Weather GW 3 And Plate Tectonics 🔴🔴 WE NEED WEATHER GW 1-2 Flashcards

1
Q

What are cyclones and where

A

Weather systems that dev over warm oceans in the tropics

Lat. 8-15• N and S of equator : requires warm waters in presence of coriolis effect
Warm waters: above 26.5•c
Move westward

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2
Q

Recall the pic of the cyclone cross section

A

Eye wall! Sun bands! Wind up! Rain!!

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3
Q

Cyclones: storm surges

A

Sudden rise of sea level : water is piled up against coastline beyond normal conditions. Causes property damage and massive flooding thus damage and death.

2008 hurricane ike caused storm surge between 4-6 metres in Texas. Est property damage was 24.9 bil usd

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4
Q

Cyclones: Strong winds

A

Strong force of winds damage or destroy infrastructure and injure ppl
Causes loose debris to fly and hit ppl and buildings
Large impact area

1992 hurricane Andrew had wind speeds up to 117 km per hour - widespread damage to Bahamas and parts of USA. Damage to infra and disrupted power supply - 150k homes w/o electricity

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5
Q

Cyclones: torrential rains

A

Large amt of rainfall that result in flooding inland : sudden water adds to rivers and streams- overflow

2003 hurricane Isabel flooded rivers in Virginia, Maryland, Delaware, and Washington DC in USA. Flood area abt 120 times sg, damages of >US 2.23 bil

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6
Q

Physical impacts of cyclones (2)

A

Damage to infrastructure : storm surges- huge waves crash down, flooding, damage

Disruption of comms : electrical wires topple, Comm buildings destroyed - ppl cannot go to work- econ affected // - ppl cannot seek help- death and injuries

2009 typhoon Ketsuna damaged road network in Philippines, Cambodia and Laos. 80% of health centres in Manila (Philippines) was destroyed. Difficult to distribute meds and food

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7
Q

Economic impact of cyclones (2)

A

Cost to repair infrastructure: storm surges- lots of buildings destroyed - costly repairs- less $ to dev other parts of food

Hurricane Katrina 2005 hit East Coast of USA cost 81 bil usd, large part was repair of 200k homes

Loss of income due to destroyed crops: farmlands destroyed- no crops to sell- loss of income, food shortage

Cyclone Yasu hit North Queensland Australia 2012, 75% banana crop (US350 mil) destroyed

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8
Q

Social impacts of cyclones 3

A

Disruption to water supply : water pipes burst/ contaminated

2009 cyclone alia hit West Bengal India caused cholera outbreak 1000 infected 14 deaths

Spread of diseases : flooding- breeding ground for mosquitoes (mosquito borne diseases)

Hurricane Mitch 1998, cases of dengue in Guatemala and Nicaragua due to flooding.

Displacement of ppl from homes : flooding- homes destroyed - homelessness

Hurricane Katrina struck New Orleans USA in 2005 thousands of ppl lost homes

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9
Q

Responses and measures to cyclones: emergency action

A

Emergency action- weather warnings and advisories :
evac to cyclone proof shelters, reduce death
eg. India and
Bangladesh - lower death during 2009 Aila due to network of 2500 shelters and sms warning

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10
Q

Responses and measures for cyclones : prediction and warning

A

Establishes pattern of occurrence and severity of damage: by analysing pattern, predict
Meteorologists studying 2005 Katrina warned for evacuation before 2008 Ike moved into Texas
L: records only indicate frequency, no accurate details

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11
Q

Response and measures for cyclones: regulate land use

A

Regulates land use - flood/coastal plain management
Practiced in hurricane prone areas eg. New Orleans and coastal japan and Taiwan - vulnerable to storm surges
L: authorities need to enforce the rules- req time and manpower. Coastal residents often reluctant to move out- costly to buy back land

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12
Q

Response and measures to cyclones: Reducing infrastructure vulnerability

A

Buildings designed to resistant against wind and water damage
- galvanised steel hurricane tiles on roof: not blown off
- secondary water resistant layer on roof, prevents leaking
Houses with such in Florida USA survived 2005 Wilma

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13
Q

Earthquake preparedness measure: infrastructure

A

Advanced engineering can withstand earthquake vibrations - use of steel and reinforced concrete, damping devices such as shock absorbers and heavy wide bases

