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

Map of the Philippines and the western Pacific: 10 m wind speed and sea-level pressure on 7 November 2013 at 18 UTC, with a compact low over the central Philippines.
7 Nov, 18 UTC, hours before landfall: 10 m wind (colours, arrows) and sea-level pressure (white lines). ERA5.

895hPa

Central pressure at landfall

Estimated from satellite and the surge analysis.S1

5–6m

Storm surge in Leyte Gulf

Higher still in places, amplified by the shape of the gulf.S1

6,300

Deaths

The official count of the national disaster council; most drowned in the surge.N1

4.1million

People displaced

N1

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

  1. 7 Nov, 00 UTC

    Haiyan lies east of Mindanao and Samar, heading west-north-west.

  2. 7 Nov, 20:40 UTC

    Landfall at Guiuan, Samar (8 Nov, 04:40 local time).

  3. 7–8 Nov

    The eye crosses Leyte Gulf; the surge floods Tacloban. Further landfalls on Leyte, Cebu and Panay.

  4. 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.

ERA5 10 m wind and sea-level pressure over the Philippines, 7 November 2013 00 UTC
7 Nov 00 UTC7 Nov, 00 UTC · the typhoon east of the Philippines, a 988 hPa low in ERA5. ERA5.
ERA5 10 m wind and sea-level pressure over the Philippines, 7 November 2013 18 UTC
7 Nov 18 UTC7 Nov, 18 UTC · the storm reaches Samar and Leyte. ERA5.

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.

Hourly ERA5 time series at Tacloban for 7 November 2013
Tacloban, 7 Nov (UTC) · temperature and dew point, 10 m wind and sea-level pressure, rain and cloud. The pressure falls and the wind rises through the evening as the storm arrives. ERA5.

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.

ERA5 daily precipitation over the Philippines, 8 November 2013
8 Nov · daily precipitation. The rain follows the storm's track across the central Philippines. ERA5.

Explore in the Lab

Open the event in the Climate mode

Each button opens the Lab on that view, with the date, map layer and data set already chosen.

References

News

  1. 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

  1. 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.

Maps and charts: the Climaturk Lab.

Weather: ERA5 reanalysis, Copernicus Climate Change Service (C3S) / ECMWF.