Delayed autumn phenology in the Northern Hemisphere is related to change in both climate and spring phenology

© 2016 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 22(2016), 11 vom: 15. Nov., Seite 3702-3711
1. Verfasser: Liu, Qiang (VerfasserIn)
Weitere Verfasser: Fu, Yongshuo H, Zhu, Zaichun, Liu, Yongwen, Liu, Zhuo, Huang, Mengtian, Janssens, Ivan A, Piao, Shilong
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2016
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Normalize Differenced Vegetation Index autumn phenology climate change end of growing season spring phenology
LEADER 01000naa a22002652 4500
001 NLM259243930
003 DE-627
005 20231224190756.0
007 cr uuu---uuuuu
008 231224s2016 xx |||||o 00| ||eng c
024 7 |a 10.1111/gcb.13311  |2 doi 
028 5 2 |a pubmed24n0864.xml 
035 |a (DE-627)NLM259243930 
035 |a (NLM)27061925 
040 |a DE-627  |b ger  |c DE-627  |e rakwb 
041 |a eng 
100 1 |a Liu, Qiang  |e verfasserin  |4 aut 
245 1 0 |a Delayed autumn phenology in the Northern Hemisphere is related to change in both climate and spring phenology 
264 1 |c 2016 
336 |a Text  |b txt  |2 rdacontent 
337 |a ƒaComputermedien  |b c  |2 rdamedia 
338 |a ƒa Online-Ressource  |b cr  |2 rdacarrier 
500 |a Date Completed 14.09.2017 
500 |a Date Revised 02.12.2018 
500 |a published: Print-Electronic 
500 |a Citation Status MEDLINE 
520 |a © 2016 John Wiley & Sons Ltd. 
520 |a The timing of the end of the vegetation growing season (EOS) plays a key role in terrestrial ecosystem carbon and nutrient cycles. Autumn phenology is, however, still poorly understood, and previous studies generally focused on few species or were very limited in scale. In this study, we applied four methods to extract EOS dates from NDVI records between 1982 and 2011 for the Northern Hemisphere, and determined the temporal correlations between EOS and environmental factors (i.e., temperature, precipitation and insolation), as well as the correlation between spring and autumn phenology, using partial correlation analyses. Overall, we observed a trend toward later EOS in ~70% of the pixels in Northern Hemisphere, with a mean rate of 0.18 ± 0.38 days yr-1 . Warming preseason temperature was positively associated with the rate of EOS in most of our study area, except for arid/semi-arid regions, where the precipitation sum played a dominant positive role. Interestingly, increased preseason insolation sum might also lead to a later date of EOS. In addition to the climatic effects on EOS, we found an influence of spring vegetation green-up dates on EOS, albeit biome dependent. Our study, therefore, suggests that both environmental factors and spring phenology should be included in the modeling of EOS to improve the predictions of autumn phenology as well as our understanding of the global carbon and nutrient balances 
650 4 |a Journal Article 
650 4 |a Normalize Differenced Vegetation Index 
650 4 |a autumn phenology 
650 4 |a climate change 
650 4 |a end of growing season 
650 4 |a spring phenology 
700 1 |a Fu, Yongshuo H  |e verfasserin  |4 aut 
700 1 |a Zhu, Zaichun  |e verfasserin  |4 aut 
700 1 |a Liu, Yongwen  |e verfasserin  |4 aut 
700 1 |a Liu, Zhuo  |e verfasserin  |4 aut 
700 1 |a Huang, Mengtian  |e verfasserin  |4 aut 
700 1 |a Janssens, Ivan A  |e verfasserin  |4 aut 
700 1 |a Piao, Shilong  |e verfasserin  |4 aut 
773 0 8 |i Enthalten in  |t Global change biology  |d 1999  |g 22(2016), 11 vom: 15. Nov., Seite 3702-3711  |w (DE-627)NLM098239996  |x 1365-2486  |7 nnns 
773 1 8 |g volume:22  |g year:2016  |g number:11  |g day:15  |g month:11  |g pages:3702-3711 
856 4 0 |u http://dx.doi.org/10.1111/gcb.13311  |3 Volltext 
912 |a GBV_USEFLAG_A 
912 |a SYSFLAG_A 
912 |a GBV_NLM 
912 |a GBV_ILN_350 
951 |a AR 
952 |d 22  |j 2016  |e 11  |b 15  |c 11  |h 3702-3711