AcharyaChanakya/simple-wikipedia huggingface dataset:
He died during a European tour in Sweden on September 24, 1986 when Metallica was celebrating the success of their album Master of Puppets. The band’s tour bus skidded off the road and flipped over. Burton was thrown out of the bus window and the bus fell on him. They attempted to rescue Burton from underneath the bus by lifting it with a crane, but the crane slipped, and the bus landed down on top of Burton a second time.By that time, he was already dead at just 24 years old.
Beipiaosaurus
Beipiaosaurus is a therizinosaur theropod dinosaur. It lived in the Lower Cretaceous, about 125 million years ago. Its fossil was found in the Yixian Formation near Beipiao, Liaoning Province of China. The theroziosaurs were a group of theropods which became herbivorous. "Beipiaosaurus" had a toothless beak, cheek teeth, and protofeathers.
Prime Minister of Russia
The Prime Minister of Russia (, "Prem'er-ministr Rossii") is Russia's head of government. He is the second most powerful leader in the Russian Federation.
The Prime Minister serves the same time as the President of Russia, and has a term of office of six years but may be appointed again.
The President appoints the Prime Minister and must be approved by the State Duma. Only two acting Prime Ministers: Yegor Gaidar and Viktor Chernomyrdin were appointed by the President, but not approved by the Duma. The most recent Prime Minister is Mikhail Mishustin since 16 January 2020.
As of 2020, there are eight living former Prime Ministers. The most recent death of a former Prime Minister was that of Yevgeny Primakov (1998–1999) on 26 June 2015, aged 85.
Brian Guebert
Brian Guebert (born December 19, 1981) is a Canadian Football League defensive end who last played for the Winnipeg Blue Bombers.
Guebert went to Lutheran Collegiate Bible Institute in Outlook, Saskatchewan. His team won the six-man Saskatchewan High School Provincial Football Championship in 1998. He was selected as the Defensive MVP in the 1999 Can-Am Bowl, and was chosen as the Outstanding Defensive Lineman in the 1999 Saskatchewan Senior Bowl.
Guebert played with the Saskatoon Hilltops, and he won the Canadian Junior Football League championship in 2001, 2002, and 2003. In both 2002 and 2003, Guebert was picked as the Prairie Football Conference Outstanding Defensive Lineman. He was also chosen as the Hilltops' Outstanding Lineman in 2002 and their Outstanding Graduate in 2003.
After his time with the Hilltops, Guebert moved on to play university football with the University of Saskatchewan Huskies. He was picked as a Canada West All-Star in 2004, and both a Canada West All-Star and First Team All-Canadian in 2006. His team played in the Vanier Cup in 2004, 2005, and 2006.
Guebert is a member of the 2004–05 Huskie Athletics All Academic 1st Team and 2004–05 CIS Academic All-Canadian Team.
Guebert went to training camp with the Saskatchewan Roughriders in 2003, playing in one exhibition game against Winnipeg.
Guebert was signed as a free agent with Winnipeg on May 30, 2007 and was a good special teams player. He was let go following the 2008 season.
Iran Air Flight 227
Iran Air Flight 277 was a passenger plane which, on , 2011, crashed while trying to land in bad weather at Urmia Airport, West Azarbaijan province, Iran. The aircraft that crashed was going between Mehrabad International Airport, Tehran, Iran, and Urmia. It was an Iran Air Boeing 727-286Adv, registration EP-IRP.
The aircraft that crashed was a Boeing 727-286Adv. It was registered EP-IRP and was built in 1974. The aircraft spent a long time out of service, and was in Baghdad, Iraq from 1984-90, and then stored from 1991-2002. After that, it was fixed and went back to flying.
The flight was going between Tehran and Urmia. The plane crashed when it was about to land. It crashed near a lake. The crash happened at around 19:45 (16:15 UTC), and was thought to be caused by bad weather. The aircraft had missed its first try at landing, and it either crashed during a go-around, or while trying to return to Tehran. The weather at the time of the accident included snow and it was hard to see. When it crashed, the plane broke into more than one piece, but there was no fire or explosion. There were different reports right after the crash as to the type of aircraft that it happened to. Either a Fokker 100 or a Boeing 727 was thought to have crashed, but it was later made clear that the plane was a 727.
The number of people on board was not known; RIA Novosti said that 95 passengers were on the plane, but Reuters said there were 156 passengers and the Associated Press said there were 105 passengers. Later reports said there were either 105 or 106 people on board. Between 10 and 12 were crew and either 95 or 94 were passengers. The Iran Civil Aviation Organization said the day after the crash that a total of 93 passengers and 12 crew were on board.
At least 77 people were killed and 26 were hurt. It was hard to rescue people because there was a lot of snow at the time. A local official said that "[the] problem at the moment for rescue work is the heavy snow," which he said was around deep at the site of the crash. After the crash, 36 ambulances and 11 hospitals were used in the rescue.
