Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia

An extreme flooding event occurred from June to July 2017 in the Indigirka River lowland of northeastern Siberia. We used Landsat 8 satellite surface reflectance data to detect the flood inundation area and extract water color for delineating different water sources. We also took direct samples of d...

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Published in:Polar Science
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15932
http://id.nii.ac.jp/1291/00015825/
id ftnipr:oai:nipr.repo.nii.ac.jp:00015932
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00015932 2023-05-15T15:07:22+02:00 Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia 2019-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15932 http://id.nii.ac.jp/1291/00015825/ en eng https://doi.org/10.1016/j.polar.2019.01.005 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15932 http://id.nii.ac.jp/1291/00015825/ Polar Science, 21, 186-194(2019-09) 18739652 Flooding Dissolved methane concentration Arctic Landsat 8 Journal Article 2019 ftnipr https://doi.org/10.1016/j.polar.2019.01.005 2022-12-03T19:43:16Z An extreme flooding event occurred from June to July 2017 in the Indigirka River lowland of northeastern Siberia. We used Landsat 8 satellite surface reflectance data to detect the flood inundation area and extract water color for delineating different water sources. We also took direct samples of dissolved methane concentrations in the river water. Relatively high concentrations of dissolved methane (0.7–1.1 μmol l−1, or μM) were observed in four tributary areas in 2017 during the flood's recession, while the values remained low in the main channel (0.2–0.3 μM). In contrast, the concentrations of dissolved methane were low in both the main channel and tributaries during the non-flood period of 2016 (0.1–0.2 μM). We then used 2017 satellite reflectance data with an empirical model to estimate the spatial differences of dissolved methane concentration for water sources contributing to the methane-poor main channel and methane-rich tributaries and applied the results to the calculation of riverine methane in the study region (approx. 200 × 300 km). This approach to estimating dissolved methane concentrations using satellite reflectance can provide a new tool for environmental monitoring of flood events in remote areas. Article in Journal/Newspaper Arctic Polar Science Polar Science Siberia National Institute of Polar Research Repository, Japan Arctic Indigirka ENVELOPE(149.609,149.609,70.929,70.929) Polar Science 21 186 194
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic Flooding
Dissolved methane concentration
Arctic
Landsat 8
spellingShingle Flooding
Dissolved methane concentration
Arctic
Landsat 8
Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia
topic_facet Flooding
Dissolved methane concentration
Arctic
Landsat 8
description An extreme flooding event occurred from June to July 2017 in the Indigirka River lowland of northeastern Siberia. We used Landsat 8 satellite surface reflectance data to detect the flood inundation area and extract water color for delineating different water sources. We also took direct samples of dissolved methane concentrations in the river water. Relatively high concentrations of dissolved methane (0.7–1.1 μmol l−1, or μM) were observed in four tributary areas in 2017 during the flood's recession, while the values remained low in the main channel (0.2–0.3 μM). In contrast, the concentrations of dissolved methane were low in both the main channel and tributaries during the non-flood period of 2016 (0.1–0.2 μM). We then used 2017 satellite reflectance data with an empirical model to estimate the spatial differences of dissolved methane concentration for water sources contributing to the methane-poor main channel and methane-rich tributaries and applied the results to the calculation of riverine methane in the study region (approx. 200 × 300 km). This approach to estimating dissolved methane concentrations using satellite reflectance can provide a new tool for environmental monitoring of flood events in remote areas.
format Article in Journal/Newspaper
title Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia
title_short Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia
title_full Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia
title_fullStr Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia
title_full_unstemmed Usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern Siberia
title_sort usability of water surface reflectance for the determination of riverine dissolved methane during extreme flooding in northeastern siberia
publishDate 2019
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15932
http://id.nii.ac.jp/1291/00015825/
long_lat ENVELOPE(149.609,149.609,70.929,70.929)
geographic Arctic
Indigirka
geographic_facet Arctic
Indigirka
genre Arctic
Polar Science
Polar Science
Siberia
genre_facet Arctic
Polar Science
Polar Science
Siberia
op_relation https://doi.org/10.1016/j.polar.2019.01.005
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15932
http://id.nii.ac.jp/1291/00015825/
Polar Science, 21, 186-194(2019-09)
18739652
op_doi https://doi.org/10.1016/j.polar.2019.01.005
container_title Polar Science
container_volume 21
container_start_page 186
op_container_end_page 194
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