Unit 2 - The natural environment Flashcards

1
Q

Structure of the earth

A
  • Crust - 100km thick - oceanic & continental crust
  • upper mantle - 400km deep 100-1300˚C
  • Lower mantle - 700km deep 200-2500˚C
  • Outer core - 2900km deep 2500-3000˚C
  • Inner core - 5150km deep 4000-5000˚C
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2
Q

Oceanic crust

A

Thin but very dense

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3
Q

Continental crust

A

Thick but less dense

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4
Q

4 types of plate boundaries

A
  • Divergent
  • Convergent
  • Collision
  • Transform
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5
Q

Divergent plate boundary

A
  • Two plates move apart
  • Magma rises and fills gap - erupts as Laval and solidifies to make new crust
  • Also known as a constructive boundary
  • Example: Mid-Atlantic ridge - North American and Eurasian plate
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6
Q

Convergent plate boundary

A
  • Plates move towards each other
  • When continental and oceanic plates come together - denser oceanic sinks and continental rises - forms subduction zone
  • Friction between plates and the mantle melts oceanic crust
  • Magma rises and erupts as a volcano
  • Also known as a destructive boundary
  • volcanoes and earthquakes occur
  • Example: Nazca plate subjects under South American plate
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7
Q

Collision plate boundary

A
  • When two continental plates of similar densities move towards each other
  • Crust pushed up and forms fold mountains
  • Only earthquakes occur
  • Example: Himalayas growing with Indian & Eurasian plate
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8
Q

Transform plate boundary

A
  • Plates move pas each other in opposite directions or in same direction at different speeds
  • Also known as a conservative boundary
  • Volcanoes and earthquakes occur
  • Example: San Andreas Fault - USA
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9
Q

Convection currents in the mantle

A

Hotter less dense material due to outer core rises and colder denser material sinks

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10
Q

Cause of earthquakes

A
  • Convection currents cause movement of plates
  • Plates can get stuck and build up pressure
  • When pressure is too high the boundary suddenly moves
  • All stored energy is released in seismic waves
  • Waves move through the crust and cause shaking
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11
Q

Focus

A

The point underground where the release of seismic energy happens

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12
Q

Epicentre

A

The point above the focus on the surface of the crust

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13
Q

Scales of earthquake magnitude

A
  • Richter scale - energy released
  • Moment magnitude scale - distance the fault line has moves
  • Mercalli scale - visible damage
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14
Q

Causes of volcanoes

A
  • Formed when ruptures on the crust allow lava, volcanic ash and hot gases to erupt
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15
Q

Features of volcanoes

A
  • Magma chamber
  • Layers of ash and lava
  • vent
  • Crater
  • Lava flow
  • Ash cloud
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16
Q

Places where volcanoes occur

A
  • Divergent plate boundaries
  • Convergent plate boundaries
  • Hot-spots - areas of super-heated plumes of magma under the crust
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17
Q

Active volcano

A

Erupts regularly

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18
Q

Dormant volcano

A

Potential to become active, gap of eruptions from less than a year to over 10000

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19
Q

Extinct volcano

A

No activity detected in human history - will not erupt again

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20
Q

4 types of Volcanoes

A
  • Stratovolcano/composite
  • Shield volcano
  • Cinder cone
  • Fissure vent
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21
Q

Stratovolcano/composite

A
  • Forms at convergent boundaries
  • Erupts violently and unpredictably
  • Lava is thick and slow moving
  • Steep sides and classic cone shape
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22
Q

Shield volcanoes

A
  • Forms at divergent boundaries and hot-spots
  • Eruptions are less explosive and more predictable
  • Lava is runny and flows for long distances
  • Gently sloping sides
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23
Q

Cinder cone

A
  • Hot lava and ash blasts into the air
  • Substances cool, fall and stick to the cone’s slope as opposed to flowing
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24
Q

