Abstract
The analysis of changes in the catchment vegetation cover as a result of industrial development of its territory, primarily deforestation, was carried out. For processing Landsat images, the spectral space modeling method was used, which provides higher reliability of the classification results compared to traditional methods. The most significant changes in the catchment occurred from the 1930s (the beginning of large-scale logging), until the end of the 1990s. Significantly, by more than 60 %, the area of old-growth forests decreased, their large fragments remained only in nature protected areas, as well as around large lakes and along large rivers, due to the presence of water protection zones. In the period from 2000 to 2018 due to deforestation, the area of productive forests decreased even more. Nevertheless, by 2019 the occurrence of secondary reforestation on significant areas (up to 70 %) is noted, which indicates a sufficiently high regeneration potential of the catchment ecosystems. To restore the spatial structure of the forest cover in the period before the start of the Landsat 5 operation, the method of tracking the trajectories of reforestation successions in the spectral space was used. A comparison with the results of the Global Forest Change 2000—2018 data (loss/gain) showed almost complete coincidence in cuttings (loss), but the method of reforestation trajectories showed many times higher results in forest gain, since it reveals forest regeneration at a much earlier stage. The developed methodology will be applied on the catchments of other tributaries of the White Sea, and the results will be used as input to an environmental-socio-economic cognitive model that predicts the state of ecosystems under climate changes and economic priorities.
Highlights
Арктической зоны России; площадь водосбора 710 000 км[2]
which provides higher reliability of the classification results compared to traditional methods
most significant changes in the catchment occurred from the 1930s
Summary
Арктической зоны России; площадь водосбора 710 000 км[2]. Регион имеет большое практическое значение в рамках освоения ресурсов Арктики, в связи с чем в настоящее время Карельский НЦ РАН проводит системные исследования происходящих здесь социо-эколого-экономических процессов. Территория водосбора служила модельным полигоном для разработки нового метода извлечения информации из сканерных снимков [Литинский, 2018], который и применялся в данном исследовании. Результаты исследований динамики лесного покрова необходимы для прогнозирования как экологических, так и экономических и социальных процессов. Одновременно проводилась предварительная оценка степени пригодности для оценки динамики растительности конкретных территорий глобальных данных Global Forest Change [Hansen et al, 2013].
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.