曹玲, 徐士琦, 杨雪艳, 刘柏鑫, 房一禾, 王航, 谷佳桐. 夏季东北冷涡气候特征及其对吉林省大豆生育期的影响[J]. 沙漠与绿洲气象, 2022, 16(5): 135-143.
引用本文: 曹玲, 徐士琦, 杨雪艳, 刘柏鑫, 房一禾, 王航, 谷佳桐. 夏季东北冷涡气候特征及其对吉林省大豆生育期的影响[J]. 沙漠与绿洲气象, 2022, 16(5): 135-143.
CAO Ling, XU Shiqi, YANG Xueyan, LIU Baixin, FANG Yihe, WANG Hang, GU Jiatong. Climate Characteristics of Northeast Cold Vortex in Summer and the Effects on Growth Period of Soybean in Jilin Province[J]. Desert and Oasis Meteorology, 2022, 16(5): 135-143.
Citation: CAO Ling, XU Shiqi, YANG Xueyan, LIU Baixin, FANG Yihe, WANG Hang, GU Jiatong. Climate Characteristics of Northeast Cold Vortex in Summer and the Effects on Growth Period of Soybean in Jilin Province[J]. Desert and Oasis Meteorology, 2022, 16(5): 135-143.

夏季东北冷涡气候特征及其对吉林省大豆生育期的影响

Climate Characteristics of Northeast Cold Vortex in Summer and the Effects on Growth Period of Soybean in Jilin Province

  • 摘要: 基于NCEP/NCAR再分析资料和国家气候中心160站月平均气温、降水资料,以及吉林省大豆生育期资料,从对农作物生育期天气气候有重要影响的东北冷涡活动入手,统计分析1981—2018年夏季(5—9月)东北冷涡活动特征,初步分析吉林省大豆近年来生育期情况及其对不同类型东北冷涡(中涡、北涡)活动的响应。结果表明:东北冷涡为持续时间较长且较为频繁的系统,平均寿命5 d左右,夏季(5—9月)冷涡活动占比三分之一以上,主要集中在115°~130°E、40°~55°N区域;冷涡活动6月最多、8月最少。中涡对东北地区环流影响最显著,有利于鄂霍次克海地区位势高度增强,中高纬度环流经向特征明显,偏北冷空气向南输送;东北地区高度场以负距平为主,有利于北太平洋气流向东北地区输送。东北冷涡天数偏多时,吉林省大豆播种—开花期气温偏低、降水偏多、生育期间隔天数延长。从平均气温影响看,播种—出苗期榆树主要受北涡影响,延吉主要受中涡影响;出苗—开花期延吉同时受北涡和中涡影响;出苗—开花期的间隔日数榆树和桦甸主要受北涡影响。此外,榆树和延吉的降水量在播种—出苗期间主要受中涡影响,出苗—开花期间主要受北涡影响。

     

    Abstract: Based on the NCEP/NCAR reanalysis data,the monthly average temperature and precipitation data of the 160 stations of the National Climate Center,and the soybean growth period data of Jilin province,this paper started from the northeast cold vortex(NECV),which had an important impact on the weather and climate of crops during the growing season,and statistics on the climatological characteristics of the NECV activity in summer(May-September) from 1981 to 2018. The climatological characteristics of soybean fertility in Jilin Province in recent years and its response to different types of NECV(central-type and northern-type)were initially analyzed.Results showed that the NECV was a long-lasting and relatively frequent system with an average lifetime of about 5 days.More than one-third of the NECV in summer was concentrated in the region of 115°-130°E and 40°-55°N;the NECV was the most frequent in June and the least in August.The central-type NECV had the most significant influence on the circulation in the northeast China,which was conducive to the enhancement of the potential height in the Okhotsk Sea,the obvious meridional characteristics of the mid-high latitude circulation,and the transport of cold air from north to south;the northeast China was dominated by a negative geopotential height anomaly,which was conducive to the transport of airflow from the North Pacific to northeast China.When NECV days were active,the temperature during the sowing-flowering period of soybean in Jilin Province was lower,precipitation was more,and the days between fertility periods increased.In terms of mean temperature,during the sowing-flowering period,Yushu was mainly affected by the northern-type NECV,while Yanji was mainly affected by the central-type NECV;during the sowing-flowering period,Yanji was affected by both the northern-type and central-type NECV;the days between sowing and flowering were mainly affected by the northern-type NECV in Yushu and Huadian.In addition,the precipitation in Yushu and Yanji was mainly influenced by the central-type NECV during the seeding-sowing period and by the northern-type NECV during the seeding-flowering period.

     

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