Thermodynamic basis for the demarcation of Arctic and alpine treelines

Abstract At the edge of alpine and Arctic ecosystems all over the world, a transition zone exists beyond which it is either infeasible or unfavorable for trees to exist, colloquially identified as the treeline. We explore the possibility of a thermodynamic basis behind this demarcation in vegetation...

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Published in:Scientific Reports
Main Authors: Meredith Richardson Martin, Praveen Kumar, Oliver Sonnentag, Philip Marsh
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2022
Subjects:
R
Q
Online Access:https://doi.org/10.1038/s41598-022-16462-2
https://doaj.org/article/4b5e1cf996cf473493d2a3da8038f1fa
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spelling ftdoajarticles:oai:doaj.org/article:4b5e1cf996cf473493d2a3da8038f1fa 2023-05-15T14:51:52+02:00 Thermodynamic basis for the demarcation of Arctic and alpine treelines Meredith Richardson Martin Praveen Kumar Oliver Sonnentag Philip Marsh 2022-07-01T00:00:00Z https://doi.org/10.1038/s41598-022-16462-2 https://doaj.org/article/4b5e1cf996cf473493d2a3da8038f1fa EN eng Nature Portfolio https://doi.org/10.1038/s41598-022-16462-2 https://doaj.org/toc/2045-2322 doi:10.1038/s41598-022-16462-2 2045-2322 https://doaj.org/article/4b5e1cf996cf473493d2a3da8038f1fa Scientific Reports, Vol 12, Iss 1, Pp 1-14 (2022) Medicine R Science Q article 2022 ftdoajarticles https://doi.org/10.1038/s41598-022-16462-2 2022-12-30T22:19:14Z Abstract At the edge of alpine and Arctic ecosystems all over the world, a transition zone exists beyond which it is either infeasible or unfavorable for trees to exist, colloquially identified as the treeline. We explore the possibility of a thermodynamic basis behind this demarcation in vegetation by considering ecosystems as open systems driven by thermodynamic advantage—defined by vegetation’s ability to dissipate heat from the earth’s surface to the air above the canopy. To deduce whether forests would be more thermodynamically advantageous than existing ecosystems beyond treelines, we construct and examine counterfactual scenarios in which trees exist beyond a treeline instead of the existing alpine meadow or Arctic tundra. Meteorological data from the Italian Alps, United States Rocky Mountains, and Western Canadian Taiga-Tundra are used as forcing for model computation of ecosystem work and temperature gradients at sites on both sides of each treeline with and without trees. Model results indicate that the alpine sites do not support trees beyond the treeline, as their presence would result in excessive CO $$_2$$ 2 loss and extended periods of snowpack due to temperature inversions (i.e., positive temperature gradient from the earth surface to the atmosphere). Further, both Arctic and alpine sites exhibit negative work resulting in positive feedback between vegetation heat dissipation and temperature gradient, thereby extending the duration of temperature inversions. These conditions demonstrate thermodynamic infeasibility associated with the counterfactual scenario of trees existing beyond a treeline. Thus, we conclude that, in addition to resource constraints, a treeline is an outcome of an ecosystem’s ability to self-organize towards the most advantageous vegetation structure facilitated by thermodynamic feasibility. Article in Journal/Newspaper Arctic taiga Tundra Directory of Open Access Journals: DOAJ Articles Arctic Scientific Reports 12 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Meredith Richardson Martin
Praveen Kumar
Oliver Sonnentag
Philip Marsh
Thermodynamic basis for the demarcation of Arctic and alpine treelines
topic_facet Medicine
R
Science
Q
description Abstract At the edge of alpine and Arctic ecosystems all over the world, a transition zone exists beyond which it is either infeasible or unfavorable for trees to exist, colloquially identified as the treeline. We explore the possibility of a thermodynamic basis behind this demarcation in vegetation by considering ecosystems as open systems driven by thermodynamic advantage—defined by vegetation’s ability to dissipate heat from the earth’s surface to the air above the canopy. To deduce whether forests would be more thermodynamically advantageous than existing ecosystems beyond treelines, we construct and examine counterfactual scenarios in which trees exist beyond a treeline instead of the existing alpine meadow or Arctic tundra. Meteorological data from the Italian Alps, United States Rocky Mountains, and Western Canadian Taiga-Tundra are used as forcing for model computation of ecosystem work and temperature gradients at sites on both sides of each treeline with and without trees. Model results indicate that the alpine sites do not support trees beyond the treeline, as their presence would result in excessive CO $$_2$$ 2 loss and extended periods of snowpack due to temperature inversions (i.e., positive temperature gradient from the earth surface to the atmosphere). Further, both Arctic and alpine sites exhibit negative work resulting in positive feedback between vegetation heat dissipation and temperature gradient, thereby extending the duration of temperature inversions. These conditions demonstrate thermodynamic infeasibility associated with the counterfactual scenario of trees existing beyond a treeline. Thus, we conclude that, in addition to resource constraints, a treeline is an outcome of an ecosystem’s ability to self-organize towards the most advantageous vegetation structure facilitated by thermodynamic feasibility.
format Article in Journal/Newspaper
author Meredith Richardson Martin
Praveen Kumar
Oliver Sonnentag
Philip Marsh
author_facet Meredith Richardson Martin
Praveen Kumar
Oliver Sonnentag
Philip Marsh
author_sort Meredith Richardson Martin
title Thermodynamic basis for the demarcation of Arctic and alpine treelines
title_short Thermodynamic basis for the demarcation of Arctic and alpine treelines
title_full Thermodynamic basis for the demarcation of Arctic and alpine treelines
title_fullStr Thermodynamic basis for the demarcation of Arctic and alpine treelines
title_full_unstemmed Thermodynamic basis for the demarcation of Arctic and alpine treelines
title_sort thermodynamic basis for the demarcation of arctic and alpine treelines
publisher Nature Portfolio
publishDate 2022
url https://doi.org/10.1038/s41598-022-16462-2
https://doaj.org/article/4b5e1cf996cf473493d2a3da8038f1fa
geographic Arctic
geographic_facet Arctic
genre Arctic
taiga
Tundra
genre_facet Arctic
taiga
Tundra
op_source Scientific Reports, Vol 12, Iss 1, Pp 1-14 (2022)
op_relation https://doi.org/10.1038/s41598-022-16462-2
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doi:10.1038/s41598-022-16462-2
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op_doi https://doi.org/10.1038/s41598-022-16462-2
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