Climatological normal
Climatological normal or climate normal (CN) is a 30-year average of a weather variable for a given
time of year.[1]
Most commonly, a CN refers to a particular day of year and even hourly scale.[3]
Climatological normals are used as an average or baseline to evaluate climate events and provide context for year-to-year variability. Normals can be calculated for a variety of weather variables including temperature and precipitation and rely on data from
climate variability looks at the magnitude of extremes.[1]
Climatological standard normals are overlapping periods updated every decade: 1971–2000, 1981–2010, 1991–2020, etc.
The term "normal" first appeared in the literature by
International Meteorological Committee in 1872.[4] The use of the 30-year period of normals began in 1935 with the 1901-30 period.[5] The continued use of 30 year normals has increasingly been called into question due to substantial evidence that the stationarity of climate statistics can no longer be taken for granted due to climate change.[4][6] This has led to alternative definitions such as "Optimal Climate Normal" and the "Hinge Fit" approach to supplement the standard 30 year normals which are still commonly used.[7]
See also
- Climate anomaly
- Climatology
- Seasonality
References
- ^ a b Climate Variability and Climate Change Archived 2014-05-17 at the Wayback Machine; WHAT IS THE DIFFERENCE? Michigan Sea Grant
- ^ "WMO Guidelines on the Calculation of Climate Normals". World Meteorological Organization. 2017. Retrieved 3 July 2021.
- . Retrieved 3 July 2021.
- ^ ISSN 1520-0477.
- ^ Trewin, Blair C. (2007). The Role of Climatological Normals in a Changing Climate. World Climate Data and Monitoring Programme. World Meteorological Organization. p. 7.
- . Retrieved 3 July 2021.
- ^ "Defining Climate Normals in New Ways". National Centers for Environmental Information. NOAA. Archived from the original on 14 April 2022. Retrieved 3 July 2021.