Weather is the state of the atmosphere, describing for example the degree to which it is hot or cold, wet or dry, calm or stormy, clear or cloudy. On Earth, most weather phenomena occur in the lowest layer of the planet's atmosphere, the troposphere, just below the stratosphere. Weather refers to day-to-day temperature, precipitation, and other atmospheric conditions, whereas climate is the term for the averaging of atmospheric conditions over longer periods of time. When used without qualification, "weather" is generally understood to mean the weather of Earth.
Weather is driven by air pressure, temperature, and moisture differences between one place and another. These differences can occur due to the Sun's angle at any particular spot, which varies with latitude. The strong temperature contrast between polar and tropical air gives rise to the largest scale atmospheric circulations: the Hadley cell, the Ferrel cell, the polar cell, and the jet stream. Weather systems in the middle latitudes, such as extratropical cyclones, are caused by instabilities of the jet streamflow. Because Earth's axis is tilted relative to its orbital plane (called the ecliptic), sunlight is incident at different angles at different times of the year. On Earth's surface, temperatures usually range ±40 °C (−40 °F to 104 °F) annually. Over thousands of years, changes in Earth's orbit can affect the amount and distribution of solar energy received by Earth, thus influencing long-term climate and global climate change.
Surface temperature differences in turn cause pressure differences. Higher altitudes are cooler than lower altitudes, as most atmospheric heating is due to contact with the Earth's surface while radiative losses to space are mostly constant. Weather forecasting is the application of science and technology to predict the state of the atmosphere for a future time and a given location. Earth's weather system is a chaotic system; as a result, small changes to one part of the system can grow to have large effects on the system as a whole. Human attempts to control the weather have occurred throughout history, and there is evidence that human activities such as agriculture and industry have modified weather patterns
Studying how the weather works on other planets has been helpful in understanding how weather works on Earth. A famous landmark in the Solar System, Jupiter's Great Red Spot, is an anticyclonic storm known to have existed for at least 300 years. However, the weather is not limited to planetary bodies. A star's corona is constantly being lost to space, creating what is essentially a very thin atmosphere throughout the Solar System. The movement of mass ejected from the Sun is known as the solar wind.
On Earth, the common weather phenomena include wind, cloud, rain, snow, fog and dust storms. Less common events include natural disasters such as tornadoes, hurricanes, typhoons and ice storms. Almost all familiar weather phenomena occur in the troposphere (the lower part of the atmosphere). Weather does occur in the stratosphere and can affect weather lower down in the troposphere, but the exact mechanisms are poorly understood.
Weather occurs primarily due to air pressure, temperature and moisture differences between one place to another. These differences can occur due to the sun angle at any particular spot, which varies by latitude from the tropics. In other words, the farther from the tropics one lies, the lower the sun angle is, which causes those locations to be cooler due to the spread of the sunlight over a greater surface. The strong temperature contrast between polar and tropical air gives rise to the large scale atmospheric circulation cells and the jet stream. Weather systems in the mid-latitudes, such as extratropical cyclones, are caused by instabilities of the jet stream flow (see baroclinity). Weather systems in the tropics, such as monsoons or organized thunderstorm systems, are caused by different processes.
Because the Earth's axis is tilted relative to its orbital plane, sunlight is incident at different angles at different times of the year. In June the Northern Hemisphere is tilted towards the sun, so at any given Northern Hemisphere latitude sunlight falls more directly on that spot than in December (see Effect of sun angle on climate). This effect causes seasons. Over thousands to hundreds of thousands of years, changes in Earth's orbital parameters affect the amount and distribution of solar energy received by the Earth and influence long-term climate. (See Milankovitch cycles).
The uneven solar heating (the formation of zones of temperature and moisture gradients, or frontogenesis) can also be due to the weather itself in the form of cloudiness and precipitation. Higher altitudes are typically cooler than lower altitudes, which the result of higher surface temperature and radiational heating, which produces the adiabatic lapse rate. In some situations, the temperature actually increases with height. This phenomenon is known as an inversion and can cause mountaintops to be warmer than the valleys below. Inversions can lead to the formation of fog and often act as a cap that suppresses thunderstorm development. On local scales, temperature differences can occur because different surfaces (such as oceans, forests, ice sheets, or man-made objects) have differing physical characteristics such as reflectivity, roughness, or moisture content.
