Climate

Climate is the long-term weather pattern in a region, typically averaged over 30 years.[1][2] 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.[1] The climate of a location is affected by its latitude, longitude, terrain, altitude, land use and nearby water bodies and their currents.[3]

For other uses, see Climate (disambiguation).

Atmospheric sciences
Meteorology
Climatology
Aeronomy
Glossaries

Climates can be classified according to the average and typical variables, most commonly temperature and precipitation. The most widely used classification scheme was the Köppen climate classification. The Thornthwaite system,[4] in use since 1948, incorporates evapotranspiration along with temperature and precipitation information and is used in studying biological diversity and how climate change affects it. The major classifications in Thornthwaite’s climate classification are microthermal, mesothermal, and megathermal.[5]

Finally, the Bergeron and Spatial Synoptic Classification systems focus on the origin of air masses that define the climate of a region.

Paleoclimatology is the study of ancient climates. Paleoclimatologists seek to explain climate variations for all parts of the Earth during any given geologic period, beginning with the time of the Earth's formation.[6] Since very few direct observations of climate were available before the 19th century, paleoclimates are inferred from proxy variables. They include non-biotic evidence—such as sediments found in lake beds and ice cores—and biotic evidence—such as tree rings and coral. Climate models are mathematical models of past, present, and future climates. Climate change may occur over long and short timescales from various factors. Recent warming is discussed in terms of global warming, which results in redistributions of biota. For example, as climate scientist Lesley Ann Hughes has written: "a 3 °C [5 °F] change in mean annual temperature corresponds to a shift in isotherms of approximately 300–400 km [190–250 mi] in latitude (in the temperate zone) or 500 m [1,600 ft] in elevation. Therefore, species are expected to move upwards in elevation or towards the poles in latitude in response to shifting climate zones."[7][8]

Definition

Climate (from Ancient Greek κλίμα 'inclination') is commonly defined as the weather averaged over a long period.[9] The standard averaging period is 30 years,[10] but other periods may be used depending on the purpose. Climate also includes statistics other than the average, such as the magnitudes of day-to-day or year-to-year variations. The Intergovernmental Panel on Climate Change (IPCC) 2001 glossary definition is as follows:

Climate in a narrow sense is usually defined as the "average weather", or more rigorously, as the statistical description in terms of the mean and variability of relevant quantities over a period ranging from months to thousands or millions of years. The classical period is 30 years, as defined by the World Meteorological Organization (WMO). These quantities are most often surface variables such as temperature, precipitation, and wind. Climate in a wider sense is the state, including a statistical description, of the climate system.[11]

The World Meteorological Organization (WMO) describes "climate normals" as "reference points used by climatologists to compare current climatological trends to that of the past or what is considered typical. A climate normal is defined as the arithmetic average of a climate element (e.g. temperature) over a 30-year period. A 30-year period is used as it is long enough to filter out any interannual variation or anomalies such as El Niño–Southern Oscillation, but also short enough to be able to show longer climatic trends."[12]

The WMO originated from the International Meteorological Organization which set up a technical commission for climatology in 1929. At its 1934 Wiesbaden meeting, the technical commission designated the thirty-year period from 1901 to 1930 as the reference time frame for climatological standard normals. In 1982, the WMO agreed to update climate normals, and these were subsequently completed on the basis of climate data from 1 January 1961 to 31 December 1990.[13] The 1961–1990 climate normals serve as the baseline reference period. The next set of climate normals to be published by WMO is from 1991 to 2010.[14] Aside from collecting from the most common atmospheric variables (air temperature, pressure, precipitation and wind), other variables such as humidity, visibility, cloud amount, solar radiation, soil temperature, pan evaporation rate, days with thunder and days with hail are also collected to measure change in climate conditions.[15]

