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Physically controlled CO2 effluxes from a reservoir surface in the upper Mekong River Basin: a case study in the Gongguoqiao Reservoir

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Figure

Figure 1. Sampling points in the Gongguoqiao Reservoir and its po-sition within the Mekong River Basin
Figure 2. Monthly water discharge of the inflow at the main stem (a) and the tributary (the Bijiang River, b) into the GGQ
Figure 3. Box plots ofspring pCO2 in the rivers (R), permanent flooded area of the reservoir (P), downstream (D) and littoral zone (L) in the (a), summer (b), autumn (c) and winter (d)
Figure 5. Longitudinal variation in effluxes along the main stem indifferent seasons. The points and error bars refer to mean values andstandard deviations, respectively.
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