Surface temperature differences in turn cause pressure differences. A hot surface warms the air above it causing it to expand and lower the density and the resulting surface air pressure. The resulting horizontal pressure gradient moves the air from higher to lower pressure regions, creating a wind, and the Earth's rotation then causes deflection of this airflow due to the Coriolis effect. The simple systems thus formed can then display emergent behaviour to produce more complex systems and thus other weather phenomena. Large scale examples include the Hadley cell while a smaller scale example would be coastal breezes.
The atmosphere is a chaotic system. As a result, small changes to one part of the system can accumulate and magnify to cause large effects on the system as a whole. This atmospheric instability makes weather forecasting less predictable than tides or eclipses. Although it is difficult to accurately predict weather more than a few days in advance, weather forecasters are continually working to extend this limit through meteorological research and refining current methodologies in weather prediction. However, it is theoretically impossible to make useful day-to-day predictions more than about two weeks ahead, imposing an upper limit to potential for improved prediction skill.
Shaping the planet Earth
Weather is one of the fundamental processes that shape the Earth. The process of weathering breaks down the rocks and soils into smaller fragments and then into their constituent substances. During rains precipitation, the water droplets absorb and dissolve carbon dioxide from the surrounding air. This causes the rainwater to be slightly acidic, which aids the erosive properties of water. The released sediment and chemicals are then free to take part in chemical reactions that can affect the surface further (such as acid rain), and sodium and chloride ions (salt) deposited in the seas/oceans. The sediment may reform in time and by geological forces into other rocks and soils. In this way, weather plays a major role in erosion of the surface.
Effect on humans
Weather, seen from an anthropological perspective, is something all humans in the world constantly experience through their senses, at least while being outside. There are socially and scientifically constructed understandings of what weather is, what makes it change, the effect it has on humans in different situations, etc. Therefore, weather is something people often communicate about. The National Weather Service has an annual report for fatalities, injury, and total damage costs which include crop and property. They gather this data via National Weather Service offices located throughout the 50 states in the United States as well as Puerto Rico, Guam, and the Virgin Islands. As of 2019, tornadoes have had the greatest impact on humans with 42 fatalities while costing crop and property damage over 3 billion dollars.
Effects on populations
The weather has played a large and sometimes direct part in human history. Aside from climatic changes that have caused the gradual drift of populations (for example the desertification of the Middle East, and the formation of land bridges during glacial periods), extreme weather events have caused smaller scale population movements and intruded directly in historical events. One such event is the saving of Japan from invasion by the Mongol fleet of Kublai Khan by the Kamikaze winds in 1281. French claims to Florida came to an end in 1565 when a hurricane destroyed the French fleet, allowing Spain to conquer Fort Caroline. More recently, Hurricane Katrina redistributed over one million people from the central Gulf coast elsewhere across the United States, becoming the largest diaspora in the history of the United States.
The Little Ice Age caused crop failures and famines in Europe. During the period known as the Grindelwald Fluctuation (1560-1630), volcanic forcing events seem to have led to more extreme weather events. These included droughts, storms and unseasonal blizzards, as well as causing the Swiss Grindelwald Glacier to expand. The 1690s saw the worst famine in France since the Middle Ages. Finland suffered a severe famine in 1696–1697, during which about one-third of the Finnish population died.
Weather forecasting is the application of science and technology to predict the state of the atmosphere for a future time and a given location. Human beings have attempted to predict the weather informally for millennia, and formally since at least the nineteenth century. Weather forecasts are made by collecting quantitative data about the current state of the atmosphere and using scientific understanding of atmospheric processes to project how the atmosphere will evolve.
Once an all-human endeavor based mainly upon changes in barometric pressure, current weather conditions, and sky condition, forecast models are now used to determine future conditions. On the other hand, human input is still required to pick the best possible forecast model to base the forecast upon, which involve many disciplines such as pattern recognition skills, teleconnections, knowledge of model performance, and knowledge of model biases.
The chaotic nature of the atmosphere, the massive computational power required to solve the equations that describe the atmosphere, the error involved in measuring the initial conditions, and an incomplete understanding of atmospheric processes mean that forecasts become less accurate as of the difference in current time and the time for which the forecast is being made (the range of the forecast) increases. The use of ensembles and model consensus helps to narrow the error and pick the most likely outcome.
