Phenology shifts at start vs. end of growing season in temperate vegetation over the Northern Hemisphere for the period 1982-2008

Changes in vegetative growing seasons are dominant indicators of the dynamic response of ecosystems to climate change. Therefore, knowledge of growing seasons over the past decades is essential to predict ecosystem changes. In this study, the long-term changes in the growing seasons of temperate veg...

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Published in:	Global change biology Vol. 17; no. 7; pp. 2385 - 2399
Main Authors:	JEONG, SU-JONG, HO, CHANG-HOI, GIM, HYEON-JU, BROWN, MOLLY E
Format:	Journal Article
Language:	English
Published:	Oxford, UK Blackwell Publishing Ltd 01-07-2011 Wiley-Blackwell
Subjects:	Animal and plant ecology Animal, plant and microbial ecology autumn Biological and medical sciences Climate change Climatology. Bioclimatology. Climate change Earth, ocean, space ecosystems Exact sciences and technology External geophysics Fundamental and applied biological sciences. Psychology General aspects Global warming growing season Indexing in process leaves Meteorology NDVI (normalized difference vegetation index) Northern Hemisphere phenology Saissetia coffeae senescence temperate vegetation temperature Terrestrial ecosystems Vegetation Northern Hemisphere Dynamical climatology Climate change Vegetation index Northern Hemisphere Phenology Growing season Vegetation temperate vegetation NDVI (normalized difference vegetation index)
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Abstract	Changes in vegetative growing seasons are dominant indicators of the dynamic response of ecosystems to climate change. Therefore, knowledge of growing seasons over the past decades is essential to predict ecosystem changes. In this study, the long-term changes in the growing seasons of temperate vegetation over the Northern Hemisphere were examined by analyzing satellite-measured normalized difference vegetation index and reanalysis temperature during 1982-2008. Results showed that the length of the growing season (LOS) increased over the analysis period; however, the role of changes at the start of the growing season (SOS) and at the end of the growing season (EOS) differed depending on the time period. On a hemispheric scale, SOS advanced by 5.2 days in the early period (1982-1999) but advanced by only 0.2 days in the later period (2000-2008). EOS was delayed by 4.3 days in the early period, and it was further delayed by another 2.3 days in the later period. The difference between SOS and EOS in the later period was due to less warming during the preseason (January-April) before SOS compared with the magnitude of warming in the preseason (June-September) before EOS. At a regional scale, delayed EOS in later periods was shown. In North America, EOS was delayed by 8.1 days in the early period and delayed by another 1.3 days in the later period. In Europe, the delayed EOS by 8.2 days was more significant than the advanced SOS by 3.2 days in the later period. However, in East Asia, the overall increase in LOS during the early period was weakened in the later period. Admitting regional heterogeneity, changes in hemispheric features suggest that the longer-lasting vegetation growth in recent decades can be attributed to extended leaf senescence in autumn rather than earlier spring leaf-out.
AbstractList	Changes in vegetative growing seasons are dominant indicators of the dynamic response of ecosystems to climate change. Therefore, knowledge of growing seasons over the past decades is essential to predict ecosystem changes. In this study, the long‐term changes in the growing seasons of temperate vegetation over the Northern Hemisphere were examined by analyzing satellite‐measured normalized difference vegetation index and reanalysis temperature during 1982–2008. Results showed that the length of the growing season (LOS) increased over the analysis period; however, the role of changes at the start of the growing season (SOS) and at the end of the growing season (EOS) differed depending on the time period. On a hemispheric scale, SOS advanced by 5.2 days in the early period (1982–1999) but advanced by only 0.2 days in the later period (2000–2008). EOS was delayed by 4.3 days in the early period, and it was further delayed by another 2.3 days in the later period. The difference between SOS and EOS in the later period was due to less warming during the preseason (January–April) before SOS compared with the magnitude of warming in the preseason (June–September) before EOS. At a regional scale, delayed EOS in later periods was shown. In North America, EOS was delayed by 8.1 days in the early period and delayed by another 1.3 days in the later period. In Europe, the delayed EOS by 8.2 days was more significant than the advanced SOS by 3.2 days in the later period. However, in East Asia, the overall increase in LOS during the early period was weakened in the later period. Admitting regional heterogeneity, changes in hemispheric features suggest that the longer‐lasting vegetation growth in recent decades can be attributed to extended leaf senescence in autumn rather than earlier spring leaf‐out. Abstract Changes in vegetative growing seasons are dominant indicators of the dynamic response of ecosystems to climate change. Therefore, knowledge of growing seasons over the past decades is essential to predict ecosystem changes. In this study, the long-term changes in the growing seasons of temperate vegetation