Global Hazards Flashcards

(43 cards)

1
Q

Define Weather

A

The day to day conditions of the atmosphere.

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2
Q

Define Climate

A

The average weather recorded over at least a 30 year period.

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3
Q

What are the 3 types of cells in the Tri-cellular model?

A

Polar Cells
Ferrel Cells
Hadley Cells

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4
Q

Explain the Tri-cellular model

A

ITCZ: Intense heating from sun at equator creates rising air + low pressure = Hot, wet climate

• Rising air is pushed north at Equator, cooling and descending around 30 degrees and then rises, creating high pressure + clear skies = Hot, dry climate (Replicated in southern hemisphere)

Polar Cells: Cold air descends and creates high pressure. Winds blow South/North and rise, causing low pressure on opposite side (cold, dry climate in cell).

• The rising and falling of winds of high and low pressure creates Hadley and Polar cells, they don’t meet which creates the Ferrel cell

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5
Q

What is High Pressure and Low Pressure?

A

High Pressure: When an air mass descends and presses down on Earth.

Low Pressure: When an air mass rises through the Earth’s atmosphere.

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6
Q

Describe how circulation around a Hadley cell works

A

• At the equator, warm air rises and creates low pressure and precipitation: the ITCZ
• North/South of the Equator, cool air sinks and creates high pressure (forming a warm + dry climate)
• As warm air rises its movement is determined by winds that cause it to constantly move around the cell

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7
Q

Affect of Latitude on Temperature

A

• Due to earth’s curvature some areas are affected by more concentrated solar rays (eg. Equator)
• The shorter the distance the sun’s rays pass through, the less radiation that can be reflected
• This creates higher temperatures in exposed areas like the Equator and Lower temperatures in the poles as the sun is heating a larger area due to the Earth’s axis

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8
Q

Affect of Altitude on Temperature

A

• High altitude = low air pressure + colder temperatures
• -1 degree per 100m of altitude

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9
Q

Affect of Winds on Temperature

A

• Surface winds move heat between different pressure belts
• Trade winds blow from high pressure to low pressure belts

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10
Q

Affect of Albedo Effect on Temperature

A

• How much surfaces absorb/reflect solar rays
• Polar caps = high Albedo + cold climate
• Rainforests = low Albedo + hot climate

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11
Q

Affect of Cloud Cover on Temperature

A

• Clouds reflect sun’s rays
• Thicker cloud cover reduces temperature
• Insolation is stronger the less cloud cover ( more rays reach earth’s surface)

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12
Q

Affect of Ocean Currents on Temperature

A

• Ocean currents move heat across the globe
• Example: North Atlantic Drift; Cold Peruvian Current but warms UK through circulation

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13
Q

Define Precipitation

A

Condensed water vapour that forms clouds and is released as either rain, sleet, hail or snow.

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14
Q

What is Convectional Rainfall?

A

• Where the sun warms up ground + air
• Warm air rises as convection currents and cools at high altitudes
• Cool water vapour condenses and forms clouds

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15
Q

What is Frontal Rainfall?

A

• Where warm air meets cold air: A Front
• Warm air rises over cool air + forms clouds
• Eventually form steady rainfall, common in the UK

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16
Q

What is Relief Rainfall?

A

• Where winds force warm air to rise at mountains
• Cooling, condensation and precipitation on windward side
• Air descends on leeward side and forms rain shadow

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17
Q

What are the wettest and driest places on Earth?

A

Wettest = Khasi Hills, Northern India
Driest = The Atacama Desert, Chile

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18
Q

What is a Tropical Storm?

A

A powerful, rotating storm in the tropics : known as Cyclones, Hurricanes and Typhoons.

19
Q

What are Katabatic and Trade Winds?

A

Katabatic: Downslope winds caused by gravity causing high density air masses to fall on lower density air masses.

Trade: Winds that blow from high to low pressure belts.

20
Q

Where are Tropical storms found?

A

Hurricanes: North + Central America
Typhoons: East Asia
Cyclones: All around Indian Ocean + Eastern Australia

21
Q

Where are Droughts normally found?

A

Areas around the Tropics of Capricorn and Cancer

22
Q

What are the characteristics of Tropical Storms?

