High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America

The velocity of climate change and its subsequent impact on vegetation has been well characterized at high elevations and latitudes, including the Arctic. But whether species and ecosystems are keeping pace with the velocity of temperature change is not as well documented. Some evidence indicates th...

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Published in:PLOS Climate
Main Authors: Kellner, James R., Kendrick, Joseph, Sax, Dov F.
Other Authors: Behera, Mukunda Dev, Institute at Brown for Environment and Society, Brown University
Format: Article in Journal/Newspaper
Language:English
Published: Public Library of Science (PLoS) 2023
Subjects:
Online Access:http://dx.doi.org/10.1371/journal.pclm.0000071
https://dx.plos.org/10.1371/journal.pclm.0000071
id crplos:10.1371/journal.pclm.0000071
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spelling crplos:10.1371/journal.pclm.0000071 2024-10-06T13:46:51+00:00 High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America Kellner, James R. Kendrick, Joseph Sax, Dov F. Behera, Mukunda Dev Institute at Brown for Environment and Society, Brown University Institute at Brown for Environment and Society, Brown University 2023 http://dx.doi.org/10.1371/journal.pclm.0000071 https://dx.plos.org/10.1371/journal.pclm.0000071 en eng Public Library of Science (PLoS) http://creativecommons.org/licenses/by/4.0/ PLOS Climate volume 2, issue 2, page e0000071 ISSN 2767-3200 journal-article 2023 crplos https://doi.org/10.1371/journal.pclm.0000071 2024-09-10T04:16:39Z The velocity of climate change and its subsequent impact on vegetation has been well characterized at high elevations and latitudes, including the Arctic. But whether species and ecosystems are keeping pace with the velocity of temperature change is not as well documented. Some evidence indicates that species are less able to keep pace with the velocity of climate change along elevational gradients than latitudinal ones. If substantiated this finding could warrant reconsideration of a current cornerstone of conservation planning. Here we use 27 years of high-resolution satellite data to quantify changes in vegetation cover across elevation within nine mountain ranges in western North America, spanning tropical Mexico to subarctic Canada and from coastal California to interior deserts. Across these ranges we show a uniform pattern at the highest elevations in each range, where increases in vegetation have occurred ubiquitously over the past three decades. At these highest elevations, the realized velocity of vegetation varies among mountain ranges from 19.8–112.8 m · decade -1 (mean = 67.3 m · decade -1 ). This is equivalent, with respect to gradients in temperature, to a 14.4–104.3 km · decade -1 poleward shift (mean = 56.1 km · decade -1 ). This realized velocity is 4.4 times larger than previously reported for plants, and is among the fastest rates predicted for the velocity of climate change. However, in three of the five mountain ranges with long-term climate data, realized velocities fail to keep pace with changes in temperature, a finding with important implications for conservation of biological diversity. Article in Journal/Newspaper Arctic Climate change Subarctic PLOS Arctic Canada PLOS Climate 2 2 e0000071
institution Open Polar
collection PLOS
op_collection_id crplos
language English
description The velocity of climate change and its subsequent impact on vegetation has been well characterized at high elevations and latitudes, including the Arctic. But whether species and ecosystems are keeping pace with the velocity of temperature change is not as well documented. Some evidence indicates that species are less able to keep pace with the velocity of climate change along elevational gradients than latitudinal ones. If substantiated this finding could warrant reconsideration of a current cornerstone of conservation planning. Here we use 27 years of high-resolution satellite data to quantify changes in vegetation cover across elevation within nine mountain ranges in western North America, spanning tropical Mexico to subarctic Canada and from coastal California to interior deserts. Across these ranges we show a uniform pattern at the highest elevations in each range, where increases in vegetation have occurred ubiquitously over the past three decades. At these highest elevations, the realized velocity of vegetation varies among mountain ranges from 19.8–112.8 m · decade -1 (mean = 67.3 m · decade -1 ). This is equivalent, with respect to gradients in temperature, to a 14.4–104.3 km · decade -1 poleward shift (mean = 56.1 km · decade -1 ). This realized velocity is 4.4 times larger than previously reported for plants, and is among the fastest rates predicted for the velocity of climate change. However, in three of the five mountain ranges with long-term climate data, realized velocities fail to keep pace with changes in temperature, a finding with important implications for conservation of biological diversity.
author2 Behera, Mukunda Dev
Institute at Brown for Environment and Society, Brown University
Institute at Brown for Environment and Society, Brown University
format Article in Journal/Newspaper
author Kellner, James R.
Kendrick, Joseph
Sax, Dov F.
spellingShingle Kellner, James R.
Kendrick, Joseph
Sax, Dov F.
High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America
author_facet Kellner, James R.
Kendrick, Joseph
Sax, Dov F.
author_sort Kellner, James R.
title High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America
title_short High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America
title_full High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America
title_fullStr High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America
title_full_unstemmed High-velocity upward shifts in vegetation are ubiquitous in mountains of western North America
title_sort high-velocity upward shifts in vegetation are ubiquitous in mountains of western north america
publisher Public Library of Science (PLoS)
publishDate 2023
url http://dx.doi.org/10.1371/journal.pclm.0000071
https://dx.plos.org/10.1371/journal.pclm.0000071
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Climate change
Subarctic
genre_facet Arctic
Climate change
Subarctic
op_source PLOS Climate
volume 2, issue 2, page e0000071
ISSN 2767-3200
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1371/journal.pclm.0000071
container_title PLOS Climate
container_volume 2
container_issue 2
container_start_page e0000071
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