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Journal Article
JA0421-11
Article TitleWinter and spring warming result in delayed spring phenology on the Tibetan Plateau
AuthorYu Haiying, Eike Luedeling and Xu Jianchu
Year2010
Journal TitleProceedings of National Academy of Science, USA (PNAS)
InstitutionThe National Academy of Sciences of the USA
Volume107
Issue51
Pages22151–22156
Call NumberJA0421-11
Abstract:
Climate change has caused advances in spring phases of many plant species. Theoretically, however, strong warming in winter could slowthe fulfillment of chilling requirements,whichmay delay spring phenology. This phenomenon should be particularly pronounced in regions that are experiencing rapid temperature increases and are characterized by highly temperature-responsive vegetation. To test this hypothesis, we used the Normalized Difference Vegetation Index ratio method to determine the beginning, end, and length of the growing season of meadow and steppe vegetation of the Tibetan Plateau in Western China between 1982 and 2006.We then correlated observed phenological dates with monthly temperatures for the entire period on record. For both vegetation types, spring phenology initially advanced, but started retreating in the mid-1990s in spite of continued warming. Together with an advancing end of the growing season for steppe vegetation, this led to a shortening of the growing period. Partial least-squares regression indicated that temperatures in both winter and spring had strong effects on spring phenology. Although warm springs led to an advance of the growing season, warm conditions in winter caused a delay of the spring phases. This delay appeared to be related to later fulfillment of chilling requirements. Because most plants from temperate and cold climates experience a period of dormancy in winter, it seems likely that similar effects occur in other environments. Continued warming may strengthen this effect and attenuate or even reverse the advancing trend in spring phenology that has dominated climate-change responses of plants thus far.
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