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中国农学通报 ›› 2019, Vol. 35 ›› Issue (13): 107-111.doi: 10.11924/j.issn.1000-6850.casb18110012

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

黑龙江省夏季降雨量及暴雨时空分布特征研究

刘春生, 徐永清, 刘赫男, 王波, 魏磊   

  1. 黑龙江省气候中心
  • 收稿日期:2018-11-05 修回日期:2018-11-23 接受日期:2018-12-11 出版日期:2019-05-05 发布日期:2019-05-05
  • 通讯作者: 徐永清
  • 基金资助:
    中国气象局气候变化专项“季节性冻土区冻土和地温场变化及影响研究——以东北为例”(CCSF201710)。

Spatial and Temporal Distribution Characteristics of Summer Rainfall and Rainstorm in Heilongjiang

  • Received:2018-11-05 Revised:2018-11-23 Accepted:2018-12-11 Online:2019-05-05 Published:2019-05-05

摘要: 利用黑龙江省80个气象站夏季(6-8月)逐日降水资料,分析近55年(1961-2015年)黑龙江省夏季降雨量和暴雨的变化特征,为粮食生产提供科学依据。[方法]从夏季降雨量、降雨量变化趋势、暴雨次数、暴雨变化趋势等方面,利用趋势系数等统计方法和GIS空间插值技术,分析黑龙江省夏季降雨量和暴雨的时空分布特征。[结果]结果表明黑龙江省夏季降雨量在中部的小兴安岭和张广才岭西部地区最高,在360mm以上,东部三江平原和西部松嫩平原地区最低,在300-320mm之间。夏季降雨量在松嫩平原和大兴安岭地区呈增加趋势,小兴安岭和三江平原地区呈减少趋势。全省夏季平均降雨量呈减少趋势,平均每10年减少2mm,20世纪70年代平均降雨量最低,80年代最高。小兴安岭西南部和张广才岭西部地区平均暴雨日数最多,其次为三江平原和松嫩平原地区,大兴安岭地区最少。暴雨发生站次呈明显升高趋势,每10年增加2.3站次,20世纪70年代暴雨发生站次最少,2010年以后最多。最大日降雨量基本上从西南向东北部递减,西南部地区绝大部分地区最大日降雨量都在120mm以上,东北部地区都在120mm以下。

关键词: 琯溪蜜柚, 琯溪蜜柚, 山地果园, 立地条件, 径流, 氮,

Abstract: Based on the daily precipitation data of 80 meteorological stations in Heilongjiang, the variation characteristics of summer rainfall and rainstorm in recent 55 years (1961 to 2015) were analyzed to provide a basis for grain production. The study was carried out by using trend coefficients and GIS spatial interpolation techniques from the aspects of summer rainfall, the trend of rainfall variation, rainstorm frequency and the trend of rainstorm variation. The results showed that the Lesser Khingan Mountains and the Zhangguangcai Mountains had the highest summer rainfall of above 360 mm, the lowest was in the Sanjiang Plain and the Songnen Plain, which was between 300 to 320 mm. The summer rainfall increased in the Songnen Plain and the Great Khingan Mountains, and decreased in the Lesser Khingan Mountains and Sanjiang Plains. The average summer rainfall of Heilongjiang showed a decreasing trend, with an average decrease of 2 mm every 10 years, the lowest was in the 1970s and the highest was in the 1980s. The most average number of rainstorm days occurred in the southwest of the Lesser Khingan Mountains and the west of Zhangguangcai Mountains, followed by the Sanjiang Plain and the Songnen Plain, the Great Khingan Mountains had the least rainstorm days. Rainstorm occurrence stations showed a significant upward trend, increased by 2.3 stations every 10 years, the number of rainstorm occurrence stations was the least in 1970s and the most after 2010. The maximum daily rainfall basically decreased from southwest to northeast. The maximum daily rainfall in most areas of southwest was above 120 mm, and that in northeast was below 120 mm.