State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Institute of Ecology, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Int J Environ Res Public Health. 2023 Feb 26;20(5):4198. doi: 10.3390/ijerph20054198.
Accurately assessing the variation in the frost-free season (FFS) can provide decision support for improving agricultural adaptability and reducing frost harm; however, related studies were inadequate in terms of the Qinghai-Tibet Plateau (QTP). This study analyzed the spatiotemporal changes in the first frost day in autumn (FFA), last frost day in spring (LFS), FFS length and effective accumulated temperature (EAT) during the 1978-2017 period, and their influences on spring wheat potential yield on the QTP, based on daily climatic data and the methodology of Sen's slope and correlation analysis. The results showed that the annual average FFA and LFS occurred later and earlier from northwest to southeast, respectively, and both the FFS length and EAT increased. From 1978 to 2017, the average regional FFA and LFS were delayed and advanced at rates of 2.2 and 3.4 days per decade, and the FFS and EAT increased by 5.6 days and 102.7 °C·d per decade, respectively. Spatially, the increase rate of FFS length ranged from 2.8 to 11.2 days per decade throughout the QTP, and it was observed to be larger in northern Qinghai, central Tibet and Yunnan, and smaller mainly in eastern Sichuan and southern Tibet. Correspondingly, the increase rate for EAT ranged from 16.2 to 173.3 °C·d per decade and generally showed a downward trend from north to south. For a one-day increase in the FFS period, the spring wheat potential yield would decrease by 17.4 and 9.0 kg/ha in altitude ranges of <2000 m and 2000-3000 m, but decrease by 24.9 and 66.5 kg/ha in the ranges of 3000-4000 m and >4000 m, respectively. Future studies should be focused on exploring the influence of multiple climatic factors on crop production using experimental field data and model technologies to provide policy suggestions.
准确评估无霜期(FFS)的变化可以为提高农业适应性和减少霜冻危害提供决策支持;然而,青藏高原(QTP)相关研究还不够充分。本研究利用逐日气候资料和 Sen 斜率法、相关分析法,分析了 1978-2017 年秋季初霜日(FFA)、春季终霜日(LFS)、无霜期长度和有效积温(EAT)的时空变化及其对 QTP 春小麦潜在产量的影响。结果表明,年平均 FFA 和 LFS 自西北向东南呈滞后和提前趋势,FFS 长度和 EAT 增加。1978-2017 年,平均区域 FFA 和 LFS 分别以 2.2 和 3.4 天/十年的速度推迟和提前,FFS 和 EAT 分别增加了 5.6 天和 102.7°C·d/十年。空间上,QTP 范围内 FFS 长度的增加率在 2.8-11.2 天/十年之间,在青海北部、西藏中部和云南地区较大,在四川东部和西藏南部较小。相应地,EAT 的增加率在 16.2-173.3°C·d/十年之间,总体呈从北到南的下降趋势。FFS 期每增加一天,海拔<2000 m 和 2000-3000 m 范围内春小麦潜在产量将分别减少 17.4 和 9.0 kg/ha,但在 3000-4000 m 和>4000 m 范围内将分别减少 24.9 和 66.5 kg/ha。未来的研究应集中利用田间试验数据和模型技术,探索多种气候因素对作物生产的影响,为政策制定提供建议。