Floating villages in the Tonle Sap

[asakiyume]

Tonle Sap is a lake in Cambodia that expands and contracts dramatically, depending on whether it's the rainy season or the dry season--it goes from being no more than a meter deep and 2,700 square kilometers in area to being 9 meters deep and 16,000 square kilometers in area (says Wikipedia). The floating villages of Siem Reap, on one of its feeder rivers, are well known, but on the lake itself there are also floating villages. When dudeshoes saw this New York Times article ("A Push to Save Cambodia's Tonle Sap Lake," by Chris Berdik), about how the lake was threatened, she sent me the link, knowing I'd be interested.


Girl from the floating village of Akol, Cambodia. Photo by Chris Berdik for the New York Times

The article is largely about the creation of a model to try to predict what will happen to the lake and how much influence the various factors have, and about the problems in designing the model, and with the model more generally. I was more interested, though, in other aspects of the story--in the fact that farmers displaced by grants to agribusiness have come to make a living on the lake, in the mysterious statement that "tropical dams typically generate power for just a few decades" (why is that?), in the fact that there are tiny fish there called money fish, and sharks that will fit in the palm of your hand.


The black shark, Labeo chrysophekadion. Photo by Chris Berdik for the New York Times

1.5 million people depend on the Tonle Sap. Climate change, hydro dams, increased population pressures--all these things spell change for the lake. Since change is coming, it's best to be planning for it:

A food-security expert, Dr. Fraser has studied some of history’s worst famines, as well as those prevented by tactics like stockpiling food and distributing drought-resistant seeds. His research suggests that no matter how the Tonle Sap changes in the coming years, the right adaptive strategies could mean the difference between a tolerable transition and a disaster.

“The policy and development challenge is one of managing the transition,” he said. “There’s no way to stop it.”

Comments

Re: I never thought you were a fangirl ;)

[joycemocha.livejournal.com]

Probably less-steep canyons. All reservoirs silt up, eventually. Dredging isn't exactly feasible. It's more likely that it happens more quickly in a flatter tropical basin.

Re: I never thought you were a fangirl ;)

[asakiyume.livejournal.com]

*nodding*

[c-maxx.livejournal.com]

I believe JoyceM has the main part of it. As reservoirs silt up vertically, there is less vertical in a shallow tropical lake. Maybe more sediment load too. I understand most of Bangladesh in delta sediment.

I was at a talk in school discussing the Aswan Dam in Egypt, which has cut off the nutrient-filled sediment from central Africa, along with several other issues. They said it too was rapidly filling with sediment, although a deep reservoir.

The speaker discussed a deep-location sediment outlet tho I have never heard of anyone building one- under lots more pressure at the bottom of the res, much more difficult to build...

[asakiyume.livejournal.com]

I remember hearing that the Aswan Dam contributed to the spread of schistosomiasis, because the snails that are carriers of the parasitic worm live better in … whatever circumstances it is that the dam causes.

Giant infrastructure projects are less in vogue as forms of aid, and for good reason. As lots of people have pointed out, the global donor-aid-industrial complex can be as much about recolonialization and maintaining control (and benefiting the donor country) as it is about actual aid.