欢迎访问《中国农学通报》,

中国农学通报 ›› 2014, Vol. 30 ›› Issue (32): 276-281.doi: 10.11924/j.issn.1000-6850.2014-0279

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

安徽省寒露风初日的时空分布特征及气候趋势预测

段春锋,徐敏,曹雯,付敏   

  1. 安徽省气候中心,安徽省气候中心,安徽省气象科学研究所,马鞍山市气象局
  • 收稿日期:2014-01-29 修回日期:2014-10-29 接受日期:2014-04-15 出版日期:2014-11-20 发布日期:2014-11-20
  • 通讯作者: 段春锋
  • 基金资助:
    安徽省气象局气象科技发展基金项目“安徽主汛期降水分离时间尺度的降尺度模型的建立和应用”(KM201302);安徽省自然科学基金资 助项目“安徽省梅汛期极端降水事件的时空特征及其与东北冷涡的联系”(1308085QD69);淮河流域气象开放研究基金资助项目“近50 年淮河流域气 候资源评估及利用”(HRM201209)。

Spatiotemporal Characteristics and Climatic Forecast of the Cold Dew Wind First Day in Anhui Province

  • Received:2014-01-29 Revised:2014-10-29 Accepted:2014-04-15 Online:2014-11-20 Published:2014-11-20

摘要: 利用安徽省沿江江南日平均气温资料,统计分析了安徽省寒露风初日的时空分布特征及其与9月气温的联系,在此基础上,利用逐步回归法构建基于前期物理因子的区域寒露风初日趋势预测模型。结果表明:气候平均态下,寒露风初日江南早于沿江,沿江东部早于西部,1981—2010 年相对1961—1990 年寒露风初日平均值明显推迟2~3 天;在气候变暖背景下,1961—2013 年沿江江南大部地区寒露风初日呈现推迟趋势,其中沿江东部最为显著,其次是江南东部和南部,再次是江南北部。寒露风初日与9 月平均气温不论是气候平均态和多年变化趋势的空间分布型,还是两者在1961—2013 年的时间演变特征均十分一致,为利用9 月平均气温趋势预测寒露风初日趋势提供科学依据。1961—2013 年区域寒露风初日虽然趋于推迟,但仍会出现异常偏早的情况。构建了基于前期物理因子的区域寒露风初日趋势预测模型,该预测模型不论在1981—2010 年交叉检验时段,还是在2011—2013 年独立检验时段,对于寒露风初日趋势的预测正确率明显优于目前业务上直接利用9 月平均气温距平符号的趋势预测方法。

关键词: 消毒, 消毒

Abstract: Based on the daily mean air temperature data of the area along and south to the Yangtze River in Anhui Province, the spatiotemporal characteristics of the cold dew wind first day and the relationship between the cold dew wind first day and the air temperature of September were analyzed. Furthermore, the stepwise regression method was used to establish the climatic forecast model of the regional cold dew wind first day based on the earlier physical factors. Results showed that the cold dew wind early day was generally earlier in the area south to the Yangtze River than in the area along the Yangtze River and was earlier in the eastern part along the Yangtze River compared to the western part. The average date of the cold dew wind first day obviously postponed 2-3 days during 1981 to 2010 compared to the period during 1961 to 1990. Under the background of global warming, the cold dew wind first day of the area along and south to the Yangtze River showed a delayed trend during 1961 to 2010. The trend was most significant in the eastern part along the Yangtze River, followed by the eastern and southern parts south to the Yangtze River, and the northern part was less significant. Several features of the cold dew wind first day and the air temperature of September, including the mean climatic state, the spatial distribution of change trends and the temporal evolution characteristics during 1961 to 2013 were fairly consistent. This would provide a scientific basis for using the air temperature trend of September to forecast the trend of the cold dew wind first day. The regional cold dew wind first day still appeared to advance abnormally although the entire trend postponed during 1961 to 2013. The forecast model of the regional cold dew wind first day based on the earlier physical factors was significantly better than the method directly using the air temperature of September, whether for the cross-examination period from 1981 to 2010 or for the independent testing period from 2011 to 2013.