Loading ...
A Thermodynamic PathwayLeadingto Rapid Intensification of Tropical Cyclones under Shear
The primary instabilityleadsto the formation of large - scale turbulent flow structures in the shear layer
The shear - layer forcingcreatesperiodic coherent vortical structures in the shear layer that convect at the shear - layer convective velocity
the northern portion of the wave ... Islands[1]—the same troughcontributedto the development of Hurricane Ophelia.[2 ... As a result of the low wind shear
This conditioncausesnet advection of hurricane structural elements that extend into the lower stratosphere away from the hurricane center
which is typically located over the Caribbean in Maycreatinghigh wind shear that interferes with hurricane development
the jet stream , which had been farther north during summer ... southcreateshigh wind shear in the prime area for hurricane formation
Fluctuations in the horizontal wind speedcan causelocal wind shear near the top of the Stratocumulus topped boundary layer
viscosity decreases with increases in temperatureleadingto faster rates of shear at the boundary layer
to systematic phase fluctuationsleadto systematic phase fluctuations
soil - structure interaction effects on nonlinear structural response become significantcausessoil - structure interaction effects on nonlinear structural response become significant
Deep cycle mixing(passive) is triggered byDeep cycle mixing
A substantial part of this loss increase close to the wall(passive) is caused byA substantial part of this loss increase close to the wall
to increased product entrainment levelsleadto increased product entrainment levels
Fred to diminish to a tropical stormcausingFred to diminish to a tropical storm
to increased product recirculation levelsleadto increased product recirculation levels
jet noise(passive) is caused byjet noise
sea surface cooling(passive) was caused bysea surface cooling
Radial vortices 21(passive) created byRadial vortices 21