Fissure vent

A
  • Linear volcanic vent where lava erupts
  • Often few meters wide and kilometers long
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25
Factors that increase risk and vulnerability
- Urbanization - densely populated areas with less robust buildings increases vulnerability - Economic development - LEDCs have poorer infrastructure, planning, preparation, healthcare, systems and emergency responses
26
Primary effects
Direct result of earthquakes or eruption
27
Secondary effects
As a result of primary effects
28
Primary effects of volcanic eruptions
- Deaths and injuries - Crop damage - Roads and infrastructure damage
29
Secondary effects of volcanic eruptions
- Spread of disease - Homelessness - Shortage of resources - Loss of jobs and businesses - Transport difficulties - Tsunamis - Mudflow - Fires
30
Primary effects of earthquakes
- Deaths and injuries - Road and infrastructure damage
31
Secondary effects of earthquakes
- Spread of disease - Homelessness - Shortage of resources - Loss of jobs and businesses - Tsunami - Landslides - Fires
32
Causes of volcano effects
- Pyroclastic flow - Lava flow - Tephra - Volcanic bombs - Toxic gas cloud
33
Causes of earthquake effects
- Collapse of buildings - Falling objects
34
Reducing risk of earthquakes
- Earthquake resistant buildings - Education - drills, practice and planning - Hazard mapping - identify areas of high risk
35
Features of earthquake resistant buildings
- Reinforced elevator shaft - Automatic shutters to prevent glass falling - Fire-resistant materials - Deep foundations - Rubber shock absorbers in foundation - Flexible joints for building to move - Interlocking steel frame - Counterweights on roof for vibrations
36
Predicting volcanoes
- Seismometers - detect tremors in ground before eruption - Tiltometer - detect changes in angle of slope - magma chamber grows - Gases - gases released in increasing quantities before eruption e.g. CO2 - Satellite observation - hot areas detected under earth's surface - Helicopter observation - aerial perspective can show danger under the surface - Volcano's history - frequency and violence of previous eruptions - Volcanologist - people skilled at predicting volcanoes
37
Pyroclastic flow
Mixture of ash, pumice and hot gases that flows down a volcano
38
Lahar
Fast deadly mudslide made of water, mud and volcanic debris
39
Opportunities of volcanoes
- Fertile soil - high in magnesium and potassium - Popular attraction - good for tourism industry - Rare metals - gold, copper, zinc, silver, rubies and diamonds - Geothermal energy - heat from rising magma
40
Drainage basin
An area of land which a river and its tributaries drain water from
41
Watershed
- Edge of the drainage basin
42
Source of the river
- Where the river starts - Located at high elevation - Usually takes form of a spring in a mountain range or glacier melting
43
Mouth of the river
- End of the river - River water leaves the drainage basin to flow into a sea, ocean or sometimes a lake
44
Tributaries
- Other small rivers
45
Confluence
- The point at which two rivers meet
46
Hydrological cycle
- The movement of water into, around and out of the drainage basin
47
Inputs
- Where water is added to the drainage basin system
48
Flows
- Processes by which the water within the drainage basin moves
49
Stores
- Where water is stored to be moved in the future
50
Outputs
- Where water leaves the drainage basin system
51
Types of inputs for a river
- Precipitation - Water released from clouds as rain, snow, sleet or hail
52
Types of stores for a river
- Interception - trees, vegetation or man-made objects stop precipitation reaching the land - Surface Storage - Soil moisture - Groundwater
53
Types of flows for a river
- Infiltration - Surface water and precipitation soaks into the soil - Percolation - Overland flow - Water flowing across the surface of the land - also called surface run-off - Through flow - Water travels through the soil towards a river or lake - Groundwater flow - Movement of water through rocks creating underground water stores called aquifers
54
Types of outputs for a river
- River channel - Evaporation - Surface water is heated by the sun and rises into the sky as water vapor - Transpiration
55
Bradshaw Model
- Discharge, width, depth, speed of flow and load quantity increases downstream - Load size and gradient decreases downstream
56
Long Profile of the upper course of a river
