convection currents(passive) created byconvection cells
random non - uniformities in the water and air(passive) can be caused byconvection cells
rising and sinking of mantle material of different temperatures and densitiescreatesa convection cell
then rise in the warm tubecreatinga convection cell
The cycle of heating and cooling continues ,creatinga convection cell
The rising and sinking of warm and cooler materialcreatesa convection cell
horizontal windscreatinga “ convection cell
The motion describedcreatesa convection cell
the plume(passive) created byConvection cells
Models based upon what we know about fluids and thermodynamics in such systems determineswill createconvection cells
density - driven salinization ( Kooi(passive) caused byconvection cells
up ... temperature differences in the room(passive) set ... byconvection cells
This cooler mantle material will begin to sinkthus creatinga convection cell
This is counteracted by the upper atmosphere air movement in the opposite directioncreatinga convection cell
The source of heat ... it is believedto createa convection cell
up ... the solder being heated from the center(passive) set ... bythe convection cell
The wind ... uneven heating and the latitude of the wind(passive) is caused byThe wind ... uneven heating and the latitude of the wind
from feedback heating of Venus ' lower clouds , J. Meteorresultingfrom feedback heating of Venus ' lower clouds , J. Meteor
what is known as granulation on the surface of the sunalso causewhat is known as granulation on the surface of the sun
even surface inhomogeneities(passive) caused byeven surface inhomogeneities
from the uneven heating of a fluidresultsfrom the uneven heating of a fluid
large variations in wind speed(passive) caused bylarge variations in wind speed
to simultaneous high solar and wind variabilityleadsto simultaneous high solar and wind variability
strong winds which may also assist in seed dispersalcreatestrong winds which may also assist in seed dispersal
a slight " wind " that blows up from the bottom , through the screen and the load , and out at the topcreatesa slight " wind " that blows up from the bottom , through the screen and the load , and out at the top
plates to collide , rip apart , and plunge back into the mantle 31causesplates to collide , rip apart , and plunge back into the mantle 31
in the form of a rolling vortex made up of a flow loop of rising and then falling gas close to the plate surfaceare createdin the form of a rolling vortex made up of a flow loop of rising and then falling gas close to the plate surface
both high and low pressure beltscreateboth high and low pressure belts
a circular pattern of movement of fluids caused by rising warm fluids and sinking cool fluidscreatea circular pattern of movement of fluids caused by rising warm fluids and sinking cool fluids
desertscreatedeserts
B. They(passive) are created byB. They
regions of high and low pressure c. a and ccauseregions of high and low pressure c. a and c
the following types of air movement in the atmosphere : local winds and Hadley cellscausethe following types of air movement in the atmosphere : local winds and Hadley cells
to atmospheric circulation patternscontributeto atmospheric circulation patterns
in the asthenosphere due to the immense heat in the Earthcreatedin the asthenosphere due to the immense heat in the Earth
Tension Convergent Compression Divergent Tensional and compressive forces(passive) created byTension Convergent Compression Divergent Tensional and compressive forces
The granular pattern(passive) is caused byThe granular pattern
as the liquid crystals flow ( rotate / revolve ) in closed patterns around the nucleus in response to this slight separation of the differently charged ionsresultas the liquid crystals flow ( rotate / revolve ) in closed patterns around the nucleus in response to this slight separation of the differently charged ions
ridges and trenches within the crustsalso createridges and trenches within the crusts
land and sea breezes , mountain and valley breezes , and monsoonscan causeland and sea breezes , mountain and valley breezes , and monsoons
hotspot in which magma drills up during a divergent boundarycreatehotspot in which magma drills up during a divergent boundary
from CFHresultingfrom CFH
and how they workare createdand how they work
to storm from lower rightleadingto storm from lower right
tectonic plates to push against each other forming mountain ranges such as the Himalayascan causetectonic plates to push against each other forming mountain ranges such as the Himalayas
a dozen or so huge rigid plates(passive) caused bya dozen or so huge rigid plates
frictional drag on lithosphere Plate /Destructive margins Subduction zones Driving Mechanisms for Plate Motionscausefrictional drag on lithosphere Plate /Destructive margins Subduction zones Driving Mechanisms for Plate Motions
their lower density(passive) caused bytheir lower density
because of the doorway further speeding the cooling processis createdbecause of the doorway further speeding the cooling process
up ... the star would by that point already be burningsetup ... the star would by that point already be burning
a breeze from you to the candlecreatesa breeze from you to the candle
material to swirl around in the atmospherecausematerial to swirl around in the atmosphere