Increasing temperatureleadsto an increase in vertical wind shear which may inhibit the formation of hurricanes ( Vecchi 2007
This conditioncausesnet advection of hurricane structural elements that extend into the lower stratosphere away from the hurricane center
Precipitation of alteration minerals due to fluid flowleadsto changes in P - wave velocities within seismic Layer 2A ( the uppermost layer of the oceanic crust
an approaching troughcausedweakening by increasing wind shear ... while also forcing the storm eastward
Such a patternwould resultfrom tectonic shearing along the deep - rooted structure at the time of mineralization
a processcausesrapid intensification of a storm ... usually seen in a hurricane
by the wake disturbance(passive) caused bythe elevated turbulence and earlier shear layer breakdown
forces or deformations ... the leading edgeleadto critical ( shear ) stresses in the boundary layer between ice and structure
the interaction of streamwise velocity streaks of finite lengthcan leadto turbulent breakdown in the flat - plate boundary layer flow
Other factorsinfluencehurricane development ( i.e. wind shear
the bridgedesignedto span a busy highway and withstand hurricane - force winds
stronger - than - normal trade windscauseshear and interrupt hurricane development
Those windsare causingmoderate vertical wind shear which is inhibiting the intensification of Tropical Storm Saola
northern Mexicocausedincreased wind shear on Tropical Storm Fefa
The cloud bandsoriginatefrom the convergence along the typhoon shear lines
global warmingcausedintensification of the hurricane 's strength
a large concrete domedesignedto structurally withstand hurricane - force winds and storm surge
a large concrete domedesignedto structurally withstand storm surge and hurricane - force winds of
the surface pressure to decrease rapidlycontributedto the rapid intensification of Hurricane Delta
the storm ... northern Mexicocausedincreased wind shear on Tropical Storm Fefa
24 hoursleadsto rapid intensification of a mid - latitude cyclone
a sudden and extreme drop in barometric pressure of at least 24 millibarsleadsto rapid intensification of a mid - latitude cyclone
at least 24 millibars over 24 hoursleadsto rapid intensification of a mid - latitude cyclone
a sudden and extreme drop in barometric pressure of at least 24 millibars over 24 hoursleadsto rapid intensification of a mid - latitude cyclone
a sudden and extreme drop in barometric pressure of at least 24 millibars ... 24 hoursleadsto rapid intensification of a mid - latitude cyclone
This changes dramatically after detachment from the Roche lobe ; while the helium core barely contracts and spins up only slightly above the orbital frequency , the extended hydrogen envelope spins up significantly during contractionresultingin strong shear at the core - envelope boundary
the cylinderresultingin a rapid growth of the laminar boundary layer and separation
A powerful feedback processcan contributeto rapid hurricane intensification
Land interactioncausedrapid diminishing in the cyclone 's structure
The white layers observed in cross sections of hard cut surfaces exhibit a similar ultrafine , equiaxed grain structuresimilarly resultingfrom intense shear in the tertiary shear zone
Ideal simulations(passive) are designedIdeal simulations
large mean distortion of the jet and rapid turbulent mixingcauselarge mean distortion of the jet and rapid turbulent mixing
to their formationalso contributeto their formation
massivecausedmassive
to enhanced modulus gels where storage modulus scales as a power law with the pre - shear stressleadsto enhanced modulus gels where storage modulus scales as a power law with the pre - shear stress
Fracture of the window(passive) is caused byFracture of the window
most of the deep convection to be displaced to the southwest of the storm 's centercausedmost of the deep convection to be displaced to the southwest of the storm 's center
the forecasters at the National Hurricane Center to say that Franklin could be torn apart in the next few daysledthe forecasters at the National Hurricane Center to say that Franklin could be torn apart in the next few days
the average temperature in the primary shear zone to drop with decreased uncut chip thickness , giving rise to the size effect phenomenoncausesthe average temperature in the primary shear zone to drop with decreased uncut chip thickness , giving rise to the size effect phenomenon
in organized severe storms where serious flash floods risk will exist due to combined strong orographic and convective rainfallshould resultin organized severe storms where serious flash floods risk will exist due to combined strong orographic and convective rainfall
to instabilityleadingto instability
to partial blocking of the storm - relative flow aloft and channeling of the flow below The channeling of the storm - relative flowledto partial blocking of the storm - relative flow aloft and channeling of the flow below The channeling of the storm - relative flow
high - frequency pressure fluctuations that propagate millimeters or centimeters into the snowcauseshigh - frequency pressure fluctuations that propagate millimeters or centimeters into the snow
the convection to dwindle to the northeastcausingthe convection to dwindle to the northeast
to more organized storm systemsleadsto more organized storm systems
Fred to diminish to a tropical stormcausingFred to diminish to a tropical storm
weakeningshould causeweakening
weakeningshould causeweakening
weakeningshould causeweakening
solid particles to separate from the fluid carriercausingsolid particles to separate from the fluid carrier
it to turn westward over the Florida Keys by August 26causedit to turn westward over the Florida Keys by August 26
the eye to deteriorate by early on October 16causingthe eye to deteriorate by early on October 16
more disruptionwill causemore disruption
in the introduction of downward turbulence from aloftresultingin the introduction of downward turbulence from aloft