- Higher reliefs as nearer to source - Narrow and shallow - Steep gradient of land - Features such as rapids, potholes and waterfalls - Vertical erosion since water is moving rapidly & is turbulent
57
Long Profile of the middle course of a river
- Relief is less steep - Key features are meanders, oxbow lakes and flood plains - River is wider and deeper & Average speed of flow of water is higher - Main erosion is lateral
58
Long Profile of the lower course of a river
- Relief is mainly flat - Key features are levées and deltas
59
4 types of erosion in rivers
- Hydraulic action - Abrasion/Corrasion - Attrition - Solution/Corrosion
60
Hydraulic action in rivers
- Force and impact of moving water on banks and bed - air gets trapped in cracks and chunks break off as pressure increases
61
Abrasion / corrasion in rivers
- Sediment carried by the river rubs against the banks and beds - largest cause in a river
62
Attrition in rivers
- Sediment carried by the river crashes into each other and the banks - material becomes smoother and rounder
63
Solution / corrosion in rivers
- Rocks dissolve in water or minerals e.g. limestone
64
Vertical erosion in rivers
Erosion is predominantly downward - happens when water is moving downstream from the source in the upper course
65
Lateral erosion in rivers
- Erosion is predominantly sideways and tends to occur in the middle and lower courses
66
4 types of transportation in rivers
- Suspension - Solution - Traction - Saltation
67
Suspension in rivers
- Fine, light material carried along the river within the channel - not much energy needed
68
Traction in rivers
- Large boulders and rocks rolled along the river bed - too heavy to be picked up and carried
69
Solution in rivers
Minerals dissolved in water and hence are being transported
70
Saltation in rivers
- Small pebbles and stones bounced along the river bed - river has enough energy to pick up medium sized material but can't carry it far
71
Deposition in rivers
- River starts to deposit because from source to mouth, gradient reduces and therefore energy for unit water decreases - Large material is deposited first and finest material carried to the lower course to make flood plains & levées
72
V - Shaped valleys - rivers
- Vertical erosion via abrasion & hydraulic action & solution results in steep sided - Sides are weakened by weathering & vertical erosion - Gradual mass movement of material down the valley creates the v shape - Loose material can be transported - Can have interlocking spurs, narrow river channel and large angular boulders due to hydraulic action
73
Waterfalls & gorges - rivers
- Layer of hard rock is located over a layer of soft rock - Soft tock is eroded by hydraulic action and abrasion - Plunge pool is created & erodes backwards - Layer of hard rock left - overhang - Eventually collapses due to a lack of support - Causes waterfall to retreat upstream - creates a gorge
74
Potholes - rivers
- Caused by abrasion - Fast-flowing river causes water to swirl in areas where bed is not flat - Material e.g. pebbles carried by the river create small holes through abrasion - Material can get trapped and wear away the river bed even more - causes potholes
75
Meanders - rivers
- Water is pushed to outer bend - creates a faster flow - Faster water can transport more material - causes greater erosion via abrasion - can create a river cliff - Water flows slowly on the inside of the meander - less material & deposition which leads to a slip-off slope
76
Oxbow lakes - rivers
- Oxbow lake forms from the outside of the meander having faster flow and hence erosion - Particularly in flood, the river will erode through the narrow part between the loop to make a straight channel for water to travel faster - Leaves an oxbow lake
77
Flood plains and levées - rivers
- Fine material carried in the river via suspension - High precipitation causes flooding - water breaks over top and spreads across the floor plain - Friction at river banks as flood water leaves - causes largest & coarsest material to be deposited at channel edges - creates levées - Finer material carried further across the flood plane - material known as alluvium - Levées help hold more water and reduce flooding but can raise level with increased deposition
78
Deltas
- Forms at mouths of largest rivers - Flat area of sand and silt built into the sea and formed by deposition - River carrying large volumes of fine material enters a sea or lake - Speed of flow of the river slows due to decrease in relief and causes load to be deposited in layers - River then creates smaller channels - distributaries due to deposited materials forming small islands and diverting the main channel - Over time - deposited material builds out into sea - creating the delta
