paragraph_text: The January daily average is 33.0 °F (0.6 °C), though, in a normal winter, the temperature frequently rises to 50 °F (10 °C) during thaws and dips to 10 °F (−12 °C) for 2 or 3 nights. July averages 78.1 °F (25.6 °C), although heat waves accompanied by high humidity and heat indices are frequent; highs reach or exceed 90 °F (32 °C) on 27 days of the year. The average window for freezing temperatures is November 6 thru April 2, allowing a growing season of 217 days. Early fall and late winter are generally dry; February's average of 2.64 inches (67 mm) makes it the area's driest month. The dewpoint in the summer averages between 59.1 °F (15 °C) to 64.5 °F (18 °C).

paragraph_text: The climate of Islamabad has a humid subtropical climate (Köppen climate classifion, with five seasons: Winter (Nov − Feb), Spring (March − April), Summer (May − June), Rainy Monsoon (July − August) and Autumn (September − October). The hottest month is June, where average highs routinely exceed 38 ° C (100.4 ° F). The wettest month is July, with heavy rainfall and evening thunderstorms with the possibility of cloudburst. The coolest month is January, with temperatures variable by location. In Islamabad, temperatures vary from cold to mild, routinely dropping below zero. In the hills there is sparse snowfall. The weather ranges from a minimum of − 3.9 ° C (25.0 ° F) in January to a maximum of 46.1 ° C (115.0 ° F) in June. The average low is 2 ° C (35.6 ° F) in January, while the average high is 38.1 ° C (100.6 ° F) in June. The highest temperature recorded was 46.5 ° C (115.7 ° F) in June, while the lowest temperature was − 4 ° C (24.8 ° F) in January. On 23 July 2001, Islamabad received a record breaking 620 millimetres (24 in) of rain fell in just 10 hours. It was the heaviest rainfall in 24 hours in Islamabad and at any locality in Pakistan during the past 100 years. Following is the weather observed over Islamabad Airport, which is actually located in Rawalpindi.

paragraph_text: Istanbul's persistently high humidity reaches 80 percent most mornings. Because of this, fog is very common, although more so in northern parts of the city and away from the city center. Dense fog disrupts transportation in the region, including on the Bosphorus, and is common during the autumn and winter months when the humidity remains high into the afternoon. The humid conditions and the fog tend to dissipate by midday during the summer months, but the lingering humidity exacerbates the moderately high summer temperatures. During these summer months, high temperatures average around 29 °C (84 °F) and rainfall is uncommon; there are only about fifteen days with measurable precipitation between June and August. The summer months also have the highest concentration of thunderstorms.Winter is colder in Istanbul than in most other cities around the Mediterranean Basin, with low temperatures averaging 1–4 °C (34–39 °F). Lake-effect snow from the Black Sea is common, although difficult to forecast, with the potential to be heavy and—as with the fog—disruptive to the city's infrastructure. Spring and autumn are mild, but often wet and unpredictable; chilly winds from the northwest and warm gusts from the south—sometimes in the same day—tend to cause fluctuations in temperature. Overall, Istanbul has an annual average of 130 days with significant precipitation, which amounts to 810 millimeters (31.9 in) per year. The highest and lowest temperatures ever recorded in the city center on the Marmara coast are 40.5 °C (105 °F) and −16.1 °C (3 °F). The greatest rainfall recorded in a day is 227 millimeters (8.9 in), and the highest recorded snow cover is 80 centimeters (31 in).

paragraph_text: Mean monthly temperatures range from around 53 F in January to 82 F in July. High temperatures average 64 to 92 °F (18 to 33 °C) throughout the year. High heat indices are common for the summer months in the area, with indices above 110 °F (43.3 °C) possible. The highest temperature recorded was 104 °F (40 °C) on July 11, 1879 and July 28, 1872. It is common for thunderstorms to erupt during a typical summer afternoon. These are caused by the rapid heating of the land relative to the water, combined with extremely high humidity.

paragraph_text: The Kopet-Dag mountain range is about 25 kilometres (16 mi) to the south, and Ashgabat's northern boundary touches the Kara-Kum desert. Because of this Ashgabat has a cold desert climate (Köppen climate classification: BWk) with hot, dry summers and cool, short winters. The average high temperature in July is 38.3 °C (100.9 °F). Nighttimes in the summer are warm, with an average minimum temperature in July of 23.8 °C (75 °F). The average January high temperature is 8.6 °C (47.5 °F), and the average low temperature is −0.4 °C (31.3 °F). The highest temperature ever recorded in Ashgabat is 47.2 °C (117 °F), recorded in June 2015. A low temperature of −24.1 °C (−11 °F) was recorded in January 1969. Snow is infrequent in the area. Annual precipitation is only 201 millimetres (7.91 in); March and April are the wettest months, and summer drought, from late June to September, is virtually absolute.

