Warming-induced tipping points of Arctic and alpine shrub recruitment.
Shrub recruitment, a key component of vegetation dynamics beyond forests, is a highly sensitive indicator of climate and environmental change. Warming-induced tipping points in Arctic and alpine treeless ecosystems are, however, little understood. Here, we compare two long-term recruitment datasets...
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Proceedings of the National Academy of Sciences
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ftunivcam:oai:www.repository.cam.ac.uk:1810/335411 2024-02-04T09:57:14+01:00 Warming-induced tipping points of Arctic and alpine shrub recruitment. Lu, Xiaoming Liang, Eryuan Babst, Flurin Camarero, J Julio Büntgen, Ulf 2022-03-28T19:06:17Z application/pdf https://www.repository.cam.ac.uk/handle/1810/335411 https://doi.org/10.17863/CAM.82840 eng eng Proceedings of the National Academy of Sciences http://dx.doi.org/10.1073/pnas.2118120119 Proc Natl Acad Sci U S A https://www.repository.cam.ac.uk/handle/1810/335411 doi:10.17863/CAM.82840 Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ essn: 1091-6490 nlmid: 7505876 Arctic alpine climate change shrub recruitment tipping point Arctic Regions Ecosystem Greenland Plant Development Temperature Tibet Article 2022 ftunivcam https://doi.org/10.17863/CAM.82840 2024-01-11T23:29:06Z Shrub recruitment, a key component of vegetation dynamics beyond forests, is a highly sensitive indicator of climate and environmental change. Warming-induced tipping points in Arctic and alpine treeless ecosystems are, however, little understood. Here, we compare two long-term recruitment datasets of 2,770 shrubs from coastal East Greenland and from the Tibetan Plateau against atmospheric circulation patterns between 1871 and 2010 Common Era. Increasing rates of shrub recruitment since 1871 reached critical tipping points in the 1930s and 1960s on the Tibetan Plateau and in East Greenland, respectively. A recent decline in shrub recruitment in both datasets was likely related to warmer and drier climates, with a stronger May to July El Niño Southern Oscillation over the Tibetan Plateau and a stronger June to July Atlantic Multidecadal Oscillation over Greenland. Exceeding the thermal optimum of shrub recruitment, the recent warming trend may cause soil moisture deficit. Our findings suggest that changes in atmospheric circulation explain regional climate dynamics and associated response patterns in Arctic and alpine shrub communities, knowledge that should be considered to protect vulnerable high-elevation and high-latitude ecosystems from the cascading effects of anthropogenic warming. Article in Journal/Newspaper Arctic Climate change East Greenland Greenland Apollo - University of Cambridge Repository Arctic Greenland |
institution |
Open Polar |
collection |
Apollo - University of Cambridge Repository |
op_collection_id |
ftunivcam |
language |
English |
topic |
Arctic alpine climate change shrub recruitment tipping point Arctic Regions Ecosystem Greenland Plant Development Temperature Tibet |
spellingShingle |
Arctic alpine climate change shrub recruitment tipping point Arctic Regions Ecosystem Greenland Plant Development Temperature Tibet Lu, Xiaoming Liang, Eryuan Babst, Flurin Camarero, J Julio Büntgen, Ulf Warming-induced tipping points of Arctic and alpine shrub recruitment. |
topic_facet |
Arctic alpine climate change shrub recruitment tipping point Arctic Regions Ecosystem Greenland Plant Development Temperature Tibet |
description |
Shrub recruitment, a key component of vegetation dynamics beyond forests, is a highly sensitive indicator of climate and environmental change. Warming-induced tipping points in Arctic and alpine treeless ecosystems are, however, little understood. Here, we compare two long-term recruitment datasets of 2,770 shrubs from coastal East Greenland and from the Tibetan Plateau against atmospheric circulation patterns between 1871 and 2010 Common Era. Increasing rates of shrub recruitment since 1871 reached critical tipping points in the 1930s and 1960s on the Tibetan Plateau and in East Greenland, respectively. A recent decline in shrub recruitment in both datasets was likely related to warmer and drier climates, with a stronger May to July El Niño Southern Oscillation over the Tibetan Plateau and a stronger June to July Atlantic Multidecadal Oscillation over Greenland. Exceeding the thermal optimum of shrub recruitment, the recent warming trend may cause soil moisture deficit. Our findings suggest that changes in atmospheric circulation explain regional climate dynamics and associated response patterns in Arctic and alpine shrub communities, knowledge that should be considered to protect vulnerable high-elevation and high-latitude ecosystems from the cascading effects of anthropogenic warming. |
format |
Article in Journal/Newspaper |
author |
Lu, Xiaoming Liang, Eryuan Babst, Flurin Camarero, J Julio Büntgen, Ulf |
author_facet |
Lu, Xiaoming Liang, Eryuan Babst, Flurin Camarero, J Julio Büntgen, Ulf |
author_sort |
Lu, Xiaoming |
title |
Warming-induced tipping points of Arctic and alpine shrub recruitment. |
title_short |
Warming-induced tipping points of Arctic and alpine shrub recruitment. |
title_full |
Warming-induced tipping points of Arctic and alpine shrub recruitment. |
title_fullStr |
Warming-induced tipping points of Arctic and alpine shrub recruitment. |
title_full_unstemmed |
Warming-induced tipping points of Arctic and alpine shrub recruitment. |
title_sort |
warming-induced tipping points of arctic and alpine shrub recruitment. |
publisher |
Proceedings of the National Academy of Sciences |
publishDate |
2022 |
url |
https://www.repository.cam.ac.uk/handle/1810/335411 https://doi.org/10.17863/CAM.82840 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Climate change East Greenland Greenland |
genre_facet |
Arctic Climate change East Greenland Greenland |
op_source |
essn: 1091-6490 nlmid: 7505876 |
op_relation |
https://www.repository.cam.ac.uk/handle/1810/335411 doi:10.17863/CAM.82840 |
op_rights |
Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.17863/CAM.82840 |
_version_ |
1789961567222104064 |