thermal wind वाक्य
उदाहरण वाक्य
मोबाइल
- As the temperature gradient steepens during frontogenesis, the thermal wind becomes imbalanced.
- The thermal wind equation does not determine the wind in the tropics.
- Shallow, warm water and constant thermal wind make learning here a pure joy.
- Q-vectors and all ageostrophic flow exist to preserve thermal wind balance.
- Jet streams ( shown in pink ) are well-known examples of thermal wind.
- All these facts are consequences of the thermal wind relation.
- During frontogenesis, the temperature gradient tightens and as a result, the thermal wind becomes imbalanced.
- Also called "'baroclinic flow "', the thermal wind varies with height in proportion to the horizontal temperature gradient.
- Mathematically, the thermal wind relation defines a vertical wind shear-- a variation in wind speed or direction with height.
- From February May Hua Hin has a southerly thermal wind that gusts to 15 20 knots in the afternoon.
- Note that thermal wind is at right angles to the horizontal temperature gradient, counter clockwise in the northern hemisphere.
- The difference in horizontal wind speed with height that results is a vertical wind shear, traditionally called the thermal wind.
- The "'Thermal wind "'is wind that varies with height due to a balance between the pressure-gradient forces in the atmosphere.
- Vasiliki is a well known windsurfing spot during the summer months due to a local thermal wind known amongst windsurfers as'Eric '.
- Many authors retain the " thermal wind " moniker, even though it describes a wind gradient, sometimes offering a clarification to that effect.
- They wanted to land by midmorning before the heat of the sun built up the terrific thermal winds that make desert touchdowns treacherous.
- However, one can view the thermal wind as a geostrophic wind that varies with height, so that the term " wind " seems appropriate.
- The thermal wind relation results from hydrostatic balance and geostrophic balance in the presence of a temperature gradient along constant pressure surfaces, or isobars.
- A thermal wind system develops with wind toward the poles in the upper level and wind away from the poles in the lower level.
- Such isobaric surfaces will also be isothermal surfaces, hence ( from the thermal wind equation ) the geostrophic wind will not vary with depth.
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