There are a variety of end users to weather forecasts. Weather warnings are important forecasts because they are used to protect life and property. Forecasts based on temperature and precipitation are important to agriculture, and therefore to commodity traders within stock markets. Temperature forecasts are used by utility companies to estimate demand over coming days.
In some areas, people use weather forecasts to determine what to wear on a given day. Since outdoor activities are severely curtailed by heavy rain, snow and the wind chill, forecasts can be used to plan activities around these events and to plan ahead to survive through them.
Tropical weather forecasting is different from that at higher latitudes. The sun shines more directly on the tropics than on higher latitudes (at least in the average over a year), which makes the tropics warm (Stevens 2011). And, the vertical direction (up, as one stands on the Earth's surface) is perpendicular to the Earth's axis of rotation at the equator, while the axis of rotation and the vertical are the same at the pole; this causes the Earth's rotation to influence the atmospheric circulation more strongly at high latitudes than low. Because of these two factors, clouds and rainstorms in the tropics can occur more spontaneously compared to those at higher latitudes, where they are more tightly controlled by larger-scale forces in the atmosphere. Because of these differences, clouds and rain are more difficult to forecast in the tropics than at higher latitudes. On the other hand, the temperature is easily forecast in the tropics, because it doesn't change much.
The aspiration to control the weather is evident throughout human history: from ancient rituals intended to bring rain for crops to the U.S. Military Operation Popeye, an attempt to disrupt supply lines by lengthening the North Vietnamese monsoon. The most successful attempts at influencing weather involve cloud seeding; they include the fog- and low stratus dispersion techniques employed by major airports, techniques used to increase winter precipitation over mountains, and techniques to suppress hail. A recent example of weather control was China's preparation for the 2008 Summer Olympic Games. China shot 1,104 rain dispersal rockets from 21 sites in the city of Beijing in an effort to keep rain away from the opening ceremony of the games on 8 August 2008. Guo Hu, head of the Beijing Municipal Meteorological Bureau (BMB), confirmed the success of the operation with 100 millimeters falling in Baoding City of Hebei Province, to the southwest and Beijing's Fangshan District recording a rainfall of 25 millimeters.
Whereas there is inconclusive evidence for these techniques' efficacy, there is extensive evidence that human activity such as agriculture and industry results in inadvertent weather modification:
- Acid rain, caused by industrial emission of sulfur dioxide and nitrogen oxides into the atmosphere, adversely affects freshwater lakes, vegetation, and structures.
- Anthropogenic pollutants reduce air quality and visibility.
- Climate change caused by human activities that emit greenhouse gases into the air is expected to affect the frequency of extreme weather events such as drought, extreme temperatures, flooding, high winds, and severe storms.
- Heat, generated by large metropolitan areas have been shown to minutely affect nearby weather, even at distances as far as 1,600 kilometres (990 mi).
The effects of inadvertent weather modification may pose serious threats to many aspects of civilization, including ecosystems, natural resources, food and fiber production, economic development, and human health.
Microscale meteorology is the study of short-lived atmospheric phenomena smaller than mesoscale, about 1 km or less. These two branches of meteorology are sometimes grouped together as "mesoscale and microscale meteorology" (MMM) and together study all phenomena smaller than synoptic scale; that is they study features generally too small to be depicted on a weather map. These include small and generally fleeting cloud "puffs" and other small cloud features.
Extremes on Earth
On Earth, temperatures usually range ±40 °C (100 °F to −40 °F) annually. The range of climates and latitudes across the planet can offer extremes of temperature outside this range. The coldest air temperature ever recorded on Earth is −89.2 °C (−128.6 °F), at Vostok Station, Antarctica on 21 July 1983. The hottest air temperature ever recorded was 57.7 °C (135.9 °F) at 'Aziziya, Libya, on 13 September 1922, but that reading is queried. The highest recorded average annual temperature was 34.4 °C (93.9 °F) at Dallol, Ethiopia. The coldest recorded average annual temperature was −55.1 °C (−67.2 °F) at Vostok Station, Antarctica.
The windiest place ever recorded is in Antarctica, Commonwealth Bay (George V Coast). Here the gales reach 199 mph (320 km/h). Furthermore, the greatest snowfall in a period of twelve months occurred in Mount Rainier, Washington, USA. It was recorded as 31,102 mm (102.04 ft) of snow.
