The table below lists the Finnish Meteorological Institute's data on annual extreme temperatures in Finland since 1961. [1]
Year | Location | Temperature °C (°F) | Date |
---|---|---|---|
1961 | Kemi-Tornio Airport | 30.8 °C (87.4 °F) | July 14 |
1962 | Kronoby | 26.0 °C (78.8 °F) | June 20 |
1963 | Utti | 32.8 °C (91.0 °F) | August 2 |
1964 | Kronoby | 31.0 °C (87.8 °F) | June 15 |
1965 | Utti | 29.0 °C (84.2 °F) | July 21 |
1966 | Varkaus Käpykangas | 32.0 °C (89.6 °F) | June 20 |
1967 | Utti | 31.2 °C (88.2 °F) | August 3 |
1968 | Lahti Laune | 30.4 °C (86.7 °F) | June 19 |
1969 | Naantali | 31.5 °C (88.7 °F) | August 1 |
1970 | Kemi-Tornio Airport | 32.9 °C (91.2 °F) | July 20 |
1971 | Hattula Leteensuo | 29.3 °C (84.7 °F) | July 6 |
1972 | Outokumpu | 33.6 °C (92.5 °F) | July 8 |
1973 | Anjalankoski Anjala | 32.5 °C (90.5 °F) | July 6 |
1974 | Utsjoki Kevo | 32.8 °C (91.0 °F) | June 18 |
1975 | Ruotsinpyhtää Keitala | 32.0 °C (89.6 °F) | August 8 |
1976 | Muhos kk Laitasaari | 27.0 °C (80.6 °F) | August 14 |
1977 | Kankaanpää Niinisalo | 32.5 °C (90.5 °F) | June 15 |
1978 | Kuopio Inkilänmäki | 29.6 °C (85.3 °F) | August 1 |
1979 | Tuusula Hyrylä | 30.5 °C (86.9 °F) | June 8 |
1980 | Lapinjärvi Ingermanninkylä | 31.5 °C (88.7 °F) | July 31 |
1981 | Kotka Sunila | 29.6 °C (85.3 °F) | July 10 |
1982 | Ylistaro Pelma | 30.2 °C (86.4 °F) | July 16 |
1983 | Kotka Sunila | 32.3 °C (90.1 °F) | July 10 |
1984 | Utti | 29.1 °C (84.4 °F) | May 17 |
1985 | Lappeenranta | 30.4 °C (86.7 °F) | August 10 |
1986 | Lapinjärvi Ingermanninkylä | 31.5 °C (88.7 °F) | June 27 |
1987 | Utsjoki Kevo | 30.0 °C (86.0 °F) | July 20 |
1988 | Utsjoki Kevo | 32.9 °C (91.2 °F) | July 20 |
1989 | Lapinjärvi Ingermanninkylä | 31.1 °C (88.0 °F) | July 9 |
1990 | Utsjoki Kevo | 29.2 °C (84.6 °F) | June 25 |
1991 | Lapinjärvi Ingermanninkylä | 30.0 °C (86.0 °F) | July 31 |
1992 | Vihti Maasoja | 33.2 °C (91.8 °F) | July 17 |
1993 | Lapinjärvi Ingermanninkylä | 30.0 °C (86.0 °F) | May 20 |
1994 | Jyväskylä | 33.3 °C (91.9 °F) | July 28 |
1995 | Ylämaa Ylijärvi | 31.2 °C (88.2 °F) | June 15 |
1996 | Utti | 28.2 °C (82.8 °F) | August 21 |
1997 | Kauhava lentokenttä | 31.5 °C (88.7 °F) | July 1 |
1998 | Joensuu | 32.0 °C (89.6 °F) | June 16 |
1999 | Joensuu, Vieremä Kaarakkala | 32.5 °C (90.5 °F) | July 16 |
2000 | Inari Sevettijärvi | 32.4 °C (90.3 °F) | July 19 |
2001 | Savonlinna Ruunavuori | 31.9 °C (89.4 °F) | July 18 |
2002 | Pori | 30.0 °C (86.0 °F) | August 13 |
2003 | Mietoinen Saari | 33.3 °C (91.9 °F) | July 15 |
2004 | Inari Sevettijärvi | 29.8 °C (85.6 °F) | July 3 |
2005 | Inari Sevettijärvi | 30.8 °C (87.4 °F) | July 9 |
2006 | Lammi Evo | 32.1 °C (89.8 °F) | July 8 |
2007 | Parikkala Koitsanlahti | 30.7 °C (87.3 °F) | August 14 |
2008 | Salo Kiikala airport | 29.7 °C (85.5 °F) | June 6 |
2009 | Jämsä (Halli ) Lentoasemantie | 29.8 °C (85.6 °F) | July 4 |
2010 | Joensuu Airport | 37.2 °C (99.0 °F) | July 29 [2] |