79
Opportunities of rivers
- Access to water for domestic use e.g. cooking, cleaning and drinking - Access to water to use in manufacturing - Access to water to irrigate crops and use in farming - Rivers used to transport goods from one town to another - Hydroelectric power - Recreation e.g. tourism, fishing - Flood plains create flat land suitable for building on as well as roads & transport routes - Deposition of alluvium creates fertile soils that farmers can use to grow crops
80
Hazards of rivers
- Flooding can occur which can lead to: - Death & injury - Flooded and damaged homes - Lower property values and higher insurance costs for houses that are at risk of flooding - Disruption or destruction to transportation routes - Crops can be lost from farm land and livestock at risk of drowning - Damage to leisure facilities e.g. riverside parks or golf courses
81
Flood hydrograph
- Chart that shows how discharge of a river reacts to a storm event - used to help manage the impact of flooding
82
Hard engineering
- Building costly permanent structures that will affect river flow and stop water from causing damage & destruction
83
Hard engineering examples
- Dams - Hold back water and can be used for hydroelectric power, water storage and tourism - can also form reservoirs - Barriers & flood walls - can control or stoop load waters from entering the city - can be expensive and stop ships moving up & downstream - Embankments or artificial levées - Increase amount of water which can be stored within the river channel - raise level of river channel and can increase severity of flooding - Dredging and straightening river channels - removes silt from river bed and increases water that can be stored to reduce floor risk - can increase risk & severity downstream
84
Soft engineering
- Alternatives that work with the river and don't involve permanent structures or a lot of construction - cost less
85
Soft engineering examples
- Afforestation - increasing number of trees in the area to increase interception and lag time to reduce peak discharge - Flood zoning Land of little value allowed to flood to prevent downstream flooding - Land-use zoning - Buildings of little or no cost built in areas of risk
86
Flood protection methods
- Procedures to attempt to protect people and property from a flood - Stores of sand & sandbags to build emergency flood barriers - System of sirens & warnings - Evacuation procedures that local emergency services are aware of and have practiced - Temporary, moveable metal barriers that can be installed quickly to protect individual houses
87
Waves
- Caused by wind - created by friction between the wind and the surface of the water - Size is affected by wind speed and fetch
88
Fetch
- The distance that the wave travels
89
Swash
- When water moves up the beach towards the land - usually approaches at an angle due to the prevailing wind
90
Backwash
- When the water flows back down the beach towards the sea - moves at a right angle to the beach
91
Constructive waves
- Low & wide - Long wavelength, low frequency - Swash is stronger than the backwash - Material is deposited adding to the size of the beach - Forms a wide, sloping beach
92
Destructive waves
- High & steep - Short wavelength, high frequency - Stronger backwash than swash - Material is removed from the beach by the waves - Waves erode the beach
93
4 types of coastal erosion
- Hydraulic action - Abrasion / corrasion - Attrition - solution / corrosion
94
Hydraulic action - coasts
- Waves break against the cliffs - water & air into cracks in the rock - pressure forces cracks to get bigger and eventually break rocks apart
95
Abrasion / corrasion - coasts
- Waves carry rocks and sediment that scrape against the cliffs as waves hit them - erode cliffs
96
Attrition - coasts
- Rocks and sediment within the waves hut each other - breaks them into rounder smoother pieces
97
Solution / Corrosion - coasts
- Seawater dissolves some of the coastal rocks
98
Factors that affect rate of erosion on coasts
- Rock type - Wave strength - Coastline shape - Exposure to waves and wind
99
- Discordant coastline
- More resistant and less resistant rocks formed in alternating bands at right angles to the coast - creates headland and bays
100
Concordant coastline
- Rocks are parallel to the coastline - erosion happens evenly
101
