Instruct: Given a question, retrieve documents that can help answer the question.
Query: What is the average summer temperature in Mecca?
Mecca features a hot desert climate. Mecca retains its hot temperature in winter, which can range from 18°C (64°F) at night to 30°C (86°F) in the day. Summer temperatures are extremely hot, often being over 40°C (104°F) during the day, dropping to 30°C (86°F) at night.[1] Rain usually falls in Mecca in small amounts between November and January. The rainfall, as scant as it is, also presents the threat of flooding and has been a danger since the earliest times. According to Al-Kurdī, there had been 89 historic floods by 1965, including several in the period. In the last century the most severe one occurred in 1942. Since then, dams have been constructed to ameliorate the problem.
Red Lake Reservation has extreme climate conditions. Winters are long and cold, while summers are short and warm. During the winter months of December, January, and February, the average low temperatures at Red Lake are 0, -8, and -3. Average high temperatures for the same winter months at Red Lake are 19, 13, and 20. Average high temperatures for the summer months of June, July, and August at Red Lake are 73, 78, and 76. Average low temperatures for the same summer months at Red Lake are 51, 57, and 54.
Compared to other places on a similar latitude (paticularly those in the northern hemisphere), there are relatively small variations in temperature between summer and winter, as well as relatively small temperature variations throughout the day. This is due to the proximity and influence of the surrounding ocean curtailing any extremes in temperature. Air temperatures below and above are rare, both being recorded on average only once every 2 years. The maximum recorded temperature is and minimum . Average summer daily maximum & minimum temperatures are around and . Humidity in summer can at times be oppressive and tropical-like with Dew Point temperatures often exceeding and approaching . Average winter daily maximum & minimum temperatures are around and . Mean annual temperature is .
The Kopet-Dag mountain range is about 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 . Nighttimes in the summer are warm, with an average minimum temperature in July of . The average January high temperature is , and the average low temperature is . The highest temperature ever recorded in Ashgabat is , recorded in June 2015. A low temperature of was recorded in January 1969. Snow is infrequent in the area. Annual precipitation is only ; March and April are the wettest months, and summer drought, from late June to September, is virtually absolute.
Scotland occupies the cooler northern section of Great Britain, so temperatures are generally lower than in the rest of the British Isles, with the coldest ever UK temperature of recorded at Braemar in the Grampian Mountains, on 10 January 1982 and also at Altnaharra, Highland, on 30 December 1995. Winters in Scotland have an average low of around , with summer maximum temperatures averaging . In general, the western coastal areas of Scotland are warmer than the east and inland areas, due to the influence of the Atlantic currents, and the colder surface temperatures of the North Sea. The highest official temperature recorded was at Greycrook, on 9 August 2003.
For the last 100 years, the coldest winter was in 1963 (average temperature ) and the mildest was in 1989 (average ). The warmest summer was in 2003 (average ) and the coolest was in 1922 (average ). Since 1991, only five winters and four summers have been below average warmth (referring to the period 1971 – 2000).
Bad River Reservation has extreme climate conditions. Winters are long and cold, while summers are short and warm. The climate is largely affected by Lake Superior. Low temperatures during the cold winter months tend to average slightly above . High temperatures during the cold winter months average above . Average low temperatures during the summer months are near . Average high temperatures during the summer months are between . Precipitation is significant as a result of the extensive forest and Lake Superior. Average yearly precipitation is around .
The climate of Vakilan Wala varies to extreme limits. Summer temperature reaches 50° Celsius and winter temperature dips just around 0° Celsius. The average annual rainfall is only . Average maximum temperature in summer is 41.2 °C and average minimum temperature in winter is 6 °C.
The climate of Khmelnytskyi is moderately continental. The average temperature of Khmelnytskyi in its warmest month (July) is , and the average temperature in the coldest month (January) is . The maximum temperatures in the summer on average reaches , and the minimum temperatures in the winter on average is . Khmelnytskyi's average annual temperature is . Khmelnytskyi's average annual precipitation is .
In Dashkasan locale the temperature changes from -5 C to -20 C in winter and from +20 C to +35 C in summer. The average annual temperature is 0-100 in Dashkaran. The average monthly temperature in January is -2-140, the average monthly temperature of July is + 5-200. Sometimes the absolute maximum temperature of air is higher than + 20-310, the absolute minimum temperature of air is lower than 20-300 in summer. In the middle mountain range, the average absolute minimum air temperature changes from +50 to +70 during the year. The average annual soil surface temperature is + 80, the average temperature of January is -50, the average monthly July temperature is 210. The average annual relative humidity of the air is 75% and changes between 67-82% per year. The annual rainfalls in the area are 600-900 mm. Most of the rainfalls fall in the spring. The possible evaporation is  300-800 mm from the soil surface in a year.
