geopotential वाक्य
उदाहरण वाक्य
मोबाइल
- 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 ).
- 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 ).
- 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.
- 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.
- 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.
- 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.
- 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.
- 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.
- 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.
- 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:
- The barotropic vorticity equation is the simplest way for forecasting the movement of Rossby waves ( that is, the hPa geopotential height ) over a limited amount of time ( a few days ).
- The geopotential height of this point was calculated in 1986 as part of the United European Levelling Network ( UELN ), based on the Amsterdam Ordnance Datum, which represents the average level of the North Sea.
- A geopotential field U is constructed, being the sum of a gravitational potential \ Psi and the known centrifugal potential \ Phi, that " has the GRS80 reference ellipsoid as one of its equipotential surfaces ".
- "' Geopotential function "'is a function that at each point is equal to a constant minus the energy that would be acquired by a unit mass in falling from rest at infinity to the point in question.
- Since the atmosphere at a height of approximately is mostly divergence-free, the barotropic model best approximates the state of the atmosphere at a geopotential height corresponding to that altitude, which corresponds to the atmosphere's pressure surface.
- Where the \ phi _ x are geopotential height fields with \ phi _ 1 > \ phi _ 0, f is the Coriolis parameter, and \ mathbf { k } is the upward-pointing unit vector in the vertical direction.
- In the above table, " geopotential altitude " is calculated from a mathematical model that adjusts the altitude to include the variation of gravity with height, while " geometric altitude " is the standard direct vertical distance above mean sea level.
- One can construct a simple model geopotential U that has as one of its equipotential surfaces this reference ellipsoid, with the same model potential U _ 0 as the true potential W _ 0 of the geoid; this model is called a " normal potential ".
- Once a clean, smooth geopotential field U has been constructed matching the known GRS80 reference ellipsoid with an equipotential surface ( we call such a field a " normal potential " ) we can subtract it from the true ( measured ) potential W of the real Earth.
- As part of this work, he introduced normal heights, which can be calculated from geopotential numbers ( obtained from precise levelling ) without needing the uncertain value of gravity along the plumbline of a point, i . e ., inside the continental crustal rock under the point.
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