4 methods of transportation in coasts
- Traction - larger materials rolled by waves - Saltation - sediment bounces along by force of the water - Suspension - small sediment suspended - Solution - soluble minerals dissolved in the water
102
Longshore drift
- Overall process by which material is moved along the beach
103
Erosional landforms - Coasts
- Cliffs - Wave-cut platform - Cave - Arch - Stack - Stump
104
Cliffs - coasts
- Vertical faces of rock formed by erosion and weathering - most formed by one type of rock, hence concordant coasts
105
Wave-cut platform - coasts
- Erosion at the bottom creates a wave-cut notch - hydraulic action and abrasion - Notch gets larger until the cliff above can't be supported - Cliff collapses and moves backwards - creates a wave-cut platform
106
Cave, arch, stack & stump - coasts
- Headland is eroded by hydraulic action & abrasion - Cracks get larger and form a cave - Cave gets larger and erodes into an arch - Arch becomes thinner and can't be supported - Collapses and leaves a stack - Over time the stack erodes into a stump
107
Wave refraction
- When waves approach an uneven coastline - Wave its the headland and therefore the energy is reduces as they enter the bay
108
Deposition landforms - coast
- Spit - Saltmarsh - Bar - Tombolo - Barrier island
109
Spit - coasts
- Narrow stretch of sand with one end attached to the mainland - Spit forms when land changes direction and the sand is deposited - change in wind direction can make a hook at the end
110
Saltmarsh - coasts
- Saltmarsh can form on the land side of the spit - area where sediment has built up and is often flooded
111
Tombolo - coasts
- If spit joins an offshore island
112
Barrier island - coasts
- Sandy islands may form that run parallel to the coast - barrier islands and water behind is a tidal lagoon
113
Sand dunes - coasts
- Ridges or hills of sand found on the landslide of
114
Formation of coral reefs
- Formed by coral polyps - tiny animals - Build calcium carbonate exoskeletons - Zooxanthellae algae within the coral - gives it its color & provides it w/nutrients - Coral provides algae with carbon dioxide - symbiotic relationships
115
Coral reef location
- Subtropical and tropical regions - between 30˚north and south - Warm water - 23-25˚C - ejects water at 27˚C - Salt water - coral can't be in develop in fresh water - Clear, shallow water less than 60m deep and lots of sunshine for photosynthesis - silt and nutrients block sunlight
116
Types of coral reefs
- Fringing reefs - most common type - form along coastlines of tropical areas and are usually separated from the land by a shallow lagoon - Barrier reefs - similar to fringing but the water that separates it from land is a deep-water lagoon - Atolls - rings of reef which form when fringing reefs develop around volcanic islands 0 island sinks below the water level leaving the atoll reef and a lagoon in the middle
117
Benefits of coral reefs
- Diverse - 1500 species of fish - Tourist attraction benefits the economy - Great Barrier Reef supports 64,000 jobs and $6.4 billion AUD - Organisms can be used in medicines including treatment for cancer - Acts as coastal protection & absorb energy of waves during topical storms and tsunamis - reduce coastal erosion and flooding
118
Threats to coral reefs
- 75% under threat - Overfishing - affects food webs and reduces plant-eating fish - Pollution - chemicals disturb functions of coral and growth - eutrophication - Soil erosion - silt and sediment enter water & affect clarity - prevents photosynthesis - Temperature increase - thermal stress - coral ejects algae and therefore bleaches coral - Sea level rise - coral needs shallow water for sunlight - will die without photosynthesis - Increasing storm frequency and severity - severe storms damage coral - Ocean acidification - changes pH levels & - oceans absorb more CO2 and carbonate that coral needs - acid weakens existing coral - Tourism - boat trips spill diesel and anchors damage coral and tourists take bits as souvenirs
119
Mangrove
- Tree or shrub that is a halophyte - grows in saline water - Mangrove swamps or forests - groups of trees and shrubs
120
Mangrove adaptations
- Prop roots to support the trees due to little soil & absorb oxygen above the water - Leaves are waxy to reduce transpiration & leaves and roots excrete salt to get rid of it from the plant - old leaves store it and fall off - Seeds stay attached to trees and shrubs until they germinate so they can float on the water after falling
121