Taipei 101 has a damping device: reduce swaying by up to 40%

Less destruction , less buildings collapse , less econ and lives lost

Expensive, developing countries cannot afford

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14
Q

Earthquake preparedness measure: emergency drills

A

Practice of what to do during earthquake
Japan drills - 1st September to commemorate disaster prevention day
Ppl know what to do
Ppl may panic and forget

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15
Q

Earthquake preparedness measure: earthquake and tsunami monitoring systems

A

Earthquakes monitored by study of history of when and where, est of frequency and magnitude at fault line: prediction

Earthquake motion data gathered from observation stations in Japan
Tsunami: network of pressure sensors and seismographs, deep ocean tsunami detectors located in Hawaii

Allows ppl to evac, less loss of lives

L: only a general indication, not precise. Expensive to install and use, many not provide sufficient time, false warnings

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16
Q

Earthquake short term responses : search and rescue

A

Ppl trapped in collapsed buildings are located and freed

2011, Tohoku Japan : heat sensors and sniffer dogs were deployed

Many ppl rescued, reducing death rate

Rescue ppl have 72 hours (3 days) to find survivors

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17
Q

Earthquake short term responses: emergency food and medical supplies

A

Injured treated, provide clean drinking water - prevent dehydration and disease spread

2002 Afyon, turkey - Turkish red crescent society delivered 20k rents 50k blankets and 3k heaters

Reduce loss of lives, help injured, reduce spread of diseases

Meds and food may not be sufficient : social unrest eg. 2010 Haiti, looting and fighting broke out

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18
Q

Long term responses earthquake: rebuilding of infrastructure

A

Rebuilt and improved, dev structure building codes, endeared higher safety level than before

1995 Kobe Japan, billions spent to dev tech to build more resistant buildings

Less damage to infrastructure, less cost of rebuilding, less loss of lives

Reinforced buildings not necessarily prot against tsunamis (add. prot in form of coastal structure)
Eg. Many buildings in Chile resistant, but coastal area tsunami damage in 2010

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19
Q

Long term responses earthquakes: provision of healthcare

A

Health options such as long term counselling

A year after 2011 Christchurch NZ, significant depression and anxiety amongst affected population: more health workers in area

-

Improving health options eg. Restoring resilience
can be challenging

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20
Q

Why do tectonic plates move?

A

Convection currents
1. Mantle mat heated by core
2. Expands rises spreads out
3. Plates dragged along
4. Mantle mat sinks pulling plates along
5. Heats up and repeats

Slab pull force
1. Dense sinking oceanic plates at subduction zones pull rest of plate
2. Drives downward motion of CC
3. Mantle mat away from sub zone drives rising CC

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21
Q

Internal structure of earth (the pie)

A

Crust
- basalt, granite rocks
- few km to >10km thick

Mantle
- mostly solid rock : flows under ^temp and ^pressure
- 2900km thick
- 800-3k deg celcius

Core
Mostly iron and nickel
Liquid outer and solid inner
Temps of 3000-5000

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22
Q

Divergent O-O (diagram, steps, location)

A

The tree trunk island with ocean on both sides (the ridge)

  1. 2 O plates diverge, fractures formed @ plate boundary
  2. Magma rises @ zone of divergence, creates ridge of new ocean floor (mid-o ridge)
  3. @ various points, magma builds and solidifies into undersea volcanoes
  4. Volcanoes grow above sea level -> volcanic islands
  5. Sea floor spreading occurs

Mid-Atlantic ridge , NA and Eurasian

23
Q

Divergent C-C (diagram, steps, example)

A

The layered valley thing

  1. 2 C plates diverge, resulting in faulting, forming fault lines
  2. Land between the 2 C plates sinks (forming linear depression- Rift Valley)
  3. Remaining highland - block mountain

East African Rift Valley system, Nubian and Somalian

24
Q

Convergent O-O (diagram, steps, example)

A

Goes down on one side and goes up the other. Volcano on upside with ocean around

  1. 2 O plates converge, denser O subducts beneath less dense
  2. Deep O trench at subduction zone
  3. Subducted o plante mantle melts and forms magma
  4. Magma roses thru crust to form volcanoes and island chains
  5. Earthquakes due to friction

Mariana Trench, Mariana islands ,, pacific and Philippine

25
Q

Convergent C-C (diagram, steps, location)

