Loading ...
high pressure to the north and a low over Morocco(passive) created bya gradient wind
friction between the ground and the wind(passive) are caused byWind gradients
a tightening pressure gradient(passive) are caused byGradient winds
tight barometric pressure readings(passive) are caused byGradient winds
differing barometric pressures between high and low air - pressure systems(passive) created byGradient Winds Wind
a tightening of the air pressure isobars(passive) caused bygradient winds
low and high pressure(passive) caused byGradient winds
large - scale weather systems(passive) 's caused byThe gradient wind
when large air masses move across the face of the warming earth(passive) are createdGradient winds
the edge of the vast high - pressure system currently in the North Pacific(passive) caused bygradient winds
Moisture from the ' white front ' combined with tight pressurecould resultgradient winds
The difference in velocitycreatesa wind gradient
friction between the wind , water surface and waves(passive) is caused byWind Gradient
the air flowing from an " Atlantic High " ( sometimes " Azores High " ) toward a " Columbian Low(passive) caused bythe gradient wind
the earths friction(passive) caused bythe wind gradient
this speed ... the higher it getscausesa “ wind gradient
Both the tower shadow effect andcontributethe wind gradient
the ground 's frictioncauseswind gradient
The forcesinfluencegradient wind
conditions in the Gulf of Mexico(passive) caused bya “ gradient ” wind
this speed increases the higher this speed getscausesa “ wind gradient
difference between cold water and hot aircreatesa wind gradient
as it was a large airfield without too many buildingsto causewind gradient
a reduction of 40 % to 50 % of the geostrophic wind speed aloft ... while over open water or ice , the reduction is between 10 % and 30%.[8][13][14could causea reduction of 40 % to 50 % of the geostrophic wind speed aloft ... while over open water or ice , the reduction is between 10 % and 30%.[8][13][14
a reduction of 40 % to 50 % of the geostrophic wind speed aloft ... while over open water or ice , the reduction may be only 20 % to 30%.[9could causea reduction of 40 % to 50 % of the geostrophic wind speed aloft ... while over open water or ice , the reduction may be only 20 % to 30%.[9
a reduction of 40 % to 50 % of the geostrophic wind speed aloft ... while over open water or ice , the reduction may be only 20 % to 30%.[13][14could causea reduction of 40 % to 50 % of the geostrophic wind speed aloft ... while over open water or ice , the reduction may be only 20 % to 30%.[13][14
a large bending moment in the shaft of a two bladed turbinecan createa large bending moment in the shaft of a two bladed turbine
unpredictable firescauseunpredictable fires
to sound hopping and formation of shadow zonescan leadto sound hopping and formation of shadow zones
increases of up to 5 dB over theanticipated normal propagation ... but they can cause excess attenuationlosses of up to 20 dB. Temperature gradients , however , may typically causegains or losses of the order of 5 dB. In practical termscan causeincreases of up to 5 dB over theanticipated normal propagation ... but they can cause excess attenuationlosses of up to 20 dB. Temperature gradients , however , may typically causegains or losses of the order of 5 dB. In practical terms
a pressure difference(passive) created bya pressure difference
ealy next week bringing gusty winds to the north central and eastern Gulfwill setealy next week bringing gusty winds to the north central and eastern Gulf
in light shifty conditionsresultingin light shifty conditions
in an hour of waiting until the sea breeze won ... giving the Optimist sailors 10 to 12 knots for afternoon racingresultedin an hour of waiting until the sea breeze won ... giving the Optimist sailors 10 to 12 knots for afternoon racing
turbulence for airplanescreatingturbulence for airplanes
The rolling force(passive) created byThe rolling force
a reduction of up to 50 % of the wind speed aloftcould causea reduction of up to 50 % of the wind speed aloft
from what Carney described as a strong high pressure system over Texas and low pressure over northeast Iowa producing a temperature difference between the two pressure systems causing non - thunderstorm , non - tornado induced windresultedfrom what Carney described as a strong high pressure system over Texas and low pressure over northeast Iowa producing a temperature difference between the two pressure systems causing non - thunderstorm , non - tornado induced wind
the glider 's high wingcan causethe glider 's high wing
your airspeed to drop off as you approach the groundmay causeyour airspeed to drop off as you approach the ground
a reduction of 40 % to 50 % in wind speeds ... while over open water or ice , the reduction may be only 20 % to 30 %could causea reduction of 40 % to 50 % in wind speeds ... while over open water or ice , the reduction may be only 20 % to 30 %
a reduction of 40 % to 50 % of the wind speed aloft ... while over open water or icecould causea reduction of 40 % to 50 % of the wind speed aloft ... while over open water or ice
very shifty conditions which made for some close racingcreatingvery shifty conditions which made for some close racing
your airspeed to suddenly decrease during the last part of your approachcausesyour airspeed to suddenly decrease during the last part of your approach
the formation of the dust storm over Abu Dhabi on April 2triggeringthe formation of the dust storm over Abu Dhabi on April 2
in the pilot measuring a totally misleading wind speedcan resultin the pilot measuring a totally misleading wind speed
huge differences in wind velocity between launch and flights to upper cliffscan createhuge differences in wind velocity between launch and flights to upper cliffs
a very real potential for being blown back over the upper ridge into the rotor just behind the ridge topcausesa very real potential for being blown back over the upper ridge into the rotor just behind the ridge top
the loss of airspeed on approach(passive) to be caused bythe loss of airspeed on approach
Normallyto resultNormally
similar effectscan causesimilar effects
model replicas of study sites and their surroundings ... typically at a scale of 1:400createmodel replicas of study sites and their surroundings ... typically at a scale of 1:400
from the use of the negative rootresultingfrom the use of the negative root
the disturbances(passive) caused bythe disturbances
a positive feedbackcausesa positive feedback
modular dampers that facilitate simple and more flexible damper installationhas inventedmodular dampers that facilitate simple and more flexible damper installation