Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density.
Black lines represent modelled relationships from linear mixed effects models with random effects of grid (2 levels) and plot (46 levels) nested within grid. Shading represents 95% confidence regions. See Table 2 for model results.
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Online Access: | https://doi.org/10.1371/journal.pone.0258558.g003 |
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ftsmithonian:oai:figshare.com:article/16899230 2023-05-15T13:09:42+02:00 Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density. Xanthe J. Walker (3715783) Brain K. Howard (11619743) Mélanie Jean (3715789) Jill F. Johnstone (8027336) Carl Roland (6504848) Brendan M. Rogers (9184067) Edward A. G. Schuur (2663494) Kylen K. Solvik (11619746) Michelle C. Mack (8949893) 2021-10-28T17:44:11Z https://doi.org/10.1371/journal.pone.0258558.g003 unknown https://figshare.com/articles/figure/Burn_depth_residual_soil_organic_layer_SOL_depth_and_proportion_of_pre-fire_SOL_combusted_as_a_function_of_pre-fire_SOL_depth_and_conifer_density_/16899230 doi:10.1371/journal.pone.0258558.g003 CC BY 4.0 CC-BY Cell Biology Molecular Biology Evolutionary Biology Ecology Sociology Developmental Biology Plant Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified understory vegetation composition occur without increases drier landscape positions denali national park active layer thickness 6 ± 4 18 ± 1 density spruce stands seed rain observations extensive 2013 wildfire fire tree regeneration conifer tree recruitment seeding experiment indicate div >< p 13 kg c fire conifer density assessed wildfire severity induced forest infilling increased alt post increased density seeding experiment conifer trees recruitment potential alt ) wildfire throughout wildfire severity wildfire frequency seed availability organic soil north slope make predictions increasing throughout higher post global carbon future flammability ecosystem structure central alaska c emissions burn depth also located almost 95 alaska range 5 cm Image Figure 2021 ftsmithonian https://doi.org/10.1371/journal.pone.0258558.g003 2021-12-19T23:06:32Z Black lines represent modelled relationships from linear mixed effects models with random effects of grid (2 levels) and plot (46 levels) nested within grid. Shading represents 95% confidence regions. See Table 2 for model results. Still Image alaska range north slope Alaska Unknown |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftsmithonian |
language |
unknown |
topic |
Cell Biology Molecular Biology Evolutionary Biology Ecology Sociology Developmental Biology Plant Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified understory vegetation composition occur without increases drier landscape positions denali national park active layer thickness 6 ± 4 18 ± 1 density spruce stands seed rain observations extensive 2013 wildfire fire tree regeneration conifer tree recruitment seeding experiment indicate div >< p 13 kg c fire conifer density assessed wildfire severity induced forest infilling increased alt post increased density seeding experiment conifer trees recruitment potential alt ) wildfire throughout wildfire severity wildfire frequency seed availability organic soil north slope make predictions increasing throughout higher post global carbon future flammability ecosystem structure central alaska c emissions burn depth also located almost 95 alaska range 5 cm |
spellingShingle |
Cell Biology Molecular Biology Evolutionary Biology Ecology Sociology Developmental Biology Plant Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified understory vegetation composition occur without increases drier landscape positions denali national park active layer thickness 6 ± 4 18 ± 1 density spruce stands seed rain observations extensive 2013 wildfire fire tree regeneration conifer tree recruitment seeding experiment indicate div >< p 13 kg c fire conifer density assessed wildfire severity induced forest infilling increased alt post increased density seeding experiment conifer trees recruitment potential alt ) wildfire throughout wildfire severity wildfire frequency seed availability organic soil north slope make predictions increasing throughout higher post global carbon future flammability ecosystem structure central alaska c emissions burn depth also located almost 95 alaska range 5 cm Xanthe J. Walker (3715783) Brain K. Howard (11619743) Mélanie Jean (3715789) Jill F. Johnstone (8027336) Carl Roland (6504848) Brendan M. Rogers (9184067) Edward A. G. Schuur (2663494) Kylen K. Solvik (11619746) Michelle C. Mack (8949893) Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density. |
topic_facet |
Cell Biology Molecular Biology Evolutionary Biology Ecology Sociology Developmental Biology Plant Biology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified understory vegetation composition occur without increases drier landscape positions denali national park active layer thickness 6 ± 4 18 ± 1 density spruce stands seed rain observations extensive 2013 wildfire fire tree regeneration conifer tree recruitment seeding experiment indicate div >< p 13 kg c fire conifer density assessed wildfire severity induced forest infilling increased alt post increased density seeding experiment conifer trees recruitment potential alt ) wildfire throughout wildfire severity wildfire frequency seed availability organic soil north slope make predictions increasing throughout higher post global carbon future flammability ecosystem structure central alaska c emissions burn depth also located almost 95 alaska range 5 cm |
description |
Black lines represent modelled relationships from linear mixed effects models with random effects of grid (2 levels) and plot (46 levels) nested within grid. Shading represents 95% confidence regions. See Table 2 for model results. |
format |
Still Image |
author |
Xanthe J. Walker (3715783) Brain K. Howard (11619743) Mélanie Jean (3715789) Jill F. Johnstone (8027336) Carl Roland (6504848) Brendan M. Rogers (9184067) Edward A. G. Schuur (2663494) Kylen K. Solvik (11619746) Michelle C. Mack (8949893) |
author_facet |
Xanthe J. Walker (3715783) Brain K. Howard (11619743) Mélanie Jean (3715789) Jill F. Johnstone (8027336) Carl Roland (6504848) Brendan M. Rogers (9184067) Edward A. G. Schuur (2663494) Kylen K. Solvik (11619746) Michelle C. Mack (8949893) |
author_sort |
Xanthe J. Walker (3715783) |
title |
Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density. |
title_short |
Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density. |
title_full |
Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density. |
title_fullStr |
Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density. |
title_full_unstemmed |
Burn depth, residual soil organic layer (SOL) depth, and proportion of pre-fire SOL combusted as a function of pre-fire SOL depth and conifer density. |
title_sort |
burn depth, residual soil organic layer (sol) depth, and proportion of pre-fire sol combusted as a function of pre-fire sol depth and conifer density. |
publishDate |
2021 |
url |
https://doi.org/10.1371/journal.pone.0258558.g003 |
genre |
alaska range north slope Alaska |
genre_facet |
alaska range north slope Alaska |
op_relation |
https://figshare.com/articles/figure/Burn_depth_residual_soil_organic_layer_SOL_depth_and_proportion_of_pre-fire_SOL_combusted_as_a_function_of_pre-fire_SOL_depth_and_conifer_density_/16899230 doi:10.1371/journal.pone.0258558.g003 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1371/journal.pone.0258558.g003 |
_version_ |
1766194729356099584 |