Temperature
Winds
Moisture
Location
When considered in relation to weather phenomena forming over land
When considered in relation to weather phenomena forming over bodies of water.
When considered in relation to weather phenomena forming over cities
When considered in relation to weather phenomena forming over mountainous regions
Occurs in different intensities and times
Occurs in different forms
Occurs in different temperatures
It doesnt have any affect
Condensation
Evaporation
Sublimation
Fusion
Direction, speed, and gustiness
Speed, and gustiness
Direction and speed
Speed and supporting weather elements
Summation winds
Vectorial average.
Wind gust potential
Wind size
Distance and season
Time and date
Cloud cover and sung angle
Rain or shine
12 hours
6 hours
8 hours
16 hours
Creates high and low centers
Creates the seasons
Creates the summer weather
Creates winter weather
The Rockies and the Alps
The Himalayas and the Rockies
The Himalayas and the Alps.
The Chinese Ing Dun Range and the Swiss Matterhorn
Leeward sides
South side
Windward sides
North side
Northward
Southward
Eastward
Westward
Frictional effects of the wind
Precipitation
Deep underwater swells
Tectonic movement
Mountain ranges
Differential Heating
Coriolis Force
Ocean dynamics
Upwelling is the process by which the colder subsurface waters are brought to the top of the ocean
Upwelling is the process by which the warmer subsurface waters are brought to the top of the ocean
Upwelling is the process by which the colder subsurface waters are brought to the bottom of the ocean
Upwelling is the process by which ocean currents are brought to the top of the ocean
The west coast
The east coast
The gulf coast
Rivers and lakes
55–75 miles per day or 5–9 knots
55–105 miles per day or 10–15 knots
35–45 miles per day or 3–6 knots
25–75 miles per day or 1–3 knots
Middle
Beginning
End
Makes the entire system
Causes the climate to be much colder than ordinarily expected
Causes the climate to be much milder than ordinarily expected
Causes the climate to be much hotter than ordinarily expected
Does nto affect the climate there
The western coast of Northern America
The western coast of Central America
The western coast of South East America
The western coast of Modern America
The Gulf Stream system.
The North Atlantic system
The East Coast system
The Middle Atlantic system
Kuroshio Extension, Kuroshio Flow, and the North Pacific Current.
Kuroshio Current, the Kuroshio Extension, and the North Pacific Current.
Kuroshio Current and the Kuroshio Extension
Kuroshio Extension, and the North Pacific Current.
Monsoonal flow
Ocean currents
Unequal heating
Earths rotation
Lower maximums and higher minimums
Higher maximums and lower minimums
There is no noticeable effect
More precipitation annually
The Torrid (or Tropical) Zone, the two Temperate Zones, and the two Polar Zones (or Frigid Zones).
The Torro (or Extratropical) Zone, the two Temperate Zones, and the two Polar Zones (or Frigid Zones).
The Torrid (or Tropical) Zone, the two Moderate Zones, and the two Polar Zones (or Frigid Zones).
The Torrid (or Tropical) Zone, the two Temperate Zones, and the two Frozen Zones (or Freezing Zones).
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