Global atmospheric circulation and climate change Flashcards
How does the equator getting more solar radiation create air pressure
The equator gets most of the suns radiation, causing a difference in temp creating air pressure.
How does air pressure effect wind
Wind goes from areas of high pressure to areas of low pressure, which transfers heat from the equator
What is global atmospheric circulation cells
They are loops which have warm air rising creating a low pressure belt, and cool air falling, creating a high pressure belt.
What are the names of the three belts
1 Hadely, 2 Ferrel and 3 Polar cells
Why do some parts of the Earth get more solar radiation than others
The thickness of the atmosphere
The size/area of what is getting heaten up (less distrupution)
What happens to the air at low pressure
As air heats it rises and becomes less dense as it cools and condenses. As the air leaves the surface, it causes low air pressure (rainfall and clouds)
What happens to air at high pressure
When air cools it becomes more dense meaning it falls, transfering heat to the surface (clear skiesand wind)
Direction of air through the cells
From the equator (low pressure belt) the air rises to 30° north and south (high pressure belt), then 60° (low pressure belt)
What happens at 30° of the equator
Cool air sinks, creating a high pressure belt. As it reaches the ground it moves as surface winds to the equator or pole with cloudless skies
Trade winds
Surfaces winds blowing to the equator. They blow from the SE in the south hemisphere and the NE in the north hemisphere
Westerlies
Surface winds blowing towards the Pole. They blow from the NW in the south hemisphere and the SW in the north hemisphere
What happens at 60° from the equator
Warmer surface winds meet colder air from the poles. The warm air is less dense so it rises, creating low pressure and frontal rain
What happens at the poles to air
Cool air sinks creating high pressure which is drawn back to the equator as surface winds
How do ocean currents transfer heat
They are large scale movements that transfer heat energy from warmer areas to cooler areas by surface currents and deep ocean currents
Surface currents
Caused by winds, they help transfer heat away from the equator
Example of surface currents
Gulfstream brings warm water to the Carrabisn keeping Western Europe warm
Deep ocean currents
They are driven by differences in water density. As water freezes at the poles, the surrounding water gets saltier, increaing in density. This thermohaline circulation
What is thermohaline circulation
water sinks causing warmer water to rise creating a current and cycle called thermohaline circulation
Arid climate
Sinking air from hadely and ferrel cells meeting causes high pressure climate
Location of Arid areas
Approx close to the 30°
Tropical climate
Rising air from Hadely cells meeting caises low pressure
Tropical loaction
Inbetween 30°