There are two different equations for computing density at various height regimes below 86 geometric km ( 84 852 geopotential meters or 278, 385.8 geopotential feet ).
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There are two different equations for computing density at various height regimes below 86 geometric km ( 84 852 geopotential meters or 278, 385.8 geopotential feet ).
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In sea water with respect to the gravity variation, the latitude and the geopotential anomaly the pressure can be converted into meters depth according to an empirical formula ( UNESCO Tech.
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Zonal mean temperature, wind, and geopotential height exert varying deviations from their normal values before and after early breakups, while the deviations remain constant before and after late breakups.
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Later models substituted the geometric z coordinate with a pressure coordinate system, in which the geopotential heights of constant-pressure surfaces become dependent variables, greatly simplifying the primitive equations.
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Alternatively, it can also be used to predict the evolution of the geopotential field given an initial distribution of { \ Phi } and suitable boundary conditions by using an inversion process.
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Both orthometric and normal heights are heights in metres above sea level, whereas geopotential numbers are measures of potential energy ( unit : m 2 s " 2 ) and not metric.
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A plot of geopotential height for a single pressure level shows the troughs and ridges, hPa and 1000 hPa geopotential heights for example is proportional to mean virtual temperature in that layer.
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A plot of geopotential height for a single pressure level shows the troughs and ridges, hPa and 1000 hPa geopotential heights for example is proportional to mean virtual temperature in that layer.
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Other variants of the equation are possible; for example, the geostrophic wind vector can be expressed in terms of the gradient of the geopotential height ? on a surface of constant pressure:
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