Definition
Climate. Time average of atmospheric properties. The objective of the temporal averaging is to establish a background state of behavior that is the most likely state of the atmosphere at any given time. Weather variations are considered to be superimposed on the background climate, while at any given location the climate is viewed as changing through the year; thus, a location has a different climate state for each month of the year. Spatial averaging is generally used as well, but if sufficiently detailed observations are available, microclimates of any desired scale can be defined. Climate variability is the year-to-year change in climate at a given location and time of year; if temporal and/or spatial coherence can be identified in these variations, coherent modes of climate variability such as the El Niño/Southern Oscillation (ENSO) or the North Atlantic Oscillation (NAO) may be described.
Climate monitoring. The practice of describing the current state of the climate...
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Sapiano, M.R.P. (2014). Climate Monitoring and Prediction. In: Njoku, E.G. (eds) Encyclopedia of Remote Sensing. Encyclopedia of Earth Sciences Series. Springer, New York, NY. https://doi.org/10.1007/978-0-387-36699-9_16
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