Extraterrestrial within the Solar System
Studying how the weather works on other planets has been seen as helpful in understanding how it works on Earth. Weather on other planets follows many of the same physical principles as weather on Earth, but occurs on different scales and in atmospheres having different chemical composition. The Cassini–Huygens mission to Titan discovered clouds formed from methane or ethane which deposit rain composed of liquid methane and other organic compounds. Earth's atmosphere includes six latitudinal circulation zones, three in each hemisphere. In contrast, Jupiter's banded appearance shows many such zones, Titan has a single jet stream near the 50th parallel north latitude, and Venus has a single jet near the equator.
One of the most famous landmarks in the Solar System, Jupiter's Great Red Spot, is an anticyclonic storm known to have existed for at least 300 years. On other gas giants, the lack of a surface allows the wind to reach enormous speeds: gusts of up to 600 metres per second (about 2,100 km/h or 1,300 mph) have been measured on the planet Neptune. This has created a puzzle for planetary scientists. The weather is ultimately created by solar energy and the amount of energy received by Neptune is only about 1⁄900 of that received by Earth, yet the intensity of weather phenomena on Neptune is far greater than on Earth. The strongest planetary winds discovered so far are on the extrasolar planet HD 189733 b, which is thought to have easterly winds moving at more than 9,600 kilometres per hour (6,000 mph).
Weather is not limited to planetary bodies. Like all stars, the Sun's corona is constantly being lost to space, creating what is essentially a very thin atmosphere throughout the Solar System. The movement of mass ejected from the Sun is known as the solar wind. Inconsistencies in this wind and larger events on the surface of the star, such as coronal mass ejections, form a system that has features analogous to conventional weather systems (such as pressure and wind) and is generally known as space weather. Coronal mass ejections have been tracked as far out in the Solar System as Saturn. The activity of this system can affect planetary atmospheres and occasionally surfaces. The interaction of the solar wind with the terrestrial atmosphere can produce spectacular aurorae, and can play havoc with electrically sensitive systems such as electricity grids and radio signals.
- Merriam-Webster Dictionary. Weather. Retrieved on 27 June 2008.
- Glossary of Meteorology. Hydrosphere. Archived 15 March 2012 at the Wayback Machine Retrieved on 27 June 2008.
- "Troposphere". Glossary of Meteorology. 28 September 2012. Archived from the original on 28 September 2012. Retrieved 11 October 2020.
- "Climate". Glossary of Meteorology. American Meteorological Society. Retrieved 14 May 2008.
- O'Carroll, Cynthia M. (18 October 2001). "Weather Forecasters May Look Sky-high For Answers". Goddard Space Flight Center (NASA). Archived from the original on 12 July 2009.
- NASA. World Book at NASA: Weather. Archived copy at WebCite (10 March 2013). Retrieved on 27 June 2008.
- John P. Stimac.  Air pressure and wind. Retrieved on 8 May 2008.
- Carlyle H. Wash, Stacey H. Heikkinen, Chi-Sann Liou, and Wendell A. Nuss. A Rapid Cyclogenesis Event during GALE IOP 9. Retrieved on 28 June 2008.
- Brown, Dwayne; Cabbage, Michael; McCarthy, Leslie; Norton, Karen (20 January 2016). "NASA, NOAA Analyses Reveal Record-Shattering Global Warm Temperatures in 2015". NASA. Retrieved 21 January 2016.
- Windows to the Universe. Earth's Tilt Is the Reason for the Seasons! Archived 8 August 2007 at the Wayback Machine Retrieved on 28 June 2008.
- Milankovitch, Milutin. Canon of Insolation and the Ice Age Problem. Zavod za Udz̆benike i Nastavna Sredstva: Belgrade, 1941. ISBN 86-17-06619-9.
- Ron W. Przybylinski. The Concept of Frontogenesis and its Application to Winter Weather Forecasting. Retrieved on 28 June 2008.
- Mark Zachary Jacobson (2005). Fundamentals of Atmospheric Modeling (2nd ed.). Cambridge University Press. ISBN 978-0-521-83970-9. OCLC 243560910.
- C. Donald Ahrens (2006). Meteorology Today (8th ed.). Brooks/Cole Publishing. ISBN 978-0-495-01162-0. OCLC 224863929.
- Michel Moncuquet. Relation between density and temperature. Retrieved on 28 June 2008.
- Encyclopedia of Earth. Wind. Retrieved on 28 June 2008.
- Spencer Weart. The Discovery of Global Warming. Retrieved on 28 June 2008.
