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2006-2010年成都市气温、降雨量与蚊密度监测 被引量:9

Monitoring the mosquito density,rainfall and temperature of Chengdu during 2006 to 2010
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摘要 目的分析平均气温与降水量对成都监测点蚊密度监测的影响,为提高国家病媒生物监测质量提供参考。方法使用2006-2010年国家成都病媒监测点蚊密度(诱蚊灯)监测结果,与监测日当旬平均气温与旬旬降水量由SPSS软件计算Spearman秩相关系数,偏相关系数。结果成都蚊密度监测结果与平均气温呈不同程度正相关(r∶0.21-0.91,P∶0.00-0.04),降水量则与蚊密度关系较弱(r∶-0.04-0.59,P∶0.02-0.05)。结论降雨量对蚊密度监测结果有正反两方面影响(r∶-0.32-0.38,P∶0.02-0.04),蚊密度监测需注意规避降雨日。 Objective To analysis the effect of average temperature and precipitation on influence the mosquito density monitoring in Chengdu monitoring sites,in order to improve the quality of national biology vector monitoring.Method Using the monitoring results of mosquito density in Chengdu monitoring sites during 2006 to 2010(trapping lamp) and then calculation the Spearman rank correlation coefficient with average temperature and precipitation of ten days by SPSS software.Results There was a positive correlation between monitoring mosquito density and average temperature(r∶ 0.21-0.9,P∶ 0.00-0.04),the relationship between mosquito density and rainfall was weak(r∶-0.04-0.59,P∶ 0.02-0.05).Conclusions Rainfall had both positive and negative sides on mosquito density(r∶-0.32-0.38,P∶ 0.02-0.04),so it need to pay attention to avoid raining day when monitoring the mosquito density.
出处 《医学动物防制》 2011年第9期817-818,共2页 Journal of Medical Pest Control
关键词 平均气温 降雨量 蚊密度监测 Average temperature Precipitation Mosquito density monitoring
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参考文献6

  • 1卫生部办公厅.关于印发全国病媒监测方案(试行)的通知[Z].2005. 被引量:1
  • 2张孝曦.昆虫生态及预测预报(3版)[M].北京:中国农业出版社,2002. 被引量:1
  • 3M Hurtado - Diaz, H Riojas - Rodriguez, S J Rothenberg, et al. Short communications : impact of climate variability on the incidence of den- gue in Mexico [J] .Trop Med Int health, 2007, 12 (11) : 1 327 - 1 337. 被引量:1
  • 4张方敏,申双和.湿润指数时空变化及与降水量线对比研究[C]//中国气象学会2007年会论文集.北京:气象出版社,2007. 被引量:1
  • 5卫捷,马柱国.Palmer干旱指数、地表湿润指数与降水距平的比较[J].地理学报,2003,58(z1):117-124. 被引量:178
  • 6沈佐锐编著..昆虫生态学及害虫防治的生态学原理[M].北京:中国农业大学出版社,2009:529.

二级参考文献10

  • 1[4]Van Rooy M P. A rainfall anomaly index independent of time and space. Notos, 1965, (14): 43. 被引量:1
  • 2[5]Bhalme H N, D A Mooley. Large-scale drought/floods and monsoon circulation. Mon. Wea. Rev., 1980, 108:1197-1211. 被引量:1
  • 3[6]N B Guttman. Comparing the Palmer drought index and the standardized precipitation index. Journal of the American Water Resources Association, 1998, 34:113-121. 被引量:1
  • 4[7]Palmer W C. Meteorological Drought. U. S. Weather Bureau. Res. Pap., 1965, 45: 1-58. 被引量:1
  • 5[8]Shafer B A, L E Dezman. Development of a surface water supply index (SWSI) to assess the severity of drought conditions in snow pack runoff areas. Proc. Western Snow Conf., 1982. 164-175. 被引量:1
  • 6[9]Weghorst K M. The reclamation drought index: guidelines and practical applications. Bureau of Reclamation, Denver.CO 1996.6. 被引量:1
  • 7[10]Byun Hi-Ryong, Donald A Wilhith. Objective quantification of drought severity and duration. J. Climate, 1999, 12:2747-2755. 被引量:1
  • 8[12]Cook E R et al. Drought reconstructions for continental United States. J. Climate, 1999, 12:1145-1163. 被引量:1
  • 9[13]Aiguo Dai, Kevin E Trenberth, Thomas R Karl. Global variations in droughts and wet spells. Geophysical Research Letters, 1998, 25(17): 3367-3370. 被引量:1
  • 10[15]Alley W M. The Palmer severity drought index: limitations and assumptions. J. Climiate Appl. Meteor., 1984, 23:1100-1109. 被引量:1

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