2011 | Ylitornio Meltosjärvi | 32.8 °C (91.0 °F) | June 10 |
2012 | Lieksa Lampela | 31.0 °C (87.8 °F) | July 30 |
2013 | Liperi Tuiskavanluoto | 32.4 °C (90.3 °F) | June 26 |
2014 | Pori Railway Station | 32.8 °C (91.0 °F) | August 4 |
2015 | Kouvola Utti Lentoportintie | 33.3 °C (91.9 °F) | July 2 |
2016 | Utsjoki Kevo | 29.1 °C (84.4 °F) | July 23 |
2017 | Utsjoki Kevo | 27.6 °C (81.7 °F) | July 28 |
2018 | Vaasa Klemettilä | 33.7 °C (92.7 °F) | July 18 |
2019 | Porvoo Emäsalo | 33.7 °C (92.7 °F) | July 28 [3] |
2020 | Kankaanpää Niinisalo | 33.5 °C (92.3 °F) | June 25 |
2021 | Heinola Asemantaus | 34.0 °C (93.2 °F) | July 15 |
2022 | Utsjoki | 32.5 °C (90.5 °F) | June 29 [4] |
2023 | Rauma Pyynpää | 33.6 °C (92.5 °F) | August 7 |
2024 | Asemantaus Heinola | 31.4 °C (88.5 °F) | June 28 |
Year | Location | Temperature °C (°F) | Date |
---|---|---|---|
1961 | Sodankylä Vuotso | −41.2 °C (−42.2 °F) | February 6 |
1962 | Inari /Ivalo | −41.4 °C (−42.5 °F) | January 24 |
1963 | Sodankylä Vuotso | −43.2 °C (−45.8 °F) | December 19 |
1964 | Sodankylä Lokka | −40.4 °C (−40.7 °F) | January 26 |
1965 | Enontekiö Kalmankaltio | −40.3 °C (−40.5 °F) | January 11 |
1966 | Inari/Ivalo | −48.6 °C (−55.5 °F) | February 1 |
1967 | Enontekiö Kilpisjärvi | −44.2 °C (−47.6 °F) | January 27 |
1968 | Alajärvi Möksy | −42.0 °C (−43.6 °F) | January 12 |
1969 | Taivalkoski kk | −41.6 °C (−42.9 °F) | February 5 |
1970 | Utsjoki Kevo | −43.2 °C (−45.8 °F) | February 16 |
1971 | Salla Tuntsa | −46.0 °C (−50.8 °F) | February 28 |
1972 | Salla Tuntsa | −39.7 °C (−39.5 °F) | March 10 |
1973 | Kittilä Kaukonen | −40.3 °C (−40.5 °F) | December 8 |
1974 | Kittilä Pokka | −37.7 °C (−35.9 °F) | January 29 |
1975 | Salla Naruskajärvi | −40.2 °C (−40.4 °F) | February 18 |
1976 | Salla Naruskajärvi | −44.2 °C (−47.6 °F) | February 1 |
1977 | Kittilä Pokka | −44.5 °C (−48.1 °F) | January 23 |
1978 | Salla Naruskajärvi | −45.5 °C (−49.9 °F) | January 27 |
1979 | Salla Naruskajärvi | −43.2 °C (−45.8 °F) | February 13 |
1980 | Salla Naruskajärvi | −43.3 °C (−45.9 °F) | January 26 |
1981 | Kittilä Pokka | −42.8 °C (−45.0 °F) | March 12 |
1982 | Salla Naruskajärvi | −43.5 °C (−46.3 °F) | January 1 |
1983 | Salla Naruskajärvi | −40.1 °C (−40.2 °F) | December 10 |
1984 | Kittilä Pokka | −39.1 °C (−38.4 °F) | January 25 |
1985 | Salla Naruskajärvi | −50.4 °C (−58.7 °F) | January 6 |
1986 | Muonio kk Alamuonio | −41.9 °C (−43.4 °F) | December 20 |
1987 | Salla Naruskajärvi | −45.5 °C (−49.9 °F) | January 8 |
1988 | Salla Naruskajärvi | −41.4 °C (−42.5 °F) | December 22 |
1989 | Kuusamo Kiutaköngäs | −37.4 °C (−35.3 °F) | January 1 |
1990 | Inari/Ivalo | −40.6 °C (−41.1 °F) | January 11 |
1991 | Salla Naruska | −38.5 °C (−37.3 °F) | January 29 |
1992 | Utsjoki Kevo | −35.3 °C (−31.5 °F) | January 10 |
1993 | Utsjoki Kevo, Kittilä Pulju and Pokka | −37.2 °C (−35.0 °F) | January 15 and 20 |