- Lorenz, Edward (July 1969). "How Much Better Can Weather Prediction Become?" (PDF). web.mit.edu/. Massachusetts Institute of Technology. Archived from the original (PDF) on 17 April 2016. Retrieved 21 July 2017.
- "The Discovery of Global Warming: Chaos in the Atmosphere". history.aip.org. January 2017. Retrieved 21 July 2017.
- NASA. NASA Mission Finds New Clues to Guide Search for Life on Mars. Retrieved on 28 June 2008.
- West Gulf River Forecast Center. Glossary of Hydrologic Terms: E Retrieved on 28 June 2008.
- Crate, Susan A; Nuttall, Mark, eds. (2009). Anthropology and Climate Change: From Encounters to Actions (PDF). Walnut Creek, CA: Left Coast Press. pp. 70–86, i.e. the chapter 'Climate and weather discourse in anthropology: from determinism to uncertain futures' by Nicholas Peterson & Kenneth Broad.
- United States. National Weather Service. Office of Climate, Water, Weather Services, & National Climatic Data Center. (2000). Weather Related Fatality and Injury Statistics.
- James P. Delgado. Relics of the Kamikaze. Retrieved on 28 June 2008.
- Mike Strong. Fort Caroline National Memorial. Archived 17 November 2012 at the Wayback Machine Retrieved on 28 June 2008.
- Anthony E. Ladd, John Marszalek, and Duane A. Gill. The Other Diaspora: New Orleans Student Evacuation Impacts and Responses Surrounding Hurricane Katrina. Archived 24 June 2008 at the Wayback Machine Retrieved on 29 March 2008.
- Jason Wolfe, Volcanoes and Climate Change, NASA, 28 July 2020). Date retrieved: 28 May 2021.
- Jones, Evan T.; Hewlett, Rose; Mackay, Anson W. (5 May 2021). "Weird weather in Bristol during the Grindelwald Fluctuation (1560–1630)". Weather. 76 (4): 104–110. Bibcode:2021Wthr...76..104J. doi:10.1002/wea.3846 – via Wiley Online Library.
- "Famine in Scotland: The 'Ill Years' of the 1690s". Karen J. Cullen (2010). Edinburgh University Press. p. 21. ISBN 0-7486-3887-3
- Eric D. Craft. An Economic History of Weather Forecasting. Archived 3 May 2007 at the Wayback Machine Retrieved on 15 April 2007.
- NASA. Weather Forecasting Through the Ages. Archived 10 September 2005 at the Wayback Machine Retrieved on 25 May 2008.
- Weather Doctor. Applying The Barometer To Weather Watching. Retrieved on 25 May 2008.
- Mark Moore. Field Forecasting: A Short Summary. Archived 25 March 2009 at the Wayback Machine Retrieved on 25 May 2008.
- Klaus Weickmann, Jeff Whitaker, Andres Roubicek and Catherine Smith. The Use of Ensemble Forecasts to Produce Improved Medium Range (3–15 days) Weather Forecasts. Archived 15 December 2007 at the Wayback Machine Retrieved on 16 February 2007.
- Todd Kimberlain. Tropical cyclone motion and intensity talk (June 2007). Retrieved on 21 July 2007.
- Richard J. Pasch, Mike Fiorino, and Chris Landsea. TPC/NHC’S REVIEW OF THE NCEP PRODUCTION SUITE FOR 2006.[permanent dead link] Retrieved on 5 May 2008.
- National Weather Service. National Weather Service Mission Statement. Archived 24 November 2013 at the Wayback Machine Retrieved on 25 May 2008.
- "National Meteorological Service of Slovenia". Archived from the original on 18 June 2012. Retrieved 25 February 2012.
- Blair Fannin. Dry weather conditions continue for Texas. Archived 3 July 2009 at the Wayback Machine Retrieved on 26 May 2008.
- Dr. Terry Mader. Drought Corn Silage. Archived 5 October 2011 at the Wayback Machine Retrieved on 26 May 2008.
- Kathryn C. Taylor. Peach Orchard Establishment and Young Tree Care. Archived 24 December 2008 at the Wayback Machine Retrieved on 26 May 2008.
- Associated Press. After Freeze, Counting Losses to Orange Crop. Retrieved on 26 May 2008.
- The New York Times. FUTURES/OPTIONS; Cold Weather Brings Surge In Prices of Heating Fuels. Retrieved on 25 May 2008.
