Image Details
Caption: Figure 3.
Discharge, calculated using the Darcy–Weisbach equation (Equations (1)–(4)), varies with water depth in the inlet channels of the Hypanis, Nanedi, Jezero, No-name, Eberswalde, Rypin, and Balvicar Deltas. The results are presented in logarithmic scale graphs: (a) maximum water discharge and (b) minimum water discharge.
© 2026. The Author(s). Published by the American Astronomical Society.