that day, the JMA furhter upgraded the system into a Tropical Storm, naming it Nock-Ten. Early on July 27, the JMA reported that Nock-ten continued to strengthen and upgraded it into a Severe Tropical Storm. A few hours later, the JTWC reported that Nock-ten rapidly intensified to a category 1 typhoon and made its landfall over northern Aurora (province) and started weakening
. Later the same day, the JMA reported that Nock-ten has exited the Luzon island at Candon maintaining severe tropical storm strength. However, overnight, the storm rapidly weakened and the JMA downgraded it into a minor tropical storm the next day. However, on July 29, the storm gradually regained strength and approached south China coast at Qionghai, China. Later that day, the storm strengthened over land and headed north towards Hainan's provincial capital region Haikou. Over the next day, the storm drifted to the west and made landfall over Northern Vietnam. The storm weakened rapidly and at midnight that day, the JMA, issuing their final warning on the system, Downgraded it into a tropical low.
The provinces of Albay and Camarines were reported to be completely flooded by the rain. Minor damage to rice crops was reported. More heavier rains were expected throughout the day as the system has exited land into south china sea and will soon start reintensifying. The number of missing was also pushed up to 31 after 25 crewmembers of a fishing boat were reported missing when their fishing boat was caught in the storm off Masbate. Nock-ten suspended all classes in Luzon from Pre-school to college levels on July 26 and 27. In Northern Luzon, Nock-ten poured down heavy rainfall becoming widespread flooding in the area. The national roads were impassable and landslides were also reported. About 26 domestic flights were cancelled from July 26 to 27 due to heavy rains and strong winds.

Typhoon Muifa (Kabayan)
Late on July 23, an area of low pressure formed to the southeast of Chuuk. the system gradually drifted to the west and on July 25, the JTWC upgraded the low pressure area to a tropical depression. At that time, it was about  to the west of Guam. At midnight, that day, the JMA started monitoring the system as a tropical depression. Early on July 28, the JTWC upgraded the system into a Tropical Storm. A few hours later, the JMA too upgraded the system to a tropical storm, naming it Muifa. Soon, the storm moved into the Philippine Area of Responsibility (PAR), and the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) named it Kabayan. The storm gradually drifted north over the next day maintaining strength. On the night of July 29, Muifa was upgraded into a Severe Tropical Storm. Overnight, the storm strengthened rapidly and was upgraded into a Typhoon the next morning
. The storm strengthened so rapidly, and the JTWC reported that the storm's peak winds were reaching  (1-min sustained), as it strengthened into a Category 5 Typhoon. However, the typhoon could not maintain Category 5 strength for a long time. According to the JTWC, On July 31, the typhoon interacted with an upper-level trough and weakened into a Category 4 Typhoon on the SSHS. The system gradually moved north, then turned west and drifted towards Okinawa, before turning northwest again, when it was finally downgraded into a Tropical Storm by the JTWC. Soon afterwards, the JMA too downgraded Muifa to a Severe Tropical storm. After weakening to a tropical storm, Muifa made landfall at the estuary of the Yalu River on August 8, and the JTWC issued the final warning. Early on August 9, Muifa weakened to a tropical depression in Northeast China and became a low pressure area later.
Muifa killed 2 men, as their boat was capsized in the vicinity of Hagonoy, Bulacan and Pampanga Delta. Due to the southwest monsoon enhanced by Muifa, it caused heavy rains in several parts of Luzon including Metro Manila. Early of August 2, the Malacañang Palace suspended government offices and Pre-school to college level in NCR. Nearby provinces like Calabarzon (Region IV-A) also suspended their classes. In Marikina 200 residents or 31 families living in communities along the Marikina River have sought shelter in evacuation centers.

Tropical Depression (Lando)
On July 28, an area of low pressure formed about  to the West of Guam. Over the next few days, the system gradually drifted to the northwest and on July 31, the Japan Meteorological Agency (JMA) upgraded the low into a Tropical Depression to the west of Philippines. Later that day, The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) started monitoring the system as a tropical depression and named it Lando. The system slowly tracked northward. However, on the next day, due to Fujiwhara effect, Typhoon Muifa the much more powerful system, just to the northeast of Lando, weakened Lando. As a result, the PAGASA issued their final warning on the system, downgrading it to a tropical low. But despite this, Tropical Depression Lando regenerated soon afterwards, and the JMA reissued their advisories on Lando. Tropical Depression Lando continued to persist for another day, as it slowly tracked eastward, just off the western coast of Luzon
. Then, during the late afternoon of August 2, the JMA stopped tracking Lando, as it had dissipated. Early on August 3, the remmants of Tropical Depression Lando dissipated completely, without ever reaching Luzon.
Early on August 3, the Japan Meteorological Agency (JMA) upgraded an area of low pressure near Wake Island to a tropical depression. The system intensified rapidly and just 6 hours later, the JMA upgraded the system to a tropical storm, naming it Merbok. Soon, the Joint Typhoon Warning Center (JTWC) started monitoring the system as a tropical depression, and upgraded it to a tropical storm later. Merbok began to move westward slowly, but soon afterwards, it turned northwest and gradually drifted in that direction. Late on August 5, the JMA upgraded Merbok into a Severe Tropical Storm. Early on August 6, the JTWC upgraded Merbok into a Category 1 Typhoon  East-southeast of Tokyo, Japan. Early the next day, the storm's winds reached a peak of  (1-min sustained) on the SSHS. Later that day, the system was caught in a moderate Vertical Wind Shear and started weakening
. On August 8, the system started accelerating towards north at the speed of  and was gradually diminishing because of colder and colder sea surface temperatures and unfavorable conditions. As a result, the JMA reporting that the system was no longer a Severe Tropical Storm, downgraded Merbok to a Tropical Storm. Late on that day, the system started showing extratropical characteristics as the convection near the eye dissipated rapidly. Thus, the JTWC issued their final warning on the system reporting that the system was no longer tropical. Later, the JMA, issuing their final warning on the system, reported that the system was no longer tropical.
Tropical Depression

Early on August 3, a tropical depression formed near the Bonin Islands. The system slowly began to track northwestwards, towards Japan. Late on August 4, the system dissipated near the Kii Peninsula.

