Preprints
https://doi.org/10.5194/tc-2022-54
https://doi.org/10.5194/tc-2022-54
 
11 Apr 2022
11 Apr 2022
Status: a revised version of this preprint is currently under review for the journal TC.

Brief communication: Hydrologic connectivity of a tidewater glacier characterized with Sentinel-2 satellite images – a case study of Nordenskiöldbreen, Svalbard

Jan Kavan1,2 and Vincent Haagmans3,4 Jan Kavan and Vincent Haagmans
  • 1Polar-Geo-Lab, Department of Geography, Faculty of Science, Masaryk University, Brno, CZ
  • 2Alfred Jahn Cold Region Research Centre, Institute of Geography and Regional Development, University of Wroclaw, Wroclaw, PO
  • 3WSL Institute for Snow and Avalanche Research SLF, Davos Dorf, CH
  • 4Institute of Environmental Engineering, ETH Zürich, Zürich, CH

Abstract. Direct measurements of glacier hydrological processes are usually restricted to short periods and a limited number of sites due to logistical, financial, and meteorological constraints. As a result, the indirect study of glacier hydrology through remote sensing has gained traction while the accessibility of high-resolution publicly available remote sensing data has also increased. By quantifying the areal extents of key dynamic features of a tidewater glacier (i.e. the evolution of sea ice, supraglacial lakes, meltwater plumes) as proxies of its hydrological cycle using Sentinel-2 observations, a simple alternative amidst the outlined logistical constraints is potentially available. Here we demonstrate the usefulness of Sentinel-2 satellite images as a simple and accessible tool with high temporal coverage for studying glacier hydrology. To make this case for the Nordenskiöld tidewater glacier, the evolution of its supraglacial hydrological system and respective meltwater plumes areal extents were monitored for the 2016–2020 melting seasons. Hydrological connectivity of supra- and subglacial systems and the resulting meltwater plumes are illustrated. Meltwater is stored on the glacier surface at the beginning of the melt season (June) which is observed through the filling of the supraglacial lakes. The stored meltwater is later released (June/July), probably through englacial conduits and moulins, and consequently reaches the subglacial drainage system. The resulting occurrence of meltwater plumes clearly indicates the latter in Adolfbukta at the glacier terminus. This signals the transport of significant volumes of water in contact with the glacier bed. The meltwater plume activity peaks during late July, and its appearance continues until mid-September. The duration of the glacier melt season is reflected through the filling of supraglacial lakes and later in the appearance of meltwater plumes. The temporal pattern of the hydrologic processes is relatively uniform during the study period, contrasting the large variability of sea ice cover duration. The observed behavior of Nordenskiöld’s supraglacial lakes is in good agreement with similar tidewater glaciers in Svalbard.

Jan Kavan and Vincent Haagmans

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2022-54', William Armstrong, 09 Jun 2022
    • AC1: 'Reply on RC1', Jan Kavan, 18 Jul 2022
  • RC2: 'Comment on tc-2022-54', Sierra Melton, 12 Jun 2022
    • AC2: 'Reply on RC2', Jan Kavan, 18 Jul 2022

Jan Kavan and Vincent Haagmans

Jan Kavan and Vincent Haagmans

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Short summary
The direct observation of hydrologic processes within a large glacier is rather difficult, therefore we used publicly available remote sensing data in order to describe hydrologic processes of a marine terminating glacier and demonstrated that such tools and data can be easily used. Spatial and temporal pattern of melting dynamics during five consecutive years was described through mapping of supraglacial lakes and sediment plumes areal extent.