2023
DOI: 10.1139/as-2022-0028
|View full text |Cite
|
Sign up to set email alerts
|

Shoreline change rates and land to sea sediment and soil organic carbon transfer in eastern Parry Peninsula from 1965 to 2020 (Amundsen Gulf, Canada)

Abstract: As the Arctic warms, permafrost coasts are eroding faster, threatening coastal communities, habitats, and altering sediment and nutrient budgets. The western Canadian Arctic is eroding at a rapid pace, however little is known on changes occurring in the Amundsen Gulf area. This study was conducted in the eastern coast of Parry Peninsula, a neglected rock-dominated coastal area. We used orthorectified aerial photos of 1965 and 1993 and very-high resolution satellite imagery of 2020 to manually delineate the sho… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
9
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
6
2

Relationship

1
7

Authors

Journals

citations
Cited by 8 publications
(9 citation statements)
references
References 39 publications
0
9
0
Order By: Relevance
“…The phases values are correctly represented with a correlation coefficient (R 2 ) of 0.9; however, the amplitudes are not correctly represented, varying by one order of magnitude from those obtained in previous studies [68]. Therefore, it was decided that we would evaluate different values of Chèzy (45,65,100) to perform a sensitivity study. Figure 7 shows how when changing the Chèzy coefficient, the values do not vary by more than 30% in the peaks, and in the rest, they follow a trend with a maximum variation of 3%.…”
Section: Model Calibrationmentioning
confidence: 96%
See 1 more Smart Citation
“…The phases values are correctly represented with a correlation coefficient (R 2 ) of 0.9; however, the amplitudes are not correctly represented, varying by one order of magnitude from those obtained in previous studies [68]. Therefore, it was decided that we would evaluate different values of Chèzy (45,65,100) to perform a sensitivity study. Figure 7 shows how when changing the Chèzy coefficient, the values do not vary by more than 30% in the peaks, and in the rest, they follow a trend with a maximum variation of 3%.…”
Section: Model Calibrationmentioning
confidence: 96%
“…In addition, DSAS v5 software was used to evaluate dynamic rates derived by comparing coastlines from 1970, 2003, and 2020 in a second step. This software is an ArcGIS extension [64] and a powerful tool specifically designed for the analysis and monitoring of coastlines using geospatial data [65,66]. Specifically, this application was used in this study to visualise and assess changes in the position over time and identify vulnerable areas.…”
Section: Coastline Evolutionmentioning
confidence: 99%
“…] LU/LC (1) Habitat GaoFen3-SAR (4.5-5 m) No --[416] LU/LC Habitat GaoFen5-HIS (30 m) (2) No --[417,418] LU/LC (1) Habitat HSI ZiYuan1-02D (30 m) (2) No -[419] -LU/LC (1) Habitat Landsat ( -LU/LC (1) LST Landsat (15-30 m) No - [112] -LU/LC (1) LST Sentinel-2 (10-20-60 m) No - [112] -LU/LC (1) LU/LC change -Yes --[433,434] LU/LC (1) LU/LC change Aerial photos No [364] [435,436] -LU/LC (1) LU/LC change GaoFen-5-HIS (30 m) (2) No -[219] -LU/LC (1) LU -LU/LC (1) LU/LC change MODIS (…”
Section: Parametermentioning
confidence: 99%
“…In the same year, ref. [45] studied shoreline changes using orthophoto aerial photographs and high-resolution satellite imagery (Pleiades) for the east coast of the Parry Peninsula, Canada. Like previous studies, the shoreline was manually delineated, and the DSAS tool was used to measure the erosion rate.…”
Section: Manual Visual Interpretationmentioning
confidence: 99%