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Geography hazardous earth part 1
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Global circulation
1. Hot
air rises
at
equator
2. Causes
low pressure
3.
Air spreads out
and
sinks
at tropics
4. Causes
high pressure
5.
Air
flows back towards
equator
ITCZ
Band of
rainfall
at the
equator
ITCZ moves
Due to
tilt
of Earth's axis as it orbits the
Sun
ITCZ causes
rainy
seasons in
West Africa
Global circulation cells
1.
Hadley
cell
2.
Ferrel
cell
3.
Polar
cell
High
pressure
Causes
dry
,
desert
conditions
Low
pressure
Causes
rainfall
Air always flows from
high
pressure to
low
pressure
Ocean currents
Move
heat
from
equator
to poles
Ocean currents
prevent
overheating
of the planet
Rainfall
zones
Rainfall in areas of
low
pressure
Dry
, desert conditions in areas of
high
pressure
West Africa experiences
rainy
and dry seasons due to movement in and out of the
ITCZ
Natural causes of climate change
Volcanic
eruptions
Asteroid
collisions
Sunspot
activity
Orbital
changes
Volcanic
eruptions
Release
sulfur dioxide
and ash, causing global
cooling
in the short-term
Asteroid collisions
Throw up
dust
, causing global
cooling
in the short-term
Sunspot activity
More
sunspots
= hotter
sun
= global warming/cooling over longer periods
Orbital changes
Changes in Earth's
orbit
and axis tilt cause global
heating
and cooling over very long periods
Circular orbit
Orbit around the
sun
where the
distance
to the sun is equal at any point
Elliptical orbit
Orbit around the
sun
where the distance to the sun varies, sometimes further away (cooler) and sometimes closer (
hotter
)
Axis tilt
The planet's axis is not
straight
, it is on an angle and wobbles over a
41,000
year period
This puts the planet
closer
or further from the sun, impacting
heating
and cooling
Ice cores
contain
trapped carbon dioxide
, which indicates past climate conditions
High CO2
in ice cores
Indicates it was
warmer
in the past
Low CO2 in ice cores
Indicates it was
colder
in the past
Tree rings
Narrow
rings indicate a
short growing season
and colder temperatures
Wide rings indicate a
long growing season
and
warmer
temperatures
Historical sources
like old photographs, drawings, and written accounts are less
reliable
for determining past climate
Satellite images are very
reliable
for determining
current
climate
Greenhouse effect
Greenhouse gases in the atmosphere trap outgoing
long-wave
radiation, causing the planet to
heat up
Some greenhouse gases are
naturally
occurring, but human activities are
enhancing
the greenhouse effect
Thermal expansion
As the oceans
heat
up, the water molecules expand, causing
sea
levels to rise
Future climate change scenarios
Option C (best case):
Low
population growth,
renewable
energy, 30cm sea level rise
Option B (moderate):
Lower
population growth, some
renewable
energy, 1.5C warming
Option A (worst case): High population growth,
fossil fuel
use,
1m
+ sea level rise
Impacts of climate change
More frequent
flooding
More frequent and stronger
hurricanes
/cyclones
Changes to
farming
and
agriculture
Tropical cyclones
/
hurricanes
/typhoons
Large rotating storms
that form in the tropics, measured on the
Saffir-Simpson
scale from 1-5 based on wind speed
Hazards of tropical cyclones
Strong
winds
Storm
surges
Coastal
flooding
Intense
rainfall
Landslides
Formation of tropical cyclones
1. Require
warm
ocean temperatures
2.
Coriolis
effect to spin
3. Often form over
West
Africa and move across the
Atlantic
Formation of hurricanes
1.
Warm
water required
2.
Coriolis
effect
3.
Storms
form over
West Africa
4. Storms merge due to
Coriolis
effect
5.
Low wind
shear in
upper
atmosphere
required
6. Sea surface temperatures of
27 degrees
required
7. Occurs over
oceans
8.
Dissipates
when hits
land
Hurricanes
Swirling winds and clouds due to
Coriolis
effect
Very
low
pressure, often below
1000
millibars
Lower the pressure
Stronger
the
winds
Hurricanes
have greater impacts in
low-income
countries compared to high-income countries
Bangladesh
Very low-lying, only 2 metres above sea level
Located on a river
delta
Coastal
location
Storm surges and heavy rainfall
Cause
flooding
in
Bangladesh
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