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El Salvador - GFDRR

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I. DESCRIPTION OF THE EVENT | 7<br />

The intense rain also resulted in flooding and erosion in rivers and landslides on steeper slopes. The<br />

mix of water, mud and sediment—material carried by the current—saturated riverbeds, already considerably<br />

silted by prior events, causing widespread flooding on the plain and affecting settlements, towns and<br />

urban areas, with damages to urban, rural and transport infrastructure.<br />

In addition, the lahar on slopes caused significant soil losses, and floods caused sediment to accumulate<br />

on agricultural lands, with damages to terrain and plantations and crop losses.<br />

Tropical Storm Ida began November 4 th on the Atlantic coast of Nicaragua, near Bluefields. By the<br />

next day, Thursday the 5 th , it had become a hurricane (Level 1 on the Saffir-Simpson scale). Upon making<br />

landfall in Nicaragua, it lost strength as it moved to the northwest. On Friday the 6 th , now only a tropical<br />

depression, it continued moving and crossed Honduras on a north-northwesterly path, while a lowpressure<br />

front persisted in the direction of southwestern <strong>El</strong> <strong>Salvador</strong>, causing the abundant humidity to<br />

move toward this country.<br />

IMAGE 1. IDA’s PATH AND IMAGE OF RECORDED RAINFALL<br />

Source: Joint Research Center of the European Commission (JRC).

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