2026-04-18T06:59:01Zhttps://recercat.cat/oai/request

oai:recercat.cat:2445/2182232025-11-20T13:56:50Zcom_2072_1057col_2072_478778col_2072_478909col_2072_478917

00925njm 22002777a 4500 dc Keller, Philipp S. author Marcé Romero, Rafael author Obrador Sala, Biel author Koschorreck, Matthias author 2025-01-30T14:18:21Z 2025-01-30T14:18:21Z 2021-06 2025-01-30T14:18:21Z Reservoir drawdown areas¿where sediment is exposed to the atmosphere due to water-level fluctuations¿are hotspots for carbon dioxide (CO2) emissions. However, the global extent of drawdown areas is unknown, precluding an accurate assessment of the carbon budget of reservoirs. Here we show, on the basis of satellite observations of 6,794 reservoirs between 1985 and 2015, that 15% of the global reservoir area was dry. Exposure of drawdown areas was most pronounced in reservoirs close to the tropics and shows a complex dependence on climatic (precipitation, temperature) and anthropogenic (water use) drivers. We re-assessed the global carbon emissions from reservoirs by apportioning CO2 and methane emissions to water surfaces and drawdown areas using published areal emission rates. The new estimate assigns 26.2 (15-40) (95% confidence interval) TgCO2-C yr−1 to drawdown areas, and increases current global CO2 emissions from reservoirs by 53% (60.3 (43.2-79.5) TgCO2-C yr−1). Taking into account drawdown areas, the ratio between carbon emissions and carbon burial in sediments is 2.02 (1.04-4.26). This suggests that reservoirs emit more carbon than they bury, challenging the current understanding that reservoirs are net carbon sinks. Thus, consideration of drawdown areas overturns our conception of the role of reservoirs in the carbon cycle. Pantans (Enginyeria civil) Diòxid de carboni Reservoirs Carbon dioxide Global carbon budget of reservoirs is overturned by the quantification of drawdown areas