over the Northern Hemisphere were examined by analyzing satellite-measured normalized difference vegetation index and reanalysis temperature during 1982-2008. Results showed that the length of the growing season (LOS) increased over the analysis period; however, the role of changes at the start of the growing season (SOS) and at the end of the growing season (EOS) differed depending on the time period. On a hemispheric scale, SOS advanced by 5.2 days in the early period (1982-1999) but advanced by only 0.2 days in the later period (2000-2008). EOS was delayed by 4.3 days in the early period, and it was further delayed by another 2.3 days in the later period. The difference between SOS and EOS in the later period was due to less warming during the preseason (January-April) before SOS compared with the magnitude of warming in the preseason (June-September) before EOS. At a regional scale, delayed EOS in later periods was shown. In North America, EOS was delayed by 8.1 days in the early period and delayed by another 1.3 days in the later period. In Europe, the delayed EOS by 8.2 days was more significant than the advanced SOS by 3.2 days in the later period. However, in East Asia, the overall increase in LOS during the early period was weakened in the later period. Admitting regional heterogeneity, changes in hemispheric features suggest that the longer-lasting vegetation growth in recent decades can be attributed to extended leaf senescence in autumn rather than earlier spring leaf-out. [PUBLICATION ABSTRACT]
Author	BROWN, MOLLY E JEONG, SU-JONG HO, CHANG-HOI GIM, HYEON-JU
Author_xml	– sequence: 1 fullname: JEONG, SU-JONG – sequence: 2 fullname: HO, CHANG-HOI – sequence: 3 fullname: GIM, HYEON-JU – sequence: 4 fullname: BROWN, MOLLY E
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Keywords	Dynamical climatology Climate change Vegetation index Northern Hemisphere Phenology Growing season Vegetation temperate vegetation NDVI (normalized difference vegetation index)
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phenological change, past and present, in UK farming publication-title: Annals of Applied Biology – volume: 19 start-page: 257 year: 2002 end-page: 264 article-title: Annual and spatial variability of the beginning of growing season in Europe in relation to temperature changes publication-title: Climate Research – year: 2011 article-title: Impact of vegetation feedback on the temperature and its diurnal range over the Northern Hemisphere during summer in a 2 × CO climate publication-title: Climate Dynamics – volume: 36 start-page: L0270 year: 2009a article-title: Increase in vegetation greenness and decrease in spring time warming over East Asia publication-title: Geophysical Research Letters – volume: 104 start-page: 4249 year: 2007 end-page: 4254 article-title: The changing carbon cycle at Mauna Loa observatory publication-title: Proceedings of the National Academe Science – volume: 21 start-page: 4257 year: 2008 end-page: 4279 article-title: Northern annular mode effects on the land 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analyses using optimum interpolation publication-title: Journal of Climate – volume: 5 start-page: 703 year: 1994 end-page: 714 article-title: Measuring phenological variability from satellite imagery publication-title: Journal of Vegetation Science – volume: 34 start-page: L19405 year: 2007 article-title: Diverse response of vegetation phenology to a warming climate publication-title: Geophysical Research Letters – volume: 108 start-page: 4066 year: 2003 article-title: Detection of large‐scale climate signals in spring vegetation index (normalized difference vegetation index) over the Northern Hemisphere publication-title: Journal of Geophysical Research – volume: 12 start-page: 343 year: 2006 end-page: 351 article-title: Onset of spring starting earlier across the northern hemisphere publication-title: Global Change Biology – volume: 31 start-page: 261 year: 2007 end-page: 285 article-title: A review of vegetation‐atmosphere interactions and their influences on mesoscale phenomena 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Snippet	Changes in vegetative growing seasons are dominant indicators of the dynamic response of ecosystems to climate change. Therefore, knowledge of growing seasons... Abstract Changes in vegetative growing seasons are dominant indicators of the dynamic response of ecosystems to climate change. Therefore, knowledge of growing...
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SubjectTerms	Animal and plant ecology Animal, plant and microbial ecology autumn Biological and medical sciences Climate change Climatology. Bioclimatology. Climate change Earth, ocean, space ecosystems Exact sciences and technology External geophysics Fundamental and applied biological sciences. Psychology General aspects Global warming growing season Indexing in process leaves Meteorology NDVI (normalized difference vegetation index) Northern Hemisphere phenology Saissetia coffeae senescence temperate vegetation temperature Terrestrial ecosystems Vegetation
Title	Phenology shifts at start vs. end of growing season in temperate vegetation over the Northern Hemisphere for the period 1982-2008
URI	https://api.istex.fr/ark:/67375/WNG-K87KQ124-S/fulltext.pdf https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fj.1365-2486.2011.02397.x https://www.proquest.com/docview/869436983 https://search.proquest.com/docview/902364867
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