Weather hazards and climate change Flashcards
Features of global atmospheric circulation
- Transfer of heat from equator to the poles
- Three circulation cells - hadley, ferrel & ; polar
- Jet streams impact on the movement of heat energy
- The spin of the earth creates the coriolis effect
Hadley cell
- Hadley cells stretch from the equator to 30N and 30S
- Warm trade winds blow towards the equator
- At the equator the trade winds from each hemisphere meet. The warm air rises rapidly causing thunderstorms.An area of low pressure is formed where the air from the 2 cells meet over the equator
- The air at the top of the troposphere moves towards 30N and 30S where the air cools and sinks towards the ground forming the subtropical high-pressure zone.
- As the air sinks, it becomes warmer and drier. This creates an area of little cloud and low rainfall, where deserts are found.
- The Hadley cell is then complete. The air completes the cycle and flows back towards the equator as the trade winds.
Ferrel cell
The Ferrel cell occurs between 30N and 60N and 30S and 60S
- Air on the surface is pulled towards the poles, forming the warm south-westerly winds in the northern hemisphere and north-westerly winds in the southern hemisphere.
- These winds pick up moisture as they travel over the oceans. At around 60 degrees N and 60 degrees S, they meet cold air, which has drifted from the poles.
- The warmer air from the tropics is lighter than the dense, cold polar air and so it rises as the two air masses meet.
- This uplift of air causes low pressure at the surface and the unstable weather conditions that are associated with the mid-latitude depressions. Much of our wet and windy weather in the UK is determined by this.
Polar cells
- Polar cell stretch from latitudes 60N and 60S to the nrth and south poles
- At the poles, air is cooled and sinks towards the ground forming high pressure, this known as the Polar high.
- It then flows towards the lower latitudes.
- At about 60N and S, the cold polar air mixes with warmer tropical air and rises upwards, creating a zone of low pressure called the subpolar low.
- The boundary between the warm and cold air is called the polar front and is what accounts for a great deal of the unstable weather experienced in these latitudes
Ocean currents
- Heat from the tropics can be transferred to the cold polar regions, by large-scale water movement within the oceans.
- Each ocean has its own circular pattern of currents.
- Heat is transferred by warm ocean currents, such as the North Atlantic Drift in the Atlantic Ocean, from low latitudes to high latitudes.
- Ocean currents are set in motion by the prevailing surface winds associated with the general atmospheric circulation.
- The direction of water movement is also deflected by the Coriolis force.
What have been recent temperature changes?
In last 250 years Earth’s temperature has risen significantly compared to before. Average temperatures in middle of last Ice age was about 5 degrees Celsius below today’s average temperature.
Natural causes of climate change
Milankovitch cycles:
What is the Eccentricity cycle:
Earth’s orbit changes approximately every 100,000 years.
-Colder months occur when its more circular, warmer months when it is more elliptical
Natural causes of climate change
Milankovitch cycles:
What is axial tilt cycle?
- Roughly every 40,000 years tilt of Earth’s axis varies.
- A greater degree of tilt is associated with the world having a higher average temperature
What are greenhouse gases released by?
human activities including industry, transport, energy production and farming.
What is the enhanced greenhouse effect?
Human activity releases increasing levels of co2 and other greenhouse gases into atmosphere, increasing greenhouse effect-more warming.
What is the process of solar radiation entering and leaving Earth?
- Heat energy from sun passes through atmosphere and heats up Earth.
- Much of heat energy is radiated back into space.
- Greenhouse gases in atmosphere, e.g. co2, trap some of heat.
How does industry help the human cause of climate change?
Rising demand for consumer good increases production, burning more fossil fuels, which release greenhouse gases.
How does energy help the human cause of climate change?
New technologies and population increase demand for electricity production from coal, oil and natural gas, which all produce greenhousse gases,
How does farming help the human cause of climate change?
- Livestock, particularly cattle, produce methane as pat of their digestion - 1/3 of methane emissions in agricultural sector
- Global population growth increases demand for food.
- Mechanisation burns more fuel, and demand for meat for western-style diets increase methane levels.
How does transport help the human cause of climate change?
Rising affluence increases car ownership and air travel, releasing more greenhouse gases into atmosphere.
Where the UK located from the equator?
between 50 degrees North and 60 degrees North.
How does maritime influence impact on the UK’s climate?
Most of air reaching UK contains lots of moisture as we are surrounded by sea, leading to rainfall all year.
How does prevailing winds impact on the UK’s climate?
-Main or prevailing wind for UK comes from South West. -Air travels long distances over Atlantic Ocean, bringing moisture, leading to more rainfall.
How does Atmospheric circulation impact on the UK’s climate?
UK is near ‘boundary’ between northern Ferrel and Polar circulation cells. Where warmer air from south and cooler air from north meet, causing unsettled weather.
How do tropical cyclones form?
- Need source of warm ocean temperatures (27 plus).
- Rising warm air causes thunderstorms which group together, making a strong flow.
- An area of very low pressure forms at and up, forming a tropical cyclone.
What are tropical cyclones?
A tropical cyclone is a very powerful low-pressure weather system which results in strong winds (over 120 km/h) and heavy rainfall (up to 250 mm in one day).
What are tropical cyclone characteristics?
- They develop over tropical and subtropical oceans, between the tropic of cancer and tropic of Capricorn
- Average wind speed is 120kmph but speeds of 400kmph have been known
- Move from east to west with the trade winds
- They have an ‘eye’ which is the calm centre of the storm
What are the frequency of tropical cyclones?
- Happen June-November in northern tropics,
- November-April in southern tropics.
- More likely to happen in cooler years, but numbers are hard to predict.
What is the movement of tropical cyclones?
- Cyclone movement is determined by prevailing winds and ocean currents.
- Cyclone’s track is influenced by how far it travels over the ocean: it will collect more moisture, increasing its strength.
- Tropical cyclones can travel 600 km a day at 40 km/h.
- Cyclone movement can be forecast using satellite images.
How are high winds hazardous?.
Tropical cyclones are hazards due to the high winds.
- The high winds can be as strong as 80mph,can uproot trees and buildings potentially causing injuries and loss of life
- The high winds due to cyclones can rip of house roofs and in some cases the houses can simply fall over.
How is intense rainfall hazardous?
Heavy persistent rainfall can lead to flooding, damaging poverty and leaving people stranded.
- Intense rainfall is experienced frequently during tropical cyclones.
- In October 2012, during hurricane sandy there was 250mm of rainfall in many places in a few hours!
- The heavy rainfall can cause the river banks to explode and crops get destroyed
How are storm surges hazardous?
Tropical cyclones can cause a large mass of water to hit land, causing damage to beaches and coastal habitats.
How are landslides hazardous?
- Intense rainfall causes soil to be saturated and become heavy. Saturated soil then slides downhill.
- It cause land slides in many countries, which have been known to destroy the whole village
How is coastal flooding hazardous?
Damage to property and lives is increased due to flooding.
How did hurricane sandy travel?
- Across Caribbean Sea, affecting island nations of Jamaica, Cuba and Haiti, before moving north to reach USA, reached New Jersey on 29th October 2012.
- By time reached land wind speeds of 129km/h were recorded. Storm surges caused most damage to East coasts states.
How was social media used in sandy?
helped with damage assessment.
Environmental impacts of hurricane sandy in Cuba
- Around 2600 hectares of banana crops were destroyed.
- In Santiago de Cuba trees were uprooted and stripped of their leaves.
- Coffee plantation in mountainous areas were swept away.
- Area is close to the coast were flooded, with beaches being swept away, destroying wildlife.