Typhoon Haiyan Location
Philippines, near Tacloban (in Leyte) on 8th November 2013 at 4:40am. It also went over Vietnam and China.
Typhoon Haiyan Key Stats
Cat 5 typhoon
wind speeds of up to 200km/h and wind gusts of 314 kph waves up to 14m
600km long
Formed on November 3 2013, died on November 11 2013. Fatalities 6,352 total, Injuries 28,781
Around 25% of the Philippines was already homeless before the typhoon.
Typhoon Haiyan Causes
Physical - there were winds, in the correct latitude, the water was really warm - 30, the water was deep and there was low pressure, Phillipines is an island, so no power was lost when the typhoon passed over it
Human - slow warnings, poor construction housing, limited resources to make blockades/shelters
Typhoon Haiyan Social Consequences
Social Damages
- Mass homelessness: 1.1 million houses were destroyed, leaving 4.1 million people homeless.
- High human toll: Over 6,000 deaths, 29,000 injuries, and 1,400 people missing.
- Widespread impact: 14.1 million people affected, with outbreaks of disease and rising violence due to lack of resources.
Typhoon Haiyan Economic Consequences
Economic Damages
- Massive financial loss: Total damage estimated at $12 billion, with $2.9 billion lost in agriculture.
- Livelihoods destroyed: 30,000 fishing boats lost, 6 million people lost jobs or income.
- Farmland devastation: 600,000 hectares and 1.1 million tonnes of crops damaged, affecting 1 million farmers.
Typhoon Haiyan Environmental Consequences
Environmental Damages
- Infrastructure collapse: Electricity poles, roads, and the airport were severely damaged; some areas had no power for a month.
- Severe flooding: A 5-meter storm surge and 400mm of rainfall flooded areas up to 1km inland.
- Pollution crisis: An oil tanker spill contaminated fishing waters with 800,000 litres of oil.
Typhoon Haiyan Immediate Responses
Immediate Response
- Basic needs met: 1,000 tonnes of rice, clean water, and emergency shelters were provided by various countries and organizations.
- Shelter and medical aid: The UK sent shelter kits; France, Belgium, and Israel set up field hospitals to treat the injured.
- Evacuation support: Over 1,200 evacuation centres were established for displaced individuals.
Typhoon Haiyan Long-term Responses
Long-Term Recovery
- Infrastructure rebuilt: Damaged roads, bridges, and airports were reconstructed.
- Livelihood restoration: Aid agencies replaced fishing boats to help communities regain income.
- Future protection: Cyclone shelters were built in coastal areas to safeguard people from future tropical storms.
Australia Millenium Drought Location
Overall most of Australia, but mainly South east Australia and the Murray-Darling Basin in 1997-2010.
Australia Millenium Drought Key Stats
One in a thousand drought
Australia has a very low annual rainfall of 450 mm per year
It is mainly arid land or desert
It is the dryest land in the world where people live
Australia Millenium Drought Causes
Australia Millenium Drought Social Consequences
Australia Millenium Drought Economic Consequences
Irrigation bans due to depleted reservoirs caused:
- Crop failures and livestock deaths.
- A 1% drop in the $940 million regional economy.
- Government response included exit grants for farmers forced to abandon their farms to buy their land for money.
Australia Millenium Drought Environmental Consequences
Drying river systems (especially Murray and Darling) led to:
- Loss of wetland habitats.
- Decline in native fish stocks.
- Severe land degradation and increased bushfire risk
Australia Millenium Drought Immediate Responses
Australia Millenium Drought Long-Term Responses
Storm Desmond- Carlisle Flood Location
5th and 6th December 2015 in Cumbria (North West of England, south of the Scottish border, Carlisle, at the mouth of the river Eden)
Storm Desmond- Carlisle Flood Key Stats
130km/h winds
Record breaking rainfall that lead to worst flooding in 600 years
341mm in 24hours
Storm Desmond- Carlisle Flood Causes
Physical:
-Warm and cold air met, causing the warm air to rise, cool, and condense—leading to heavy rainfall.
- Sudden drop in pressure intensified the storm system, triggering rapid and intense precipitation.
- Relief Rainfall from the Cumbrian Mountains – Moist air was forced to rise over the mountains, cooled, and condensed into heavy rain, intensifying local rainfall levels.
- The area had already experienced twice its monthly average rainfall, so the ground was oversaturated, meaning that rainfall ran off the surface of the ground
Human:
- Urbanisation – The spread of buildings and roads created more impermeable surfaces, reducing infiltration and causing rainwater to flow rapidly into rivers and drains.
- Deforestation for Farming – Trees had been cleared centuries earlier, removing natural vegetation that would have absorbed rainfall and slowed runoff.
- Flood Embankments Upstream – Barriers built to protect upstream areas redirected excess water downstream, increasing discharge into Carlisle and worsening the flood impact
Storm Desmond- Carlisle Flood Social Consequences
Storm Desmond- Carlisle Flood Economic Consequences
Storm Desmond- Carlisle Flood Environmental Consequences
Storm Desmond- Carlisle Flood Immediate Responses
Storm Desmond- Carlisle Flood Long-Term Responses