- BBC. Heatwave causes electricity surge. Retrieved on 25 May 2008.
- Toronto Catholic Schools. The Seven Key Messages of the Energy Drill Program. Archived 17 February 2012 at the Wayback Machine Retrieved on 25 May 2008.
- "Tropical Weather | Learn Science at Scitable". www.nature.com. Retrieved 8 February 2020.
- American Meteorological Society Archived 12 June 2010 at the Wayback Machine
- Huanet, Xin (9 August 2008). "Beijing disperses rain to dry Olympic night". Chinaview. Retrieved 24 August 2008.
- Intergovernmental Panel on Climate Change
- Zhang, Guang (28 January 2012). "Cities Affect Temperatures for Thousands of Miles". ScienceDaily.
- Intergovernmental Panel on Climate Change
- Rogers, R. (1989). A Short Course in Cloud Physics. Oxford: Butterworth-Heinemann. pp. 61–62. ISBN 978-0-7506-3215-7.
- "Mean Monthly Temperature Records Across the Globe / July 2021 Global Land and Ocean". NCDC.NOAA.gov. National Climatic Data Center (NCDC) of the National Oceanographic and Atmospheric Administration (NOAA). August 2021. Archived from the original on 2 September 2021.
- Global Measured Extremes of Temperature and Precipitation. National Climatic Data Center. Retrieved on 21 June 2007.
- Glenn Elert. Hottest Temperature on Earth. Retrieved on 28 June 2008.
- Glenn Elert. Coldest Temperature On Earth. Archived 10 September 2007 at the Wayback Machine Retrieved on 28 June 2008.
- "Canadian Climate Normals 1971–2000 – Eureka". Archived from the original on 11 November 2007. Retrieved 28 June 2008.
- "Greatest snowfall in 12 months". Guinness World Records. Retrieved 11 February 2021.
- Britt, Robert Roy (6 March 2001). "The Worst Weather in the Solar System". Space.com. Archived from the original on 2 May 2001.
- M. Fulchignoni; F. Ferri; F. Angrilli; A. Bar-Nun; M.A. Barucci; G. Bianchini; et al. (2002). "The Characterisation of Titan's Atmospheric Physical Properties by the Huygens Atmospheric Structure Instrument (Hasi)". Space Science Reviews. 104 (1): 395–431. Bibcode:2002SSRv..104..395F. doi:10.1023/A:1023688607077. S2CID 189778612.
- Jet Propulsion Laboratory. Overview – Climate: The Spherical Shape of the Earth: Climatic Zones. Archived 26 July 2009 at the Wayback Machine Retrieved on 28 June 2008.
- Anne Minard. Jupiter's "Jet Stream" Heated by Surface, Not Sun. Retrieved on 28 June 2008.
- ESA: Cassini–Huygens. The jet stream of Titan. Retrieved on 28 June 2008.
- Georgia State University. The Environment of Venus. Retrieved on 28 June 2008.
- Ellen Cohen. "Jupiter's Great Red Spot". Hayden Planetarium. Archived from the original on 8 August 2007. Retrieved 16 November 2007.
- Suomi, V.E.; Limaye, S.S.; Johnson, D.R. (1991). "High Winds of Neptune: A possible mechanism". Science. 251 (4996): 929–932. Bibcode:1991Sci...251..929S. doi:10.1126/science.251.4996.929. PMID 17847386. S2CID 46419483.
- Sromovsky, Lawrence A. (14 October 1998). "Hubble Provides a Moving Look at Neptune's Stormy Disposition". HubbleSite.
- Knutson, Heather A.; David Charbonneau; Lori E. Allen; Jonathan J. Fortney; Eric Agol; Nicolas B. Cowan; et al. (10 May 2007). "A map of the day–night contrast of the extrasolar planet HD 189733b". Nature. 447 (7141): 183–186. arXiv:0705.0993. Bibcode:2007Natur.447..183K. doi:10.1038/nature05782. PMID 17495920. S2CID 4402268.
- Bill Christensen. Shock to the (Solar) System: Coronal Mass Ejection Tracked to Saturn. Retrieved on 28 June 2008.
- AlaskaReport. What Causes the Aurora Borealis? Retrieved on 28 June 2008.
- Rodney Viereck. Space Weather: What is it? How Will it Affect You?[permanent dead link] Retrieved on 28 June 2008.