Twenty-one people are reported to have died in the the Philippines, as a result of Typhoon Hagupit (known locally as Typhoon Ruby), according the Philippine National Red Cross. The majority of the victims are said to be in the municipality of Borongan in Eastern Samar, where 16 people have lost their lives, with two other fatalities on the island of Samar and three in the province of Iloilo on the south of Panay Island. The majority of the victims are reported to have drowned in a storm surge caused by the typhoon, and it is though that the number of deaths would have been much higher but for a massive evacuation of low-lying areas organised by authorities in the Philippines.
Storm surge on a beach at Legazpi in Albay Province on Sunday 7 December 2014. Aaron Favila/AP.
Typhoon Hagupuit made landfall on Saturday night near the town of Delores in Eastern Samar, bringing with it winds gusting at up to 170 km per hour, but lost energy as it past over the islands, with the highest wind speeds recorded as it passed over Manila on the west coast of Luzon Island being about 135 km per hour.
Damage to homes in Delores in East Samar Province, caused by Typhoon Hagupit. EPA.
Tropical storms are caused by solar energy heating the air above the
oceans, which causes the air to rise leading to an inrush of air. If
this happens over a large enough area the in rushing air will start to
circulate, as the rotation of the Earth causes the winds closer to the
equator to move eastwards compared to those further away (the Coriolis
Effect). This leads to tropical storms rotating clockwise in the
southern hemisphere and anticlockwise in the northern hemisphere.These
storms tend to grow in strength as they move across the ocean and lose
it as they pass over land (this is not completely true: many tropical
storms peter out without reaching land due to wider atmospheric
patterns), since the land tends to absorb solar energy while the sea
reflects it.
Damage to homes in Tacloban, in the Eastern Visayas caused by Typhoon Hagupit. Maria Byrne/BBC.
The low pressure above tropical storms causes water to rise there by ~1
cm for every millibar drop in pressure, leading to a storm surge that
can overwhelm low-lying coastal areas, while at the same time the heat
leads to high levels of evaporation from the sea - and subsequently high
levels of rainfall. This can cause additional flooding on land, as well
as landslides, which are are a common problem after severe weather
events, as excess pore water pressure can overcome cohesion in soil and
sediments, allowing them to flow like liquids. Approximately 90% of all
landslides are caused by heavy rainfall.
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