Tropical cyclone · Central Philippines
Haiyan: the strongest landfall on record
In the early hours of 8 November 2013, local time, Super Typhoon Haiyan, known in the Philippines as Yolanda, came ashore on Samar with sustained winds near 300 km h⁻¹ and a central pressure around 895 hPa. Its surge, several metres high, drove the sea into Tacloban and the towns around Leyte Gulf. More than 6,000 people died and four million were displaced.
7–8 November 2013 · Leyte and Samar, Philippines · ERA5
What happened
Haiyan formed in the western Pacific near Micronesia and crossed the warm western Pacific at speed, intensifying into one of the strongest tropical cyclones ever observed. It made landfall at Guiuan, on the southern tip of Samar, then crossed Leyte Gulf and Leyte itself before moving into the South China Sea.
The wind alone was devastating, but the sea did most of the killing. Leyte Gulf narrows towards Tacloban, and the surge rose there to 5–6 metres, higher in places, flattening the waterfront districts.S1N1
7 Nov, 00 UTC
Haiyan lies east of Mindanao and Samar, heading west-north-west.
7 Nov, 20:40 UTC
Landfall at Guiuan, Samar (8 Nov, 04:40 local time).
7–8 Nov
The eye crosses Leyte Gulf; the surge floods Tacloban. Further landfalls on Leyte, Cebu and Panay.
8 Nov
The storm leaves the Philippines for the South China Sea.
Haiyan on the Lab's maps
ERA5 places the storm well. Twenty hours before landfall a closed low sits east of the islands; by the evening of 7 November it reaches Samar and Leyte, with the strongest winds wrapped round its centre.
What a reanalysis cannot see
988hPa
Haiyan's lowest pressure on ERA5's map on 7 November, against about 895 hPa in reality. The difference is the size of the storm's core: its eye was a few tens of kilometres across, its strongest winds in a ring only a little wider.
ERA5's grid is 0.25°, about 28 km, and the model behind it cannot build a core as tight and deep as Haiyan's. The reanalysis spreads the storm out: the pressure falls far less, and at Tacloban the wind on 8 November peaks near 18 m s⁻¹ rather than the 70 m s⁻¹ and more that hit Samar. The track and timing are right; the intensity is not.
This is true of every intense tropical cyclone in a global reanalysis, and worth remembering when reading the other storms in these pages: the Lab shows where and when, and the rain and wind around a storm, far better than its peak.
The rain
Haiyan moved fast, about 30 km h⁻¹, so its rain was heavy but brief at any one place: ERA5 puts 72 mm at Tacloban on 8 November. The daily map shows the rain band crossing the Visayas from east to west.
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Open the event in the Climate mode
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References
News
- N1Philippine Daily Inquirer. Yolanda toll now at 6,300 – NDRRMC. April 2014.The final death toll and the number of people displaced.
Studies and guidelines
- S1Mori, N., et al. (2014). Local amplification of storm surge by Super Typhoon Haiyan in Leyte Gulf. Geophysical Research Letters, 41.The storm surge in Leyte Gulf, its amplification and the storm's intensity.