geostrophic wind वाक्य
उदाहरण वाक्य
मोबाइल
- In the free atmosphere, geostrophic wind relationships should be used.
- In other words, no vertical wind shear of the geostrophic wind.
- Unlike geostrophic currents, and geostrophic winds are examples of inertial waves.
- They follow the principle of geostrophic winds.
- Isallobaric gradients are important components of the wind as they increase or decrease the geostrophic wind.
- The geostrophic wind component is the result of the balance between Coriolis force and pressure gradient force.
- Look at geostrophic wind article in wikipedia and you will be able to solve this problem without difficulty.
- The gradient wind is similar to the geostrophic wind but also includes centrifugal force ( or centripetal acceleration ).
- To maintain balance, the geostrophic wind aloft and below adjust, such that regions of divergence / convergence form.
- Such isobaric surfaces will also be isothermal surfaces, hence ( from the thermal wind equation ) the geostrophic wind will not vary with depth.
- However, one can view the thermal wind as a geostrophic wind that varies with height, so that the term " wind " seems appropriate.
- It flows parallel to ageostrophic wind component is the difference between actual and geostrophic wind, which is responsible for air " filling up " cyclones over time.
- Geopotential height contours can be used to calculate the geostrophic wind, which is faster where the contours are more closely spaced and tangential to the geopotential height contours.
- The geostrophic wind neglects frictional effects, which is usually a good approximation for the Quasigeostrophic and Semigeostrophic theory are used to model flows in the atmosphere more widely.
- "' Barotropic "'models assume the atmosphere is nearly barotropic, which means that the direction and speed of the geostrophic wind are independent of height.
- 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:
- Inertial waves are observed most commonly in planetary atmospheres ( Rossby waves, geostrophic winds ) and in oceans and lakes ( geostrophic currents ), where they are responsible for much of the mixing that takes place.
- There are two distinct local weather phenomenon, marked downslope lee winds caused by the proximity of the Pennines, leading to super geostrophic winds which can reach in excess of 70 mph, most commonly in winter and spring.
- Calculate the geostrophic wind speed ( ms ^-1 ) when tha distance between the 1000 and 1002 hPa isobars at 28?S is 1.2cm on a map with a scale 1 : 20 * 10 ^ 6.
- There are two distinct local weather phenomena, marked downslope lee winds caused by the proximity of the Pennines, leading to super geostrophic winds which can reach in excess of 60 KT ( 70 mph ), most commonly in winter and spring.
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