1994 | Salla Naruska | −41.1 °C (−42.0 °F) | February 11 |
1995 | Kittilä Pokka | −42.0 °C (−43.6 °F) | December 29 |
1996 | Sodankylä Lisma Aapa | −37.0 °C (−34.6 °F) | January 6 |
1997 | Kuusamo Kiutaköngäs | −41.4 °C (−42.5 °F) | February 10 |
1998 | Sodankylä Lokka | −43.1 °C (−45.6 °F) | February 17 |
1999 | Kittilä Pokka | −51.5 °C (−60.7 °F) | January 28 [5] |
2000 | Kuusamo Kiutaköngäs | −36.5 °C (−33.7 °F) | December 27 |
2001 | Pyhäjärvi Ol. Ojakylä | −42.5 °C (−44.5 °F) | February 8 |
2002 | Taivalkoski Fire Station | −40.7 °C (−41.3 °F) | December 31 |
2003 | Kuusamo Kiutaköngäs | −41.9 °C (−43.4 °F) | January 7 |
2004 | Salla Naruska | −38.7 °C (−37.7 °F) | February 11 |
2005 | Salla Naruska | −36.5 °C (−33.7 °F) | January 29 |
2006 | Kittilä Pokka | −43.6 °C (−46.5 °F) | January 20 |
2007 | Salla Naruska | −39.9 °C (−39.8 °F) | February 6 |
2008 | Kittilä Pokka | −33.7 °C (−28.7 °F) | February 24 |
2009 | Inari Sevettijärvi | −37.6 °C (−35.7 °F) | February 7 |
2010 | Kuhmo Kalliojoki | −41.3 °C (−42.3 °F) | February 20 |
2011 | Salla Naruska | −41.8 °C (−43.2 °F) | February 18 |
2012 | Inari Kaamanen | −42.7 °C (−44.9 °F) | February 6 |
2013 | Sodankylä Vuotso | −39.7 °C (−39.5 °F) | December 9 |
2014 | Utsjoki Kevojärvi | −40.7 °C (−41.3 °F) | January 20 |
2015 | Utsjoki Kevojärvi | −39.6 °C (−39.3 °F) | January 11 |
2016 | Muonio Kirkonkylä | −41.2 °C (−42.2 °F) | January 7 |
2017 | Muonio Kirkonkylä | −41.7 °C (−43.1 °F) | January 5 |
2018 | Utsjoki Kevo Kevojärvi | −37.1 °C (−34.8 °F) | February 4 |
2019 | Utsjoki Kevo Kevojärvi | −39.1 °C (−38.4 °F) | February 5 |
2020 | Utsjoki Kevo Kevojärvi | −41.1 °C (−42.0 °F) | December 27 |
2021 | Utsjoki Kevo Kevojärvi | −39.7 °C (−39.5 °F) | February 20 |
2022 | Enontekiö Airport | −35.7 °C (−32.3 °F) | January 8 |
2023 | Kittilä Airport | −37.5 °C (−35.5 °F) | March 24 |
2024 | Enontekiö Airport | −44.3 °C (−47.7 °F) | January 5 |
Climate is the long-term weather pattern in a region, typically averaged over 30 years. More rigorously, it is the mean and variability of meteorological variables over a time spanning from months to millions of years. Some of the meteorological variables that are commonly measured are temperature, humidity, atmospheric pressure, wind, and precipitation. In a broader sense, climate is the state of the components of the climate system, including the atmosphere, hydrosphere, cryosphere, lithosphere and biosphere and the interactions between them. The climate of a location is affected by its latitude, longitude, terrain, altitude, land use and nearby water bodies and their currents.
Hail is a form of solid precipitation. It is distinct from ice pellets, though the two are often confused. It consists of balls or irregular lumps of ice, each of which is called a hailstone. Ice pellets generally fall in cold weather, while hail growth is greatly inhibited during low surface temperatures.
