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[PDF] Top 20 Weak interaction in the African Easterly Jet

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Weak interaction in the African Easterly Jet

Weak interaction in the African Easterly Jet

... The duration of the interaction between waves is given by half of the period of the elliptic function (2K), since ε k is proportional to ψ 2 k . The energy ε k of each wave as a function of time for N 2 /N 1 =0.7 ... See full document

7

Saharan dust and the African easterly jet–African easterly wave system: Structure, location and energetics

Saharan dust and the African easterly jet–African easterly wave system: Structure, location and energetics

... precipitation: the SMD increases total accumulated rainfall by ∼10% and shifts the region of precipitation ∼5° north. The strength of AEWs and their track locations are also important for tropical cyclogenesis, since ... See full document

32

The Influences of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons

The Influences of the North Atlantic Subtropical High and the African Easterly Jet on Hurricane Tracks During Strong and Weak Seasons

... note was that during these seasons the AEJ propagated northward, moving into the Saharan Desert rather than staying by the rainforests to the south. This result is easier seen using the every 10 day plots rather than ... See full document

19

The Interaction Between Moist Convection and African Easterly Waves.

The Interaction Between Moist Convection and African Easterly Waves.

... 6.2.3 Forecasting Implications There are significant implications of these findings for the modeling of AEWs and down- stream systems such as tropical cyclones. In the previous section we highlighted the inability of ... See full document

161

Long-lived African Easterly Waves.

Long-lived African Easterly Waves.

... − ωk × du ′ dp + Solenoid + F riction (3.4) where η is the 2D absolute vorticity calculated using the wave relative winds, u’, and ω is the pressure coordinate vertical velocity. Consistent with the previous studies, the ... See full document

88

On the Non Development of an Intense African Easterly Wave;

On the Non Development of an Intense African Easterly Wave;

... A large region of dry air was also present to the north of the disturbance. Dur- ing this time the Hurricane Severe Storm Sentinel field campaign was making observations of tropical cyclones with an unmanned global hawk ... See full document

44

African Easterly Wave Storm Track Dynamics.

African Easterly Wave Storm Track Dynamics.

... very weak modes can change the spacing of these consecutive peaks in EKE, but 6 grid points is roughly the distance of half-wavelengths for these simulated ... See full document

157

Nonlinear Structure and Evolution of African Easterly Waves

Nonlinear Structure and Evolution of African Easterly Waves

... only level with a vortex of multiple contours is 600 hPa, shown in panel b. All other levels at this time exhibit a weak signal of an AEW, which dissipates completely by the next six hour reanalysis. Composite ... See full document

143

Sensitivity of African easterly waves to boundary layer conditions

Sensitivity of African easterly waves to boundary layer conditions

... the African easterly jet (AEJ), is used to study the instability properties of the environment of the West African wave ...the African easterly waves (AEW) can be well ... See full document

9

The Role of Energy Dispersion in the Genesis and Life Cycle of African Easterly Waves.

The Role of Energy Dispersion in the Genesis and Life Cycle of African Easterly Waves.

... the instability was easily recovered, with the southern track AEWs dominating over the northern track AEWs. As noted in section 4.3.3, the barotropic instability, which is less prone to friction, is removed very quickly ... See full document

167

Links between African easterly waves, midlatitude circulation and intraseasonal pulsations of the West African heat low

Links between African easterly waves, midlatitude circulation and intraseasonal pulsations of the West African heat low

... The weak- ening of the WAHL is consistent with an increase of convective activity during this period over the Sahel, as derived from the satellite-based CLAUS long-term ... See full document

19

African Easterly Waves: Evolution in Potential Vorticity Fields and Interactions with Upper-level Troughs.

African Easterly Waves: Evolution in Potential Vorticity Fields and Interactions with Upper-level Troughs.

... be associated with tropical intensification due to upper-level trough interactions, but other en- vironmental factors must be considered in this determination besides tangential velocity flux convergence. Hanley et al. ... See full document

79

The Maintenance and Propagation of African Easterly Waves Across Northern Africa: A Case Study and Analysis of the Environment

The Maintenance and Propagation of African Easterly Waves Across Northern Africa: A Case Study and Analysis of the Environment

... the jet where the Sub-Saharan baroclinic zone ...the African Easterly Jet (AEJ) due to the interactions between the opposite sign PV gradients and form on the northern flank of the AEJ due to ... See full document

128

Linking African easterly wave activity with equatorial waves and the influence of Rossby waves from the Southern Hemisphere

Linking African easterly wave activity with equatorial waves and the influence of Rossby waves from the Southern Hemisphere

... This study has focused on the influence of background zonal flow on wave propagation characteristics. How- ever, it does not preclude two-way interaction where the TEJ is stronger as a result of greater AEW ... See full document

29

Using Data Assimilation To Investigate The Effect Of African Easterly Waves, Mesoscale  Convective Systems, And Orography On Tropical Cyclogenesis Over Eastern Pacific

Using Data Assimilation To Investigate The Effect Of African Easterly Waves, Mesoscale Convective Systems, And Orography On Tropical Cyclogenesis Over Eastern Pacific

... to African easterly waves that set off the coast of West ...were weak and disorganized at the initial stage with little or no convection; however they gradually developed into a tropical depression ... See full document

95

Jet-edge interaction tones

Jet-edge interaction tones

... 5. Conclusion Experiments have been performed involving an isothermal, round, turbulent jet that grazes a sharp edge whose streamwise position is varied. This leads to rich tonal dynamics and sound that cannot be ... See full document

26

A Theory of Weak Interaction Dynamics

A Theory of Weak Interaction Dynamics

... the weak field that mediate the interaction between the weak dipoles? 2) What is the form of the weak interaction term of the system’s Lagrangian density? A resolution of the first ... See full document

10

Numerical Simulation of Lateral Jet Interaction

Numerical Simulation of Lateral Jet Interaction

... Direct force induced by Reverse Control System (RCS) lateral jet can supple- ment the ability of control system as well as improve maneuvering and rapid re- sponse ability. This technology has been utilized ... See full document

8

Further Aspects of Weak Interaction Dynamics

Further Aspects of Weak Interaction Dynamics

... published weak interactions theory which is derived from a Lagrangian density  w ...The interaction which is carried by an appropriate mediating field is consistent with the Fermi coupl- ing constant of ... See full document

11

African Adventure by Luxury Private Jet

African Adventure by Luxury Private Jet

... With a small group of just 15 like-minded travelers, you’ll be pampered while aloft in your spacious and comfortable seat in the VIP Jet by the hand-chosen crew. The personal attention continues in each ... See full document

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