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Some of the precipitation changes are associated with large scale changes to atmospheric wind patterns that are moving climate zones.
These regional anomalies result from changes in atmospheric wind patterns associated with phenomena such as El Niño and the so-called North Atlantic Oscillation.
The weighted amplitude wave superposition (WAWS) method is used to generate atmospheric wind turbulence.
In this paper, for upper atmospheric wind measurement, according to the requirement of the optical path difference, we present a stable, high throughput and wide field-of-view modified Sagnac interferometer for upper atmospheric wind measurement.
A high fidelity approach for wind turbine aero-elastic simulations including explicit representation of the atmospheric wind turbulence is presented.
Today, geostationary satellites can observe atmospheric wind vectors associated with TCs in the upper-troposphere with high temporal and spatial resolution (Bessho et al. 2016).
Similar(30)
In contrast, atmospheric winds typically have a vertical shear profile in the lower atmosphere, and the plumes from large volcanic eruptions may ascend beyond the tropopause and encounter jet streams with locally high wind speeds (Bursik 2001; Bursik et al. 2009).
It's atmospheric, winding streets are now abandoned, but still seem full of history.
Atmospheric winds and temperatures in the MLT region are necessary to investigate the possible role of convective or dynamic instabilities.
The assumption does not consider several factors such as temperatures and pressures change, atmospheric winds perturbation with altitude, etc.
This confirms that the observed MSTIDs were primarily due to GWs because the atmospheric winds pose a directional filter.
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