A

• Form over tropical areas
• Wind speeds of 120+ km/h
• Diameter of at least 650km
• Severe + extreme weather lasting for 6-14 days

23
Q

What is a Drought?

A

Periods when there is much less precipitation over a specific time than is usual for the area.

24
Q

What are the characteristics of Droughts?

A

• Long periods of high air pressure
• More evaporation than precipitation
• Food shortages, hunger and death
• Varied features based on location

25
What are the causes of Tropical Storms?
**Ocean Surface Temperatures**: 26.5+ degrees, gives storms enough energy to form **Ocean Depth**: 60m+ deep to provide sufficient amount of evaporation **Coriolis Effect**: Spinning of Earth creates winds that cause spiral shape of storms **Low Air Pressure**: Low air pressure sucks in trade winds at ocean surface and absorbs moisture quick enough for the storm to grow.
26
How are Tropical storms measured?
The Saffir-Simpson Scale
27
What makes weather extreme?
High intensity or volume of various weather conditions that cause danger to life or civilisation.
28
What are the extreme weather conditions associated with Tropical Storms?
• Strong Winds of 120+ km/h • **Heavy Rainfall** (leads to Flash flooding + mass movement) • Storm surges (dangerously high rise in sea level)
29
What industries do Tropical Storms affect?
Tourism Fishing Shipping Transport
30
What is El Niño?
When trade winds that blow from east to west are weaker, increasing the surface temperature of the ocean and causing increased rainfall in South/North America and decreased rainfall in Australia/Asia.
31
What is La Niña?
Where the trade winds are stronger and cause decreased ocean surface temperatures: resulting in increased rainfall in Australia + Asia and weaker rainfall in North + South America.
32
What effects does El Niño have on Asia?
• Food + water shortages • Bush fires and poor air quality • Power cuts in countries reliant on hydroelectric power (eg. Nepal)
33
What are the 4 types of Plate Boundary?
Conservative Constructive Destructive Collision
34
What is a Hot Spot?
A place where magma rises up through very thin oceanic crust and creates volcanic activity.
35
What is a Constructive plate boundary?
• Where two plates are pulled apart by convection currents • Magma rises up to fill the gap • This forms a shield volcano and can cause earthquakes • The magma hardens to form crust, sometimes high enough to create volcanic islands
36
What is a Conservative plate boundary?
• Where two plate boundaries are moving past each other • The movement creates a build up of pressure and friction • The plates lurch past each other and release the pressure as earthquakes
37
What is a destructive plate boundary?
• Two plates are moving towards each other • Subduction of less dense oceanic crust and formation of deep ocean trench • Continental plate is crumpled to form fold mountains • Build up of friction and pressure released as earthquakes • Magma forces to surface forms composite volcano
38
What is a collision plate boundary?
• Two continental crust plates are push together by convection currents • They collide and force each other to fold upwards and form fold mountains • The collision creates violent earthquakes
39
Characteristics of Shield Volcanoes
• Found at constructive plate boundaries • Gentle eruptions as no trapped gases by rising magma (low pressure • Basic, runny lava that flows quickly • Gentle slope/gradient (like a shield)
40
Characteristics of Composite Volcanoes
• Found at destructive plate boundaries • Contains trapped seawater + hot gases that build up pressure • Dangerous, explosive eruptions with viscous lava • Steep sides and composite layers of cooled ash and magma • Cooled rock can form plug at top of volcano (building up even more pressure each eruption)
41
Characteristics of Shallow-focus Earthquakes
• Form 0-70km below Earth’s surface • Common earthquakes at all boundaries (except constructive) • 1.0-5.0 on Richter scale • Horizontally radiating seismic waves • Widespread damage
42
Characteristics of Deep-Focus Earthquakes
• Form 70-700km below Earth’s surface • Rare earthquakes only at destructive plate boundaries (need subduction) • 6.0-8.0 on Richter Scale • Vertically radiating seismic waves • Localised damage
43
How can buildings be designed to withstand Earthquakes?
• Deep foundations • Strong safety glass • Shock absorbers in framework • Cross bracing structure in roof to prevent collapse • Dampers in roof to reduce sway • Automatically shutting down gas pipes