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中国农学通报 ›› 2022, Vol. 38 ›› Issue (20): 29-37.doi: 10.11924/j.issn.1000-6850.casb2022-0182

所属专题: 生物技术 园艺 农业气象 农业生态

• 林学·园艺·园林 • 上一篇    下一篇

气候变化对大兴安岭西麓林牧交错带木本植物物候期的影响

王彦平1(), 金磊1, 高健2, 王志春3()   

  1. 1内蒙古呼伦贝尔市气象局,内蒙古海拉尔 021008
    2内蒙古兴安盟气象局,内蒙古乌兰浩特 137400
    3内蒙古赤峰市气象局,内蒙古赤峰 024000
  • 收稿日期:2021-03-17 修回日期:2022-05-23 出版日期:2022-07-15 发布日期:2022-08-23
  • 通讯作者: 王志春
  • 作者简介:王彦平,女,1974年出生,内蒙古锡林郭勒人,高级工程师,硕士研究生,研究方向:农牧林业气象研究。通信地址:021008 内蒙古呼伦贝尔市海拉尔区根河路108号 呼伦贝尔市气象局,E-mail: fei_ping@sohu.com
  • 基金资助:
    内蒙古自治区气象局科技创新项目“大豆优质丰产气象指标试验研究及应用示范”(nmqxkjcx202102);内蒙古自然科学基金“内蒙古草地生产力对气候变化的响应与适应”(2019MS04002);中国气象局气候变化专项(CCSF202025)

Effects of Climate Change on Phenophase of Woody Plants in the Forest-Pasture Ecotone at the Western Foot of the Great Khingan Mountains

WANG Yanping1(), JIN Lei1, GAO Jian2, WANG Zhichun3()   

  1. 1Hulun Buir Meteorological Office, Hailar, Inner Mongolia 021008
    2Xing'an League Meteorological Office, Ulanhot, Inner Mongolia 137400
    3Chifeng Meteorological Office, Chifeng, Inner Mongolia 024000
  • Received:2021-03-17 Revised:2022-05-23 Online:2022-07-15 Published:2022-08-23
  • Contact: WANG Zhichun

摘要:

为了揭示气候变化背景下林牧交错带木本植物物候期的变化趋势及对气候变化的响应,为林草交错带固沙防风等生态恢复工程提供科学气象参考依据,利用内蒙古呼伦贝尔市鄂温克牧业气象试验站1994—2019年观测的榆树、小叶杨和紫丁香3种木本植物物候观测资料及同期气象数据,采用线性倾向估计、Pearson 相关系数、散点图等方法,分析了近26 年气候变化对大兴安岭西麓林牧交错带木本植物物候期的影响。结果表明:近26 年,大兴安岭西麓植物生长季气温显著升高,降水变化趋势不明显。榆树、小叶杨和紫丁香3种木本植物花芽开放期提前,落叶末期推后,且落叶末期推迟天数较多,平均每10 年分别推迟9.6、7.5 和8.5天。生长季显著延长,平均生长季分别为160~164天。气温是影响榆树、小叶杨和紫丁香春季花芽开放期和秋季落叶末期的关键气象因子。3种木本植物春季花芽开放期的提前对温度上升的响应是显著负相关关系,落叶末期推后对温度上升的响应显著正正相关关系。说明气候变暖背景下,3种木本植物花芽开放期提前,落叶末期推迟,生长期长度增加;且推迟天数较花芽开放期提前天数更大,说明气候变化对木本植物落叶末期影响更明显,落叶末期对生长季长度增加的贡献更大;大兴安岭西麓林牧交错带木本植物物候期的变化主要是受气温的影响,与降水量关系不大。

关键词: 大兴安岭西麓, 气候变化, 木本植物, 物候期, 相关分析

Abstract:

The purpose of the study is to reveal the change trend of woody plants’ phenophase and its response to climate change in the forest-pasture ecotone, and provide meteorological reference for guiding the ecological restoration projects of sand fixation and wind prevention. The phenophase observation data of three kinds of woody plants, Ulmus pumila, Populus simonii Carr and Syringa oblate, and simultaneous meteorological data from Ewenki meteorological experimental station in Inner Mongolia from 1994 to 2019 were used to analyze the influence of climate change on the phenophase of woody plants in the forest-pasture ecotone at the western foot of the Great Khingan Mountains by linear tendency estimation, Pearson correlation coefficient, scatter diagram and other methods. The results showed that in the 26 years, the temperature increased significantly in the plant growing season in this region, and the change trend of precipitation was not obvious. The flowering period of Ulmus pumila, Populus simonii Carr and Syringa oblate was earlier, and the late abscission period was postponed by 9.6, 7.5, and 8.5 d every 10 years, respectively. The growing season was prolonged significantly, and the average growing season was 160-164 d. The air temperature was the key meteorological factor affecting the flowering period in spring and the late abscission period in autumn. The advanced flowering period of the three woody plants had a significantly negative correlation with the rise of temperature in spring, and the postponing of the late abscission period was significantly and positively correlated with the rise of temperature. In conclusion, under the background of climate warming, the earlier flowering period and the delayed late abscission period of the three woody plants have been observed, and the growth period is extended. The postponing days of the late abscission period are more than the earlier days of the flowering period, indicating that climate change has a more obvious impact on the late abscission period of woody plants, and the late abscission period has a greater contribution to the extension of the growing season. The phenophase change of woody plants is mainly influenced by temperature and has little correlation with precipitation in the forest-pasture ecotone at the western foot of the Great Khingan Mountains.

Key words: the western foot of the Great Khingan Mountains, climate change, woody plants, phenophase, correlation analysis

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