The United Kingdom straddles the higher mid-latitudes between 49° and 61°N on the western seaboard of Europe. Since the UK is always in or close to the path of the polar front jet stream, frequent changes in pressure and unsettled weather are typical. Many types of weather can be experienced in a single day.
Pershore is a market town and civil parish in the Wychavon district in Worcestershire, England, on the banks of the River Avon. At the 2011 census, the population was 7,125. The town is best known for Pershore Abbey. Pershore is situated 6 miles (10 km) west of Evesham and 6 miles (10 km) east of Upton-upon-Severn in the Vale of Evesham.
The climate of Mumbai is an extreme version of a tropical wet and dry climate with a lengthy, practically rainless dry season and a relatively short, but extremely rainy wet season due to the Southwest Monsoon and orographic influences from the nearby Western Ghats. Some suburbs are sufficiently wet to qualify as a tropical monsoon climate. Mumbai's climate can be best described as moderately hot with a high level of humidity. Its coastal nature and tropical location ensure temperatures do not fluctuate much throughout the year.
Aldergrove is a hamlet and townland sub-division in County Antrim, Northern Ireland. It is within the townland of Seacash and parish of Killead – 6 miles (9.7 km) south of Antrim and 18 miles (29 km) west of Belfast. It is part of the Borough of Antrim and Newtownabbey.
Antrim is a town and civil parish in County Antrim in the northeast of Northern Ireland, on the banks of the Six Mile Water, on the northeast shore of Lough Neagh. It had a population of 25,606 people in the 2021 Census. It is the county town of County Antrim and was the administrative centre of Antrim Borough Council until its 2015 merger with Newtownabbey Borough Council to form Antrim and Newtownabbey Borough Council. It is 22 miles (35 km) northwest of Belfast.
London is the largest urban area and capital city of the United Kingdom. It is located in the southeast of Great Britain. The London region covers an area of 1,579 square kilometres (610 sq mi), and had a population of 8.982 million in 2019 and a population density of 5,596 people per square km as of 2021. A larger area, referred to as the London Metropolitan Region or the London Metropolitan Agglomeration covers an area of 8,382 square kilometres (3,236 sq mi), and had a population of 12,653,500 and a population density of 1,510 people per square kilometre.
Boulmer is a village in Northumberland, England, on the North Sea coast east of Alnwick. It is home to RAF Boulmer. Boulmer has an independent volunteer lifeboat station.
Helen's Bay is a village on the northern coast of County Down, Northern Ireland. It is within the townland of Ballygrot, between Holywood, Crawfordsburn and Bangor. It is served by a railway station and had a population of 1,390 in the 2011 Census. It is part of the Ards and North Down Borough Council area.
The climate of Delhi is an overlap between monsoon-influenced humid subtropical and semi-arid, with high variation between summer and winter temperatures and precipitation. Delhi's version of a humid subtropical climate is markedly different from many other humid subtropical cities such as São Paulo, Houston, and Brisbane in that the city features dust storms and wildfire haze due to its semi-arid climate.
Australia's climate is governed mostly by its size and by the hot, sinking air of the subtropical high pressure belt. This moves north-west and north-east with the seasons. The climate is variable, with frequent droughts lasting several seasons, thought to be caused in part by the El Niño-Southern Oscillation. Australia has a wide variety of climates due to its large geographical size. The largest part of Australia is desert or semi-arid. Only the south-east and south-west corners have a temperate climate and moderately fertile soil. The northern part of the country has a tropical climate, varying between grasslands and desert. Australia holds many heat-related records: the continent has the hottest extended region year-round, the areas with the hottest summer climate, and the highest sunshine duration.
The climate of West Bengal is varied, with tropical savannahs in the southern portions of the state, to humid subtropical areas in the north. Temperatures vary widely, and there are five distinct seasons. The area is vulnerable to heavy rainfall, monsoons, and cyclones. There are some mountains in the area which are generally cold all year round.
Malta has a Subtropical-Mediterranean climate according to the Köppen climate classification (Csa), with very mild winters and warm to hot summers. Rain occurs mainly in winter, with summer being generally dry. According to the Troll-Paffen climate classification and the Siegmund/Frankenberg climate classification, Malta lies within the subtropical zone, being at 35ºN latitude.
The climate of Serbia is between a continental climate in the north, with cold dry winters, and warm, humid summers with well distributed rainfall patterns, and a more Mediterranean climate in the south with hot, dry summers and autumns and average relatively cool and more rainy winters with heavy mountain snowfall. Differences in elevation, proximity to the Adriatic Sea and Aegean Sea and large river basins, as well as exposure to the winds account for climate differences.
The climate of Agra features a semi-arid climate that borders on a humid subtropical climate. The city features mild winters, hot and dry summers and a monsoon season. The monsoon, though substantial in Agra, is not quite as heavy as the monsoon in other parts of India. The average monsoon rainfall during June to September is 628.6 millimeters. Agra is reputation of being one of the hottest and the coldest towns in India. In summers the city witnesses a sudden surge in temperature and at times, mercury goes beyond the 46 °C mark in addition to a very high level of humidity. During summer, the daytime temperature hovers around 46-50 °C. Nights are relatively cooler and temperature lowers to 30 °C. Winter minimum temperatures sometimes goes as low as 3 or 3.5 °C but usually hovers in the range of 6 to 8 °C.
The 2013 heatwave in the United Kingdom and Ireland was a period of unusually hot weather primarily in July 2013, with isolated warm days in June and August. A prolonged high pressure system over Britain and Ireland caused higher than average temperatures for 19 consecutive days in July, reaching 33.5 °C (92.3 °F) at Heathrow and Northolt.
Perth, the capital city of the state of Western Australia, has a Mediterranean climate, with hot, dry summers and mild, wet winters. February is the hottest month of the year, with an average high of 31.6 °C (88.9 °F), and July is the coldest month of the year, with an average low of 7.9 °C (46.2 °F). 77% of rain in Perth falls between May and September. Perth has an average of 8.8 hours of sunshine per day, which equates to around 3,200 hours of annual sunshine, and 138.7 clear days annually, making it the sunniest capital city in Australia.
The climate of Liverpool features a temperate maritime variety, with relatively mild summers, cool winters and rainfall spread fairly evenly throughout the year. Since 1867, rainfall and temperature records for the city have been kept at Bidston Observatory, as well as atmospheric pressure records since 1846. However, the site closed down in 2002, and a weather station in Crosby has been used by the Met Office since. Irregular meteorological observations have been taken in the city since at least 1768, with unbroken records extending for long periods of time. This includes observations taken at the Liverpool Dock from 1768 to 1798, an unspecified location from 1772 to 1799 and West Derby from 1830 to 1859 and at other unspecified locations in the city from at least 1860 onward. Continuous observations in different areas of the city have been taken since 1830. In modern times, there have also been other stations to operate in the Liverpool area, including stations at West Kirby (1912–1979), Aigburth (1967–1994), and Liverpool John Lennon Airport (1946–present).
The climate of Nottingham features a temperate maritime climate with relatively mild summers, cool winters and abundant rainfall throughout the year. Since 1960, rainfall and temperature records for the city have been kept at the Nottingham Weather Centre in Watnall. There is also another weather station operating at the University of Nottingham's agricultural campus in Sutton Bonington.
The 2021 Britain and Ireland heat wave was a period of unusually hot weather in July 2021 that led to record-breaking temperatures in the UK and Ireland.
