atmospheric stability वाक्य
उदाहरण वाक्य
मोबाइल
- While relative humidity is high, rainfall is very low due to strong atmospheric stability.
- Some of these climatic variables include humidity, aridity, winds, and atmospheric stability.
- Cold air blowing over warm water decreases atmospheric stability, allowing convection to form and grow into showers.
- They are found at low altitudes, and is a good sign of atmospheric stability, which indicates continuous stable weather.
- He developed a simple method for assessing atmospheric stability based on wind speed, solar radiation, cloud cover, and time of day.
- This resulted in a continuation of the spring weather pattern over the Atlantic Ocean, with strong vertical wind shear, mid-level moisture, and atmospheric stability.
- The neutral atmospheric stability assumption discussed above is reasonable when the hourly mean wind speed at a height of 10 m exceeds 10 m / s where turbulent mixing overpowers atmospheric instability.
- If the M43 had been used in open terrain under neutral atmospheric stability it could have potentially incapacitated about 94 % of the target with a fatality rate no greater than 2 %.
- This resulted in continuation of the spring weather pattern over the Atlantic Ocean, with strong vertical wind shear, mid-level moisture, and atmospheric stability, which suppressed tropical cyclogenesis.
- The program includes a complex terrain flow model, a roughness change model, a model for sheltering obstacles, a wind turbine wake model and a model for the average atmospheric stability conditions at the site.
- The wind profile of the atmospheric boundary layer ( surface to around 2000 metres ) is generally logarithmic in nature and is best approximated using the log wind profile equation that accounts for surface roughness and atmospheric stability.
- \sigma _ z and \ sigma _ y are functions of the atmospheric stability class ( i . e ., a measure of the turbulence in the ambient atmosphere ) and of the downwind distance to the receptor.
- The vertical range of sodars is approximately 0.2 to 2 kilometers ( km ) and is a function of frequency, power output, atmospheric stability, turbulence, and, most importantly, the pulse length and maximum altitude.
- The lack of heavy rainfall arises from high atmospheric stability caused, in turn, by the combination of cool waters from semi-permanent coastal upwelling and the presence of the cold Humboldt Current and warm air aloft associated with the South Pacific anticyclone.
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