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Shira River live camera — Kumamoto

From the Aso caldera through central Kumamoto. Carrying volcanic ash, the water takes on a distinctive murk when it rises.

Sample frame from Shira River (August 2026)Sample August 2026

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What you are looking at

The colour of the turbidity is different because this river comes out of the inside of a volcano. What it carries is fine soil containing Aso's ash, a different colour from ordinary brown murk. Once your eye is used to it, the colour alone tells you the river is up. Open it the day after rain has fallen on Aso and the city stretch alone can be a different colour.

This river also bears on Kumamoto's water itself. Water held in the paddies of its middle reaches soaks down and feeds the groundwater the city's supply depends on. The river on the surface and the water underground are connected.

The source is Mount Neko, one of the central cones of Aso. The river comes down the southern valley of the caldera, joins the Kurokawa from the northern valley at Tateno, and heads west across the lava plateau. The channel is 74 kilometres and the basin 480 square kilometres. The basin is shaped something like a funnel, and about eighty per cent of it is the upstream Aso country. It is a shape that collects rain upstream.

That rain falling on Aso comes out in a city shows directly in the disaster record. The flood of June 1953 left 422 dead or missing in Kumamoto and Aso and inundated over 31,000 houses. In the northern Kyushu downpour of July 2012 the reference gauge at Yotsugi Bridge recorded its highest level ever. Even with clear skies over the city, the level rises if it is raining upstream.

The headwaters are in the mountains, so the level rises even when no rain is falling on the city. Leave evacuation decisions to the local authorities.

About this camera

PlaceKumamoto
FormatLive video, rotating
Time zoneAsia/Tokyo (UTC+9)
CategoryRiver
OperatorMLIT river live streams
Terms of useGovernment Standard Terms 2.0

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