Location of mangrove swamps
- Located off the coast - Found in tropical areas - Only grow in areas where temperature is 20˚C
122
Benefits of mangrove swamps
- Diverse - have many species - Reduce and prevent coastal erosion by absorbing energy of waves - can reduce flooding - Can trap and filter pollutants released into the water - trap extra sediment from soil erosion - Provide income for local communities & source for timber that can be sold or used - Some plants can be used in medicines - Absorb CO2 & store it - Fishing
123
Threats to mangrove swamps
- Tourism - buildings destroy swamps or are removed for better views - Waste - solid waste collects among trees and shrubs causing danger - Soil erosion - sediments from soil erosion flow out of the rivers into the mangrove swamps and clog up roots and habitats - Pollution - pollutants can affect plants and wildlife - herbicides kill weeds but can hurt mangroves - Overharvesting - felling too many trees - not sustainable - Agriculture or shrimp farming - felling and clearance of mangrove swamps - Urbanization - expansion of coastal cities threatens mangroves - Dams and irrigation - reduces water flow and therefore increases salinity - mangroves cannot survive - Rising sea levels - mangroves can't survive large changes - Destruction of the coral reef - coral reef destruction exposes mangroves
124
Opportunities of coasts
- Tourism - Fishing - Often flat land is near - good for building settlements - Opportunities for ports for trading through imports and exports & ferry routes
125
Hazards of coasts
- Storms / tropical storms - wind speeds of 120-250km/h - cause storm surges / temporary increase in sea level - cause flooding, coastal erosion, infrastructure damage and death/injury - Tsunamis - created by earthquakes, up to 30m high, storm surges, flooding, death/injury, building damage - Coastal erosion - Rise in sea level
126
Hard engineering methods for coasts
- Sea wall - Groynes - Gabions - Rock armour - Revetments
127
Sea wall - coastal protection
- Concrete wall to prevent waves from reaching behind - wall is curved at the top to reflect water back - Hardwearing, lasts a long time, prevents erosion & flooding - Expensive, erodes eventually, needs maintenance
128
Groynes - coastal protection
- Wooden barriers at right angles to the beach to slow longshore drift and absorb wave energy - Increases size of beach, improved tourism, absorbs wave energy, relatively cheap - May increase erosion along the coast due to less sediment, visually unattractive
129
Gabions - coastal protection
- Cages of rocks to absorb wave energy & reduce erosion - Cheap, easy to construct, absorbs wave energy - Visually unattractive, cages eventually rust
130
Rock armour (rip rap)
- Rocks or boulders at the bottom of a cliff to absorb wave energy & slow erosion - Looks more natural than sea wall & gabions - Strong waves can move the rocks - need to be replaced, expensive to transport rocks and boulders
131
Revetments
- Made of wood or concrete - placed at the top of the beach and are sloped to break waves & reduce erosion - Relatively cheap, less visual impact than sea wall or gabions - Reduces movement of sediment to other areas
132
Soft engineering coastal methods
- Beach nourishment - Beach reprofiling - Sand dune stabilization - Managed retreat
133
Beach nourishment - coastal protection
- Build beach by adding sand - creates higher and wider beach - forces waves to break earlier - Relatively cheap, larger beach is nicer too tourists - Removes sand from other areas and hence increases erosion - sand addition must be regular
134
Beach reprofiling - coastal protection
- Moving sand to the top of the beach nearest land - increases steepness so waves break before reaching land - reduces erosion - Requires constant maintenance
135
Sand dune stabilization - coastal protection
- Keeps sand dunes in place as a barrier between land and sea - dunes absorb energy & reduce erosion - low cost - plant marram grass that grows and roots hold the sand together
136
Managed retreat - coastal protection
- land is allowed to erode in areas of low value - Only costs are in compensation for landowners
137
Weather
- State of the atmosphere experienced day-to-day
138
Climate
- 30-year average of weather conditions taken into account with temperature and precipitation - Weather occurs in lowest part of atmosphere - troposphere
139
Stevenson screen
