“…Over the last decade, a combination of field data, high-resolution satellite imagery, and conceptual and numerical modelling has been used to document the flood hydrology and channel-floodplain morphodynamics approaching the terminus of the Río Colorado, and assess the sedimentological implications (e.g. Donselaar et al, 2013Donselaar et al, , 2022Li et al, 2014Li et al, , 2018Li et al, , 2019Li et al, , 2020aSandén, 2016;van Toorenenburg et al, 2018). Similar to the lower reaches of many other ephemeral dryland rivers, there is a significant downstream decrease in the crosssectional area of the river from ~80 m 2 to <5 m 2 and its associated sediment transport capacity (Donselaar et al, 2013(Donselaar et al, , 2022.…”