Case Study: Typhoon Haiyan — Philippines, November 2013
Part of Weather Hazards — GCSE Geography
This key facts covers Case Study: Typhoon Haiyan — Philippines, November 2013 within Weather Hazards for GCSE Geography. Revise Weather Hazards in The Challenge of Natural Hazards for GCSE Geography with 15 exam-style questions and 24 flashcards. This topic shows up very often in GCSE exams, so students should be able to explain it clearly, not just recognise the term. It is section 5 of 14 in this topic. Use this key facts to connect the idea to the wider topic before moving on to questions and flashcards.
Topic position
Section 5 of 14
Practice
15 questions
Recall
24 flashcards
📋 Case Study: Typhoon Haiyan — Philippines, November 2013
Background and Formation
Typhoon Haiyan (known in the Philippines as Yolanda) formed on 2 November 2013 over the warm waters of the western Pacific Ocean, where sea surface temperatures of 29–30°C provided exceptional energy far above the 26°C minimum. The storm intensified rapidly to Category 5 super typhoon status and tracked north-westward across the Philippines, making several landfalls before exiting into the South China Sea.
| Statistic | Value |
|---|---|
| Date of main landfall | 8 November 2013, 4:40am (Guiuan, Eastern Samar) |
| Sustained wind speed at landfall | 195 mph (315 km/h) — strongest landfalling storm ever recorded |
| Storm surge height (Tacloban) | 7.5 metres |
| Deaths | 6,300+ confirmed; many estimates put true total higher |
| People displaced | 4.1 million — largest displacement since the 2004 Indian Ocean tsunami |
| Homes damaged or destroyed | 1.1 million |
| People affected (total) | 16 million across 44 provinces |
| Economic damage | $12 billion |
Primary Effects (within 24 hours)
- Storm surge of 7.5 metres — the primary killer: The surge swept several kilometres inland across low-lying coastal areas of Leyte and Samar. People who had evacuated vertically into attics and upper floors were still overwhelmed. The shallow continental shelf off Leyte amplified the surge far above what wind speed alone would have suggested. Most of the 6,300+ deaths were drowning, not wind injury
- 195 mph sustained winds: Roofs were ripped from reinforced concrete buildings. Bamboo and wooden structures — the majority of housing in Tacloban — were destroyed entirely. Flying debris caused severe injuries. The Tacloban airport terminal was inundated by the surge, initially preventing relief aircraft from landing
- 80% of Tacloban (population ~220,000) destroyed: Roads, bridges, water pipes, and power lines across Leyte and Samar were washed away or blocked by debris, cutting off communities for days
- Agricultural destruction: An estimated 33 million coconut trees destroyed (coconut oil is a major export crop); fishing boats and equipment lost; fields flooded with salt water
Secondary Effects (days to months later)
- Disease outbreak risk: Destruction of water infrastructure and sewage systems created conditions for cholera and leptospirosis (spread through flood water contaminated with animal waste). WHO deployed medical teams; a major outbreak was largely prevented through rapid intervention
- Displacement crisis: 4.1 million people in evacuation centres — some for months. Coastal communities designated too dangerous to return to required permanent relocation
- Economic collapse: Fishing and rice/coconut farming — the economic base of the Visayas — were devastated. Tourism to the region collapsed for over a year
- Psychological trauma: Survivors who witnessed family members swept away, or who survived by clinging to floating debris for hours, reported severe PTSD, anxiety, and depression — requiring long-term support that was largely unavailable
Short-Term Responses (days to weeks)
- Philippine government declared a national state of calamity within 24 hours; deployed 30,000 military and police personnel to the disaster zone
- The USA sent the USS George Washington carrier group with 5,000 personnel, helicopters, and medical capacity — a significant logistical contribution to reaching isolated islands
- More than 60 countries pledged assistance; UN OCHA coordinated the international response; over $1.5 billion pledged in emergency aid within the first weeks
- Emergency food, water, and medicine were airlifted within 48 hours to Tacloban; roads were cleared by bulldozers within the first week
- Controversy arose when Philippines authorities initially restricted international military aircraft access, delaying some aid — later resolved
Long-Term Responses (months to years)
- 'Build Back Better' programme: New housing constructed to higher standards — storm-resistant concrete frames instead of bamboo and wood; communities relocated away from the most surge-vulnerable coastlines
- No-build zones: A 40-metre no-build zone declared along Tacloban's waterfront. Controversial because displaced families with sea-based livelihoods had nowhere else to go — highlighting the tension between safety and economic reality in a low-income context
- Storm surge warning reform: PAGASA (Philippine weather agency) now issues surge warnings separately from wind warnings, using language that allows people to visualise actual water depths. This was a direct lesson from Haiyan, where surge danger was not communicated clearly enough to change behaviour
- Mangrove restoration: Large-scale replanting along coastlines to act as natural buffer; mangroves can reduce wave energy by 50–70%, replacing forests previously cleared for fish ponds
- The Philippines is now considered one of the world's best-prepared nations for tropical storm response — Haiyan fundamentally reformed the country's disaster risk reduction framework, even though reconstruction took 3–5 years
Quick Check: Explain why the storm surge was more deadly than the wind in Typhoon Haiyan.
The storm surge reached 7.5 metres in Tacloban — far taller than single or double-storey housing. People who evacuated vertically into attics or upper floors were still overwhelmed and drowned. The surge moved rapidly inland with enormous force, carrying heavy debris. Crucially, residents had been warned about extreme winds and prepared accordingly — but most did not understand what a 7.5 m wall of ocean water would mean. The shallow continental shelf off Leyte amplified the surge height beyond what wind speed alone would predict. Most of the 6,300+ deaths were caused by drowning in the surge, not by wind damage.