The difference between climate and weather is usefully summarized by the popular phrase "Climate is what you expect, weather is what you get."[16] Over historical time spans, there are a number of nearly constant variables that determine climate, including latitude, altitude, proportion of land to water, and proximity to oceans and mountains. All of these variables change only over periods of millions of years due to processes such as plate tectonics. Other climate determinants are more dynamic: the thermohaline circulation of the ocean leads to a 5 °C (41 °F) warming of the northern Atlantic Ocean compared to other ocean basins.[17] Other ocean currents redistribute heat between land and water on a more regional scale. The density and type of vegetation coverage affects solar heat absorption,[18] water retention, and rainfall on a regional level. Alterations in the quantity of atmospheric greenhouse gases determines the amount of solar energy retained by the planet, leading to global warming or global cooling. The variables which determine climate are numerous and the interactions complex, but there is general agreement that the broad outlines are understood, at least insofar as the determinants of historical climate change are concerned.[19]

Climate classification
Main article: Climate classification
Map of world dividing climate zones, largely influenced by latitude. The zones, going from the equator upward (and downward) are Tropical, Dry, Moderate, Continental and Polar. There are subzones within these zones.
Worldwide Köppen climate classifications

Climate classifications are systems that categorize the world's climates. A climate classification may correlate closely with a biome classification, as climate is a major influence on life in a region. One of the most used is the Köppen climate classification scheme first developed in 1899.[20]

There are several ways to classify climates into similar regimes. Originally, climes were defined in Ancient Greece to describe the weather depending upon a location's latitude. Modern climate classification methods can be broadly divided into genetic methods, which focus on the causes of climate, and empiric methods, which focus on the effects of climate. Examples of genetic classification include methods based on the relative frequency of different air mass types or locations within synoptic weather disturbances. Examples of empiric classifications include climate zones defined by plant hardiness,[21] evapotranspiration,[22] or more generally the Köppen climate classification which was originally designed to identify the climates associated with certain biomes. A common shortcoming of these classification schemes is that they produce distinct boundaries between the zones they define, rather than the gradual transition of climate properties more common in nature.

Record

Paleoclimatology
Main article: Paleoclimatology

Paleoclimatology is the study of past climate over a great period of the Earth's history. It uses evidence with different time scales (from decades to millennia) from ice sheets, tree rings, sediments, pollen, coral, and rocks to determine the past state of the climate. It demonstrates periods of stability and periods of change and can indicate whether changes follow patterns such as regular cycles.[23]

Modern
See also: Instrumental temperature record and Satellite temperature measurements

Details of the modern climate record are known through the taking of measurements from such weather instruments as thermometers, barometers, and anemometers during the past few centuries. The instruments used to study weather over the modern time scale, their observation frequency, their known error, their immediate environment, and their exposure have changed over the years, which must be considered when studying the climate of centuries past.[24] Long-term modern climate records skew towards population centres and affluent countries.[25] Since the 1960s, the launch of satellites allow records to be gathered on a global scale, including areas with little to no human presence, such as the Arctic region and oceans.

Climate variability
Main article: Climate variability and change

Climate variability is the term to describe variations in the mean state and other characteristics of climate (such as chances or possibility of extreme weather, etc.) "on all spatial and temporal scales beyond that of individual weather events."[26] Some of the variability does not appear to be caused systematically and occurs at random times. Such variability is called random variability or noise. On the other hand, periodic variability occurs relatively regularly and in distinct modes of variability or climate patterns.[27]

There are close correlations between Earth's climate oscillations and astronomical factors (barycenter changes, solar variation, cosmic ray flux, cloud albedo feedback, Milankovic cycles), and modes of heat distribution between the ocean-atmosphere climate system. In some cases, current, historical and paleoclimatological natural oscillations may be masked by significant volcanic eruptions, impact events, irregularities in climate proxy data, positive feedback processes or anthropogenic emissions of substances such as greenhouse gases.[28]

Over the years, the definitions of climate variability and the related term climate change have shifted. While the term climate change now implies change that is both long-term and of human causation, in the 1960s the word climate change was used for what we now describe as climate variability, that is, climatic inconsistencies and anomalies.[27]

Climate change
Average surface air temperatures from 2011 to 2021 compared to the 1956–1976 average. Source: NASA
Observed temperature from NASA[29] vs the 1850–1900 average used by the IPCC as a pre-industrial baseline.[30] The primary driver for increased global temperatures in the industrial era is human activity, with natural forces adding variability.[31]
Main article: Climate change
See also: Global temperature record, List of weather records, and Attribution of recent climate change

