paragraph_text: The monsoon of South Asia is among several geographically distributed global monsoons. It affects the Indian subcontinent, where it is one of the oldest and most anticipated weather phenomena and an economically important pattern every year from June through September. Yet it is only partly understood and notoriously difficult to predict. Several theories have been proposed to explain the origin, process, strength, variability, distribution, and general vagaries of the monsoon, but understanding and predictability are still evolving.

paragraph_text: The Indian Institute of Tropical Meteorology (IITM) is a scientific institution based in Pune, India for expanding research in tropical Indian Ocean (formerly on tropical meteorology), of the tropics in general with special reference to monsoon meteorology, and air-sea interaction of Indian monsoon.

paragraph_text: The North American monsoon, variously known as the Southwest monsoon, the Mexican monsoon, the New Mexican monsoon, or the Arizona monsoon, is a pattern of pronounced increase in thunderstorms and rainfall over large areas of the southwestern United States and northwestern Mexico, typically occurring between July and mid September. During the monsoon, thunderstorms are fueled by daytime heating and build up during the late afternoon - early evening. Typically, these storms dissipate by late night, and the next day starts out fair, with the cycle repeating daily. The monsoon typically loses its energy by mid-September when drier and cooler conditions are reestablished over the region. Geographically, the North American monsoon precipitation region is centered over the Sierra Madre Occidental in the Mexican states of Sinaloa, Durango, Sonora and Chihuahua.

paragraph_text: Western Disturbances mostly occur during the winter months and cause light to moderate showers in southern parts of the country while moderate to heavy showers with heavy snowfall in the northern parts of the country. These westerly waves are robbed of most of the moisture by the time they reach Pakistan. Fog occurs during the winter season and remains for weeks in upper Sindh, central Khyber Pakhtunkhwa and Punjab. Southwest Monsoon occurs in summer from the month of June till September in almost whole Pakistan excluding western Balochistan, FATA, Chitral and Gilgit -- Baltistan. Monsoon rains bring much awaited relief from the scorching summer heat. These monsoon rains are quite heavy by nature and can cause significant flooding, even severe flooding if they interact with westerly waves in the upper parts of the country. Tropical Storms usually form during the summer months from late April till June and then from late September till November. They affect the coastal localities of the country. Dust storms occur during summer months with peak in May and June, They are locally known as Andhi. These dust storms are quite violent. Dust storms during the early summer indicate the arrival of the monsoons while dust storms in the autumn indicate the arrival of winter. Heat waves occur during May and June, especially in southern Punjab, central Balochistan and interior Sindh. Thunderstorms most commonly occur in northern Punjab, Khyber Pakhtunkhwa and Azad Kashmir. Continental air prevails during the period when there is no precipitation in the country.

paragraph_text: Mahatma Gandhi High School, Sheragada is located in Asika subdivision of Ganjam district of Odisha. It was established in 1947.

paragraph_text: Nepal experiences five seasons: summer, monsoon, autumn, winter and spring. The Himalaya blocks cold winds from Central Asia in the winter and forms the northern limit of the monsoon wind patterns. In a land once thickly forested, deforestation is a major problem in all regions, with resulting erosion and degradation of ecosystems.

paragraph_text: Gandhi Smriti in New Delhi is the location where Mahatma Gandhi spent the last 144 days of his life and was assassinated on 30 January 1948. Rajghat is the place where Mahatma Gandhi was cremated on 31 January 1948 after his assassination and his ashes were buried and make it a final resting place beside the sanctity of the Yamuna River. The Raj Ghat in the shape of large square platform with black marble was designed by architect Vanu Bhuta.

paragraph_text: Sohra or Cherrapunji has a mild subtropical highland climate (Köppen Cwb), with monsoonal influences typical of India. The city's annual rainfall average stands at 11,777 millimetres (463.7 in). This figure places it behind only nearby Mawsynram, Meghalaya, whose average is 11,873 millimetres (467.4 in). Cherrapunji receives both the southwest and northeast monsoonal winds, giving it a single monsoon season. It lies on the windward side of the Khasi Hills, so the resulting orographic lift enhances precipitation. In the winter months it receives the northeast monsoon showers that travel down the Brahmaputra valley. The driest months are November, December, January and February.

paragraph_text: Gandhi Memorial Museum, established in 1959, is a memorial museum for Gandhi located in the city of Madurai in Tamil Nadu, India. Known as Gandhi Museum, it is now one of the five Gandhi Sanghralayas (Gandhi Museums) in the country. It includes a part of the blood-stained garment worn by Gandhi when he was assassinated by Nathuram Godse.

paragraph_text: By the end of April 1971, Prime Minister Indira Gandhi had asked the Indian army chief General Sam Manekshaw if he was ready to go to war with Pakistan. According to Manekshaw's own personal account, he refused, citing the onset of monsoon season in East Pakistan and also the fact that the army tanks were in the process of being refitted. He claimed that he offered to resign, which Indira Gandhi declined. He then said he could guarantee victory if she would allow him to prepare for the conflict on his terms, and set a date for it and Prime Minister Indira Gandhi accepted his conditions. In reality, Indira Gandhi was well aware of the difficulties of a hasty military action but she needed to get the military's views to satisfy her hawkish colleagues and the public opinion, which were critical of India's restraint.

