Atmosphere And Hydrosphere Flashcards

(51 cards)

1
Q

What is air pressure

A

The force exerted on the earth’s surface by the weight of the air above it.

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2
Q

How does pressure travel? (From what to what)

A

HIGH to LOW through wind

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3
Q

How is pressure shown?

A

Shown on a map using ISOBARS, these are like contour lines except they show areas of equal pressure, rather than height.

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4
Q

What does high pressure do?

A

Often bring good weather, clear skies or predictable sun/rain. (Air is descending)

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5
Q

What does low pressure do?

A

Often creates cloudy weather, storms or unpredictable rainfall and dramatic weather changes. (Air is rising)

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6
Q

What is weather?

A

The short term or day to day weather changes.

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7
Q

What is climate?

A

Long term averages, seasons or large area averages.

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8
Q

(What type of climate?) will need to wear specialist clothing in order to be comfortable in this weather.

A

Polar

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9
Q

(What type of climate?) a tricky place to grow crops that need lots of water

A

Arid/desert

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10
Q

(What type of climate?) is doesn’t matter when you go as it will always be the same weather

A

Tropical

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11
Q

(What type of climate?) best to wear layers and take an umbrella

A

Temperate

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12
Q

(What type of climate?) Think carefully about which season to visit in.

A

Temperate

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13
Q

(What type of climate?) guaranteed sunshine in the summer - great for holidays

A

Mediterranean

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13
Q

(What type of climate?) need to plan ahead for heavy flooding in some months of the year

A

Tropical

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14
Q

(What type of climate?) need to prepare for drought in the summer months

A

Mediterranean

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15
Q

(What type of climate?) a great place to grow crops like potatoes, wheat and barley

A

Temperate

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16
Q

What is the ITCZ?

A

Inter tropical convergence zone - the eagerly trade winds in both hemispheres converge at an area near the equator called the ITCZ, producing a narrow band of clouds and thunderstorms that encircle the globe.

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17
Q

DIAGRAM* check in book (prevailing/tropical easterlies and westerlies)

A
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18
Q

Explain differential heating

A

In the polar regions, the sun rays travel a longer distance to a larger less concentrated area. Around the equator, the sun rays travel a shorter distance to a smaller less concentrated area. This creates low pressure at the ITCZ because it’s hotter around the equator so air is constantly rising, so there’s higher pressure further up in the atmosphere and there is lower pressure at ground level.

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19
Q

Which cell in the tricellular model is closest to the poles?

A

The polar cell

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20
Q

Which cell in the tricellular model is closest to the equator?

A

The Hadley cells

21
Q

Which cell in nearest to the tropics of cancer/capricorn?

A

The Ferrell cells

22
Q

DIAGRAM* check in books for global atmospheric circulation diagram full cycle

23
Q

What are the five seas?