Mecca features a hot desert climate. Like most Saudi Arabian cities, Mecca retains warm to hot temperatures even in winter, which can range from at night to in the afternoon. Summer temperatures are extremely hot and consistently break the mark in the afternoon, dropping to in the evening. Rain usually falls in Mecca in small amounts scattered between November and January.
Mecca houses Al-Haram Mosque, the largest mosque in the world. The mosque surrounds the Kaaba, which Muslims turn towards while offering daily prayer. This mosque is also commonly known as the "Ḥaram" or "Grand Mosque".
The average yearly temperature is around during the day and at night. In the coldest months: January, February and December, the average temperature is during the day and at night. In the warmest month – July and August – the average temperature is during the day and at night. Generally, a typical summer season lasts about 4 to 6 months, from May/June to September/October. The daily temperature range is limited, with an average range of about between high and low temperatures. Rain occurs mainly in autumn, the summers being generally dry. Sunshine hours total above 2,097 per year, from an average 4 hours of sunshine duration per day in winter to average 9 hours in summer. Savona usually sees snow once or twice per year.
Savona is twinned with:
Gold Beach has cool, very wet winters and mild, relatively dry summers. According to the Köppen climate classification system, Gold Beach has a warm-summer Mediterranean climate ("Csb"). Between 1948 and 2014, the average maximum temperature in January was about , and the average minimum was about . The corresponding averages for July were and . Annually, there are high temperatures of on an average of only 0.1 days and there are low temperatures of or lower on an average of 9.2 days. The record high temperature was on September 10, 1973. The record low temperature was on January 21, 1962.
Because of its location in the Alaska Panhandle, Haines has a hemiboreal continental (Köppen "Dfb") climate, with Oceanic characteristics. Winters are mild by Alaskan standards, with an average January high temperature around , and the average low around . Summers are cool to mild, with an average July high temperature of , and an average low temperature of . Various days in the summer surpass . The highest recorded temperature in Haines is on July 31, 1976. The record low temperature in the city is on January 3, 1998.
Owing to its elevation of almost , Payson has what is classified as a Mediterranean climate (Köppen "Csa"), though atypical for this climate with its early-summer drought and late-summer rainfall. While average temperatures do reach the high 80s to mid 90s in summer, the town’s altitude usually keeps it protected from the + temperatures usually found at Arizona’s lower elevations. Monsoon storms often develop in the later afternoon, bring heavy rainfall to the area and also lower the temperature. Summer nights cool down into the 50s.
With its hot, humid summers and cool winters, Denton's climate is characterized as humid subtropical and is within USDA hardiness zone 8a. The city's all-time high temperature is , recorded in 1954. Dry winds affect the area in the summer and can bring temperatures of over , although the average summer temperature highs range from between June and August. The all-time recorded low is , and the coolest month is January, with daily low temperatures averaging . Denton lies on the southern end of what is commonly referred to as "Tornado Alley"; the National Weather Service occasionally issues tornado watches, although tornadoes rarely form in the city. The city receives about of rain per year. Flash floods and severe thunderstorms are frequent occurrences during spring. Average snowfall in Denton is similar to the Dallas–Fort Worth average of per year.
Its average annual temperature is during the day and at night. The average annual temperature of the sea is about . In the coldest month, January, the temperature typically ranges from during the day, at night and the average sea temperature is . In the warmest month, August, the typical temperature ranges from during the day, about at night and the average sea temperature is . Generally, the summer or "holiday" season lasts about six months, from May to October. Two months – April and November – are transitional; sometimes the temperature exceeds , with an average temperature of during the day and at night. December, January and February are the coldest months, with average temperatures around during the day and at night. Large fluctuations in temperature are rare, particularly in the summer months. Because of the proximity to the warm sea, frosts are very rare in the city of Barcelona. In fact, only 1 day in the last 30 years was recorded with a temperature under the freezing mark, . Snow is very infrequent.
Qinyang City is a warm temperate continental climate with four distinct seasons, dry and windy springs, hot and rainy summers, warm and cool nights in autumn, and cold and dry in winter. The annual average temperature is . The highest temperature is , the lowest temperature is . The seasonal temperature changes obviously. The average temperature in spring is , the average temperature in summer is , the average temperature in autumn is , and the average temperature in winter is . The annual average precipitation is , of which the winter precipitation is the least, the average precipitation is , accounting for 4.9% of the whole year; the spring precipitation is slightly more, the average precipitation is , accounting for 17.3% of the whole year, and the precipitation in autumn is more, averaging , accounting for 25.6% of the whole year; the summer precipitation is the most, the average precipitation is , accounting for 52.2% of the whole year; the annual maximum precipitation is , the minimum precipitation is , and the precipitation is concentrated in seven, eight and nine. Three months, the intensity of precipitation is large, often causing floods. The average annual frost-free period is 210 days.
