Save
Geography paper 1
Save
Share
Learn
Content
Leaderboard
Learn
Created by
Isabelle
Visit profile
Cards (35)
Weather hazards
Global
atmospheric
circulation
Tropical
storms
Pressure
belts
Surface
winds
How global atmospheric circulation works
1.
Air
at the
Equator rises
2.
Air flows poleward
3.
Air sinks
at
30 degrees north
and south
4.
Air flows back towards
the
Equator
Pressure belts
Equatorial low
pressure
Subtropical high
pressure
Polar low
pressure
Air
at the
Equator
Rises due to
convection
Air at the polar latitudes
Is
colder
and denser, so the air
sinks
towards the ground surface under high-pressure conditions
Air at about
60
degrees
Rises
under
low
pressure conditions
Circulation cells
Hadley
Cell
Ferrel
Cell
Polar
Cell
Surface
winds
Caused by the
circulation
cells
Formation of tropical storms
1.
Air
spirals rapidly under
low
pressure
2. Rising air draws up
moisture
3. Spinning air forms an
eye
4. Rising air cools and
condenses
, forming clouds and
rain
5. Storm loses
strength
when it meets
colder
air
Typhoon Haiyan was a category
4
or
5
tropical storm
Climate change may
increase
the intensity and frequency of tropical storms
Primary effects of Typhoon Haiyan
Widespread destruction
Flooding
Storm surge
Secondary effects of Typhoon
Haiyan
Disruption to
power
, communications, transport,
fishing
industry
Shortages of
food
and
water
Spread of
disease
Responses to Typhoon Haiyan
Emergency
aid
Rebuilding
infrastructure
Mangrove
replanting
Weather hazards in the UK
Flooding
Storms
Droughts
and
heatwaves
Extreme cold
Recent extreme weather events in the
UK
include severe storms and
flooding
Climate
change is expected to increase the frequency and intensity of extreme weather events in the
UK
Causes of climate change
Human
factors
Natural
factors
There is strong evidence for
climate
change, including rising temperatures,
sea levels
, and changes in weather patterns
Effects of climate change
Environmental
effects
Social
effects
Economic
effects
Strategies to adapt to climate change
Improving
flood defences
Changing
agricultural practices
Relocating vulnerable communities
Deforestation
is the clearing of
forests
, often for agricultural or development purposes
The rate of
deforestation
has
slowed
in recent decades but remains a significant issue
Causes of deforestation
Logging
Clearing
land for
agriculture
Mining
and
infrastructure
development
Impacts of deforestation
Loss of
biodiversity
Disruption
of local communities
Contribution to
climate change
Values of tropical rainforests
Biodiversity
Carbon
storage
Livelihoods
for indigenous communities
Potential for
medicinal
discoveries
Coastal processes include
erosion
, transportation, and deposition of
sediment
Coastal landforms
are shaped by the interaction of geology and coastal processes
Coastal landforms
Beaches
Cliffs
Caves
,
arches
, and stacks
Coastal management strategies
Hard
engineering (e.g.
sea walls
, groynes)
Soft
engineering (e.g. beach
nourishment
, managed realignment)
River processes include
erosion
, transportation, and deposition of
sediment
River
landforms
Meanders
Oxbow
lakes
Gorges
Factors affecting flood risk
Precipitation
Soil moisture
Vegetation
cover
River management
Hydrographs
Graphs showing the
volume
of water flow in a
river
over time
River management strategies
Flood
defences
River
restoration
Catchment
management