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Journal article

River discharge estimation from radar altimetry: Assessment of satellite performance, river scales and methods

From

Russian Academy of Sciences1

Geodesy and Earth Observation, National Space Institute, Technical University of Denmark2

National Space Institute, Technical University of Denmark3

Université Fédérale Toulouse Midi-Pyrénées4

The ENVISAT, Jason-2 and -3, Sentinel-3A, CryoSat-2, and AltiKa satellite altimeters were used to estimate the discharge of two Arctic rivers: the Ob and Pur in western Siberia. The accuracy of the water height estimates from ENVISAT varied with river size from 0.63 m for the Ob (~2 km in width) to 1.1 m for the Pur (~0.5 km in width).

A new method for water level estimation combining the CryoSat-2, AltiKa, and Sentinel-3A altimeters provided better height accuracy (0.49 m for the Ob). The rating curve method of discharge estimation outperforms the Manning formulation, on the Ob, with a root mean square error (RMSE) of 13% vs 20% for daily discharge and 1% vs 5% for annual discharge.

Sensitivity analysis performed on the Manning formulation showed high sensitivity to the river depth parameterisation. A functional relationship was identified between the depth of rivers, in the north of western Siberia, and their widths and deposits types. The combination, for the Ob, of the rating curve method with the multi-satellite water level retrieval algorithm provided higher discharge accuracy than previous studies relying on satellite measurements, on numerical modelling or on their combination.

A synthesis of worldwide river altimetry studies supported our finding that the accuracy of altimetric discharge estimations decreases for narrower rivers. The rating curve method applied to Jason 2/3 height measurements allows estimation of daily discharges with RMSE of 18% for the wide Ob River but 38% for the narrow Pur River.

Language: English
Year: 2020
Pages: 124561
ISSN: 18792707 and 00221694
Types: Journal article
DOI: 10.1016/j.jhydrol.2020.124561
ORCIDs: 0000-0002-2962-1439 , 0000-0002-1809-2017 and Nielsen, K.

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