wind profile उदाहरण वाक्य
उदाहरण वाक्य
- Because of the high temperature gradient between the warm and cold air masses, the cyclone underwent a phase of weather bomb " by meteorologists . research project, providing valuable data on its wind profile, temperature and humidity.
- In the field of Earth observation, projects include the ESA ADM-Aeolus wind profiling mission, for which UK industry is the prime contractor and CryoSat-2 which is directed by UK scientist Professor Duncan Wingham of University College London.
- 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.
- The "'Sandia method "'( also known as Veers method ) is a method for generating a turbulent wind profile that can be used in aero-elastic software to evaluate the fatigue imparted on a turbine in a turbulent environment.
- 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.
- The wind profile measured before the equinox of 2007 was slightly asymmetric with winds stronger in the southern hemisphere, although it turned out to be a seasonal effect as this hemisphere was continuously illuminated by the Sun before 2007.
- An idealized vertical profile of the mean flow for a neutral boundary layer is the logarithmic wind profile derived from mixing length theory, which states that the horizontal component of mean flow is proportional to the logarithm of height.
- This indeed happened in 2007 when Uranus passed an equinox : a faint northern polar collar arose, whereas the southern collar became nearly invisible, although the zonal wind profile remained asymmetric, with northern winds being slightly slower than southern.
- This indeed happened in 2007 when it passed an equinox : a faint northern polar collar arose, and the southern collar became nearly invisible, although the zonal wind profile remained slightly asymmetric, with northern winds being somewhat slower than southern.
- Other difference between IBIS-2 and IBIS-1 and LSX, is that IBIS-2 uses an empirical linear function of wind speed to estimate turbulent transfer between the soil surface and the lower vegetation canopy, and IBIS-1 and LSX use a logarithmic wind profile.