Preprints
https://doi.org/10.5194/tc-2020-197
https://doi.org/10.5194/tc-2020-197

  21 Sep 2020

21 Sep 2020

Review status: a revised version of this preprint is currently under review for the journal TC.

Hydrology and runoff routing of glacierized drainage basins in the Kongsfjord area, northwest Svalbard

Ankit Pramanik1,2,3, Jack Kohler1, Katrin Lindbäck1, Penelope How4, Ward Van Pelt5, Glen Liston6, and Thomas V. Schuler2 Ankit Pramanik et al.
  • 1Norwegian Polar Institute, Tromsø, Norway
  • 2University of Oslo, Oslo, Norway
  • 3National Centre for Polar and Ocean Research, Goa, India
  • 4Department of Remote Sensing, Asiaq Greenland Survey, Nuuk, Greenland
  • 5Department of Geosciences, Uppsala University, Uppsala, Sweden
  • 6Colorado State University, CO, USA

Abstract. Freshwater discharge from tidewater glaciers modulates fjord circulation and impacts fjord ecosystems. There can be significant delays between meltwater production at the glacier surface, and discharge into the fjord. Here, we present a hydrological analysis of the tidewater glaciers around Kongsfjorden, northwest of Svalbard, examining the pathways of glacier surface melt to the glacier fronts. To simulate discharge hydrographs at the outlets of the major drainage basins in the Kongsfjord area we use 1) a simple, heuristic routing model and 2) the physically-based model HydroFlow to route runoff derived from a coupled surface energy balance – snow model. Plume observations at one of the tidewater glacier outlets and measurements of proglacial discharge of a land-terminating glacier are used for model calibration. Our analysis suggests that the local subglacial topography diverts a substantial amount of water from the drainage area of the glacier Kongsbreen to the neighboring glacier Kronebreen, across the border of their surface catchments. This is supported by the relative sizes of the plumes observed at the respective glacier fronts. Runoff from the glaciers on the south side of the fjord is one order magnitude lower than runoff from the glaciers on the east and north sides of the fjord, reflecting differences in the size of the glaciers. We derive discharge hydrographs at all the major outlets of Kongsfjord basin, presenting here a detailed analysis of two of the glacierized basins. The average annual discharge period from the tidewater glaciers due to surface runoff was 105 ± 10 days. The largest discharge comes from Kronebreen, which is equivalent to around 40 % of the total freshwater flux to the fjord.

Ankit Pramanik et al.

 
Status: final response (author comments only)
Status: final response (author comments only)
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
[Login for authors/editors] [Subscribe to comment alert] Printer-friendly Version - Printer-friendly version Supplement - Supplement

Ankit Pramanik et al.

Ankit Pramanik et al.

Viewed

Total article views: 484 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
362 116 6 484 7 8
  • HTML: 362
  • PDF: 116
  • XML: 6
  • Total: 484
  • BibTeX: 7
  • EndNote: 8
Views and downloads (calculated since 21 Sep 2020)
Cumulative views and downloads (calculated since 21 Sep 2020)

Viewed (geographical distribution)

Total article views: 472 (including HTML, PDF, and XML) Thereof 467 with geography defined and 5 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 31 Jul 2021
Download
Short summary
Freshwater discharge from tidewater glaciers influences fjord circulation and fjord ecosystem. Glacier hydrology plays crucial role in transporting water underneath glacier ice. We investigated hydrology beneath the tidewater glaciers of Kongsfjord basin in Northwest Svalbard and found that subglacial water flow differs substantially from surface flow of glacier ice. Furthermore, we derived freshwater discharge time-series from all the glaciers to the fjord.