Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model

Tall deciduous shrubs are critically important to carbon and nutrient cycling in high-latitude ecosystems. As Arctic regions warm, shrubs expand heterogeneously across their ranges, including within unburned terrain experiencing isometric gradients of warming. To constrain the effects of widespread...

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Main Authors: Aiden Schore, Mark Lara
Format: Dataset
Language:unknown
Published: Arctic Data Center 2023
Subjects:
Online Access:https://doi.org/10.18739/A28911S58
id dataone:doi:10.18739/A28911S58
record_format openpolar
spelling dataone:doi:10.18739/A28911S58 2024-06-03T18:46:37+00:00 Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model Aiden Schore Mark Lara The central Seward Peninsula region of Alaska ENVELOPE(-167.123,-162.674,65.833,64.759) BEGINDATE: 1950-01-01T00:00:00Z ENDDATE: 2018-01-01T00:00:00Z 2023-01-01T00:00:00Z https://doi.org/10.18739/A28911S58 unknown Arctic Data Center Alaska Arctic shrub alder shrub expansion Seward willow birch tundra permafrost Dataset 2023 dataone:urn:node:ARCTIC https://doi.org/10.18739/A28911S58 2024-06-03T18:20:13Z Tall deciduous shrubs are critically important to carbon and nutrient cycling in high-latitude ecosystems. As Arctic regions warm, shrubs expand heterogeneously across their ranges, including within unburned terrain experiencing isometric gradients of warming. To constrain the effects of widespread shrub expansion in terrestrial and Earth System Models, improved knowledge of local to regional-scale patterns, rates, and controls on decadal shrub expansion is required. Here we map tall deciduous shrub canopies in the central Seward Peninsula of Alaska in 1950 using ~1 meter (m)-resolution aerial photographs from US Navy missions in three subsites (1950ShrubClass.tif and 1950AlderClass.tif) and in 2018 using 3m-resolution PlanetScope satellite imagery for the entire study region (SummerShrubExtent.tif and AlderExtent2017.tif). The timing of alder shrub senescence allowed us to separate the classification into alder and non-alder categories. We computed two change maps: one exclusively for alder and one including all deciduous tall shrubs. The change maps were modeled against a suite of environmental factors and the shrub change model was extended across the study region (SewardShrub.tif). The model was rerun for future scenarios with 10 (SewardMinus10PF.tif) and 30 (SewardMinus30PF.tif) percent reductions in permafrost probability to determine the likely effects of permafrost degradation on shrub extent. Dataset Arctic permafrost Seward Peninsula Tundra Alaska Arctic Data Center (via DataONE) Arctic ENVELOPE(-167.123,-162.674,65.833,64.759)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic Alaska
Arctic
shrub
alder
shrub expansion
Seward
willow
birch
tundra
permafrost
spellingShingle Alaska
Arctic
shrub
alder
shrub expansion
Seward
willow
birch
tundra
permafrost
Aiden Schore
Mark Lara
Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model
topic_facet Alaska
Arctic
shrub
alder
shrub expansion
Seward
willow
birch
tundra
permafrost
description Tall deciduous shrubs are critically important to carbon and nutrient cycling in high-latitude ecosystems. As Arctic regions warm, shrubs expand heterogeneously across their ranges, including within unburned terrain experiencing isometric gradients of warming. To constrain the effects of widespread shrub expansion in terrestrial and Earth System Models, improved knowledge of local to regional-scale patterns, rates, and controls on decadal shrub expansion is required. Here we map tall deciduous shrub canopies in the central Seward Peninsula of Alaska in 1950 using ~1 meter (m)-resolution aerial photographs from US Navy missions in three subsites (1950ShrubClass.tif and 1950AlderClass.tif) and in 2018 using 3m-resolution PlanetScope satellite imagery for the entire study region (SummerShrubExtent.tif and AlderExtent2017.tif). The timing of alder shrub senescence allowed us to separate the classification into alder and non-alder categories. We computed two change maps: one exclusively for alder and one including all deciduous tall shrubs. The change maps were modeled against a suite of environmental factors and the shrub change model was extended across the study region (SewardShrub.tif). The model was rerun for future scenarios with 10 (SewardMinus10PF.tif) and 30 (SewardMinus30PF.tif) percent reductions in permafrost probability to determine the likely effects of permafrost degradation on shrub extent.
format Dataset
author Aiden Schore
Mark Lara
author_facet Aiden Schore
Mark Lara
author_sort Aiden Schore
title Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model
title_short Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model
title_full Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model
title_fullStr Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model
title_full_unstemmed Central Seward Peninsula Deciduous Tall Shrub Map (1950-2018) and Suitable Habitat Model
title_sort central seward peninsula deciduous tall shrub map (1950-2018) and suitable habitat model
publisher Arctic Data Center
publishDate 2023
url https://doi.org/10.18739/A28911S58
op_coverage The central Seward Peninsula region of Alaska
ENVELOPE(-167.123,-162.674,65.833,64.759)
BEGINDATE: 1950-01-01T00:00:00Z ENDDATE: 2018-01-01T00:00:00Z
long_lat ENVELOPE(-167.123,-162.674,65.833,64.759)
geographic Arctic
geographic_facet Arctic
genre Arctic
permafrost
Seward Peninsula
Tundra
Alaska
genre_facet Arctic
permafrost
Seward Peninsula
Tundra
Alaska
op_doi https://doi.org/10.18739/A28911S58
_version_ 1800868849903468544