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中国农学通报 ›› 2015, Vol. 31 ›› Issue (35): 204-208.doi: 10.11924/j.issn.1000-6850.casb15070113

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

潍坊市1955—2014年气温日较差变化特征及影响因子分析

高学芹   

  1. 寿光市气象局
  • 收稿日期:2015-07-21 修回日期:2015-07-30 接受日期:2015-08-13 出版日期:2015-12-18 发布日期:2015-12-18
  • 通讯作者: 高学芹
  • 基金资助:
    潍坊市气象局气象科学技术研究项目“潍坊市气候变化对农业的影响及应对措施”(2014wfqxkt11)。

Analysis on the Change Features and Influence Factors of the Daily Temperature Ranges from 1955 to 2014 in Weifang City

  • Received:2015-07-21 Revised:2015-07-30 Accepted:2015-08-13 Online:2015-12-18 Published:2015-12-18

摘要: 为了揭示潍坊市气温日较差的演变规律和特征,利用1955—2014年潍坊市最高、最低气温及与日较差相关的日照、云量、风速等气象要素进行分析。结果表明:近60a来,潍坊市气温日较差呈显著下降趋势,倾向率-0.11℃/10 a。季、年日较差的年代际最大值均出现在1990s,最小值出现在2010s。春季日较差最大,夏季最小,四季日较差均呈减小趋势,夏季减小幅度最大,秋季最小。1—12月气温日较差呈波状分布,5月最大,8月最小,各月气温日较差多呈下降趋势,5月下降幅度最大,7月最小。季、年平均气温日较差在随时间变化过程中均不存在显著突变。最高、最低气温的非对称性变化是日较差下降的直接原因,气温日较差与最高气温、日照时数、日照百分率、风速呈显著正相关,与最低气温、总云量、降水量呈显著负相关,与相对湿度几乎不相关,日较差与各气象因子的关联程度随季节不同而异。

关键词: 气候变暖, 气候变暖, 冬季积温, 冬小麦发育期, 响应

Abstract: In order to reveal the evolvement rule and features of the daily temperature range in Weifang City, the highest and lowest temperatures and many meteorological factors like sunshine duration, cloud amount, wind speed, and so on from 1955 to 2014 were analyzed. The result shows that: In recent 60 years, the daily temperature range was obvious declining. The rate of inclination was -0.11℃/10a. The maximum value of inter-decadal daily temperature range among seasons and years appeared in 1990s, and the minimum value appeared in 2010s. The daily temperature range was the biggest in spring and autumn, and smallest in summer. Among four seasons, it was also declining, and the decreasing range was the biggest in summer and smallest in autumn. From January to December, the daily temperature ranges were distributed in a fluctuating way; it was the biggest in May, and smallest in August. The daily temperature ranges in all months were mostly declining; the decreasing range was the biggest in May and smallest in July. The average daily temperature ranges among seasons and years didn’t have sudden changes in the changing process along with the time. The asymmetry change of the highest and lowest temperatures was the direct reason that caused the declining of daily temperature range. It was positively correlated with the highest temperature, sunshine duration, sunshine percentage and wind speed, and negatively correlated with the lowest temperature, total cloud amount, and amount of precipitation. It was nearly not correlated with humidity. The correlative extent between the daily temperature range and each meteorological factor varies along with different seasons.

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