A

The mountains on the right and plate going down on the left

  1. 2 C plates converge so folding forming folds
  2. Upper layers of C crust fold upwards into fold mountains

Himalayas, Indian and Eurasian

26
Q

Convergent O-C (diagram, steps, example)

A

Water on left, volcano on right, mountain further right continuation. Left one goes under right one

  1. O plate and C plate converge, denser O subducts under C
  2. O trench at subduction zone
  3. C plate buckles and folds, forming fold mountains
  4. At subduction zone, sinking plate mantle mats melt to magma
  5. Magma roses forming volcano

Sunda trench, Australian and Eurasian

27
Q

Transform boundary (diagram, steps, example)

A

Two blocks going in different directions

  1. CCs pull 2 plates in parallel and opposite directions along transform boundaries
  2. Results in formation of transform fault
  3. Tremendous stress builds which is rejected in the form of violent earthquakes
  4. May result in further movement / faulting
  5. Little - no volcanic activity

North Anatolian fault - Anatolian and Eurasian

28
Q

General plate tectonics diagrams rules

A
  • label layers (crust, uppermost mantle, asthenosphere)
  • movement (arrows)
  • landforms
29
Q

Plate tectonics boundaries abs format

A
  1. Type of plate boundary (C/D/T)
  2. Type of plates (C/O)
  3. Plate movement (towards/ away/ past)
  4. Forces (compressional/ tensional/ shear)
  5. Processes + explain (subduction, folding, faulting, sea floor spreading etc)
  6. Landforms formed
  7. Specific example
30
Q

Continental plates

A
  • buoyant, do not subduct
  • instead, they fold at convergent boundaries
31
Q

Sea floor spreading

A
  1. Magma rises from mantle to form new sea floor between plates as they move apart
  2. New lava flows out onto the sea floor and cools and solidifies - mid o ridge
  3. Newly formed rocks are closer, folder are further away
32
Q

Plate boundaries (shield vs strato)

A

SH
O-O div

ST
O-O con
O-C con

33
Q

Profile (shield vs strato)

A

SH
- gently sloping base
- broad base

ST
- high
- slightly concave
- steeper at top, gentler at base

34
Q

Lava type and flow (shield vs strato)

A

SH
- Low silica/viscosity
- flows easily
- spreads over a large area before solidifying

ST
- high silica/viscosity
- more viscous
- traps gases more easily : build up of pressure

35
Q

Eruption and eruption mats (Shield vs strato)

A

SH
- not explosive
- Low silica lava

ST
- explosive
- high silica lava
- pyroclasts (ash, rock frags, volcanic bombs)
- ash

36
Q

Examples (shield vs strato)

A

Mount Washington USA

Mount Mayon, Philippines
Mount merapi, Indonesia

37
Q

Labeled diagram (shield vs strato)

A

Sloping layers of a cake with a thick strip of magma in the middle

Tall one like a traffic cone. Layers but less. One of ems thicker. Has secondary cones

38
Q

Shield volcano formation process

A
  1. CCs in mantle cause 2 O plates to diverge
  2. Molten magma erupts to earth surface
  3. Little gas and air trapped in lava : Low-silica content
  4. Successive eruptions - build up - formation of volcano w gentle slopes and broad bese
39
Q

Stratovolcano formation

A
  1. CCs in mantle - 2 O plates to converge / C&O plates to converge
  2. Heavier and denser plate subducts under less dense O/C plate
  3. Top part of subducted plate (crust?) melts to form magma
  4. Magma erupts onto earths surface as lava thru faults
  5. A lot of gas and air trapped in lava - high silica content - explosive eruption
  6. Successive eruption - build up- formation of volcano w concave, steep sides, gentle base
40
Q

Damages and dangers of volcanos (pyroclasts flows and lahars etc)

A
  • made of pyroclasts and superheated gases
  • up to 200m/s
  • pyroclasts + water
  • fast flowing mudflows
    Can engulf towns and kill ppl

Volcanic bombs can cause damage to property
Landslides can bury villages and farmland

41
Q

Pos and neg impacts of volcanoes 4, 2

A

Geothermal energy
Precious stones and minerals, building mats
Tourism
Fertile soil

Massive destruction
Pollution

42
Q

Geothermal energy (pos of volc)

A

groundwater comes in contact w hot rocks : hot water and steam : used to turn turbines and produce electricity
Renewable source to meet ppls energy needs