paragraph_text: The Celsius scale was based on 0 ° C for the freezing point of water and 100 ° C for the boiling point of water at 1 atm pressure following a change introduced in 1743 by Jean - Pierre Christin to reverse the Celsius thermometer scale (from water boiling at 0 degrees and ice melting at 100 degrees). This scale is widely taught in schools today. By international agreement the unit ``degree Celsius ''and the Celsius scale are currently defined by two different temperatures: absolute zero, and the triple point of Vienna Standard Mean Ocean Water (VSMOW), a specially purified water. This definition also precisely relates the Celsius scale to the Kelvin scale, which defines the SI base unit of thermodynamic temperature with symbol K. Absolute zero, the lowest temperature possible, is defined as being exactly 0 K and − 273.15 ° C. The temperature of the triple point of water is defined as exactly 273.16 K (0.01 ° C; 32.02 ° F).

paragraph_text: Summers in the state are generally hot and humid, with most of the state averaging a high of around 90 °F (32 °C) during the summer months. Winters tend to be mild to cool, increasing in coolness at higher elevations. Generally, for areas outside the highest mountains, the average overnight lows are near freezing for most of the state. The highest recorded temperature is 113 °F (45 °C) at Perryville on August 9, 1930 while the lowest recorded temperature is −32 °F (−36 °C) at Mountain City on December 30, 1917.

paragraph_text: The "Asama Hot Spring Center", also known as the "Hot Plaza Hall", has a configuration typical of many Japanese onsen with separate areas for males and females; each area contains multiple indoor pools, saunas and two outdoor pools, one hot and one cold. The published temperature range of this onsen is 42-47 degrees Celsius.

paragraph_text: The city has an elevation of 382.2 m (1,254 feet). In a 1984 census the city's population was 17,320.  Al Jawf receives almost no rain whatsoever, averaging only 2.5mm (.1 inch) per year. Summer high temperatures average above 37.8 °C (100 °F).

paragraph_text: Due to the protection provided by the Central Mountain Range to the east and the Miaoli hills to the north, Taichung is rarely severely affected by typhoons. However, occasional typhoons emerging from the South China Sea can pose a threat to the city as evidenced by Typhoon Wayne in 1986, which struck the west coast of Taiwan near Taichung.Due to Taichung plain's strong radiative cooling effect, Taichung City is one of the few cities of Taiwan where the year round average daily low temperature falls below 20 degrees Celsius, with even most cities of northern Taiwan, such as Taipei and Keelung having an average low of over 20.5 degrees C.

paragraph_text: Brachychiton collinus, the outcrop kurrajong, is a small deciduous tree found growing in some of the harshest climatic conditions in Australia. This small tree is commonly found between Cloncurry and Mount Isa in North-West Queensland, Australia. The North-West savannah zone of Queensland is characterised by very high summer temperatures of up to 50 degrees Celsius and an unpredictable monsoonal rainfall that may deliver the whole annual rainfall of some 50 cm overnight. This tree most often grows on rocky outcrops where little other scrub, grasses or other understory plants can survive. It is probable that this preference for bare rocky outcrops is a function of the tree's sensitivity to fire. Most brachychiton species do not survive a strong grass or brush fire.

paragraph_text: Palermo experiences a hot-summer Mediterranean climate (Köppen climate classification: Csa). Winters are cool and wet, while summers are hot and dry. Temperatures in autumn and spring are usually mild. Palermo is one of the warmest cities in Europe (mainly due to its warm nights), with an average annual air temperature of 18.5 °C (65.3 °F). It receives approximately 2,530 hours of sunshine per year. Snow is usually a rare occurrence, but it does occur occasionally if there is a cold front, as the Apennines are too distant to protect the island from cold winds blowing from the Balkans, and the mountains surrounding the city facilite the formation of snow accumulation in Palermo, especially at night. Between the 1940s and the 2000s there have been eleven times when considerable snowfall has occurred: In 1949, in 1956, when the minimum temperature went down to 0 °C (32 °F) and the city was blanketed by several centimeters of snow. Snow also occurred in 1999, 2009 and 2015. The average annual temperature of the sea is above 19 °C (66 °F); from 14 °C (57 °F) in February to 26 °C (79 °F) in August. In the period from May to November, the average sea temperature exceeds 18 °C (64 °F) and in the period from June to October, the average sea temperature exceeds 21 °C (70 °F).

paragraph_text: Another example was the Met Office who, in 1962, started publishing temperatures in both Celsius and Fahrenheit, dropping the use of Fahrenheit from their official reports in 1970.

