Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia

Simulations with the spatially explicit and individual-based Siberian forest model LAVESI (Kruse et al., 2016, 2018, 2019) were set-up for transect in four focus regions covering the East Siberian treeline and tundra area (details in Kruse & Herzschuh, submitted). The model was updated to includ...

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Main Authors: Kruse, Stefan, Herzschuh, Ulrike
Format: Other/Unknown Material
Language:English
Published: Zenodo 2022
Subjects:
IBM
Online Access:https://doi.org/10.5281/zenodo.6484111
id ftzenodo:oai:zenodo.org:6484111
record_format openpolar
spelling ftzenodo:oai:zenodo.org:6484111 2024-09-15T17:53:42+00:00 Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia Kruse, Stefan Herzschuh, Ulrike 2022-04-25 https://doi.org/10.5281/zenodo.6484111 eng eng Zenodo https://zenodo.org/communities/eu https://doi.org/10.5281/zenodo.6484110 https://doi.org/10.5281/zenodo.6484111 oai:zenodo.org:6484111 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Simulation IBM Siberia Larix Treeline info:eu-repo/semantics/other 2022 ftzenodo https://doi.org/10.5281/zenodo.648411110.5281/zenodo.6484110 2024-07-25T15:21:45Z Simulations with the spatially explicit and individual-based Siberian forest model LAVESI (Kruse et al., 2016, 2018, 2019) were set-up for transect in four focus regions covering the East Siberian treeline and tundra area (details in Kruse & Herzschuh, submitted). The model was updated to include climate forcing data for 300-800 km long and 20 m wide transects necessary for simulating the forest development between the northern taiga forests and the coast of the Arctic Ocean. Forced with climate forecasts driven by relative concentration pathway (RCP) scenarios 2.6, 4.5 and 8.5 and one with half the warming of RCP 2.6 named 2.6*. These were extended until 3000 AD either following the cooling of the scenarios after peak-warming, or with an arbitrary cooling back to levels of the 20th century. During the simulations, three key variables were extracted in 10-year steps for 2000-3000 AD: single-tree line, treeline, and, forest line, which are defined as the northernmost position of stands with >1 stem (tree > 1.3 m tall) per ha, the northernmost position of a forest cover not falling below 1 stem per ha, and, the northernmost position of a forest cover not falling below 100 stems ha per ha (see for a graphical representation Fig. 2 in Kruse et al., 2019). The determined treeline at year 2000 was used as baseline expansion and subtracted from each following years’ values. Furthermore, the tundra area was estimated for each of the four regions as the area between the treeline and the Arctic Ocean, based on interpolating the treeline position at the four transects over the complete modern treeline (Walker et al., 2005). Content of Table 1 "Kruse_and_Herzschuh_2022_Forest_expansion_in_Siberia_2010_to_3000_CE.csv": Column 1: Scenario: RCP scenario used Column 2: Region: One of the four regions, from east-to-west Taimyr Peninsula, Buor Khaya Peninsula, Kolyma River Basin, Chukotka Column 3: Year: Year in CE of the simulation in 10 year steps Column 4: Forest line in m Column 5: Treeline in m Column 6: ... Other/Unknown Material Arctic Ocean Chukotka kolyma river taiga Taimyr Tundra Siberia Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Simulation
IBM
Siberia
Larix
Treeline
spellingShingle Simulation
IBM
Siberia
Larix
Treeline
Kruse, Stefan
Herzschuh, Ulrike
Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia
topic_facet Simulation
IBM
Siberia
Larix
Treeline
description Simulations with the spatially explicit and individual-based Siberian forest model LAVESI (Kruse et al., 2016, 2018, 2019) were set-up for transect in four focus regions covering the East Siberian treeline and tundra area (details in Kruse & Herzschuh, submitted). The model was updated to include climate forcing data for 300-800 km long and 20 m wide transects necessary for simulating the forest development between the northern taiga forests and the coast of the Arctic Ocean. Forced with climate forecasts driven by relative concentration pathway (RCP) scenarios 2.6, 4.5 and 8.5 and one with half the warming of RCP 2.6 named 2.6*. These were extended until 3000 AD either following the cooling of the scenarios after peak-warming, or with an arbitrary cooling back to levels of the 20th century. During the simulations, three key variables were extracted in 10-year steps for 2000-3000 AD: single-tree line, treeline, and, forest line, which are defined as the northernmost position of stands with >1 stem (tree > 1.3 m tall) per ha, the northernmost position of a forest cover not falling below 1 stem per ha, and, the northernmost position of a forest cover not falling below 100 stems ha per ha (see for a graphical representation Fig. 2 in Kruse et al., 2019). The determined treeline at year 2000 was used as baseline expansion and subtracted from each following years’ values. Furthermore, the tundra area was estimated for each of the four regions as the area between the treeline and the Arctic Ocean, based on interpolating the treeline position at the four transects over the complete modern treeline (Walker et al., 2005). Content of Table 1 "Kruse_and_Herzschuh_2022_Forest_expansion_in_Siberia_2010_to_3000_CE.csv": Column 1: Scenario: RCP scenario used Column 2: Region: One of the four regions, from east-to-west Taimyr Peninsula, Buor Khaya Peninsula, Kolyma River Basin, Chukotka Column 3: Year: Year in CE of the simulation in 10 year steps Column 4: Forest line in m Column 5: Treeline in m Column 6: ...
format Other/Unknown Material
author Kruse, Stefan
Herzschuh, Ulrike
author_facet Kruse, Stefan
Herzschuh, Ulrike
author_sort Kruse, Stefan
title Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia
title_short Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia
title_full Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia
title_fullStr Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia
title_full_unstemmed Forest expansion for different warming scenarios simulated for 2010 to 3000 CE with LAVESI for Siberia
title_sort forest expansion for different warming scenarios simulated for 2010 to 3000 ce with lavesi for siberia
publisher Zenodo
publishDate 2022
url https://doi.org/10.5281/zenodo.6484111
genre Arctic Ocean
Chukotka
kolyma river
taiga
Taimyr
Tundra
Siberia
genre_facet Arctic Ocean
Chukotka
kolyma river
taiga
Taimyr
Tundra
Siberia
op_relation https://zenodo.org/communities/eu
https://doi.org/10.5281/zenodo.6484110
https://doi.org/10.5281/zenodo.6484111
oai:zenodo.org:6484111
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.648411110.5281/zenodo.6484110
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