- Anemometer on top to measure wind speed - Weather instruments kept inside the white box to protect from wind, rain & animals - Slats on the side of the box (louvres) to allow air flow in the box - Made of wood to prevent absorption and conduction of heat - Painted white to reflect solar radiation - Places 1.25 meters above the ground to avoid temperature gradient of the ground - Placed away from buildings or trees that can affect wind flow and temperature gradients
140
Rain Gauge
- Measures precipitation - Normally built in the ground w/top above ground to collect precipitation - Cross-sectional area known accurately - Rain falls in the top ad enters through a narrow funnel - Water flows into glass measuring cylinder so the volume can be measured - Measurement recorded at same time each day
141
Maximum-minimum thermometer
- Placed in Stevenson - out of direct sunlight - Records the minimum and maximum temperature over 24 hours - in celsius - Mercury or alcohol inside that expands when temperature increases & contracts at decrease - Moves the marker pins within the thermometer - Measurement recorded at same time each day
142
Wet and dry bulb thermometer (hygrometer)
- Placed in Stevenson screen / out of direct sunlight - Measures humidity as a percentage - Two thermometers - standard thermometer and one wrapped in a fabric connected by a wick to a container with water to keep the bulb wet - Two temperatures for humidity by comparing data to values in special reference tables
143
Sunshine recorder
- Outside to capture sunshine - Glass sphere focuses Sun's direct radiation onto a piece of card behind the glass sphere - Sunlight burns the card - length of the burn trace corresponds to duration of sunshine - Generally replaced by automated sun sensors
144
Barometer
- Measures air pressure - mass of air pressing down - Inside Stevenson Screen - Records air pressure in millibars - higher value = higher air pressure - Important because it controls day-to-day weather - low pressure associates to changeable conditions & high pressure is more settled
145
Anemometer
- Measured wind speed - on the outside of the Stevenson Screen - Can't be too close to a building or trees - Cups that spin around in the wind - Speed recording can be taken in m/s can can be converted - Actual wind speed recorded for a daily record and can calculate maximum gust speed - Wind uses Beaufort scale of 0-12 - Now many digital handheld devices that can be used
146
Wind vane
- Direction that wind blows from - Direction of wind is recorded by points of the compass
147
How clouds form
- Form in many shapes and heights through the atmosphere - Type of cloud that forms is due to weather conditions in the atmosphere
148
Cirrostratus (Cs)
- Fine wispy clouds in the sky - Cover most of the sky - Relatively transparent - Sometimes are circular like halos around the sun
149
Cirrocumulus (Cc)
- Fluffy circular clouds high in the sky - Sometimes hard to spot - Little tufts high up and look like ripples - Clouds are so high - no precipitation reaches the ground
150
Cirrus (Ci)
- Thin stripy - like horse tails - Reflect colors of the sun at night - can glow purple, orange or yellow
151
Altostratus (As)
- Form at mid-level and form in a layer - Cover the sky in a thin layer - sometimes see the sun poking through - Flat and featureless
152
Altocumulus (Ac)
- mid-level circular fluffy clouds - Patches of clouds in variety of sizes & shapes - Precipitation is rare
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Stratocumulus (Sc)
- Mixture of layers and balls of cloud at mid-level
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Cumulonimbus (Cb)
- Tall and towering - fluffy stacked clouds move from the lower layers to the mid layers - Heavy rain, thunderstorms and lightning
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Nimbostratus (Ns)
- Thick dark layer of cloud - Usually is a single that rain is coming - Thick enough to block out the sun
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Stratus (St)
- Grey layer of clouds which are low in the sky - Made of flat layers - Sometimes associated with light rain - Weather is overcast with little sunlight - May persist all day
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Cumulus (Cu)
- Fluffy, cartoon-looking clouds - Brilliant white w/sun - Detached, individual fluffy ball shapes
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Measuring cloud data
- Cloud cover measured in oktas / eights - e.g. 50% cover = 4 oktas - represents how much cloud is covering the sky at any given moment - is for all cloud types