Climate change is the variation in global or regional climates over time.[32] It reflects changes in the variability or average state of the atmosphere over time scales ranging from decades to millions of years. These changes can be caused by processes internal to the Earth, external forces (e.g. variations in sunlight intensity) or, more recently, human activities.[33][34] In recent usage, especially in the context of environmental policy, the term "climate change" often refers only to changes in modern climate, including the rise in average surface temperature known as global warming. In some cases, the term is also used with a presumption of human causation, as in the United Nations Framework Convention on Climate Change (UNFCCC). The UNFCCC uses "climate variability" for non-human caused variations.[35]

Earth has undergone periodic climate shifts in the past, including four major ice ages. These consist of glacial periods where conditions are colder than normal, separated by interglacial periods. The accumulation of snow and ice during a glacial period increases the surface albedo, reflecting more of the Sun's energy into space and maintaining a lower atmospheric temperature. Increases in greenhouse gases, such as by volcanic activity, can increase the global temperature and produce an interglacial period. Suggested causes of ice age periods include the positions of the continents, variations in the Earth's orbit, changes in the solar output, and volcanism.[36] However, these naturally-caused changes in climate occur on a much slower time scale than the present rate of change which is caused by the emission of greenhouse gases by human activities.[37]

Climate models

Climate models use quantitative methods to simulate the interactions and transfer of radiative energy between the atmosphere,[38] oceans, land surface and ice through a series of physics equations. They are used for a variety of purposes; from the study of the dynamics of the weather and climate system, to projections of future climate. All climate models balance, or very nearly balance, incoming energy as short wave (including visible) electromagnetic radiation to the Earth with outgoing energy as long wave (infrared) electromagnetic radiation from the earth. Any imbalance results in a change in the average temperature of the earth.

Climate models are available on different resolutions ranging from >100 km to 1 km. High resolutions in global climate models require significant computational resources, and so only a few global datasets exist. Global climate models can be dynamically or statistically downscaled to regional climate models to analyze impacts of climate change on a local scale. Examples are ICON[39] or mechanistically downscaled data such as CHELSA (Climatologies at high resolution for the earth's land surface areas).[40][41]

The most talked-about applications of these models in recent years have been their use to infer the consequences of increasing greenhouse gases in the atmosphere, primarily carbon dioxide (see greenhouse gas). These models predict an upward trend in the global mean surface temperature, with the most rapid increase in temperature being projected for the higher latitudes of the Northern Hemisphere.

Models can range from relatively simple to quite complex. Simple radiant heat transfer models treat the earth as a single point and average outgoing energy. This can be expanded vertically (as in radiative-convective models), or horizontally. Finally, more complex (coupled) atmosphere–ocean–sea ice global climate models discretise and solve the full equations for mass and energy transfer and radiant exchange.[42]

