Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska

Questions Is it possible to map floristic gradients in heterogeneous boreal vegetation by using remote‐sensing data? Does a continuous vegetation map enable the creation of a spatially continuous map of seasonal permafrost soil thaw depth? Location Bonanza Creek LTER, Fairbanks, Alaska, USA. Methods...

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Main Authors: Döpper, Veronika, Panda, Santosh, Waigl, Christine, Braun, Matthias, Feilhauer, Hannes
Format: Article in Journal/Newspaper
Language:English
Published: 2021
Subjects:
Online Access:https://depositonce.tu-berlin.de/handle/11303/13300
https://doi.org/10.14279/depositonce-12092
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spelling ftdepositonce:oai:depositonce.tu-berlin.de:11303/13300 2023-07-02T03:33:26+02:00 Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska Döpper, Veronika Panda, Santosh Waigl, Christine Braun, Matthias Feilhauer, Hannes 2021-02-22 application/pdf https://depositonce.tu-berlin.de/handle/11303/13300 https://doi.org/10.14279/depositonce-12092 en eng 1654-109X 1402-2001 https://depositonce.tu-berlin.de/handle/11303/13300 http://dx.doi.org/10.14279/depositonce-12092 https://creativecommons.org/licenses/by-nc/4.0/ 550 Geowissenschaften boreal vegetation ordination permafrost predictive mapping remote sensing soil–vegetation interaction Article publishedVersion 2021 ftdepositonce https://doi.org/10.14279/depositonce-12092 2023-06-12T16:20:48Z Questions Is it possible to map floristic gradients in heterogeneous boreal vegetation by using remote‐sensing data? Does a continuous vegetation map enable the creation of a spatially continuous map of seasonal permafrost soil thaw depth? Location Bonanza Creek LTER, Fairbanks, Alaska, USA. Methods Vegetation records are subjected to an ordination to extract the predominant floristic gradient. The ordination scores are then extrapolated using Sentinel 2 imagery and a digital elevation model (DEM). As the relation between vegetation pattern and seasonal thaw depth was confirmed in this study, the spatial distribution of ordination scores is then used to predict seasonal thaw depth over the same area. Results The first dimension of the ordination space separates species corresponding to moist and cold soil conditions from species associated with well‐drained soils. This floristic gradient was successfully mapped within the sampled plant communities. The extrapolated thaw depths follow the typical distribution along a topographical and geomorphological gradient for this region. Besides vegetation information also DEM derivatives show high contributions to the thaw depth modeling. Conclusion We demonstrate that floristic gradient mapping in boreal vegetation is possible. The accuracy of the thaw depth prediction model is comparable to that in previous analyses but uses a more parsimonious set of predictors, underlining the efficacy of this approach. TU Berlin, Open-Access-Mittel – 2021 Article in Journal/Newspaper permafrost Alaska TU Berlin: Deposit Once Fairbanks Bonanza ENVELOPE(-119.820,-119.820,55.917,55.917)
institution Open Polar
collection TU Berlin: Deposit Once
op_collection_id ftdepositonce
language English
topic 550 Geowissenschaften
boreal vegetation
ordination
permafrost
predictive mapping
remote sensing
soil–vegetation interaction
spellingShingle 550 Geowissenschaften
boreal vegetation
ordination
permafrost
predictive mapping
remote sensing
soil–vegetation interaction
Döpper, Veronika
Panda, Santosh
Waigl, Christine
Braun, Matthias
Feilhauer, Hannes
Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska
topic_facet 550 Geowissenschaften
boreal vegetation
ordination
permafrost
predictive mapping
remote sensing
soil–vegetation interaction
description Questions Is it possible to map floristic gradients in heterogeneous boreal vegetation by using remote‐sensing data? Does a continuous vegetation map enable the creation of a spatially continuous map of seasonal permafrost soil thaw depth? Location Bonanza Creek LTER, Fairbanks, Alaska, USA. Methods Vegetation records are subjected to an ordination to extract the predominant floristic gradient. The ordination scores are then extrapolated using Sentinel 2 imagery and a digital elevation model (DEM). As the relation between vegetation pattern and seasonal thaw depth was confirmed in this study, the spatial distribution of ordination scores is then used to predict seasonal thaw depth over the same area. Results The first dimension of the ordination space separates species corresponding to moist and cold soil conditions from species associated with well‐drained soils. This floristic gradient was successfully mapped within the sampled plant communities. The extrapolated thaw depths follow the typical distribution along a topographical and geomorphological gradient for this region. Besides vegetation information also DEM derivatives show high contributions to the thaw depth modeling. Conclusion We demonstrate that floristic gradient mapping in boreal vegetation is possible. The accuracy of the thaw depth prediction model is comparable to that in previous analyses but uses a more parsimonious set of predictors, underlining the efficacy of this approach. TU Berlin, Open-Access-Mittel – 2021
format Article in Journal/Newspaper
author Döpper, Veronika
Panda, Santosh
Waigl, Christine
Braun, Matthias
Feilhauer, Hannes
author_facet Döpper, Veronika
Panda, Santosh
Waigl, Christine
Braun, Matthias
Feilhauer, Hannes
author_sort Döpper, Veronika
title Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska
title_short Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska
title_full Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska
title_fullStr Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska
title_full_unstemmed Using floristic gradient mapping to assess seasonal thaw depth in interior Alaska
title_sort using floristic gradient mapping to assess seasonal thaw depth in interior alaska
publishDate 2021
url https://depositonce.tu-berlin.de/handle/11303/13300
https://doi.org/10.14279/depositonce-12092
long_lat ENVELOPE(-119.820,-119.820,55.917,55.917)
geographic Fairbanks
Bonanza
geographic_facet Fairbanks
Bonanza
genre permafrost
Alaska
genre_facet permafrost
Alaska
op_relation 1654-109X
1402-2001
https://depositonce.tu-berlin.de/handle/11303/13300
http://dx.doi.org/10.14279/depositonce-12092
op_rights https://creativecommons.org/licenses/by-nc/4.0/
op_doi https://doi.org/10.14279/depositonce-12092
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