中国农业气象 ›› 2015, Vol. 36 ›› Issue (01): 9-16.doi: 10.3969/j.issn.1000-6362.2015.01.002

• 论文 • 上一篇    下一篇

黑龙江省活动积温时空变化特征及其对水稻单产的影响

李赢,马世铭   

  1. 中国农业科学院农业环境与可持续发展研究所/农业部农业环境重点实验室,北京100081
  • 收稿日期:2014-07-23 出版日期:2015-02-20 发布日期:2015-05-21
  • 作者简介:李赢(1989-),女,黑龙江哈尔滨人,硕士生,主要从事气候变化影响与适应研究。Email:liying19890601@yahoo.com
  • 基金资助:

    国家科技支撑课题(2013BAC09B04)

The Spatial and Temporal Variations of the Active Accumulated Temperature and Their Impacts on the Rice Yield in Heilongjiang Province of China

Li Ying,Ma Shi ming   

  1. Institute of Environment and Sustainable Development in Agriculture,Chinese Academy of Agricultural Sciences/Key Laboratory of Agricultural Environment,Ministry of Agriculture of China,Beijing100081,China
  • Received:2014-07-23 Online:2015-02-20 Published:2015-05-21

摘要: 利用Berkeley Earth提供的高精度陆地表面日平均气温格点资料,计算1951-2012年黑龙江省≥10℃年活动积温,用自然正交分解(EOF)法对积温年代际和年际变化的时空特征,以及积温变化对全省水稻单产的影响进行分析。结果表明:研究期积温年代际变化可分成平稳期Ⅰ(1951-1993年),转换期(1993-2000年)和平稳期Ⅱ(2000-2012年),3个阶段的平均气温均呈递增趋势。平稳期Ⅱ与平稳期Ⅰ相比,平均积温全省大部普遍升高200℃·d以上,升高幅度最大的区域在该省西南部,达240~320℃·d。在平稳期Ⅱ,2100℃·d积温线已北移通过黑河地区到达大兴安岭,说明水稻种植北界可以达到北部较寒冷的黑河地区。黑龙江省水稻生长季年活动积温和水稻单产均存在准2a周期为主的短期年际变化。相关分析表明,在哈尔滨、齐齐哈尔、大庆、绥化、伊春以及佳木斯市,积温的短期年际变化对水稻产量的影响较大,而在南部的尚志、牡丹江和鸡西,其影响则不大。

关键词: 自然正交分解(EOF)方法, ≥10℃积温, 积温区划, 一阶偏差

Abstract: The active accumulated temperature(≥10℃)at the Heilongjiang province and its surrounding areas was calculated based on Berkeley Earths latitudinal/longitudinal gridded land surface daily average air temperature dataset from 1951 to 2012.The Empirical Orthogonal Function(EOF)method was used to examine spatial and temporal variations of the active accumulated temperature anomaly in the interdecadal and interannual time scales and their impact on the rice yield of Heilongjiang province.The results show that the long term trend of the accumulated temperature anomaly in the interdecadal variations can be divided into three main phases:stationary phase Ι(1951-1993),transition phase(1993-2000)and stationary phase Ⅱ(2000-2012).The average accumulated temperatures of the three phases are increasing as the phases progress.The average accumulated temperature of stationary phase Ⅱ is generally more than 200℃·d higher than that of stationary phase Ι in most of the Heilongjiang areas.The largest accumulated temperature increases were about 240~320℃·d in the southwestern areas of the province.During the stationary phase Ⅱ period,the 2100℃·d line of the accumulated temperature had moved across the Heihe area to reach the Daxinganling mountain range,indicating the rice has been able to grow in the Heihe area where the accumulated temperature was normally not high enough to grow rice in the past.In addition,there is quasibiennial oscillation in the yearly accumulated temperature and in the rice yield per hectare.The correlation analysis shows the interannual variations in the yearly accumulated temperature have significant effects on the yearly rice yield in Harbin,Qiqihar,Daqing,Suihua,Yichun and Jiamusi areas,but have little effect on the rice yield in the southern part of the Heilongjiang province such as Shangzhi,Mudanjiang and Jixi areas.

Key words: Empirical orthogonal functions(EOF)method, Accumulated temperature≥10℃, Accumulated temperature division, First difference