Abstract
Awareness of weather and concern about weather in the proximate future certainly must have accompanied the emergence of human self-consciousness. Although weather is a basic idea in human existence, it is difficult to define precisely.
This chapter was originally published as part of the Encyclopedia of Sustainability Science and Technology edited by Robert A. Meyers. DOI:10.1007/978-1-4419-0851-3
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- Assimilation:
-
The process of combining observations of the atmosphere with a “first guess” (usually a model forecast) to define the atmospheric state on a forecast model grid.
- Geostrophic balance:
-
A possible state of rotating fluids in which flow is directed along pressure gradients rather than across them.
- Gravity waves:
-
Rapidly moving atmospheric disturbances driven by gravity acting on vertical density gradients. Often arise as a consequence of spurious geostrophic imbalance in initial conditions.
- Hydrostatic balance:
-
State in which the vertical pressure gradient force cancels the downward accleration of gravity. Approximately obeyed in atmospheric flows with horizontal scales larger than several km.
- Instabilities (or unstable modes):
-
Spatial patterns in a flow that are able to extract energy from the background flow and grow in amplitude.
- Primitive equations:
-
Complete set of equations describing flow of a thin envelope of fluid or gas surrounding a sphere.
- Resolution:
-
Separation in space of notional points at which quantities are defined in a numerical model.
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Bacmeister, J.T. (2012). Weather Prediction Models. In: Rasch, P. (eds) Climate Change Modeling Methodology. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-5767-1_5
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