See also

References
  1. Matthews, J.B. Robin; Möller, Vincent; van Diemen, Renée; Fuglestvedt, Jan S.; Masson-Delmotte, Valérie; Méndez, Carlos; Semenov, Sergey; Reisinger, Andy (2021). "Annex VII. Glossary: IPCC – Intergovernmental Panel on Climate Change" (PDF). IPCC Sixth Assessment Report. p. 2222. Archived (PDF) from the original on 2022-06-05. Retrieved 2022-05-18.
  2. Shepherd, J. Marshall; Shindell, Drew; O'Carroll, Cynthia M. (1 February 2005). "What's the Difference Between Weather and Climate?". NASA. Archived from the original on 22 September 2020. Retrieved 13 November 2015.
  3. Gough, William A.; Leung, Andrew C. W. (2022). "Do Airports Have Their Own Climate?". Meteorology. 1 (2): 171–182. doi:10.3390/meteorology1020012. ISSN 2674-0494.
  4. Thornthwaite, C. W. (1948). "An Approach Toward a Rational Classification of Climate" (PDF). Geographical Review. 38 (1): 55–94. doi:10.2307/210739. JSTOR 210739. Archived from the original on 2020-09-22. Retrieved 2010-12-13.
  5. "All About Climate". education.nationalgeographic.org. Retrieved 2023-09-25.
  6. "paleoclimatology | science | Britannica". www.britannica.com. Archived from the original on 2022-09-01. Retrieved 2022-09-01.
  7. Hughes, Lesley (2000). Biological consequences of globalwarming: is the signal already. p. 56.
  8. Hughes, Leslie (1 February 2000). "Biological consequences of global warming: is the signal already apparent?". Trends in Ecology and Evolution. 15 (2): 56–61. doi:10.1016/S0169-5347(99)01764-4. PMID 10652556. Archived from the original on 12 October 2013. Retrieved November 17, 2016.
  9. "Climate". Glossary of Meteorology. American Meteorological Society. Archived from the original on 2011-07-07. Retrieved 2008-05-14.
  10. "Climate averages". Met Office. Archived from the original on 2008-07-06. Retrieved 2008-05-17.
  11. Intergovernmental Panel on Climate Change. Appendix I: Glossary. Archived 2017-01-26 at the Wayback Machine Retrieved on 2007-06-01.
  12. "Climate Data and Data Related Products". World Meteorological Organization. Archived from the original on 1 October 2014. Retrieved 1 September 2015.
  13. "Commission For Climatology: Over Eighty Years of Service" (PDF). World Meteorological Organization. 2011. pp. 6, 8, 10, 21, 26. Archived from the original (PDF) on 13 September 2015. Retrieved 1 September 2015.
  14. "WMO Climatological Normals". World Meteorological Organization. Archived from the original on 2022-08-21. Retrieved 2022-08-21.
  15. WMO Guidelines on the Calculation of Climate Normals (PDF). World Meteorological Organization. 2017. ISBN 978-92-63-11203-3. Archived from the original on 2022-08-08. Retrieved 2022-08-20.
  16. National Weather Service Office Tucson, Arizona. Main page. Archived 2017-03-12 at the Wayback Machine Retrieved on 2007-06-01.
  17. Rahmstorf, Stefan. "The Thermohaline Ocean Circulation: A Brief Fact Sheet". Potsdam Institute for Climate Impact Research. Archived from the original on 2013-03-27. Retrieved 2008-05-02.
  18. de Werk, Gertjan; Mulder, Karel (2007). "Heat Absorption Cooling For Sustainable Air Conditioning of Households" (PDF). Sustainable Urban Areas Rotterdam. Archived from the original (PDF) on 2008-05-27. Retrieved 2008-05-02.
  19. Ledley, T.S.; Sundquist, E. T.; Schwartz, S. E.; Hall, D. K.; Fellows, J. D.; Killeen, T. L. (1999). "Climate change and greenhouse gases". EOS. 80 (39): 453. Bibcode:1999EOSTr..80Q.453L. doi:10.1029/99EO00325. hdl:2060/19990109667.
  20. Beck, Hylke E.; Zimmermann, Niklaus E.; McVicar, Tim R.; Vergopolan, Noemi; Berg, Alexis; Wood, Eric F. (30 October 2018). "Present and future Köppen-Geiger climate classification maps at 1-km resolution". Scientific Data. 5: 180214. Bibcode:2018NatSD...580214B. doi:10.1038/sdata.2018.214. ISSN 2052-4463. PMC 6207062. PMID 30375988.
  21. United States National Arboretum. USDA Plant Hardiness Zone Map. Archived 2012-07-04 at the Wayback Machine Retrieved on 2008-03-09
