Contemporary Dynamics of Glacial Lakes: Comparison Between Selected Systems Developing in Northern, Central and Southern Regions in Spitsbergen
04 wrz 2024
O artykule
Data publikacji: 04 wrz 2024
Zakres stron: 135 - 146
Otrzymano: 21 lut 2024
DOI: https://doi.org/10.14746/quageo-2024-0033
Słowa kluczowe
© 2024 Iwo Wieczorek, published by Sciendo
This work is licensed under the Creative Commons Attribution 4.0 International License.
Fig. 1.

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Fig. 3.

Fig. 4.

Summary of the basic morphometric and meteorological parameters of the selected catchments_
Lake location near the glacier | Catchment area | Glacier area | Annual temperature | Annual precipitation | Altitude min-max | Glacier retreat |
---|---|---|---|---|---|---|
[km2] | [°C] | [mm] | [m a.s.l.] | [m · a−1] | ||
Gåsbreen | 30.77 | 12.59 | −4.0 |
432.9 |
18–1388 | 18 |
Crammerbreen | 9.47 | 5.5 | −2.5 |
32.4 |
55–820 | 11 |
Knivseggbreen and Neppebreen | 6.30 | 2.87 | −6.9 | 200–400 | 51–716 | 4 |
Ragnarbreen | 18.22 | 9.39 | >0 |
189.1 |
86–939 | 9 |
Comparison of glacial lake outburst flood type, area, and volume for glacial lakes in each watershed_
Classification | Unit | Knivseggbreen | Nepebreen | Crammerbreen | Goësvatnet | Ragnarbreen |
---|---|---|---|---|---|---|
Frontal morainedammed lake | Frontal morainedammed lake | Medial-moraine dammed lake | Ice-dammed lake | Frontal morainedammed lake | ||
Biggest recorded area (date) | [m2] | 115,166 (2015) | 206,859 (2022) | 418,292 (2019) | 930,000 (1938) | 546,743 (2023) |
Area before GLOF | [m2] | 49,388 | 197,264 | 418,292 | 370,000 | – |
Area after GLOF | [m2] | 0 | 145,741 | 197,395 | 50,000 | – |
Estimated GLOF volume | [m3] | 666,389 | ND | 4,624,892 | 7,391,392 | – |