Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing Data

The retreat rates of Arctic coasts have increased in recent decades at many sites, and an essential part of coasts considered accumulative before have turned erosional due to global climate changes and construction in the coastal zone. In this paper, we study a 7 km long coastal section of the weste...

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Main Authors: Nataliya Belova, Alexander Ermolov, Anna Novikova, Stanislav Ogorodov, Yulia Stanilovskaya
Format: Article
Language:English
Published: MDPI AG 2022-12-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/15/1/48
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author Nataliya Belova
Alexander Ermolov
Anna Novikova
Stanislav Ogorodov
Yulia Stanilovskaya
author_facet Nataliya Belova
Alexander Ermolov
Anna Novikova
Stanislav Ogorodov
Yulia Stanilovskaya
author_sort Nataliya Belova
collection DOAJ
description The retreat rates of Arctic coasts have increased in recent decades at many sites, and an essential part of coasts considered accumulative before have turned erosional due to global climate changes and construction in the coastal zone. In this paper, we study a 7 km long coastal section of the western Gydan Peninsula in a new construction area. Based on the interpretation of multi-temporal satellite imagery, we assessed coastal dynamics in distinct periods from 1972 to 2020. We analyzed the geological structure of the coast as well as changes in hydrometeorological parameters with time, and considering the human impact, we proposed the main drivers of spatial and temporal variations of coastal dynamics. The studied low-lying sandy accumulative marine terrace was more or less stable in the period before construction (1972–2014). However, with the area’s development, the coast dynamics changed drastically: in 2014–2017, three-quarters of the studied area experienced retreat, and the average retreat rate amounted to 5.8 m/yr, up to 28.5 m/yr near the construction sites. We relate this coastal erosion intensification to human impact combined with the growth of hydrometeorological forcing. Although coastal erosion slowed down after 2017, the retreat trend remained. In the coming years, with Arctic climate warming, erosion of the studied coast will continue.
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spelling doaj.art-86758453d9ee42b8b015ce09fe19b9b22023-12-02T00:50:40ZengMDPI AGRemote Sensing2072-42922022-12-011514810.3390/rs15010048Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing DataNataliya Belova0Alexander Ermolov1Anna Novikova2Stanislav Ogorodov3Yulia Stanilovskaya4Laboratory of Geoecology of the North, Faculty of Geography, Lomonosov Moscow State University, 1 Leninskie Gory, 119991 Moscow, RussiaLaboratory of Geoecology of the North, Faculty of Geography, Lomonosov Moscow State University, 1 Leninskie Gory, 119991 Moscow, RussiaLaboratory of Geoecology of the North, Faculty of Geography, Lomonosov Moscow State University, 1 Leninskie Gory, 119991 Moscow, RussiaLaboratory of Geoecology of the North, Faculty of Geography, Lomonosov Moscow State University, 1 Leninskie Gory, 119991 Moscow, RussiaTotalEnergies, 2 Jean Miller, La Defense, 92078 Paris, FranceThe retreat rates of Arctic coasts have increased in recent decades at many sites, and an essential part of coasts considered accumulative before have turned erosional due to global climate changes and construction in the coastal zone. In this paper, we study a 7 km long coastal section of the western Gydan Peninsula in a new construction area. Based on the interpretation of multi-temporal satellite imagery, we assessed coastal dynamics in distinct periods from 1972 to 2020. We analyzed the geological structure of the coast as well as changes in hydrometeorological parameters with time, and considering the human impact, we proposed the main drivers of spatial and temporal variations of coastal dynamics. The studied low-lying sandy accumulative marine terrace was more or less stable in the period before construction (1972–2014). However, with the area’s development, the coast dynamics changed drastically: in 2014–2017, three-quarters of the studied area experienced retreat, and the average retreat rate amounted to 5.8 m/yr, up to 28.5 m/yr near the construction sites. We relate this coastal erosion intensification to human impact combined with the growth of hydrometeorological forcing. Although coastal erosion slowed down after 2017, the retreat trend remained. In the coming years, with Arctic climate warming, erosion of the studied coast will continue.https://www.mdpi.com/2072-4292/15/1/48Arctic coastsaccumulative coastscoastal erosionGydan Peninsula
spellingShingle Nataliya Belova
Alexander Ermolov
Anna Novikova
Stanislav Ogorodov
Yulia Stanilovskaya
Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing Data
Remote Sensing
Arctic coasts
accumulative coasts
coastal erosion
Gydan Peninsula
title Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing Data
title_full Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing Data
title_fullStr Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing Data
title_full_unstemmed Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing Data
title_short Dynamics of Low-Lying Sandy Coast of the Gydan Peninsula, Kara Sea, Russia, Based on Multi-Temporal Remote Sensing Data
title_sort dynamics of low lying sandy coast of the gydan peninsula kara sea russia based on multi temporal remote sensing data
topic Arctic coasts
accumulative coasts
coastal erosion
Gydan Peninsula
url https://www.mdpi.com/2072-4292/15/1/48
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