  22. "Thornthwaite Moisture Index". Glossary of Meteorology. American Meteorological Society. Retrieved 2008-05-21.
  23. National Oceanic and Atmospheric Administration. NOAA Paleoclimatology. Archived 2020-09-22 at the Wayback Machine Retrieved on 2007-06-01.
  24. Weart, Spencer. "The Modern Temperature Trend". American Institute of Physics. Archived from the original on 2020-09-22. Retrieved 2007-06-01.
  25. Vose, R. S.; Schmoyer, R. L.; Steurer, P. M.; Peterson, T. C.; Heim, R.; Karl, T. R.; Eischeid, J. K. (1992-07-01), The Global Historical Climatology Network: Long-term monthly temperature, precipitation, sea level pressure, and station pressure data, U.S. Department of Energy. Office of Scientific and Technical Information, doi:10.2172/10178730, OSTI 10178730, archived from the original on 2022-07-26, retrieved 2022-08-21
  26. IPCC AR5 WG1 Glossary 2013, p. 1451.
  27. Rohli & Vega 2018, p. 274.
  28. Scafetta, Nicola (May 15, 2010). "Empirical evidence for a celestial origin of the climate oscillations" (PDF). Journal of Atmospheric and Solar-Terrestrial Physics. 72 (13): 951–970. arXiv:1005.4639. Bibcode:2010JASTP..72..951S. doi:10.1016/j.jastp.2010.04.015. S2CID 1626621. Archived from the original (PDF) on 10 June 2010. Retrieved 20 July 2011.
  29. "Global Annual Mean Surface Air Temperature Change". NASA. Archived from the original on 16 April 2020. Retrieved 23 February 2020..
  30. IPCC AR5 SYR Glossary 2014, p. 124.
  31. USGCRP Chapter 3 2017 Figure 3.1 panel 2 Archived 2018-04-09 at the Wayback Machine, Figure 3.3 panel 5 Archived 2018-04-09 at the Wayback Machine.
  32. "Climate Change | National Geographic Society". education.nationalgeographic.org. Archived from the original on 2022-07-30. Retrieved 2022-06-28.
  33. Arctic Climatology and Meteorology. Climate change. Archived 2010-01-18 at the Wayback Machine Retrieved on 2008-05-19.
  34. Gillis, Justin (28 November 2015). "Short Answers to Hard Questions About Climate Change". The New York Times. Archived from the original on 22 September 2020. Retrieved 29 November 2015.
  35. "Glossary". Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Intergovernmental Panel on Climate Change. 2001-01-20. Archived from the original on 2017-01-26. Retrieved 2008-05-22.
  36. Illinois State Museum (2002). Ice Ages. Archived 2010-03-26 at the Wayback Machine Retrieved on 2007-05-15.
  37. Joos, Fortunat; Spahni, Renato (2008-02-05). "Rates of change in natural and anthropogenic radiative forcing over the past 20,000 years". Proceedings of the National Academy of Sciences. 105 (5): 1425–1430. Bibcode:2008PNAS..105.1425J. doi:10.1073/pnas.0707386105. ISSN 0027-8424. PMC 2234160. PMID 18252830.
  38. Eric Maisonnave. Climate Variability. Retrieved on 2008-05-02. Archived June 10, 2008, at the Wayback Machine
  39. Dipankar, A.; Heinze, Rieke; Moseley, Christopher; Stevens, Bjorn; Zängl, Günther; Brdar, Slavko (2015). "A Large Eddy Simulation Version of ICON (ICOsahedral Nonhydrostatic): Model Description and Validation". Journal of Advances in Modeling Earth Systems. 7. doi:10.1002/2015MS000431. S2CID 56394756.
  40. Karger, D.; Conrad, O.; Böhner, J.; Kawohl, T.; Kreft, H.; Soria-Auza, R.W.; Zimmermann, N.E.; Linder, P.; Kessler, M. (2017). "Climatologies at high resolution for the Earth land surface areas". Scientific Data. 4 (4 170122): 170122. Bibcode:2017NatSD...470122K. doi:10.1038/sdata.2017.122. PMC 5584396. PMID 28872642. S2CID 3750792.
  41. Karger, D.N.; Lange, S.; Hari, C.; Reyer, C.P.O.; Zimmermann, N.E. (2021). "CHELSA-W5E5 v1.0: W5E5 v1.0 downscaled with CHELSA v2.0". ISIMIP Repository. doi:10.48364/ISIMIP.836809.
  42. Climateprediction.net. Modelling the climate. Archived 2009-02-04 at the Wayback Machine Retrieved on 2008-05-02.

Sources

Further reading
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