中国农业气象 ›› 2025, Vol. 46 ›› Issue (12): 1770-1781.doi: 10.3969/j.issn.1000-6362.2025.12.008

• 农业生物气象栏目 • 上一篇    下一篇

黑龙江省大豆食心虫气候风险区划指标构建

吕佳佳,巩敬锦,闫平,宫丽娟,王晾晾,李宇光,李秀芬,周宝才   

  1. 1.黑龙江省气象科学研究所/五营国家气候观象台,哈尔滨 150030;2.黑龙江省生态气象中心,哈尔滨 150030
  • 收稿日期:2025-01-20 出版日期:2025-12-20 发布日期:2025-12-16
  • 作者简介:吕佳佳,E-mail:wflljj@163.com
  • 基金资助:
    黑龙江省自然科学基金项目(LH2022D025);中国气象局沈阳大气环境研究所联合开放基金课题(2022SYIAEKFZD04−02)

Construction of Climatic Risk Zoning Indices for Leguminivora glycinivorella in Heilongjiang Province

LV Jia-jia, GONG Jing-jin, YAN Ping, GONG Li-juan, WANG Liang-liang, LI Yu-guang, LI Xiu-fen, ZHOU Bao-cai   

  1. 1. Heilongjiang Province Institute of Meteorological Science/Wuying National Climatological Observatory, Harbin 150030, China; 2. Heilongjiang Eco-meteorology Center, Harbin 150030
  • Received:2025-01-20 Online:2025-12-20 Published:2025-12-16

摘要:

构建省级大豆食心虫气候风险区划指标,可为农业病虫害防灾减灾、促进农业生产提质增效和气象服务高质量发展提供技术支撑。利用1980−2021年黑龙江省25个气候站点大豆食心虫虫食率资料,采用相关分析、通径分析及共线性分析方法,筛选关键特征气候因子,界定并构建大豆食心虫综合气候风险指数,采用BP人工神经网络法,分析虫食率与特征气候因子间的关系度,基于K均值聚类方法和样本极值确定综合气候风险临界值和等级,建立黑龙江省大豆食心虫气候风险区划指标及模型,基于验证后的模型开展1961−1990年、1991−2020年黑龙江大豆食心虫气候风险区划。结果表明:显著影响黑龙江省大豆食心虫虫食率的5个特征气候因子为上年9月下旬平均气温、上年12月平均气温、4月上旬平均气温、5−6月平均气温和8平均空气相对湿度。黑龙江省大豆食心虫气候低风险区、中风险区、高风险区和极高风险区的综合气候风险指数临界阈值分别为[00.47)、[0.470.58)、[0.580.68)以及[0.68,1.00],虫食率分别为[03.5%)、[3.5%7.0%)、[7.0%,10.0%)、[10.0%,43.0%]预留40个样本的验证结果显示,指标计算的气候风险等级与实际风险等级完全一致的样本占比为67.5%,相差1级的占比为27.5%1961−1990年、1991−2020年黑龙江大豆食心虫风险区域均集中于松嫩平原和三江平原,中低风险区主要分布于大小兴安岭及牡丹江半山区。与1961−1990年相比,1991−2020年新增了极高风险区,且1991−2020年高风险区域范围明显高于1961−1990年,中低风险范围明显缩小

关键词: 大豆食心虫, 气候因子, 复合指数, 风险区划

Abstract:

Provincial−level climate risk zoning indicators for the soybean pod borer, which can provide technical support for disaster prevention and mitigation of agricultural pests and diseases, promote the improvement of quality and efficiency in agricultural production, and the high−quality development of meteorological services. This study utilized data on the rate of damage caused by Leguminivora glycinivorella from 25 meteorological stations in Heilongjiang province from 1980 to 2021. Characteristic climatic factors were screened by employing methods such as correlation analysis, path analysis and collinearity analysis. A comprehensive climate risk index for Leguminivora glycinivorella was defined and constructed. The BP artificial neural network method was used to analyze the relationship between the rate of damage and the characteristic climatic factors. Based on the K–means clustering method and typical disaster years, the critical values and grades of comprehensivc climate risk were determined, and the climate risk zoning indicators and models for the occurrence of Leguminivora glycinivorella in Heilongjiang province were established. After verifying the accuracy, climate risk zoning of Leguminivora glycinivorella was conducted for the periods of 1961–1990 and 1991–2020. The results indicated that the five significant characteristic climatic factors that affected the damage rate of Leguminivora glycinivorella in Heilongjiang province were: average temperature of the last ten days of September last year, the monthly average of the daily average temperatures in December of last year, the average of the daily average temperatures in the first ten days of April, the average of the daily average temperatures for May and June and the average daily relative humidity in August. The critical thresholds of the comprehensive climate risk index for the low–risk, medium–risk, high–risk and extremely high–risk zones of Leguminivora glycinivorella in Heilongjiang province were [0, 0.47), [0.47, 0.58), [0.58, 0.68), and [0.68, 1.00], respectively. The rates of damage were [0, 3.5%), [3.5%, 7.0%), [7%, 10%), and [10%, 43%], respectively. The verification results of 40 reserved samples showed that the proportion of samples with fully consistent risk grades calculated by the indicators and the actual risk grades was 67.5% and the proportion of samples with a difference of one grade was 27.5%. This demonstrates that the indicators had indicative significance. Both high–risk regions in 19611990 and 19912020 were concentrated in the Songnen and Sanjiang plains. The medium and low–risk areas were mainly distributed in the Greater and Lesser Xing'an ranges and the semi–mountainous area of Mudanjiang. Compared with the period of 1961–1990, the period of 1991–2020 saw the emergence of extremely high–risk areas, with the range of high–risk areas was significantly larger than that in 1961–1990, while the range of medium and low–risk areas were decreased significantly.

Key words: Leguminivora glycinivorella, Climatic factors, Compound index, Risk zonation