paragraph_text: Lo-Fi is an American country band formed in Nashville, TN in 2013. led by singer/songwriter, Jamie Teachenor(vocals, piano, keyboards) and songwriter & producer, Joe West (guitars, vocals). Teachenor and West have both been independently successful in the music business, working with artists such as Justin Timberlake, Keith Urban, Luke Bryan, P. Diddy, Steve Earle, Trisha Yearwood, Tim McGraw, Emmylou Harris, Blake Shelton, Shakira, and many more, with combined sales of over 20 million albums. Their first public performance as Lo-Fi was on May 7, 2013, at the Historic Ryman Auditorium, as part of the sold out show, "Honor Thy Song", honoring late Nashville singer-songwriter and producer, Tim Johnson.

paragraph_text: Hyderabad has a tropical wet and dry climate (Köppen Aw) bordering on a hot semi-arid climate (Köppen BSh). The annual mean temperature is 26.6 °C (79.9 °F); monthly mean temperatures are 21–33 °C (70–91 °F). Summers (March–June) are hot and humid, with average highs in the mid-to-high 30s Celsius; maximum temperatures often exceed 40 °C (104 °F) between April and June. The coolest temperatures occur in December and January, when the lowest temperature occasionally dips to 10 °C (50 °F). May is the hottest month, when daily temperatures range from 26 to 39 °C (79–102 °F); December, the coldest, has temperatures varying from 14.5 to 28 °C (57–82 °F).

paragraph_text: The William R. Snodgrass Tennessee Tower (also known as the Tennessee Tower) is a skyscraper in downtown Nashville, Tennessee, that houses Tennessee government offices. The tower was built for the National Life and Accident Insurance Company and served as its National Life Center until the State of Tennessee acquired it on January 3, 1994. More than 1,000 state employees who had been assigned to numerous locations now work in the building.

paragraph_text: Paris has a typical Western European oceanic climate (Köppen climate classification: Cfb ) which is affected by the North Atlantic Current. The overall climate throughout the year is mild and moderately wet. Summer days are usually warm and pleasant with average temperatures hovering between 15 and 25 °C (59 and 77 °F), and a fair amount of sunshine. Each year, however, there are a few days where the temperature rises above 32 °C (90 °F). Some years have even witnessed long periods of harsh summer weather, such as the heat wave of 2003 when temperatures exceeded 30 °C (86 °F) for weeks, surged up to 40 °C (104 °F) on some days and seldom cooled down at night. More recently, the average temperature for July 2011 was 17.6 °C (63.7 °F), with an average minimum temperature of 12.9 °C (55.2 °F) and an average maximum temperature of 23.7 °C (74.7 °F).

paragraph_text: Bethlehem has a Mediterranean climate, with hot and dry summers and mild, wetter winters. Winter temperatures (mid-December to mid-March) can be cool and rainy. January is the coldest month, with temperatures ranging from 1 to 13 degree Celsius (33–55 °F). From May through September, the weather is warm and sunny. August is the hottest month, with a high of 30 degrees Celsius (86 °F). Bethlehem receives an average of 700 millimeters (28 in) of rainfall annually, 70% between November and January.Bethlehem's average annual relative humidity is 60% and reaches its highest rates between January and February. Humidity levels are at their lowest in May. Night dew may occur in up to 180 days per year. The city is influenced by the Mediterranean Sea breeze that occurs around mid-day. However, Bethlehem is affected also by annual waves of hot, dry, sandy and dust Khamaseen winds from the Arabian Desert, during April, May and mid-June.

paragraph_text: The island covers an area of 25 square kilometres (2,500 ha). The eastern side is wetter than the western. Although the climate is essentially arid, the rainfall does average 1000 mm annually, but with considerable variation over the terrain. Summer is from May to November, which is also the rainy season. Winter from December to April is the dry season. Sunshine is very prominent for nearly the entire year and even during the rainy season. Humidity, however, is not very high due to the winds. The average temperature is around 25 °C with day temperatures rising to 32 °C. The average high and low temperatures in January are 28 °C and 22 °C, respectively, while in July they are 30 °C and 24 °C. The lowest night temperature recorded is 13 °C. The Caribbean sea waters in the vicinity generally maintain a temperature of about 27 °C.

paragraph_text: Being located on the Atlantic coastline, Galicia has a very mild climate for the latitude and the marine influence affects most of the province to various degrees. In comparison to similar latitudes on the other side of the Atlantic, winters are exceptionally mild, with consistently heavy rainfall. Snow is rare due to temperatures rarely dropping below freezing. The warmest coastal station of Pontevedra has a yearly mean temperature of 14.8 °C (58.6 °F). Ourense located somewhat inland is only slightly warmer with 14.9 °C (58.8 °F). Due to its exposed north-westerly location, the climate is still very cool by Spanish standards. In coastal areas summers are temperered, averaging around 25 °C (77 °F) in Vigo. Temperatures are further cooler in A Coruña, with a subdued 22.8 °C (73.0 °F) normal. Temperatures do however soar in inland areas such as Ourense, where days above 30 °C (86 °F) are very regular.

Question: What is the average high temperature in Celsius during the summer in the state whose capital is where the band Lo-Fi formed?
Answer: 32