The eastern parts have an average annual temperature of . Summers are hot with mean temperatures averaging between while in winter, the mean temperatures are between . Easternmost parts of the province, which borders the Chaco region are home to the highest and lowest temperatures in the province where absolute maximum temperatures can exceed while absolute minimum temperatures can reach close to owing to the accumulation of cold air that descends from the mountains. At higher altitudes, the climate is cooler with summer temperatures averaging and winter temperatures averaging . The annual temperature in the higher altitudes is at an altitude of above sea level. Within the valleys located between the mountains, temperatures are cooler with a mean annual temperature of (summers average while winters average ) in the Tafi valley.
Situated within the Colorado Desert, Mecca's climate is that of an arid desert, which experiences an average 90 degree temperature. Low temperatures can reach into the 20s. The community sits at less than 150 feet below sea level on the edge of the Salton Sea, formerly the Salton Sink.
As the city is situated at a considerable distance from the coast, the climate is tropical savanna with most rainfall from June to October.In winter there is less rainfall than in summer. In the month of May 2015, Nizamabad recorded which was highest recorded temperature in Telangana during this summer.
The temperature goes as low as while the average is during winter, while in summer the temperature rises as high as and the average is . Average annual temperature is .The average annual rainfall is 1108 mm.
Climate of Meshchera is humid continental with long, cold and snowy winters, and short, warm and rainy summers. Annual average temperature is . The coldest month is February with average temperature of . During severe winters, temperatures can go as low as . Summers are warm, sometimes hot, with average July temperature of , and in extremely hot summers temperature can rise up to .
The climate of Svalbard is dominated by its high latitude, with the average summer temperature at to and January averages at to . The North Atlantic Current moderates Svalbard's temperatures, particularly during winter, giving it up to higher winter temperature than similar latitudes in Russia and Canada. This keeps the surrounding waters open and navigable most of the year. The interior fjord areas and valleys, sheltered by the mountains, have less temperature differences than the coast, giving about lower summer temperatures and higher winter temperatures. On the south of Spitsbergen, the temperature is slightly higher than further north and west. During winter, the temperature difference between south and north is typically , while about in summer. Bear Island has average temperatures even higher than the rest of the archipelago.
In Tucuman province, the eastern parts have an average annual temperature of . Summers are hot with mean temperatures averaging between while in winter, the mean temperatures are between . Easternmost parts of the province, which borders the Chaco region are home to the highest and lowest temperatures in the province where absolute maximum temperatures can exceed while absolute minimum temperatures can reach close to owing to the accumulation of cold air that descends from the mountains. At higher altitudes, the climate is cooler with summer temperatures averaging and winter temperatures averaging . The annual temperature in the higher altitudes is between at an altitude of above sea level. Within the valleys located between the mountains, temperatures are cooler with a mean annual temperature of (summers average while winters average ) in the Tafi valley.
Similar to Perth and most of Mandurah, Madora Bay has a Mediterranean climate with hot, dry summers and cold, wet winters. During summer months (December to February), the maximum temperature averages at around 27 °C (80 °F) whilst the minimum temperature averages to be about 19 °C (66 °F). The heat during summer can be quite extreme, so it is not unusual for a couple of days to exceed 40 °C (104 °F), during this season. Winter temperatures drop substantially, when being compared to summer temperatures, as the minimum temperature averages at 9 °C (48 °F) and the maximum averages at 15 °C (59 °F). Coastal temperatures, such as Madora Bay's, are preferred over inland temperatures because after travelling only a few kilometres inland, temperatures may be up to 5 °C warmer during summer days or cooler during winter nights.
Average summer surface temperature of the Atlantic off the Cape Peninsula is in the range 10° to 13 °C. The bottom temperature may be a few degrees colder. Minimum temperature is about 8 °C and maximum about 17 °C. Average winter surface temperature of the Atlantic off the Cape Peninsula is in the range 13° to 15 °C. The bottom temperature inshore is much the same. Average winter surface temperature of False Bay is approximately 15 °C, and the bottom temperature much the same. Average summer surface temperature of False Bay is approximately 19 °C. The bottom temperature is 1° to 3 °C lower than it is in winter.