Wind in the Atmosphere
Numerical Simulation of Acoustic Gravity Waves Propagation in a Heterogeneous Earth Atmosphere Model with Wind in the Atmosphere
... The approach proposed to the statement and solution of the problem makes it possible to simulate the effects of the wave field propagation in a unified mathematical earth-atmosphere model and to study the exchange ...
6
Mathematical Modeling of the Influence of the Wind Field Structure in the Atmosphere on the Cloud Formation Processes
... various wind field structures in the atmosphere, which included the actual structure constructed from the aerological sounding data (the Mineralnye Vody Airport, North Caucasus, Russia) of the ...
13
Identification and Interpretation of Earth’s Atmosphere Dynamics’ and Thermodynamics’ Similarities between Rogue Waves and Oceans’ Surface Geostrophic Wind
... geostrophic wind behavior in their practices to explain many meteorological phenomena such as the direction of the winds that take place around the low pres- sure ...geostrophic wind is parallel to the ...
9
Quantifying wind and pressure effects on trace gas fluxes across the soil-atmosphere interface
... linear wind tunnel on trace gas fluxes from low or moderate wind environments within the isolated toroid (the isolated toroid in this scenario is similar to the real- world scenarios of (i) a forest verge, ...
12
Formation of Vorticity of the Wind Speed Field in the Atmosphere over the Black Sea
... the wind speed field vorticity in the Black Sea region over 1979–2013 period for January and July is ...cyclonic wind vorticity, determined by the contribution of the high mountains surrounding the sea, ...
9
Simultaneous and co-located wind measurements in the middle atmosphere by lidar and rocket-borne techniques
... middle atmosphere, called DoRIS (Doppler Rayleigh Iodine Spectrometer), with a rocket-borne in situ method, which relies on measuring the horizontal drift of a target (“starute”) by a tracking ...Middle ...
9
Ocean–atmosphere–wave characterisation of a wind jet (Ebro shelf, NW Mediterranean Sea)
... the wind jet, no relevant differences were found when comparing the sig- nificant wave period and the wind intensity between the nu- merical model and observations for the observational ...and wind ...
16
A Numerical Study of the Wind over a Hydroelectric Reservoir: Effects of the Atmosphere Stratification
... the atmosphere, but the study is focused on a week, during which the data are separated in day and night ...of wind power in lakes of large hydro power plants under the most diverse ...
6
Numerical modeling of solar wind influences on the dynamics of the high-latitude upper atmosphere
... solar wind to the upper atmosphere was recently brought up by Siscoe and Siebert ...solar wind at the high- altitude end of the Region–1 current loop is transmitted to the Earth as a J ×B force ...
14
Combined wind measurements by two different lidar instruments in the Arctic middle atmosphere
... for wind measurements in the middle atmosphere from 30 up to 110 km ...simultaneous wind measurements derived from two different lidar ...vertical wind measurements and measurements of the ...
13
On the Wind and Turbulence in the Lower Atmosphere above Complex Terrain
... m) wind measurements by Meso- sphere-Stratosphere-Troposphere (MST) radar and by Lower Atmospheric Wind Profiler (LAWP) have been used to study variation of turbulence ...
16
Seasonal trends in Titan's atmosphere: haze, wind, and clouds
... Though it is Titan’s mysterious surface which initially motivated this work, this dis- sertation primarily addresses questions regarding the satellite’s atmosphere. One reason is that understanding the ...
160
Studies on the storage of potatoes. III. The composition of the atmosphere in a potato clamp
... This explains why, in the period before the sampling on 15 February, the wind of high velocity blowing along the length of the clamp, that is, with zero velocity normal to the clamp face[r] ...
7
Effect of latitudinally displaced gravity wave forcing in the lower stratosphere on the polar vortex stability
... middle atmosphere in the Ref simula- tion can be seen in ...zonal wind acceleration due to breaking GWs ...zonal wind in ...zonal wind shows maximum val- ues at the border of the mesospheric ...
17
Forest impacts on snow accumulation and ablation across an elevation gradient in a temperate montane environment
... attenuate wind speeds, thereby suppress- ing turbulent mixing of the near-surface atmosphere (Lis- ton and Sturm, 1998); modify the radiation received at the snow surface through shifts in shortwave and ...
16
Nonlinear instability of baroclinic atmosphere with reference to planetary scale disturbances
... surface represents solid body rotation. The intensity and di- rection of the wind is defined by the arbitrary parameter q . In this case, the surface integral in Eq. (24) is zero, and the suffi- cient conditions ...
8
SolarSystem.pdf
... solar atmosphere is so hot that the gas is primarily in a plasma state: electrons are no longer bound to atomic nuclei, and the gas is made up of charged particles (mostly protons and ...solar atmosphere is ...
5
Early deglacial Atlantic overturning decline and its role in atmospheric CO 2rise inferred from carbon isotopes (13(C)
... their wind stress forcing was calculated from an atmosphere only model, which was forced with a very large heat flux anomaly and leads to large areas of the subtropical North Atlantic experiencing extreme ...
18
Modelling of volcanic ashfall : a thesis presented in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Mathematics at Massey University, Albany, New Zealand
... the atmosphere in both vertical and horizontal directions, the scale of horizontal turbulence is much greater than that of vertical ...account wind speed and direction along with ...
162
QUALITY ISSUES IN RADAR WIND PROFILER
... radar wind profilers ...horizontal wind vector in the atmosphere by radar wind profiler (RWP) are a technique that has been ...horizontal wind at high temporal resolution under almost all ...
6