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Earlier-season vegetation has greater temperature sensitivity of spring phenology in northern hemisphere
In recent decades, satellite-derived start of vegetation growing season (SOS) has advanced in many northern temperate and boreal regions. Both the magnitude of temperature increase and the sensitivity of the greenness phenology to temperature-the phenological change per unit temperature-can contribu...
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Published in: | PloS one 2014-02, Vol.9 (2), p.e88178 |
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description | In recent decades, satellite-derived start of vegetation growing season (SOS) has advanced in many northern temperate and boreal regions. Both the magnitude of temperature increase and the sensitivity of the greenness phenology to temperature-the phenological change per unit temperature-can contribute the advancement. To determine the temperature-sensitivity, we examined the satellite-derived SOS and the potentially effective pre-season temperature (T eff) from 1982 to 2008 for vegetated land between 30°N and 80°N. Earlier season vegetation types, i.e., the vegetation types with earlier SOSmean (mean SOS for 1982-2008), showed greater advancement of SOS during 1982-2008. The advancing rate of SOS against year was also greater in the vegetation with earlier SOSmean even the T eff increase was the same. These results suggest that the spring phenology of vegetation may have high temperature sensitivity in a warmer area. Therefore it is important to consider temperature-sensitivity in assessing broad-scale phenological responses to climatic warming. Further studies are needed to explore the mechanisms and ecological consequences of the temperature-sensitivity of start of growing season in a warming climate. |
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Both the magnitude of temperature increase and the sensitivity of the greenness phenology to temperature-the phenological change per unit temperature-can contribute the advancement. To determine the temperature-sensitivity, we examined the satellite-derived SOS and the potentially effective pre-season temperature (T eff) from 1982 to 2008 for vegetated land between 30°N and 80°N. Earlier season vegetation types, i.e., the vegetation types with earlier SOSmean (mean SOS for 1982-2008), showed greater advancement of SOS during 1982-2008. The advancing rate of SOS against year was also greater in the vegetation with earlier SOSmean even the T eff increase was the same. These results suggest that the spring phenology of vegetation may have high temperature sensitivity in a warmer area. Therefore it is important to consider temperature-sensitivity in assessing broad-scale phenological responses to climatic warming. Further studies are needed to explore the mechanisms and ecological consequences of the temperature-sensitivity of start of growing season in a warming climate.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0088178</identifier><identifier>PMID: 24505418</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Biology ; Climate ; Climate change ; Datasets ; Earth Sciences ; Ecological monitoring ; Ecology ; Ecosystem ; Ecosystem biology ; Ecosystems ; Environmental science ; Environmental studies ; Global Warming ; Growing season ; High temperature ; Laboratories ; Northern Hemisphere ; Phenological changes ; Phenology ; Plant Development ; Remote sensing ; Seasons ; Sensitivity ; Sensitivity analysis ; Spring ; Studies ; Temperature ; Temperature effects ; Temperature rise ; Trends ; Vegetation ; Winter</subject><ispartof>PloS one, 2014-02, Vol.9 (2), p.e88178</ispartof><rights>COPYRIGHT 2014 Public Library of Science</rights><rights>2014 Shen et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/legalcode (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. 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Both the magnitude of temperature increase and the sensitivity of the greenness phenology to temperature-the phenological change per unit temperature-can contribute the advancement. To determine the temperature-sensitivity, we examined the satellite-derived SOS and the potentially effective pre-season temperature (T eff) from 1982 to 2008 for vegetated land between 30°N and 80°N. Earlier season vegetation types, i.e., the vegetation types with earlier SOSmean (mean SOS for 1982-2008), showed greater advancement of SOS during 1982-2008. The advancing rate of SOS against year was also greater in the vegetation with earlier SOSmean even the T eff increase was the same. These results suggest that the spring phenology of vegetation may have high temperature sensitivity in a warmer area. Therefore it is important to consider temperature-sensitivity in assessing broad-scale phenological responses to climatic warming. 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Cong</au><au>Cui, Xiaoyong</au><au>Yang, Yongping</au><au>Han, Lijian</au><au>Li, Le</au><au>Du, Jianhui</au><au>Zhang, Gengxin</au><au>Cong, Nan</au><au>Hui, Dafeng</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Earlier-season vegetation has greater temperature sensitivity of spring phenology in northern hemisphere</atitle><jtitle>PloS one</jtitle><addtitle>PLoS One</addtitle><date>2014-02-05</date><risdate>2014</risdate><volume>9</volume><issue>2</issue><spage>e88178</spage><pages>e88178-</pages><issn>1932-6203</issn><eissn>1932-6203</eissn><abstract>In recent decades, satellite-derived start of vegetation growing season (SOS) has advanced in many northern temperate and boreal regions. Both the magnitude of temperature increase and the sensitivity of the greenness phenology to temperature-the phenological change per unit temperature-can contribute the advancement. To determine the temperature-sensitivity, we examined the satellite-derived SOS and the potentially effective pre-season temperature (T eff) from 1982 to 2008 for vegetated land between 30°N and 80°N. Earlier season vegetation types, i.e., the vegetation types with earlier SOSmean (mean SOS for 1982-2008), showed greater advancement of SOS during 1982-2008. The advancing rate of SOS against year was also greater in the vegetation with earlier SOSmean even the T eff increase was the same. These results suggest that the spring phenology of vegetation may have high temperature sensitivity in a warmer area. Therefore it is important to consider temperature-sensitivity in assessing broad-scale phenological responses to climatic warming. Further studies are needed to explore the mechanisms and ecological consequences of the temperature-sensitivity of start of growing season in a warming climate.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>24505418</pmid><doi>10.1371/journal.pone.0088178</doi><tpages>e88178</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Biology Climate Climate change Datasets Earth Sciences Ecological monitoring Ecology Ecosystem Ecosystem biology Ecosystems Environmental science Environmental studies Global Warming Growing season High temperature Laboratories Northern Hemisphere Phenological changes Phenology Plant Development Remote sensing Seasons Sensitivity Sensitivity analysis Spring Studies Temperature Temperature effects Temperature rise Trends Vegetation Winter |
title | Earlier-season vegetation has greater temperature sensitivity of spring phenology in northern hemisphere |
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