A tornado is a violently rotating column of air that is in contact with both the surface of the Earth and a cumulonimbus cloud or, in rare cases, the base of a cumulus cloud. It is often referred to as a twister, whirlwind or cyclone, although the word cyclone is used in meteorology to name a weather system with a low-pressure area in the center around which, from an observer looking down toward the surface of the Earth, winds blow counterclockwise in the Northern Hemisphere and clockwise in the Southern. Tornadoes come in many shapes and sizes, and they are often visible in the form of a condensation funnel originating from the base of a cumulonimbus cloud, with a cloud of rotating debris and dust beneath it. Most tornadoes have wind speeds less than 180 kilometers per hour, are about 80 meters across, and travel several kilometers before dissipating. The most extreme tornadoes can attain wind speeds of more than 480 kilometers per hour (300 mph), can be more than 3 kilometers (2 mi) in diameter, and can stay on the ground for more than 100 km (62 mi).
Extreme weather includes unexpected, unusual, severe, or unseasonal weather; weather at the extremes of the historical distribution—the range that has been seen in the past. Extreme events are based on a location's recorded weather history. They are defined as lying in the most unusual ten percent. The main types of extreme weather include heat waves, cold waves and heavy precipitation or storm events, such as tropical cyclones. The effects of extreme weather events are economic costs, loss of human lives, droughts, floods, landslides. Severe weather is a particular type of extreme weather which poses risks to life and property.
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls from clouds due to gravitational pull. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation; their water vapor does not condense sufficiently to precipitate, so fog and mist do not fall. Two processes, possibly acting together, can lead to air becoming saturated with water vapor: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers.
This article lists various tornado records. The most "extreme" tornado in recorded history was the Tri-State tornado, which spread through parts of Missouri, Illinois, and Indiana on March 18, 1925. It is considered an F5 on the Fujita Scale, holds records for longest path length at 219 miles (352 km) and longest duration at about 3+1⁄2 hours, and held the fastest forward speed for a significant tornado at 73 mph (117 km/h) anywhere on Earth until 2021. In addition, it is the deadliest single tornado in United States history with 695 fatalities. It was also the second costliest tornado in history at the time, and when costs are normalized for wealth and inflation, it still ranks third today.
In meteorology, a low-pressure area, low area or low is a region where the atmospheric pressure is lower than that of surrounding locations. Low-pressure areas are commonly associated with inclement weather, while high-pressure areas are associated with lighter winds and clear skies. Winds circle anti-clockwise around lows in the northern hemisphere, and clockwise in the southern hemisphere, due to opposing Coriolis forces. Low-pressure systems form under areas of wind divergence that occur in the upper levels of the atmosphere (aloft). The formation process of a low-pressure area is known as cyclogenesis. In meteorology, atmospheric divergence aloft occurs in two kinds of places:
An outflow boundary, also known as a gust front, is a storm-scale or mesoscale boundary separating thunderstorm-cooled air (outflow) from the surrounding air; similar in effect to a cold front, with passage marked by a wind shift and usually a drop in temperature and a related pressure jump. Outflow boundaries can persist for 24 hours or more after the thunderstorms that generated them dissipate, and can travel hundreds of kilometers from their area of origin. New thunderstorms often develop along outflow boundaries, especially near the point of intersection with another boundary. Outflow boundaries can be seen either as fine lines on weather radar imagery or else as arcs of low clouds on weather satellite imagery. From the ground, outflow boundaries can be co-located with the appearance of roll clouds and shelf clouds.
Extratropical cyclones, sometimes called mid-latitude cyclones or wave cyclones, are low-pressure areas which, along with the anticyclones of high-pressure areas, drive the weather over much of the Earth. Extratropical cyclones are capable of producing anything from cloudiness and mild showers to severe hail, thunderstorms, blizzards, and tornadoes. These types of cyclones are defined as large scale (synoptic) low pressure weather systems that occur in the middle latitudes of the Earth. In contrast with tropical cyclones, extratropical cyclones produce rapid changes in temperature and dew point along broad lines, called weather fronts, about the center of the cyclone.
Natural calamities in India, many of them related to the climate of India, causes of the massive losses of life and property. Droughts, flash floods, cyclones, avalanches, landslides brought by torrential rains, and snowstorms pose the greatest threats. A natural disaster might be caused by earthquakes, flooding, volcanic eruption, landslides, hurricanes etc. In order to be classified as a disaster, it will need to have a profound environmental effect and/or human loss and frequently incurs a financial loss. Other dangers include frequent summer dust storms, which usually track from north to south; they cause extensive property damage in North India and deposit large amounts of dust and dirt from arid regions. Hail is also common in parts of India, causing severe damage to standing crops such as rice and wheat and many more crops and effects many people.
Warming stripes are data visualization graphics that use a series of coloured stripes chronologically ordered to visually portray long-term temperature trends. Warming stripes reflect a "minimalist" style, conceived to use colour alone to avoid technical distractions to intuitively convey global warming trends to non-scientists.