A

Arctic, Atlantic, pacific, southern and Indian

24
DIAGRAM* of the seas on a map
25
What is a bathymetric map
Shows the topography of the ocean floor.
26
What is the continental slope
A steady incline mark
27
Seamount
Mountains whose peaks don’t break the surface
28
Abyssal plain
Thick layers of sediment, formed by dead organisms
29
Mid-ocean ridge
Made up of many peaks along the sides of a central valley.
30
Volcanic island
Erupted ocean volcanos, where lava drys on top of
31
Continental shelf
It’s width varies near the shore
32
Trenches
Underwater canyons (some of the deepest spots on earth)
33
DIAGRAM* check book for the cross section of ocean floor
34
How are the five oceans connected
By ocean currents
35
Describe what happens in the thermohaline circulation
1. Cold, salty dense water sinks at the earth’s northan polar region and heads south along the western Atlantic basin. 2. The current is “recharged” as it travels along the coast of Antarctica and picks up more cold, salty, dense water. 3. The main current splits into two sections, one travelling northward into the Indian Ocean, while the other heads up into the western pacific. 4. The two branches of current warm and rise as they travel north, then loop back southward and westward. 5. The now-warmed surface waters continue circulating around the globe. They eventually return to the North Atlantic where the cycle begins again.
36
DIAGRAM* check book for thermohaline circulation
37
What are the five factors that affect Global climate?
- latitude - altitude - global atmospheric circulation - continentality - ocean currents
38
How does latitude affect GC
Temperatures are hotter when they’re closer to the equator because the suns rays have lost less heat and a more concentrated. Lines of latitude are invisible lines that go horizontally around the globe.
39
How does altitude affect the GC
High altitude places have colder and wetter temperatures because hot air rises and leaves cold air behind while also making clouds (and rain). As well as this, the air is thinner so energy (and heat) can’t be transferred as easily.
40
How does continentality affect GC
In winter, the sea insulates the heat as it cools down more slowly than the land. This helps to keep islands like the uk warmer that other places at the same latitude. Coasts are warmer than islands in winter because the sea retains the heat for longer, but in summer, areas of coast are cooler because the sea lakes longer to heat and cools down the land.
41
How does the global atmospheric circulation system affects the GC? 
The circulation of each cell creates ares of higher and lower pressures. High pressures are warmer and clearer but low pressure is colder because hot air rises. As well as this, movements between the high and low pressures creates wind.
42
How do ocean currents affect the GC?
An example of ocean currents is the Gulf Stream which is a small part of the thermohaline circulation system. The tip of Florida is a warm and swift current that ensures the climate of Western Europe is warmer because it takes hot water and swiftly moves it to cold areas.
43
What are some macro stores of carbon
- (oceans) some of this carbon is transported into the deep ocean - (sedement) coal, oil and gas - (living organisms) photosynthesis by plankton
44
DIAGRAM* explain using the points, the carbon cycle
1. Burning fossil fuels and cement reproduction releases extra carbon into the atmosphere. 2. Use deforestation, fires and agriculture can release carbon into the atmosphere. 3. Plants and soils absorbs and release carbon. Overall they take carbon out of the atmosphere. 4. Rivers transport carbon from rock and soil erosion to the ocean where some of it is then released back to the atmosphere. 5. Photosynthesis by plankton in the ocean absorbs carbon. 6. The ocean and atmosphere exchange gases at the surface. This leads to an overall absorption of carbon. 7. Ocean circulation transports this carbon into the deep ocean, allowing the surface to take up more carbon 8. Some of this carbon is transported to the deep ocean and conform sediments 9. Coal oil and gas made from carbon buried over 1 millions of years burning. These fuels releases carbon back into the atmosphere over decades..
45
What are some causes of ocean acidification?
- human activity/burning fossil fuels - The shift in the water is chemical make up (also reduces the availability of carbonate ions) - Different releases of carbon dioxide into our atmosphere
46
What are some impacts of ocean acidification?
- The reduction in availability of carbonate ions, makes it harder/more difficult for creatures to make their shells and skeletons of calcium carbonate - Organism such as plankton, coral and mollusks struggle to make or maintain their protective or support structures - Marine biologist say that the number of species and ecosystems facing uncertain future - Coral reduction affects reef structures and weaker structures will be more prone to damage/erosion from storms - Area service homes and protections for various important fish species, 70% of the corals will be under threat - Sea grass grows, veteran carbon rich oceans, providing new foods and meeting areas.
47
What is coral bleaching?
When corals lose their vibrant colours and turn white due to the expulsion of symbiotic algae from their tissues. It occurs when corals are stressed often by changes in water temperature or are the environmental stressors, and the algae can’t survive due to the conditions.
48
What is an example of coral bleaching?
During the 1997-98 El Niño event, many coasts in the Indian Ocean (particularly the Maldives, Sri Lanka, and Kenya) experienced widespread coral bleaching.
49
What are some environmental impacts of coral bleaching?
The decline of reef ecosystems reduce biodiversity and the increased vulnerability due to other stressors.
50
What are some human impacts of coral bleaching?
Reef degradation can lead to decline and tourism job losses and tourism related industries and increased costs associated with artificial coastal defences.