Most of icelands energy gen from this due to many volcanoes. Over 70% homes heated by volcanic steam

43
Q

Precious stones and minerals, building mats (pos impacts of volc)

A

Volcanic rocks can be rich in them and can only be extracted after millions of years
Can also be sold for ppl to earn a living and dev econ

Eg diamond, which are pressurised and heated carbon that are cooled in magma pipes. Refined diamonds used for industrial tools and sci research/ jewellery. Old volcanic rocks at Kimberley in South Africa - rich source of diamond

44
Q

Fertile soil (pos impacts of volc)

A

Lava and ash from volc eruptions break down to form fertile soils over millions of years. Richest soils on earth, favourable for agri
Farmers - greater harvest - more food and income

Volcanic soils in Java and Bali in Indonesia support crops like tea coffee and rice. Thus able to support large rural population.

45
Q

Tourism (pos impacts of volc)

A

Volcanic areas offer a variety of activities for tourists from scenery to history of the area
Tourism related jobs - more employment, income, benefits local econ

Pompeii Italy, the town was buried after the eruption of mount Vesuvius when it erupted in 79 CE. Almost 3 mil ppl visit the archeological site each year

46
Q

Massive destruction by volcanic materials (neg impacts of volc)

A

Lava, pyroclasts, Lahars, ash, rock fragments and volcanic bombs : widespread damage of property and loss of life

Eruption of Nevado del Ruiz in the Andes of South America in 1985 released p.flow. mixing of pyroclasts and glacial ice : lahar. It engulfed the town of armero and killed more than 20k ppl

Lava - high temps 500-1400, burns area
Low silica - rapidly over long distance
Pyroclastic flow- destruction, hot rock fragments (ash-boulders) at >200m/s
Inhaling gases and ash - injury and death
Volcanic bombs - damage to property
Landslides - obstruct rivers (floods), roads, buried villages and farmland

47
Q

Pollution (neg impacts of volc)

A

Ash particles/ clouds ejected during eruption disrupt human activities. It may settle on ground and block sunlight, suffocate crops and cause resp issues for ppl and animals. Can also release harmful gases.

Eruption of eyjafjallajökull in Iceland in 2010 produced extensive ash clouds which posed a danger to aircraft engines and structures. Closure of air space over much of Europe - delays to 1.2 mil passengers daily, cost the industry US1.8 bil

48
Q

Earthquake preparedness measures: land use regulation

A

A set of rules implemented to restrict developments in certain areas. A prohibition of constructing buildings in Low lying land vulnerable to tsunamis.

California USA all new buildings are not build across fault lines or areas at risk of liquefaction.

By not having developments at high risk areas - fewer buildings damaged - fewer ppl there - fewer deaths

When carried out on built or privately owned land, Govt has to compensate ppl who have to move - costly, ppl may be reluctant

49
Q

Eruption of strato steps

A
  1. As magma seeps into the magma chamber, amt of pressure builds up, erupts
  2. When erupt, pyroclasts released (force depends on pressure built up)
  3. New eruption of lava covers pyroclasts. Builds up volc
  4. Lava builds around vent and solidifies to form cone. Opening is called crater.
  5. Vent may become blocked - forces magma to find alt route - secondary cone
  6. Summit may be blown off during eruption - sides of crater collapse- forms caldera
50
Q

creation of the eye

A
  1. Area of Low pressure at eye as warm moist air over ocean expands and rises. 2. Condensation, releases latent heat. Continuous large scale release of it heats air, thus expanding and rising further.
  2. Reduces air pressure at earth surface, creating and sustaining area of Low pressure at centre.
  3. As warm air rises it cools and sinks. Descending dry air creates environment at center called The Eye.
51
Q

Why do cyclones need coriolis effect

A

Strong pressure gradient causes air to move inwards to the cyclone
Due to coriolis effect air moves at angle thus beginning the rotary motions.
They do not form 5 dev N and S due to weak C effect

NH- deflect right - rotate anti clockwise
SH- deflect left - clockwise

52
Q

Impacts of earthquakes 4

A
  • affected water pipes/ electricity affected
  • destruction of infrastructure
  • landslides
  • tsunamis
53
Q

Factors affecting compact of earthquakes

A
  • dist from epicentre
  • magnitude
  • time
  • population density
  • type of soil
  • level of prep