中国农业气象 ›› 2023, Vol. 44 ›› Issue (02): 85-95.doi: 10.3969/j.issn.1000-6362.2023.02.001

• 农业气候资源与气候变化栏目 •    下一篇

基于站点数据分析中国大陆区域喜凉/温作物界限温度的时空演变

和骅芸,胡琦,唐书玥,赵金媛,潘学标,潘志华,王靖   

  1. 1. 中国农业大学资源与环境学院,北京 100193; 2. 中国气象局−中国农业大学农业应对气候变化联合实验室,北京 100193
  • 收稿日期:2022-03-16 出版日期:2023-02-20 发布日期:2023-01-16
  • 通讯作者: 胡琦,博士,副教授,主要从事气候变化影响评价。 E-mail:huq@cau.edu.cn
  • 作者简介:和骅芸,E-mail:hehuayun0715@163.com
  • 基金资助:
    内蒙古自治区科技重大专项(2020ZD0005−0101)

Analysis of Spatio-Temporal Evolution of the Boundary Temperature of Chimonophilous/Thermophilic Crops in Chinese Mainland Based on Site Data

HE Hua-yun, HU Qi, TANG Shu-yue, ZHAO Jin-yuan, PAN Xue-biao, PAN Zhi-huan, WANG Jing   

  1. 1. College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China; 2. CMA-CAU Jointly Laboratory of Agriculture Addressing Climate Change, Beijing 100193
  • Received:2022-03-16 Online:2023-02-20 Published:2023-01-16

摘要: 喜凉/温作物界限温度的时空分布能够影响作物物候和种植区域。利用全国585个气象站点1961−2020年地面气象观测资料,以喜凉/温作物界限温度(0℃和10℃)的积温、初日、终日作为农业热量资源研究指标,基于ANUSPLIN气象插值软件,从年际和年代际时间尺度分析1961−2020年喜凉/温作物界限温度的时空演变特征,并探讨热量资源变化对全国农业生产格局的影响。结果表明:受纬度和地形影响,全国热量资源变化幅度较大,东部地区≥0℃、≥10℃积温随纬度变化呈阶梯状分布,而在西部地区主要受海拔影响,总体表现为由南向北逐渐递减。各地≥0℃和≥10℃积温范围分别为700.0~8960.0℃·d和46.3~8960.0℃·d,≥0℃和≥10℃积温气候倾向率平均为72.8℃·d·10a−1和73.7℃·d·10a−1。60a内,界限温度0℃、10℃初日分别提前9.6d和8.4d,终日分别推迟4.8d和7.8d。界限温度初日的提前和终日推迟使60a内日平均气温≥0℃和≥10℃的持续日数分别增加14.4d和16.2d。2011−2020年是研究时段内最温暖10a,与P1时段(1961−1970年)相比,P6时段(2011−2020年)≥0℃和≥10℃积温平均值分别增加了6.3%和8.2%。P6时段≥0℃积温为6000~7000℃·d的区域面积增加了2.11×105km2;≥10℃积温为5000~6000℃·d的区域面积增加了3.37×105km2。气候变暖背景下,活动积温增加对农业系统产生了重要影响,农业生产布局以及种植制度应及时做出调整,充分适应气候变化。

关键词: 气候变化, 热量资源, 界限温度, 活动积温

Abstract: The temporal and spatial distribution of the boundary temperature of chimonophilous/ thermophilic crops affect the crop phenology and planting area. Based on the surface meteorological observation data of 585 meteorological stations in Chinese from 1961 to 2020, taking the ≥0℃ and ≥10℃ thermal time, the initial and terminate days of thermal time as research indices of agricultural heat resources, based on ANUSPLIN meteorological interpolation software, the spatio-temporal evolution of boundary temperature of chimonophilous/ thermophilic crops in China were analyzed from interannual and interdecadal time scales. The influence of heat resource change on agricultural production pattern in Chinese Mainland was also discussed. The results showed that: affected by latitude and topography, the heat resources changed greatly in China. The thermal time ≥0℃ and ≥10℃ in the eastern region presented a ladder distribution with latitude, while in the western region, it was mainly affected by altitude, which decreased gradually from south to north. The thermal time ≥0℃ and ≥10℃ ranged of 700.0−8960.0℃·d and 46.3−8960.0℃·d respectively, with the average climate trend of 72.8℃·d·10y−1 and 73.7℃·d·10y−1. Within 60 years, the initial ordinal number of 0℃ and 10℃ was advanced by 9.6d and 8.4d respectively, and the terminate ordinal number was postponed by 4.8d and 7.8d, respectively. The advance of the initial day and the delay of the final day increased the number of continuous days with daily average temperature ≥0℃ and ≥10℃ by 14.4d and 16.2d in 60 years, respectively. 2011−2020(P6 period)was the warmest 10 years in the study period, that of the thermal time ≥0℃ and ≥10℃ increased by 6.3% and 8.2% respectively compared with P1 period (1961−1970). In P6 period, the area with thermal time ≥0℃ of 6000−7000℃·d increased by 2.11×105km2, the area with thermal time ≥10℃ of 5000−6000℃·d increased by 3.37×105km2. Under the background of climate warming, the increase of accumulated temperature has had an important impact on China's agricultural system. The layout of agricultural production and planting system should be adjusted in time to fully adapt to climate change.

Key words: Climate change, Heat resources, Boundary temperature, Thermal time