Mindanao Times

PH cities facing ‘slow-motion disaster’

- BY JOSHUA MELVIN

WHEN Mary Ann San Jose moved to Sitio Pariahan more than two decades ago, she could walk to the local chapel. Today, reaching it requires a swim.

The main culprit is catastroph­ic subsidence caused by groundwate­r being pumped out from below, often via unregulate­d wells for homes, factories, and farms catering to a booming population and growing economy.

The steady sinking of coastal towns and islets like Pariahan in the northern Philippine­s has caused Manila Bay’s brackish water to pour inland and displace thousands, posing a greater threat than rising sea levels due to climate change.

“It was so beautiful here before... Children were playing in the streets,” San Jose said, adding: “Now we always need to use a boat.”

Most of the former residents have scattered to other parts of the region. Just a handful of families remain in Pariahan, which had its own elementary school, a basketball court and a chapel before the water flowed in.

These days just the flooded chapel, a cluster of shacks on bamboo stilts where San Jose lives with her family, and a few homes on a bump of land remain.

The children that live there commute 20 minutes by boat to a school inland and most of the residents eke out a living by fishing.

The provinces of Pampanga and Bulacan -where Pariahan is located -- have sunk between four and six centimetre­s (1.52.4 inches) annually since 2003, according to satellite monitoring.

“It’s really a disaster that is already happening... It’s a slow-onset disaster,” explained Narod Eco, who is part of a group of scientists tracking the problem. - Threat to lives By comparison, the UN estimates average sea level rise globally is about three millimetre­s per year.

The creeping bay waters put people and property at risk, while the threat is amplified by high-tides and flooding brought by the roughly 20 storms that pound the archipelag­o every year.

Some areas have raised roads in an effort to keep up with the sinking, creating odd scenes where the street surface is at the height of door knobs on roadside buildings.

At least 5,000 people have been forced out of the mostly rural coastal areas north of Manila in recent decades as the bay water has moved further inland, regional disaster officials told AFP.

The sinking is very likely permanent because the ground in the hardest hit areas is mostly clay,

which sticks together after the water is pulled out. The fate of towns such as Pariahan provides a preview of the problems that may await some of the capital’s 13 million people. Sections of Manila along the shore of the bay are sinking too, with excess groundwate­r pumping being the most likely cause, Eco, the researcher, told AFP. The subsidence there though is at a slower rate than the northern coastal communitie­s, potentiall­y due to less pumping or difference­s in the soil, he added. A moratorium on new wells in the greater Manila area has been in place since 2004. But enforcing that ban as well as shuttering existing illegal wells, falls to the National Water Resource Board and its roughly 100 staffers who are responsibl­e for policing the whole country. “We have insufficie­nt manpower resources,” the board’s director Sevillo David told AFP. “It’s a very big challenge for us, but I think we are doing the best we can.” - Things will get worse The demand for water has soared as Manila’s population has nearly doubled since 1985, and the size of the nation’s economy has expanded roughly ten-fold over the same period. This explosive growth has created a ravenous demand for water, especially in the agricultur­e and manufactur­ing industries to the north of the capital. “The sinking is a very serious threat to people, their livelihood­s and cultures,” said Joseph Estadilla, a spokesman for alliance seeking to protect Manila Bay coastal communitie­s. “This is only going to get worse in the near future,” he insisted. Manila and its surroundin­gs are among several major cities, especially in Asia, under threat as the land collapses beneath them, though the causes for this vary.

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