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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Online Access: | http://dx.doi.org/10.1371/journal.pclm.0000071 https://dx.plos.org/10.1371/journal.pclm.0000071 |
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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 |
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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 |
_version_ |
1812175157857353728 |