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Representing atmospheric pressure
- Often a map with bending lines - isobars - Represent air pressure
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Representing wind data
- Wind rose diagram - shows direction of wind - Radial lines from the center show percentage of time in the direction that win comes from - colors represent wind speed
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Biomes
- Large-scale ecosystems - Have living plants & animals & non-living parts e.g. watee
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Biodiversity
- The variety of plants and animals within an ecosystem - Tropical rainforest is most biodiverse, hot deserts and polar regions the least
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Parts of a food web/chain
- Producer - all plants, convert sunlight, water & CO2 to oxygen & energy - energy passed in chain and oxygen released to atmosphere - Primary consumer - animals that feed on producers - Secondary consumers - eat primary consumers and producers - Tertiary consumers - eat primary & secondary consumers alongside some who eat producers
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Adaptations
- Special features developed that help an organism to survive and reproduce in its environment / ecosystem
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Equatorial climate
- Between 10˚N & 10˚S - Sun is directly overhead all year round - energy is concentrated in small area hence is warmer - Zone of low pressure - hot and wet climate
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Characteristic of an equatorial climate
- Average temperature of 26˚C - Small annual range of temperature (between 2-3˚C) - Heavy convectional rainfall of over 1500mm a year - High humidity
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Cause of equatorial climate
- Equatorial area affected by Inter Tropical Convergence Zone (ITCZ) - ITCZ - air masses from north and south of equator due to trade winds and zone of low pressure is created - Zone moves as the position of the sun moves due to tilt of the Earth - Low pressure - warm unstable air rising, cools, condenses and forms clouds with convectional rainfall - Orographic rainfall - warm moist air forced to rise as it passes over a mountain, then cools and condenses to form a cloud leading to precipitation
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Water cycle in tropical rainforests
- Heavy daily convectional rain - Trees intercept rain - Some rain reaches the ground - Trees take up water quickly - Water evaporates rapidly --> step 1
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Nutrient cycle in tropical rainforests
- Plants and trees shed leaves all year - litter forms and decomposes rapidly - Nutrients enter the soil - Plants absorb nutrients - Abundant nutrients lead to rapid plant growth --> step 1
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Deforestation
- Cutting down and clearance of trees
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Reasons for deforestation
- Land clearance for agriculture - commercial or subsistence farming - Commercial felling for timber - Clearing land for settlements - Road building - Mining - Hydroelectric power infrastructure
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Impacts of deforestation
- Biodiversity loss - Fragmented habitats - Local and international climate change - increased CO2 - Nutrient cycle broken - Increased hunting - access roads for logging give hunters access - Indigenous communities - Flooding
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Deserts
- Cover 1/5th of Earth's land surface - Found in every continent and are areas with a moisture deficit - Located around the Tropic of Cancer and Capricorn
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Climate features of deserts
- Large diurnal temperature range - can exceed 50˚C at day and fall below 0˚C at night - Low rainfall - below 250mm a year - Low humidity
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Cause of deserts
- Drier air is forced away from the equator by high altitude winds - then sinks at the tropics, warms and enables it to hold moisture making it less likely to rain - creates high pressure and therefore no clouds - Also occurs due to rain shadow / orographic rainfall
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Desertification
- Overgrazing, overcultivation and increasing populations at edges of desert push the desert outwards