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to neutral stability(passive) is setAtmospheric stability
The air pollution essay introduction of water vapours in the airinfluencesatmospheric stability
the atmosphereresultsin atmospheric stability
remotely forced changes in subsidence aloft(passive) caused byatmospheric stability
daytime sensible and latent heat fluxes ... important factorsinfluenceatmospheric stability
the advection of colder , drier air above the current ( Lee - Thorp et al .(passive) created byunstable atmospheric stability
a change in the temperature and moisture profiles(passive) caused byatmospheric stability
a weakening of the global circulation(passive) caused byatmospheric stability
the vertical temperature distributioninfluencesatmospheric stability
The latitudinal temperature gradient between the Equator and the polesinfluencesatmospheric stability
the temperature layers influencing the vertical movement of the air particles(passive) caused byatmospheric stability
high pressuresleadingto atmospheric stability
Temperature inversion periodsinfluencingatmospheric stability
north - western part of Indiaresultingin atmospheric stability
TT warming(passive) caused byatmospheric stability
Forestscontributeto atmospheric stability
a strong inversion ... the surfaceresultsin atmospheric stability
because it travels throughout the Atlanticcreating nonethelessextra atmospheric stability
the additional heat over citiescreatedatmospheric stability
this upper - level warmthcreatingatmospheric stability
significantlyinfluencessignificantly
in emission rates that more closely matched emission rates from the sonic method than Pasquill - Gifford methodsresultedin emission rates that more closely matched emission rates from the sonic method than Pasquill - Gifford methods
to downward refraction resulting from changes in the sound speed gradient alter the character and level of AM measuredleadto downward refraction resulting from changes in the sound speed gradient alter the character and level of AM measured
an error of −1 to +1 m / s in the SAR retrieved wind speed when using the GMFs that do not take into account the effect of atmospheric stabilitycan causean error of −1 to +1 m / s in the SAR retrieved wind speed when using the GMFs that do not take into account the effect of atmospheric stability
to ‘ F ’ using Pasquill Stability Classes , with ‘ A ’ being extremely unstable conditions and ‘ G ’ being extremely stable conditions [ 11is setto ‘ F ’ using Pasquill Stability Classes , with ‘ A ’ being extremely unstable conditions and ‘ G ’ being extremely stable conditions [ 11
from tropospheric temperatures that are warm relative to SSTresultingfrom tropospheric temperatures that are warm relative to SST
to dry conditionsleadsto dry conditions
the dissipation of the waves by turbulencepreventsthe dissipation of the waves by turbulence
pollution dispersionpreventspollution dispersion
up - drafts and windy conditions and raising the potential for the off - target movement of spray dropletscreatingup - drafts and windy conditions and raising the potential for the off - target movement of spray droplets
The meteorological parameters influencing eddy diffusivity and velocity profiles(passive) is influenced byThe meteorological parameters influencing eddy diffusivity and velocity profiles
highlyinfluenceshighly
to enrichment of air pollutantscontributesto enrichment of air pollutants
the development of convective weather systemsinfluencingthe development of convective weather systems
isotopic composition(passive) caused byisotopic composition
1 lt9 12 Cloud development(passive) is triggered by1 lt9 12 Cloud development
in turncausedin turn
Deposition velocities , ranged from – 60 to 20 mm / s , appeared(passive) to be mainly influenced byDeposition velocities , ranged from – 60 to 20 mm / s , appeared
in relatively sunny , dry weather for much of Oregon ( Bierlmaier and McKee , 1989resultsin relatively sunny , dry weather for much of Oregon ( Bierlmaier and McKee , 1989
to our current quality of lifecontributesto our current quality of life
to weakening of the northern portion of the squall lineleadto weakening of the northern portion of the squall line
shelterbelt efficiencywill ... influenceshelterbelt efficiency
the volcanic cloud [ 45was influencingthe volcanic cloud [ 45
This behaviour(passive) could be caused byThis behaviour
to typical arid subtropical conditions in June , July ... August with high maximum temperature valuescan leadto typical arid subtropical conditions in June , July ... August with high maximum temperature values
to increased time required for vortex dispersalwould have ... contributedto increased time required for vortex dispersal
the observed vertical distributions of BrO(passive) are influenced bythe observed vertical distributions of BrO
to convective precipitationleadingto convective precipitation
to biodiversity loss and water scarcityleadingto biodiversity loss and water scarcity
a biological cloudinfluencesa biological cloud
relative buoyancy of the wakecausesrelative buoyancy of the wake
conventional shear - driven boundary layers(passive) influenced byconventional shear - driven boundary layers
the extinction of the dominant dinosaur species of the timecausedthe extinction of the dominant dinosaur species of the time
Pinot and GuschlbauersetPinot and Guschlbauer