KAVAN, Jan, Iwo WIECZOREK, Guy D. TALLENTIRE, Mihail DEMIDIONOV, Jakub UHER and Mateusz C. STRZELECKI. Estimating Suspended Sediment Fluxes from the Largest Glacial Lake in Svalbard to Fjord System Using Sentinel-2 Data: Trebrevatnet Case Study. Water. MDPI, 2022, vol. 14, No 12, p. 1-14. ISSN 2073-4441. Available from: https://dx.doi.org/10.3390/w14121840.
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Basic information
Original name Estimating Suspended Sediment Fluxes from the Largest Glacial Lake in Svalbard to Fjord System Using Sentinel-2 Data: Trebrevatnet Case Study
Authors KAVAN, Jan (203 Czech Republic, guarantor, belonging to the institution), Iwo WIECZOREK, Guy D. TALLENTIRE, Mihail DEMIDIONOV (643 Russian Federation, belonging to the institution), Jakub UHER (203 Czech Republic, belonging to the institution) and Mateusz C. STRZELECKI.
Edition Water, MDPI, 2022, 2073-4441.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10508 Physical geography
Country of publisher Switzerland
Confidentiality degree is not subject to a state or trade secret
WWW URL
Impact factor Impact factor: 3.400
RIV identification code RIV/00216224:14310/22:00126233
Organization unit Faculty of Science
Doi http://dx.doi.org/10.3390/w14121840
UT WoS 000816034100001
Keywords in English sediment plumes; glacier meltwater; remote sensing; Sentinel-2; suspended sediment concentration; glacial lake; fjord; Arctic
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 12/7/2022 11:51.
Abstract
Glacier-fed hydrological systems in high latitude regions experience high seasonal variation in meltwater runoff. The peak in runoff usually coincides with the highest air temperatures which drive meltwater production. This process is often accompanied by the release of sediments from within the glacier system that are transported and suspended in high concentrations as they reach the proglacial realm. Sediment-laden meltwater is later transported to the marine environment and is expressed on the surface of fjords and coastal waters as sediment plumes. Direct monitoring of these processes requires complex and time-intensive fieldwork, meaning studies of these processes are rare. This paper demonstrates the seasonal dynamics of the Trebrevatnet lake complex and evolution of suspended sediment in the lake and sediment plumes in the adjacent Ekmanfjorden. We use the Normalized Difference Suspended Sediment Index (NDSSI) derived from multi-temporal Sentinel-2 images for the period between 2016-2021. We propose a new SSL index combining the areal extent of the sediment plume with the NDSSI for quantification of the sediment influx to the marine environment. The largest observed sediment plume was recorded on 30 July 2018 and extended to more than 40 km(2) and a SSL index of 10.4. We identified the greatest sediment concentrations in the lake in the beginning of August, whereas the highest activity of the sediment plumes is concentrated at the end of July. The temporal pattern of these processes stays relatively stable throughout all ablation seasons studied. Sediment plumes observed with the use of optical satellite remote sensing data may be used as a proxy for meltwater runoff from the glacier-fed Trebrevatnet system. We have shown that remote-sensing-derived suspended sediment indexes can (after proper in situ calibration) serve for large scale quantification of sediment flux to fjord and coastal environments.
Links
MUNI/A/1570/2020, interní kód MUName: Geografický výzkum dynamiky přírodních a společenských prostorových procesů (Acronym: GEODYN)
Investor: Masaryk University
MUNI/G/1540/2019, interní kód MUName: ARCTIC Centre for Human-to-Environment Oriented Studies: Impact of Climate Change and Human Activities in the Arctic (Acronym: ARCTOS MU)
Investor: Masaryk University, INTERDISCIPLINARY - Interdisciplinary research projects
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