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观测 1981-2009 年华北平原冬小麦物候的变化。

Observed changes in winter wheat phenology in the North China Plain for 1981-2009.

机构信息

Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China.

出版信息

Int J Biometeorol. 2013 Mar;57(2):275-85. doi: 10.1007/s00484-012-0552-8. Epub 2012 May 7.

Abstract

Climate change in the last three decades could have major impacts on crop phenological development and subsequently on crop productivity. In this study, trends in winter wheat phenology are investigated in 36 agro-meteorological stations in the North China Plain (NCP) for the period 1981-2009. The study shows that the dates of sowing (BBCH 00), emergence (BBCH 10) and dormancy (start of dormancy) are delayed on the average by 1.5, 1.7 and 1.5 days/decade, respectively. On the contrary, the dates of greenup (end of dormancy), anthesis (BBCH 61) and maturity (BBCH 89) occur early on the average by 1.1, 2.7 and 1.4 days/decade, respectively. In most of the investigated stations, GP2 (dormancy to greenup), GP3 (greenup to anthesis) and GP0 (entire period from emergence to maturity) of winter wheat shortened during the period 1981-2009. Due, however, to early anthesis, grain-filling stage occurs at lower temperatures than before. This, along with shifts in cultivars, slightly prolongs GP4 (anthesis to maturity). Comparison of field-observed CERES (Crop Environment Resource Synthesis)-wheat model-simulated dates of anthesis and maturity suggests that climate warming is the main driver of the changes in winter wheat phenology in the NCP. The findings of this study further suggest that climate change impact studies should be strengthened to adequately account for the complex responses and adaptations of field crops to this global phenomenon.

摘要

在过去的三十年中,气候变化可能会对作物物候发育产生重大影响,进而影响作物的生产力。本研究调查了 1981 年至 2009 年期间华北平原(NCP)36 个农业气象站冬小麦物候的变化趋势。研究表明,播种期(BBCH00)、出苗期(BBCH10)和休眠期(休眠开始)的日期平均分别延迟了 1.5、1.7 和 1.5 天/十年。相反,返青期(休眠结束)、抽穗期(BBCH61)和成熟期(BBCH89)的日期平均提前了 1.1、2.7 和 1.4 天/十年。在所调查的大部分站点中,冬小麦的 GP2(休眠到返青)、GP3(返青到抽穗)和 GP0(从出苗到成熟的整个时期)在 1981 年至 2009 年间缩短。然而,由于抽穗期较早,灌浆期发生在比以前更低的温度下。再加上品种的变化,GP4(抽穗到成熟)略有延长。田间观测的 CERES(作物环境资源综合)-小麦模型模拟的抽穗期和成熟期的比较表明,气候变暖是华北平原冬小麦物候变化的主要驱动因素。本研究的结果进一步表明,应该加强气候变化影响研究,以充分考虑到田间作物对这一全球现象的复杂反应和适应。

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