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.
Space colony
Space colony may mean:
Ford Focus (North America)
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. 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 is the same that's sold worldwide. The US Focus was discontinued after the 2018 model year.
Edward E. Smith Memorial Award
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.
Sinornithoides
Shuvuuia
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".
WWE SmackDown vs. Raw 2011
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.
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'.
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.
Pro-choice
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.
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 about psychological assessment, 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 treatment. Clinical psychologists are now regarded as experts in psychotherapy.
Clinical psychologists generally train in one of four primary academic areas – psychodynamic, humanistic, behavior therapy/cognitive behavioral, and systems or family therapy.
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 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:
Lapu-Lapu City
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 kilometer 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'.
Lapu-Lapu City is it's own island. It is surrounded by a big ocean like Mactan Channel, Cebu Strait, Camotes Sea and Bohol Sea.
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.
Lapu-Lapu City is politically subdivided into 30 barangays.
Lee Hoi-chang
Lee Hoi-chang(Korean:이회창, hanja:李會昌, June 2 1935 - ) is South korean politicians and Judges. Chairman of Comptroller's, 26th prime minister of South Korea. nickname was 'Kyungsa'(경사), 'TaeZZeok'(대쪽).
After 1960, he was served to 30years as a judge, 1993 13th Chairman of Comptroller's of South Korea, prime minister of South Korea December 17 1993 to June 2 1994.
Typhoon Xangsane
Typhoon Xangsane (international designation: 0615, JTWC designation: 18W, PAGASA name: Typhoon Milenyo) was a deadly typhoon that affected the Philippines, Vietnam, and Thailand during the 2006 Pacific typhoon season. It was the fifteenth tropical storm and ninth typhoon recognized by the Japan Meteorological Agency operationally during the season, although in post-operational analysis it became the tenth typhoon of the season with the addition of Typhoon Maria. According to the Joint Typhoon Warning Center, Xangsane was the sixteenth tropical storm and tenth typhoon of the season, and was a Category 4-equivalent typhoon in terms of 1-minute average wind speeds. The name Xangsane was submitted by Laos and means elephant.
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.
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.
Later on September 26, the JMA upgraded Xangsane to a severe tropical storm, whilst six hours later both the JMA and the JTWC upgraded Xangsane to typhoon with the JTWC reporting wind speeds equivalent to a category one typhoon. Early the next day Xangsane was upgraded to a category 2 typhoon and then over the next six hours Xangsane rapidly intensified into a category 4 typhoon with wind speeds of 115 kts (130 mph, 215 km/h). Meanwhile the JMA reported that Xangsane had reached its peak wind speeds of 85 kts (100 mph, 155 km/h). Early that afternoon the JTWC reported that Xangsane, had reached its peak wind speeds of 125 kts (145 mph, 230 km/h).
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.
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.
David Trimble
William David Trimble, Baron Trimble, PC (born 15 October 1944, in Belfast), is 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 is 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.
Stamen
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.
2011 Pacific typhoon season
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.
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.
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.
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.
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.
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.
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.
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.
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.
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.
On June 15, the JTWC started to monitor an area of disturbed weather that was about 1350 km (835 mi), to the southeast of Manila, Philippines. Over the next couple of days the system gradually developed further, before late on June 16, the JMA, JTWC and PAGASA, all reported that the system had developed into a tropical depression, with PAGASA naming it as Egay. Egay continued to develop during June 17 as it moved towards the northeast, and on June 18 the JTWC reported that Egay had intensified into a tropical storm. Late on June 19, the JTWC downgraded Egay to a tropical depression, but they upgraded Egay again to a tropical storm on June 20. Early on June 20, the JTWC downgraded Egay to a tropical depression again. On June 21, the JMA upgraded the system into a tropical storm and named it Haima, with the JTWC following suit on June 22.
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.
Early on June 20, and area of low pressure about 760 km (470 miles), east of the Philippines began to be monitored by both the JTWC and JMA. That evening, the JTWC issued a Tropical Cyclone Formation Alert. Soon afterwards, PAGASA upgraded the system into a tropical depression, naming it as "Falcon". At the time of the upgrade, Falcon was about 1000 km (620 miles), east northeast of Cebu City. During the evening of June 21, the JTWC also reported that Falcon had strengthened into a tropical depression. On June 22, both the JTWC and the JMA upgraded Falcon into a tropical storm, and the JMA named it Meari. Meari leaves Philippines with 2 deaths and 5 missing. In the afternoon on June 24, the JMA upgraded Meari to a severe tropical storm as it passed Okinawa, Japan.
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.
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
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.
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.
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.
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.
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.
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 , 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.
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 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.
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.
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.
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.
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.