中国水稻科学
中國水稻科學
중국수도과학
CHINESE JOURNAL OF RICE SCIENCE
2014年
5期
541-550
,共10页
毕建春%陈星燎%彭晓明%封传红%马利%蒋春先%李庆%王海建%杨群芳
畢建春%陳星燎%彭曉明%封傳紅%馬利%蔣春先%李慶%王海建%楊群芳
필건춘%진성료%팽효명%봉전홍%마리%장춘선%리경%왕해건%양군방
白背飞虱%虫源地%降落机制
白揹飛虱%蟲源地%降落機製
백배비슬%충원지%강락궤제
white-backed planthopper[Sogatella furcifera (Horváth)]%insect source area%landing mechanism
根据灯诱虫情,运用大气质点轨迹分析平台 HYSPLIT4.8对1991-2012年四川省叙永县白背飞虱主要迁入高峰日进行轨迹模拟,并运用气象图形处理软件 Grads 对白背飞虱主要迁入高峰日进行气象背景分析.结果表明,四川叙永白背飞虱主要在5-7月迁入.5月份,白背飞虱迁入峰次较少,虫源主要来自云南西南部,云南中部地区、缅甸北部和越南北部也可提供部分虫源;6月份和7月份,叙永上空偏南气流频次逐渐增多,白背飞虱迁入峰次也相对增加.6月份虫源主要来自云南东部和南部地区,广西西北部、缅甸北部以及云南中部地区也能够提供少量的虫源;7月份虫源主要来自云南东北部、贵州西南部和云贵交界处,另外,云南中部和广西西北部也可提供部分虫源.降水、气流的垂直运动和风向切变是造成白背飞虱在叙永大规模集中降落的主要气象因子.
根據燈誘蟲情,運用大氣質點軌跡分析平檯 HYSPLIT4.8對1991-2012年四川省敘永縣白揹飛虱主要遷入高峰日進行軌跡模擬,併運用氣象圖形處理軟件 Grads 對白揹飛虱主要遷入高峰日進行氣象揹景分析.結果錶明,四川敘永白揹飛虱主要在5-7月遷入.5月份,白揹飛虱遷入峰次較少,蟲源主要來自雲南西南部,雲南中部地區、緬甸北部和越南北部也可提供部分蟲源;6月份和7月份,敘永上空偏南氣流頻次逐漸增多,白揹飛虱遷入峰次也相對增加.6月份蟲源主要來自雲南東部和南部地區,廣西西北部、緬甸北部以及雲南中部地區也能夠提供少量的蟲源;7月份蟲源主要來自雲南東北部、貴州西南部和雲貴交界處,另外,雲南中部和廣西西北部也可提供部分蟲源.降水、氣流的垂直運動和風嚮切變是造成白揹飛虱在敘永大規模集中降落的主要氣象因子.
근거등유충정,운용대기질점궤적분석평태 HYSPLIT4.8대1991-2012년사천성서영현백배비슬주요천입고봉일진행궤적모의,병운용기상도형처리연건 Grads 대백배비슬주요천입고봉일진행기상배경분석.결과표명,사천서영백배비슬주요재5-7월천입.5월빈,백배비슬천입봉차교소,충원주요래자운남서남부,운남중부지구、면전북부화월남북부야가제공부분충원;6월빈화7월빈,서영상공편남기류빈차축점증다,백배비슬천입봉차야상대증가.6월빈충원주요래자운남동부화남부지구,엄서서북부、면전북부이급운남중부지구야능구제공소량적충원;7월빈충원주요래자운남동북부、귀주서남부화운귀교계처,령외,운남중부화엄서서북부야가제공부분충원.강수、기류적수직운동화풍향절변시조성백배비슬재서영대규모집중강락적주요기상인자.
According to the daily light-trap catches of Xuyong,Sichuan Province from 1 99 1 to 2012,we analyzed the trajectory simulation and meteorological background of immigration peaks of white-backed planthoppers [Sogatella furcifera (Horváth),WBPH]by HYSPLIT 4.8(Hybrid Single-Particle Lagrangian Integrated Trajectory)and GRADS (Grid Analysis and Display System).The results showed that the main immigration times of WBPH in Xuyong, Sichuan Province were from May to July.The immigration peaks were few in May.The source areas were mainly located in the southwest of Yunnan,and the secondary source areas were at the central region of Yunnan,the north of Myanmar and Vietnam.From June to July,with The south airflow prevailing in Xuyong,the immigration times was increased.The mass immigration of WBPH into Xuyong during June was from the east and the south of Yunnan,and some immigrants from the northwest of Guangxi,the north of Myanmar,and the central part of Yunnan.In July,the northeast of Yunnan,the southwestern Guizhou and the border of Yunnan-Guizhou were the major source areas,and the secondary source areas were the central region of Yunnan and the northwest of Guangxi.Based on the analysis on the meteorological background and rainfall distribution,it was found that the rainfall,the vertical movement of airflow and the wind shear caused mass descent of WBPH into Xuyong.