Lake Poopó, lake in west-central Bolivia, occupying a shallow depression in the Altiplano, or high plateau, at 12,090 feet (3,686 metres) above sea level. Historically the country’s second largest lake, it covered 977 square miles (2,530 square km) at low stage and was about 56 miles (90 km) long and 20 miles (32 km) wide, though only 8 to 10 feet (2.4 to 3 metres) deep. By December 2015, however, the lake had literally dried up as a result of the combined effects of climate change-exacerbated drought and sediment buildup caused by the local mining industry.
Drought also had brought about the disappearance of the lake in the mid-1990s, but a renewed rain cycle and flow from the Desaguadero and Márquez rivers fed the lake and brought it back to life. Over the next two decades, however, as global warming raised temperatures in the region, the evaporation rate for the lake tripled. Moreover, climate change also increased the frequency and intensity of El Niño, the oceanic and climatic phenomenon that produces an abundance of rain in some regions while producing drought in others, as it did for Lake Poopó. Lacking a sufficient interval of normal rainfall to replenish its waters, Lake Poopó became desiccated despite conservation efforts funded by a grant from the European Union of some $15 million. The consequences for the region’s flora and fauna were catastrophic, as were the economic consequences, especially for those who had made their living fishing in the lake. Settlement on Lake Poopó’s shores—previously made marshy by filtration of water into the lake bed—had long been sparse, but the disappearance of the lake forced many people to relocate.
The lake’s only visible outlet was the Lacajahuira River. During floods (high stage) it spilled into the Coipasa Salt Flat, 50 miles (80 km) to the southwest.