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.
22.
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.
23.
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.
24.
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.
25.
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.
26.
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.
27.
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.
28.
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.
29.
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.
30.
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.
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