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Bathymetry of Lake Tarfala, northern Sweden

Jakob Kuttenkeuler, Nina Kirchner

Newer versions of this dataset are available

The bathymetry of Lake Tarfala, located in a pro-glacial high alpine environment in the Kebnekaise mountains, northern Sweden, was mapped in September 2016. The mapping was made with an autonomous surface vessel, “ANKA”, designed to map shallow, uncharted waters. The survey had two objectives: (i) to acquire a modern bathymetric dataset of Lake Tarfala that can serve as a reference for future investigations of the lake dynamics. (ii) to test ANKA’s robustness, performance and endurance in a subpolar environment. The dataset includes a comparison with data from an earlier survey conducted in 1959.

LacustrineBathymetryAutonomous hydrographic mappingBathymetryLake Tarfala

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Name

tarfala-kirchner-2017-bathymetry

Version

1

Citation

Jakob Kuttenkeuler, Nina Kirchner (2017) Bathymetry of Lake Tarfala, northern Sweden. Dataset version 1. Bolin Centre Database. https://doi.org/10.17043/tarfala-kirchner-2017-bathymetry-1

References

Autonomous bathymetric mapping of Lake Tarfala, Arctic Sweden. Kirchner, N., Kuttenkeuler, J., Strandell Erstorp, E., Rosqvist, G., Wennbom, M., Karlin, T. Arktos (in review)

Data description

ANKA data was acquired using an echosounder of type AIRMAR® EchoRange™ Smart™ Sensor, operated at 200kHz. Data is stored in xls files, as longitude, latitude and depth. Approximately 40 000 individual single beam echo sounder pings are included. The data has been cleaned for obvious outliers. Historical data by Larje and Nyberger (1960) has been digitized and is provided as xlsx files. The dataset, available in one zip-file, includes four data files and one image file: ANKA_all_soundingsNK.xlsx ANKA_cleaned_soundingsNK.xlsx Bathymetry_Tarfala_NK.png Larje_Nybeger_cropped_soundings_digitized_NK.xlsx Larje_Nyberger_all_soundings_digitizedNK.xlsx

Comments

Pro-glacial high alpine lakes, like Lake Tarfala, potentially hold preserved sediment archives revealing changes in climatically forced glacier activity and ecosystems. Here, we present the first modern bathymetric dataset of Lake Tarfala, containing more that 38000 depth-soundings. The ANKA dataset replaces the previously best-available dataset, published in 1960 from 257 depth-soundings conducted in 1959. A comparison of the two datasets shows that the map constructed from the 1960 data is surprisingly accurate despite it lacks exact GPS positioning, but that the position of single features, e.g. the deepest point of the lake, depends on the spatial resolution of the bathymetric map. The bathymetric dataset from Lake Tarfala presented here is shared with the community with the aim to provide base data useful in future studies of the lake, as well as to inspire for further autonomous mapping campaigns in sparsely monitored high northern latitude lakes.

Project partners

Jakob Kuttenkeuler, KTH Royal Institute of Technology, Stockholm, jakob[at]kth.se

Nina Kirchner, Stockholm Universtity (SU) and KTH, nina.kirchner[at]natgeo.su.se

Elias Strandell Erstorp, KTH, eliasse[at]kth.se

Gunhild Rosqvist, SU, ninis.rosqvist[at]natgeo.su.se.

Video from mapping campaign

Autonomous Hydrographic Mapping at KTH

Project

Autonomous bathymetric mapping of Lake Tarfala, Sweden

Publisher

Bolin Centre Database

First name

Nina

Last name or organisation

Kirchner

Email address

nina.kirchner@natgeo.su.se

Address

Department of Physical Geography, Stockholm University

Postal code

SE-106 91

City

Stockholm

Country

Sweden

GCMD science keyword

Earth science > Terrestrial hydrosphere > Surface water > Lakes

GCMD location

Continent > Europe > Northern Europe > Scandinavia > Sweden

Dataset language

English

Begin date

2016-09-17

End date

2016-09-18

DOI

10.17043/tarfala-kirchner-2017-bathymetry-1

Time

2022-02-01T14:50:46.18564+00:00

Versions

  • 2 2022-02-01T14:50:46.192231+00:00
  • 1 2022-02-01T14:50:46.18564+00:00
  • 2 2022-01-26T13:47:43.770984+00:00
  • 1 2022-01-26T13:47:43.074354+00:00
  • 2 2019-04-25T06:46:00+00:00
  • 1 2017-10-19T11:55:38+00:00