EGU23-8652, updated on 26 Feb 2023
https://doi.org/10.5194/egusphere-egu23-8652
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

IRIS: Global River Surface Slopes from ICESat-2

Daniel Scherer, Christian Schwatke, Denise Dettmering, and Florian Seitz
Daniel Scherer et al.
  • Deutsches Geodätisches Forschungsinstitut (DGFI-TUM), Technische Universität München, Munich, Germany (daniel.scherer@tum.de)

The global reach-scale “ICESat-2 River Surface Slope” (IRIS, https://doi.org/10.5281/zenodo.7098113) dataset comprises average and extreme water surface slopes (WSS) derived from ICESat-2 observations between October 2018 and August 2022 as a supplement to 121,583 reaches from the “SWOT Mission River Database” (SWORD, Altenau et al., 2021). WSS is required to calculate river discharge, which is among the Essential Climate Variables as defined by the Global Climate Observing System. 

To gain full advantage of ICESat-2’s unique measurement geometry with six parallel lidar beams, the WSS is determined across pairs of beams or along individual beams, depending on the intersection angle of spacecraft orbit and river centerline. The combined results of both approaches are validated against in-situ data in a regional study at 815 reaches in Europe and North America with a median absolute error of 23 mm/km, almost complying with the SWOT science requirements of 17 mm/km (Scherer et al., 2022). 

IRIS can be used to research river dynamics, estimate river discharge, and correct water level time series from satellite altimetry for shifting ground tracks. Additionally, by referencing SWORD as a common database, IRIS may be used in combination with observations from the recently launched SWOT mission and could be easily compared against WSS measurements from SWOT’s new wide-swath sensor. 

How to cite: Scherer, D., Schwatke, C., Dettmering, D., and Seitz, F.: IRIS: Global River Surface Slopes from ICESat-2, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-8652, https://doi.org/10.5194/egusphere-egu23-8652, 2023.