Year 10 Tropical Storms And Climate Change Flashcards

1
Q

Why is the sun hottest at the equator

A

Because the sun shines in a direct way and rays don’t spread out and more condensed whereas in areas further away from sun, heat energy is spread out more making it cooler less direct

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2
Q

What happens to air at the equator

A

Heated strongly so less dense and rises to high altitude creating low pressure. This is called the equatorial zone

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3
Q

Hot air…

A

Rises, low pressure = cloud and rain

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4
Q

Cold air…

A

Sinks, high pressure = clear skies

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5
Q

What are the 3 cells called

A

Polar
Ferrel
Hadley

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6
Q

First 3 things that happen in tricellular model

A

Warm air rises as result of solar insolation cools and condenses forming clouds and rain
Air separates and moves north or south (diverges)
As air cools it begins to sink again

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7
Q

What are the next 2 things that happen in tricellular model

A

As air sinks its heated by radiation from earth then cycle repeats itself
Air moves north as well as south

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8
Q

What happens when air sinks at the North Pole

A

Air doesn’t heat so doesn’t rise
Cold and warm air mix causing warm air to rise
Warm air gets pushed up and rises over cold air - cold front

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9
Q

Conditions at equator (0*)

A

Rainforest:
Hot
wet

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10
Q

Conditions at 15*

A

Savanna:
Hot
Rain

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11
Q

Conditions at 30*

A

Desert
Hot
Dry

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12
Q

Conditions at 45*

A

Mediterranean

Warm

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13
Q

Conditions at 60*

A

Temperate
Warm/cold
Wet

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14
Q

Conditions at 75*

A

Arctic
Cold
Snow

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15
Q

Conditions at North Pole

A

Cold

Very little snow

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16
Q

How should air move

A

From high to low pressure but rotation of earth produces a problem - coriolis effect

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17
Q

What’s the coriolis effect

A

Alters direction of wind and deflects them to right in northern hemisphere and left in Southern Hemisphere

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18
Q

What type of wind does the UK get

A

Prevailing south-westerly winds

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19
Q

What direction do tropical storms travel in

A

From east to west due to earth spinning

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20
Q

What happens when tropical storms hit land

A

Lose energy source from sea
Friction from land slows them down
In northern hemisphere track right
Southern Hemisphere track left

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21
Q

Conditions for tropical storm formation

A

Ocean temp of 27* or warmer
Low pressure
Wind blowing and same direction and speed
Between 5* and 30* north and south latitude

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22
Q

How do hurricanes form

A

Strong upward movement of air draws water vapour up from ocean
Evaporated air cools and condenses forming thunderstorm clouds
As it condenses releases latent heat which powers storm and draws more water up
Thunderstorms join to form giant spinning storm
Storm developed eye
As storm carried across ocean by prevailing wind continues to get stronger from water

