Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying
Climate-driven permafrost thaw alters the strongly coupled carbon and nitrogen cycles within the Arctic tundra, influencing the availability of limiting nutrients including nitrate (NO 3 − ). Researchers have identified two primary mechanisms that increase nitrogen and NO 3 − availability within per...
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ftdoajarticles:oai:doaj.org/article:39d66e730cc34018a7ef8177b62c2466 2023-05-15T14:43:52+02:00 Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying Carli A. Arendt Jeffrey M. Heikoop Brent D. Newman Cathy J. Wilson Haruko Wainwright Jitendra Kumar Christian G. Andersen Nathan A. Wales Baptiste Dafflon Jessica Cherry Stan D. Wullschleger 2022-05-01T00:00:00Z https://doi.org/10.3390/nitrogen3020021 https://doaj.org/article/39d66e730cc34018a7ef8177b62c2466 EN eng MDPI AG https://www.mdpi.com/2504-3129/3/2/21 https://doaj.org/toc/2504-3129 doi:10.3390/nitrogen3020021 2504-3129 https://doaj.org/article/39d66e730cc34018a7ef8177b62c2466 Nitrogen, Vol 3, Iss 21, Pp 314-332 (2022) polygonal permafrost climate change Arctic nutrient availability nitrate soil moisture Ecology QH540-549.5 article 2022 ftdoajarticles https://doi.org/10.3390/nitrogen3020021 2022-12-31T02:41:15Z Climate-driven permafrost thaw alters the strongly coupled carbon and nitrogen cycles within the Arctic tundra, influencing the availability of limiting nutrients including nitrate (NO 3 − ). Researchers have identified two primary mechanisms that increase nitrogen and NO 3 − availability within permafrost soils: (1) the ‘frozen feast’, where previously frozen organic material becomes available as it thaws, and (2) ‘shrubification’, where expansion of nitrogen-fixing shrubs promotes increased soil nitrogen. Through the synthesis of original and previously published observational data, and the application of multiple geospatial approaches, this study investigates and highlights a third mechanism that increases NO 3 − availability: the hydrogeomorphic evolution of polygonal permafrost landscapes. Permafrost thaw drives changes in microtopography, increasing the drainage of topographic highs, thus increasing oxic conditions that promote NO 3 − production and accumulation. We extrapolate relationships between NO 3 − and soil moisture in elevated topographic features within our study area and the broader Alaskan Coastal Plain and investigate potential changes in NO 3 − availability in response to possible hydrogeomorphic evolution scenarios of permafrost landscapes. These approximations indicate that such changes could increase Arctic tundra NO 3 − availability by ~250–1000%. Thus, hydrogeomorphic changes that accompany continued permafrost degradation in polygonal permafrost landscapes will substantially increase soil pore water NO 3 − availability and boost future fertilization and productivity in the Arctic. Article in Journal/Newspaper Arctic Climate change permafrost Tundra Directory of Open Access Journals: DOAJ Articles Arctic Nitrogen 3 2 314 332 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
polygonal permafrost climate change Arctic nutrient availability nitrate soil moisture Ecology QH540-549.5 |
spellingShingle |
polygonal permafrost climate change Arctic nutrient availability nitrate soil moisture Ecology QH540-549.5 Carli A. Arendt Jeffrey M. Heikoop Brent D. Newman Cathy J. Wilson Haruko Wainwright Jitendra Kumar Christian G. Andersen Nathan A. Wales Baptiste Dafflon Jessica Cherry Stan D. Wullschleger Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying |
topic_facet |
polygonal permafrost climate change Arctic nutrient availability nitrate soil moisture Ecology QH540-549.5 |
description |
Climate-driven permafrost thaw alters the strongly coupled carbon and nitrogen cycles within the Arctic tundra, influencing the availability of limiting nutrients including nitrate (NO 3 − ). Researchers have identified two primary mechanisms that increase nitrogen and NO 3 − availability within permafrost soils: (1) the ‘frozen feast’, where previously frozen organic material becomes available as it thaws, and (2) ‘shrubification’, where expansion of nitrogen-fixing shrubs promotes increased soil nitrogen. Through the synthesis of original and previously published observational data, and the application of multiple geospatial approaches, this study investigates and highlights a third mechanism that increases NO 3 − availability: the hydrogeomorphic evolution of polygonal permafrost landscapes. Permafrost thaw drives changes in microtopography, increasing the drainage of topographic highs, thus increasing oxic conditions that promote NO 3 − production and accumulation. We extrapolate relationships between NO 3 − and soil moisture in elevated topographic features within our study area and the broader Alaskan Coastal Plain and investigate potential changes in NO 3 − availability in response to possible hydrogeomorphic evolution scenarios of permafrost landscapes. These approximations indicate that such changes could increase Arctic tundra NO 3 − availability by ~250–1000%. Thus, hydrogeomorphic changes that accompany continued permafrost degradation in polygonal permafrost landscapes will substantially increase soil pore water NO 3 − availability and boost future fertilization and productivity in the Arctic. |
format |
Article in Journal/Newspaper |
author |
Carli A. Arendt Jeffrey M. Heikoop Brent D. Newman Cathy J. Wilson Haruko Wainwright Jitendra Kumar Christian G. Andersen Nathan A. Wales Baptiste Dafflon Jessica Cherry Stan D. Wullschleger |
author_facet |
Carli A. Arendt Jeffrey M. Heikoop Brent D. Newman Cathy J. Wilson Haruko Wainwright Jitendra Kumar Christian G. Andersen Nathan A. Wales Baptiste Dafflon Jessica Cherry Stan D. Wullschleger |
author_sort |
Carli A. Arendt |
title |
Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying |
title_short |
Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying |
title_full |
Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying |
title_fullStr |
Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying |
title_full_unstemmed |
Increased Arctic NO 3 − Availability as a Hydrogeomorphic Consequence of Permafrost Degradation and Landscape Drying |
title_sort |
increased arctic no 3 − availability as a hydrogeomorphic consequence of permafrost degradation and landscape drying |
publisher |
MDPI AG |
publishDate |
2022 |
url |
https://doi.org/10.3390/nitrogen3020021 https://doaj.org/article/39d66e730cc34018a7ef8177b62c2466 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change permafrost Tundra |
genre_facet |
Arctic Climate change permafrost Tundra |
op_source |
Nitrogen, Vol 3, Iss 21, Pp 314-332 (2022) |
op_relation |
https://www.mdpi.com/2504-3129/3/2/21 https://doaj.org/toc/2504-3129 doi:10.3390/nitrogen3020021 2504-3129 https://doaj.org/article/39d66e730cc34018a7ef8177b62c2466 |
op_doi |
https://doi.org/10.3390/nitrogen3020021 |
container_title |
Nitrogen |
container_volume |
3 |
container_issue |
2 |
container_start_page |
314 |
op_container_end_page |
332 |
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1766315457630961664 |