Paper 1 - Section A, Weather Hazards Flashcards
Explain how the global atmospheric system affects the weather and climate of a high pressure area
- air sinks in the model which gives high pressure. Areas coincide with the earths deserts and dry areas as air is sinking so there is little condensation and no clouds
- latitudes with high pressure are 90 degrees north and south, and 30 degrees north and south
Explain how the global atmospheric system affects the weather and climate of a low pressure area in the tropics
- insulation from the sun concentrates around equator and tropics, causing air to heat up and rise
- as the air cools, starts to condense forming clouds (eg cuminilbous clouds) and forming water droplets allowing it to rain
- low pressure areas = wetter areas with lush vegetation
- latitudes with low pressure: 0 degrees, 60 degrees north and south
Which sea temperatures can tropical storms form on
26.5 degrees Celsius and above
Which limitations does the tropical storm minimum temperature (26.5 and above) cause
- limits their geographical distribution (occur in tropics 5 and 30 degrees of latitude)
- limits their seasonal distribution (happen in summer and late autumn when sea water is warmest)
How do tropical storms form
- A strong upward movement of air draws water vapour draws from ocean surface
- Evaporated air cools as it rises and condenses to form thunderstorm clouds
- As air condenses, releases heat which powers storm and draws up more water from the ocean
- Several small thunderstorms join together, when surface winds hit. 120km/h = official tropical storm
- Storm develops and eye where air decends rapidly
- As storm is carried across ocean by prevailing winds, continues to gather strength
- When reaches land, storms energy is cut off, friction with land slows it down
How do winds occur
Air molecules move from areas of high pressure to areas of low pressure
What are some important factors for forming a tropical storm
- warm sea temps
- high humidity- needs lots of moisture
- rapid cooling - air must condense quickly to generate lots of energy to power storm
- low wind shear
- Coriolis force to give storm spin
- pre-existing low-pressure disturbances - tropical storms usually form when other smaller storms come together
How will climate change affect the distribution, frequency and intensity of a tropical storm
- last few decades sea temp increased by 0.25 - 0.5 degrees Celsius in tropics => may affect distribution of tropical storms
- in future, tropical storms could affect places outside current hazard zones
- hurricanes may become more powerful
- frequency might decrease but intensity could increase
- intensity has increased linked to increase in surface sea temp
What category storm was Typhoon Haiyan 2013
category 5 storm in Phillippines
What are some primary effects of Typhoon Haiyan 2013
- over 6300 killed, most drowned by 5m storm surge in city of Tacloban
- over 1 million homes damaged by storm surge and 275km/h winds
- power lines were blown down so electricity was cut off
- trees blown over blocking roads
- 400 mm of rain caused flooding inland, destroying crops
What are some secondary effects of Typhoon Haiyan 2013
- around 600 000 people had to leave their homes (especially in Tacloban) where 90% were destroyed
- about 400 000 people were housed in 1100 emergency camps
- 10 000 schools were destroyed
- farmers couldn’t grow rice as soil contaminated by salt and rice prices rose
- outbreaks of diseases because of contamination by sewage + hospitals had been destroyed
What are some immediate responses of Typhoon Haiyan 2013
- 1.1 million people were supplied with clean water by the Red Cross to reduce the outbreak of diseases due to poor sanitation
- France, Belgium and Israel set up field hospitals to help injured
- 1200 evacuation centres set up
- US aircraft assisted search and rescue and delivery of aid
What are some long-term responses of Typhoon Haiyan 2013
- ‘cash for work’ schemes were created where people got paid to help clean up debris, this helped rebuilding and recovering from disaster but also supplied a source of income for those who had lost their jobs
- organisations like UNICEF and World Health Organisation vaccinated lots of children against diseases like polio and measles
- rice farming and fishing was quickly re-established but coconut trees take years to grow back and grow fruit so coconut farmers are still recovering
- ‘build back better’ scheme created to build 205 000 homes to re home those who had lost their homes in coastal areas
How can we use monitoring and prediction to reduce the risk of tropical storms
- satellite images provide data on cloud cover and formations, allow tropical storms to be tracked
- a radar satellite enables storms to be ‘scanned’ for rainfall (amount)
- planes and drones can fly through tropical storms. Dropsondes are dropped and are able to send data to aircraft
- forecasts are made and hurricane warnings can be issued
How can we use protection to reduce the risk of tropical storms
- wealthy people can invest in things like a basement shelter with an emergency generator
- governments can invest in high sea walls against storm surges and shelters on higher land
- houses close to the coast are built on stilts so storm surge can pass beneath