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23
Q

When does it become a tropical storm

A

When surface wind reach 120 km/hr

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24
Q

Where are the most intense conditions in a tropical storm

A

Outer edge of eye

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25
What's a storm surge
Body of water beneath storm being raised up as moist air being sucked into the clouds
26
Why don't tropical storms occur at the equator
Due to the coriolis effect
27
How has climate change affected the distribution of tropical storms
Seas surface temps have increased by 0.25-0.5* meaning hurricanes forming further north and south of equator, increasing distribution
28
How has climate change affected the frequency of tropical storms
Some models suggest less frequent but more intense but some just suggest more frequent
29
How has climate change affected the intensity of tropical storms
As seas surface temp increases so does intensity of hurricanes
30
Why is data unreliable before 1960
Because they didn't have the equipment or technology to measure tropical storms
31
What's a primary impact
Damage and destruction as a direct result of hurricanes
32
What's Secondary impacts
Damage and destruction that happens as a result of primary impacts (disease,contaminated water)
33
Introductory information about typhoon Haiyan
8 November 2013 in the Philippines. Originated second November in low low-pressure area several hundred km south south-east Category five on saffir Simpson scale, wind speed 315km/hr Waves as high as 15m
34
Effects of the storm
Tacloban airport badly damaged, 3000 fishing boats destroyed Buildings damaged and crops destroyed 40,000 houses damaged Over 400 m of rain lots of flooding. Lots of coastline devastated
35
Primary impacts on people of storm
Around 6300 people killed, over 600,000 people displaced and 40,000 homes damaged or flattened
36
Secondary impacts on people of storm
14 million people affected, many homeless, 6 million lost income Landslides blocked roads – no access remote areas Outbreaks of disease Looting and violence in Tacloban
37
Short-term response of storm
International aid agencies responded quickly with food and shelter 1200 shelters set up, UK sent shelter kits, French, Belgian and Israeli Hospital set up Philippines Red Cross delivered foods US aircraft assisted with search and rescue
38
Long-term response of storm
UK, Australia and Japan donated financial aid Rebuilding of road, bridges and airport facilities Rice farming and fishing was quickly re-established Thousands of homes built away from flood prone areas
39
How can the effects be reduced of storms
Windows, doors and roofs strengthened to withstand strong wins Storm drains put in urban areas to prevent flooding Sea walls built protecting important buildings from storm surge Coastal homes built on stilts so storm surge passes beneath
40
Hurricane watch
Advises people that hurricane conditions are likely
41
Hurricane warning
Advises that people should begin to take shelter and move to higher ground
42
Ways to protect houses from tropical storms
``` Shutters Stilts Building on high ground No dangerous vegetation around house Built out of strong materials ```
43
Planning in the USA for tropical storms
There is a National hurricane awareness week which educates people about potential damage and dangers ahead
44
Weather
State of atmosphere at the given time and place with respect to variables such as temperature, moisture, when velocity and barometric pressure
45
Climate
Average weather in the region over a long period of time
46
What is extreme weather
Events that are different from expected climate. Extremes can be very little of something or too much of something. Extreme weather depends on context of what is normal
47
Introductory information about Cockermouth floods
17th to 20th of November 2009 in Cumbria. Already been months of rain so soil was saturated so lots of surface run-off that last 36 hours and fowed to Cockermouth By the 20th river Derwent it was 10 m wider than normal and river Cockers flow was greater than the past 30 years
48
Secondary impacts on people of flood
River water contaminated with sewage – health risks 1500 homes flooded and caused £100 million of damage Debris transported by revert destroyed six important regional bridges
49
Social effects of the flood
Police officer Bill Parker killed by collapsed bridge in Workington, many people were injured
50
Economic effects of the flood
Many businesses closed and didn't reopen for a long time
51
Environmental effects of the flood
River Derwent banks eroded, causing landslide | River tore loose, carrying away hundreds of trees, damaging ecosystems
52
Short term responses to flood
Civil defence and emergency services rescue people using boats and helicopters
53
Long-term response to flood
Structural engineer's went to every bridge making sure it was secure either strengthened or demolished Government pledged £1 million to help the town Business has improved shopfronts and rebuilt town centre
54
How can the effects of the flood be reduced
£4.5 million spent on flood defences Mobile wall built so that it doesn't affect of you Environment agency provided people with improved flood warning info During winter railway companies tweet info and pictures of fallen trees so people avoid that route to work
55
Long-term responses to the flood
Flood defence half a metre higher reinforced concrete walls bridge replaced in 2010 as old one collapsed Glass panels on wall, protect view Floodgates added 120 m of high wall with automatic barrier
56
What is a top down approach
Actions taken by government to increase of population resilience to a hazard
57
What is a bottom up approach
Actions people take to increase their resilience to a hazard
58
2003 heatwave
Highest UK recorded temperature 38°C in Kent | More than 2000 people died
59
2007 floods
Several people died and many left homeless by summer floods in Hull, Sheffield and Gloucestershire
60
2008 floods
Severe flooding in south west and north east England with Somerset, Worcestershire and Northumberland badly hit
61
2009 heavy snow
Southeast and Southwest England badly affected by heavy snow. 20 cm fell in London
62
2009 floods
Cockermouth in Cumbria was hit by floods record rainfall in the lake district
63
2010 heavy snow
Much of the UK hit by heavy snow in December | Northern Ireland record low temperature of -18.7°C at Castlederg
64
2013/14 floods
Severe floods in south England causing Thames to burst banks and Somerset inundated water wettest winter in 250 years
65
2015/16 floods
Bad storms and high rainfall in north England. December 2015 wettest warmest ever recorded in the UK
66
What's a jet stream
Fast band of high winds in the atmosphere between the Ferrel and Polar cells
67
Dendrochronology
Bigger ring, better growth | Problem – very few trees exist older than 4000 years before present
68
Ice cores
Layers of ice built up over thousands of years. Removed using ice cores Thicker the layer of ice the more snow fall that year. shows oxygen and methane levels records go back 800,000 years
69
Sedimentary evidence
Deeper the sediment, older it is | Sediment can be drilled out showing remains of organisms and plankton revealing sea temp
70
Solar output
Output of sun increased from 1900-1940 recorded by satellites using radio meters. Output of sun barely changed in last 50 years so can't cause climate change since the 70s
71
Orbital changes
Orbit changes shape every 100,000 years changing distance between earth and sun. Earths axis is tilted when increases climate exaggerates Tilt moves every 4000 years
72
Volcanic activity
Temporarily cause climate change e.g mount pinatubo causing global drop in temp by 0.5* due to SO2 released which causes volcanic aerosol to reflect sunlight away from earth
73
Fossil fuels
Count for over 50% global greenhouse gas emissions | As population grows increase demand for energy which increases fossil fuel use
74
Agriculture
Contributes 20% global greenhouse gases Large amounts of methane produced as cows produce it in digestion As population grows, increased demand for meat
75
Adaptation
Actions to adjust to natural events e.g climate change to reduce potential damage, limit impacts and take advantage of opportunities or cope with consequences
76
Mitigation
Reduce or eliminate long term risk to human life and property from natural hazards such as building earthquake proof buildings
77
Alternative energy production
Reduces CO2 output, uses renewable energy sources Method becoming cheaper and more competitive Very expensive For solar there isn't always sun
78
Carbon capture and storage
Replicates way earth stores CO2 pumps CO2 into ground to store it Can be used in existing power plants (don't need new ones) Could provide 10-55% of worlds carbon mitigation until 2100 can remove CO2 from atmosphere Very expensive no long term results
79
Afforestation
Planting trees to use up CO2 in photosynthesis Could increase forest carbon storage 28% Trees take a long time to grow
80
International agreements
Reduce global emissions by setting up agreements Some countries more responsible for climate change than others Hard to convince some countries to take part