Tropical Depression (13W)
Late on August 8, the JMA upgraded a low pressure area to a tropical depression west of Guam, and the JTWC issued a TCFA. The system gradually drifted north and early on August 10, the JTWC started monitoring the system as a tropical depression and designated it with 13W. Initially, the JMA predicted the system to strengthen into a tropical storm, but on August 11, as it moved further north into cool waters and experienced unfavourable conditions, the JMA issued their final advisory. Later, the JTWC too issued their final warning on the system, reporting that it has moved into a subtropical ridge and was expected to dissipate into a remnant low. However, the JMA continued to track the remants as a weak tropical depression over the next few days until the system dissipated on August 15.

Tropical Depression
Late on August 8, the JMA upgraded an area of low pressure to a tropical depression, to the northwest of Minamitorishima. The system gradually moved to the northeast. On August 10, the system was caught in a moderate vertical wind shear and due to cold sea surface temperature, the system dissipated into a remnant low.

Tropical Depression
On August 19, a low pressure area developed east-northeast of Guam. Early on August 20, the system developed a broad area of low level circulation center and a good divergence aloft becoming more well defined. Later that day, the JMA upgraded the system to a tropical depression southeast of the Bonin Islands. On August 22, the system started interacting with an anticyclone and was exposed to a strong vertical wind shear, prompting the JMA to stop monitoring the system as a tropical depression, as the system dissipated to a remnant low. However, at midnight, the same day, the remnants regenerated, and the JMA started tracking the system as a tropical depression again, until it last appeared near Okinawa, Japan on August 25, as the system dissipated completely.

Typhoon Nanmadol (Mina)
Late on August 19, an area of low pressure developed north of Palau. Early on August 20, the system became more better organized and developed a low-level circulation center. The system then turned north and continued to drift north until on August 21, when the JMA upgraded the low pressure area to a tropical depression east of Philippines. The JTWC also issued a Tropical Cyclone Formation Alert (TCFA) on the system reporting that the system was becoming more well organized. Later that day, the PAGASA started monitoring the system as a tropical depression and named it Mina. Late on August 22, the system became more well organized prompting the JTWC to initiate advisories on the system, designating it with 14W. On August 23, the JMA upgraded 14W to a tropical storm, naming it Nanmadol. Overnight, the system continued to intensify and early on August 24, the JMA upgraded Nanmadol to a severe tropical storm. Later that day, convective banding improved and Nanmadol developed an eye-like feature
. As a result, Nanmadol continued to intensify rapidly and became a typhoon, by midnight, that day. Nanmadol continued to drift northeast and made landfall over Gonzaga, Cagayan, Philippines with strong winds of over . Nanmadol weakened significantly after interacting with land and early on August 28, the JMA downgraded Nanmadol to a severe tropical storm. Late on August 28, Nanmadol made its second landfall over Taimali in the Taitung County of Taiwan and started weakening. Landfall weakened the system rapidly prompting the JMA to downgrade Nanmadol to a tropical storm with winds of under . Soon it started experiencing strong wind shear and continued weakening. The shear pushed convection about  south of the LLCC. The system also accelerated towards China at  and weakened to a minimal tropical storm. After its third landfall over Fujian, China, Nanmadol weakened rapidly prompting both the JTWC and the JMA to issue their final warnings on the system.
On August 27, five people died after Nanmadol caused landslides. At least two Filipino fishermen were reported to be missing after Nanmadol's strong winds whipped up large waves.

Typhoon Talas
Late on August 22, an area of low pressure developed to the west of Guam. At midnight that day, the system became sufficiently well organized that the JMA started tracking it as a tropical depression. On August 23, the system moved into an environment of low wind shear and warm sea surface temperatures prompting the JTWC to issued a TCFA on it. By August 25, the system grew strong enough that the JMA upgraded it to a tropical storm, naming it Talas. Later that day, the JTWC followed suit and initiated advisories on Talas. Talas continued to strengthen and by midnight that day, it became a severe tropical storm. Over the next few days, Talas continued to drift north very slowly until late on August 29, when the JMA upgraded Talas to a typhoon. Soon, a subtropical ridge to the west of the storm weakened and the subtropical ridge to the east of the system pushed Talas to the west. As a result, Talas accelerated towards the west maintaining strength and outflow
. An upper-level cyclone over the system suppressed the convection and kept it from reaching the center. Therefore, Talas remained weak and did not strengthen further. Convection never managed to consolidate the center and convective banding remained well away from the fully exposed low-level circulation center. The convective banding continued to expand more and more with the outer rainbands already brushing parts of Japan. Coastal areas in the nation have already reported gale-force winds several hours before landfall, while the Omega block continued to drive Talas towards the nation. Land interaction weakened Talas, prompting the JMA to downgrade Talas from a typhoon to a severe tropical storm with winds of under . Early on September 3, Talas made landfall over Aki, Japan
. After landfall, Talas accelerated north at over  and its central convection became significantly eroded and was displaced to the northeast as Talas was exposed to a very strong wind shear of over  that made the LLCC very distorted and difficult to pin-point. Talas was embedded in a baroclinic zone and the JTWC anticipated an extratropical transition, which prompted them to issue their final warning on the system. On September 5, the JMA issued their final warning on the system, reporting that Talas has become extratropical on the Sea of Japan.