[目的]分析沈阳夏季的降水效率。[方法]采用胡志晋先生提出的估算云水资源的方法,利用"QFW-1型双通道微波辐射计"观测的垂直累积液态水含量与"粒子激光探测仪"(Parsivel)反演的1 m in时间间隔的雨强资料,对沈阳地区2007年7-8月的...[目的]分析沈阳夏季的降水效率。[方法]采用胡志晋先生提出的估算云水资源的方法,利用"QFW-1型双通道微波辐射计"观测的垂直累积液态水含量与"粒子激光探测仪"(Parsivel)反演的1 m in时间间隔的雨强资料,对沈阳地区2007年7-8月的降水效率进行了分析。[结果]当雨强I〈7.5 mm/h时,降水效率E平稳,为3.2%-2.7%,平均3.0%;当雨强I≥7.5 mm/h时,降水效率E随雨强I的增加呈线性增加。雨强越大,空中剩余的液态水含量越多,人工增雨潜力越大。[结论]该研究为分析空中云水资源和人工增雨潜力提供指导作用。展开更多
Based on the water resource balance,the correlation between both the Liaoning water resource and precipitation and total amount of water resource from 1991 to 2004 was analyzed by assuming Liaoning to be an enclosed r...Based on the water resource balance,the correlation between both the Liaoning water resource and precipitation and total amount of water resource from 1991 to 2004 was analyzed by assuming Liaoning to be an enclosed region.And the calculation methods were developed to quantitatively determine the increase of rainfall due to artificial precipitation,and consequently ascertain the contribution of artificial rainfall amount to water resources.展开更多
文摘[目的]分析沈阳夏季的降水效率。[方法]采用胡志晋先生提出的估算云水资源的方法,利用"QFW-1型双通道微波辐射计"观测的垂直累积液态水含量与"粒子激光探测仪"(Parsivel)反演的1 m in时间间隔的雨强资料,对沈阳地区2007年7-8月的降水效率进行了分析。[结果]当雨强I〈7.5 mm/h时,降水效率E平稳,为3.2%-2.7%,平均3.0%;当雨强I≥7.5 mm/h时,降水效率E随雨强I的增加呈线性增加。雨强越大,空中剩余的液态水含量越多,人工增雨潜力越大。[结论]该研究为分析空中云水资源和人工增雨潜力提供指导作用。
文摘Based on the water resource balance,the correlation between both the Liaoning water resource and precipitation and total amount of water resource from 1991 to 2004 was analyzed by assuming Liaoning to be an enclosed region.And the calculation methods were developed to quantitatively determine the increase of rainfall due to artificial precipitation,and consequently ascertain the contribution of artificial rainfall amount to water resources.