paragraph_text: The city generally has a climate with warm days followed by cool nights and mornings. Unpredictable weather is expected, given that temperatures can drop to 1 °C (34 °F) or less during the winter. During a 2013 cold front, the winter temperatures of Kathmandu dropped to −4 °C (25 °F), and the lowest temperature was recorded on January 10, 2013, at −9.2 °C (15.4 °F). Rainfall is mostly monsoon-based (about 65% of the total concentrated during the monsoon months of June to August), and decreases substantially (100 to 200 cm (39 to 79 in)) from eastern Nepal to western Nepal. Rainfall has been recorded at about 1,400 millimetres (55.1 in) for the Kathmandu valley, and averages 1,407 millimetres (55.4 in) for the city of Kathmandu. On average humidity is 75%. The chart below is based on data from the Nepal Bureau of Standards & Meteorology, "Weather Meteorology" for 2005. The chart provides minimum and maximum temperatures during each month. The annual amount of precipitation was 1,124 millimetres (44.3 in) for 2005, as per monthly data included in the table above. The decade of 2000-2010 saw highly variable and unprecedented precipitation anomalies in Kathmandu. This was mostly due to the annual variation of the southwest monsoon.[citation needed] For example, 2003 was the wettest year ever in Kathmandu, totalling over 2,900 mm (114 in) of precipitation due to an exceptionally strong monsoon season. In contrast, 2001 recorded only 356 mm (14 in) of precipitation due to an extraordinarily weak monsoon season.

paragraph_text: The winner of the fifth season of RuPaul's Drag Race was Jinkx Monsoon, with Alaska and Roxxxy Andrews being the runners - up.

paragraph_text: RuPaul's Drag Race Season 5 Broadcast from January 28 (2013 - 01 - 28) -- May 6, 2013 (2013 - 05 - 06) Judges RuPaul Michelle Visage Santino Rice Host (s) RuPaul Broadcaster Logo Competitors 14 Winner Jinkx Monsoon Origin Seattle, WA Runner - up Alaska Roxxxy Andrews Chronology ◀ Season 5 ▶

paragraph_text: Gandhi Maidan or Gandhi Maidan Marg is one of the most important thoroughfares in Patna, India. It is a historical place and is considered as a landmark of the city. Gandhi Maidan is the main market and commercial area of Patna with Ashok Rajpath which starts from Gandhi Maidan and Dak Bungalow Crossing and Bailey Road besides Frazer Road, Exhibition Road, Boring Road, and Boring Canal Road. There are many important institutes that have developed around the area of Gandhi Maidan.

paragraph_text: The Climate of India comprises a wide range of weather conditions across a vast geographic scale and varied topography, making generalisations difficult. Based on the Köppen system, India hosts six major climatic subtypes, ranging from arid desert in the west, alpine tundra and glaciers in the north, and humid tropical regions supporting rainforests in the southwest and the island territories. Many regions have starkly different microclimates. The country's meteorological department follows the international standard of four climatological seasons with some local adjustments: winter (December, January and February), summer (March, April and May), a monsoon rainy season (June to September), and a post-monsoon period (October to November).

paragraph_text: Bapunagar is a neighbourhood in Ahmedabad, Gujarat, India. It is located in the eastern part of the city, in the Rakhial ward. Its name derives from the word "Bapu", which refers to Gandhi, who was popularly called "Bapu", or Father.

paragraph_text: Tucson has a desert climate (Köppen BWh), with two major seasons, summer and winter; plus three minor seasons: fall, spring, and the monsoon. Tucson averages 11.8 inches (299.7 mm) of precipitation per year, more than most other locations with desert climates, but it still qualifies due to its high evapotranspiration; in other words, it experiences a high net loss of water. A similar scenario is seen in Alice Springs, Australia, which averages 11 inches (279.4 mm) a year, but has a desert climate.

paragraph_text: Post-monsoon or autumn season, lasting from October to November. In the northwest of India, October and November are usually cloudless. Tamil Nadu receives most of its annual precipitation in the northeast monsoon season.

paragraph_text: The climate of New Delhi is a monsoon-influenced humid subtropical climate (Köppen Cwa) with high variation between summer and winter in terms of both temperature and rainfall. The temperature varies from 46 °C (115 °F) in summers to around 0 °C (32 °F) in winters. The area's version of a humid subtropical climate is noticeably different from many other cities with this climate classification in that it features long and very hot summers, relatively dry and mild winters, a monsoonal period, and dust storms. Summers are long, extending from early April to October, with the monsoon season occurring in the middle of the summer. Winter starts in November and peaks in January. The annual mean temperature is around 25 °C (77 °F); monthly daily mean temperatures range from approximately 14 to 34 °C (57 to 93 °F). New Delhi's highest temperature ever recorded is 49.1 °C (120.4 °F) while the lowest temperature ever recorded is −3.2 °C (26.2 °F). Those for Delhi metropolis stand at 49.9 °C (121.8 °F) and −3.2 °C (26.2 °F) respectively. The average annual rainfall is 784 millimetres (30.9 in), most of which is during the monsoons in July and August.

paragraph_text: Guiyang has a four-season, monsoon-influenced humid subtropical climate (Köppen: Cwa), tempered by its low latitude and high elevation. It has cool winters and moderate-temperature summers; the majority of the year's 1,118 millimetres (44.0 in) of precipitation occurs from May to July. The monthly 24-hour average temperature ranges from 5.1 °C (41.2 °F) in January to 23.9 °C (75.0 °F) in July, while the annual mean is 15.35 °C (59.6 °F). Rain is common throughout the year, with occasional flurries in winter. With monthly percent possible sunshine ranging from 12 percent in January to 41 percent in August, the city receives only 1150 hours of sunshine, making it one of China's least sunny major cities. Average monthly relative humidity is consistently above 75% throughout the year.

Question: When does the monsoon season occur in the city Gandhi Smriti is located?
Answer: the middle of the summer