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中国农学通报 ›› 2017, Vol. 33 ›› Issue (12): 74-81.doi: 10.11924/j.issn.1000-6850.casb16090021

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

1965—2015年庆阳塬区气温和降水极端事件研究分析

焦美龄,路亚奇,王燕凌   

  1. 甘肃省庆阳市气象局,甘肃省庆阳市气象局,庆阳市气象局
  • 收稿日期:2016-09-05 修回日期:2017-04-17 接受日期:2017-01-19 出版日期:2017-04-28 发布日期:2017-04-28
  • 通讯作者: 路亚奇
  • 基金资助:
    甘肃省庆阳市气象局科技项目“庆阳市降雪对交通的影响分析及预报方法研究”(201409)。

Extreme Temperature and Precipitation Events: In Qingyang Loess Tableland Region, 1965-2015

焦美龄,路亚奇 and 王燕凌   

  • Received:2016-09-05 Revised:2017-04-17 Accepted:2017-01-19 Online:2017-04-28 Published:2017-04-28

摘要: 为了研究庆阳塬区气温和降水极端事件变化的特点及规律,提供防灾减灾科学依据,利用1965—2015年庆阳塬区西峰站的平均气温、日最高气温、日最低气温、降水等观测资料,应用多种方法和指标进行分析。结果表明:(1)庆阳塬区年平均降水量539 mm,极端降水阈值22.7 mm,极端降水日数4.8天,极端降水强度36.6 mm/d,暴雨32次。(2)年平均气温9.0℃,极端最高气温29.2~36.4℃,极端最低气温-22.6~-11.3℃,夏天日数65.1天,低温日数125.7天,高温31次。(3)年降水量、极端降水量、极端降水日数及强度均呈减少趋势,年最大日降水量呈不显著上升趋势,暴雨变化趋势比较平稳。(4)年平均气温、极端最高气温、极端最低气温、夏天日数均呈上升趋势,低温日数减少趋势与年平均气温、极端最低气温出现增温相对应。(5)年降水量与极端降水量之间,极端降水量与极端降水日数和强度之间均呈线性正相关,极端最低气温的升高、低温日数的减少对平均气温的升高贡献最为显著。

关键词: 水稻, 水稻, 稻曲病, 抗性鉴定, 接种方法

Abstract: To research the change characteristics and regularity of extreme temperature and precipitation events in Qingyang loess tableland region, and provide a basis for disaster prevention and mitigation, based on average temperature, daily maximum temperature, daily minimum temperature, precipitation and other observation data of Xifeng station during 1965- 2015, we conducted the analysis by applying a variety of methods and indexes. The results indicated that: (1) in Qingyang loess tableland region, the annual average precipitation was 539 mm, the extreme precipitation threshold was 22.7 mm; the extreme precipitation days were 4.8 days; the extreme precipitation intensity was 36.6 mm/d, the times of rainstorm was 32; (2) the annual average temperature was 9℃; the extreme maximum temperature was 29.2-36.4℃, the extreme minimum temperature was -22.6 ? -11.3℃, the summer days were 65.1, the low temperature days were 125.7, the high temperature frequency was 31 times; (3) the annual precipitation, the extreme precipitation, the extreme precipitation days and the intensity presented a decreasing trend, the maximum daily precipitation in the year had an insignificant upward trend, storm change trend was steady; (4) the annual average temperature, the extreme maximum temperature, the extreme minimum temperature and the total summer days all presented a rising trend, the low temperature days decreased corresponding to the increase of the annual mean temperature and the extreme minimum temperature; (5) there was a positive linear correlation between the annual precipitation and the extreme precipitation, the extreme precipitation and the extreme precipitation days and the intensity; the increase of the extreme minimum temperature and the decrease of the low temperature days significantly contributed to the increase of the average temperature.

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