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altitude(passive) is influenced byRAIN SHADOW 5 Climate
Mountainscausethe " rain shadow effect
by the mountains(passive) caused byThe " rain shadow " effect
by the order(passive) caused bythe rain shadow effect
by the Olympic Mountains(passive) is causedThe rain shadow effect
by the Olympic Mountains(passive) caused byThe rain shadow effect
by the Southern Alps ( given New Zealand 's westerly winds(passive) caused bythe rain shadow effect
by the Himalayas(passive) caused byrain shadow effect
Massive mountainsalso causerain shadow effects
mountain rangescauserain shadow effects
the tall peaks along the Sierra Nevada(passive) caused bythe large rain shadow
mountains to the westcausea bit of a rain shadow
Bukit Timah Hill(passive) caused byRain Shadow Effect
shedcausinga small rain shadow
by the higher peaks in the western mountain variety.[90(passive) designed byrain shadow check here
especially wherecausesan " anti " rain shadow
the gapcausesan " anti " rain shadow
North Africa 's Atlas Mountains and the area 's flat topography which provides no obstacle to winds(passive) caused bythe huge rain shadow
high mountainscausingrain shadows
by the high mountains , which block the rain clouds(passive) caused bya rain shadow
by the mountains(passive) caused byrain shadows
Mountainscan causerain shadows
the mountains(passive) are caused byRain shadows
by trees and other plants that block the spray(passive) caused byrain shadows
Topography Mountainscan causerain shadows
Steep mountainscauserain shadows
Desert - like conditions ... the mountainsare causingthe rain shadow
where the weather must pass over mountainscausinga rain shadow
by the mountain(passive) caused bythe rain shadows
by steady wind(passive) caused byrain shadows
by Cascade Range(passive) caused byrain shadow
by the Cascade Range(passive) caused bythe rain shadow
by the Cascade Range(passive) caused bya rain shadow
the Cascade Range(passive) caused bya rain shadow
the Cascade Range(passive) caused bythe rain shadow
high mountainscausinga rain shadow
by the Cascade Mountains(passive) caused bya rain shadow
the Cascade Mountainscausea rain shadow
by the Cascade Mountains(passive) caused byThe rain shadow
the Cascade Mountains(passive) caused byThe rain shadow
mischiefto causemischief
This system(passive) is influencedThis system
dry area ( desertscausesdry area ( deserts
in less rainresultingin less rain
to the formation of a desertcontributesto the formation of a desert
Precipitation amounts(passive) are also influenced byPrecipitation amounts
moist conditionscan causemoist conditions
from air movingresultfrom air moving
from the subsequent adiabatic warming of air that has dropped most of its moisture on windresultsfrom the subsequent adiabatic warming of air that has dropped most of its moisture on wind
the windward side of higher elevations to becausesthe windward side of higher elevations to be
to the dry desert conditions characteristic of Central Asiacontributesto the dry desert conditions characteristic of Central Asia
major flooding causemajor flooding
from the warming of air which has dropped most of its moisture on windward slopesresultsfrom the warming of air which has dropped most of its moisture on windward slopes
one side of the mountain to have forests while the other side is desertmay causeone side of the mountain to have forests while the other side is desert
from orographic liftresultingfrom orographic lift
a river or a relativecausesa river or a relative
one side of a mountain to be drier than the othercausesone side of a mountain to be drier than the other
from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopesresultsfrom the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes
from the subsequent ( adiabatic ) warming of air which has dropped most of its moisture on windward slopesresultsfrom the subsequent ( adiabatic ) warming of air which has dropped most of its moisture on windward slopes
from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes ( see orographic liftresultsfrom the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes ( see orographic lift
from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes ( see orographic liftresultsfrom the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes ( see orographic lift
from the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes ... see " orographic liftresultsfrom the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes ... see " orographic lift
from the subsequentresultsfrom the subsequent
from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes through orographic liftresultsfrom the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes through orographic lift
from the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes ( orographic liftresultsfrom the subsequent adiabatic warming of air which has dropped most of its moisture on windward slopes ( orographic lift
from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes through orographic liftresultsfrom the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes through orographic lift
from the following adiabatic warming of air which has dropped most of its moisture on windward slopes ( orographic carryresultsfrom the following adiabatic warming of air which has dropped most of its moisture on windward slopes ( orographic carry
regular monsoon seasons.[77causingregular monsoon seasons.[77
the windward side of higher elevations to be markedly more moist than the leeward sidecausesthe windward side of higher elevations to be markedly more moist than the leeward side
in a historical average of about 20 of rainresultsin a historical average of about 20 of rain
in a historical average of about 20 of rainresultsin a historical average of about 20 of rain
due to the prevailing westerly winds from the Atlantic ocean and the abundance of hilly areas on the west side of the UKis causeddue to the prevailing westerly winds from the Atlantic ocean and the abundance of hilly areas on the west side of the UK
the Patagonian Desertoriginatedthe Patagonian Desert
the Patagonian Desert to the east.[20originatedthe Patagonian Desert to the east.[20
the Patagonian Desert to the east.[18originatedthe Patagonian Desert to the east.[18
the Patagonian Desert to the east.[21originatedthe Patagonian Desert to the east.[21
forest vegetation to diecauseforest vegetation to die
to almost desert like conditionscan leadto almost desert like conditions
the region to be too dry for much crop growthcausedthe region to be too dry for much crop growth
in the city having higher rainfall in the winter than other cities in the same arearesultsin the city having higher rainfall in the winter than other cities in the same area