The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用普通法施工,利用井外水井疏干水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

形对水空间分布影响主要是通过宏观形因素性质海拔高度不同而起作用。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用多普勒雷达资料，采用一种改进后叉相关法(COTREC)建立了一种水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列岭谷形波，形成明水波状起伏分布曲线，气流越过山岭后下沉气流带来“焚风”效应，形成干热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，干侵入在此次水事件中一直维持，而且水随干侵入增强而加强，干侵入推动了水区东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水潜水入流通道，尤其要在潜水含水层底板低洼处设置水井将低洼处残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用普通法施工,利用井外降水井疏干降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

对降水空间的影响主要是通过宏观素的性质和局海拔高度不同而起作用的。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用多普勒雷达资料，采用一种改进后的叉相关法(COTREC)建立了一种降水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列的岭谷波，成明显的降水波状起曲线，气流越过山岭后下沉气流带来“焚风”效应，成干热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

析发现，干侵入在此次降水事件中一直维持，而且降水随干侵入的增强而加强，干侵入推动了降水区的东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水和潜水的入流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处的残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用普通法施工,利用井外降水井疏降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

地形对降水空间分布的影响主要是通过宏观地形因素的性质和局地海拔高度不同而起作用的。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用多普勒雷达资料，采用一种改进后的叉相关法(COTREC)建立了一种降水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列的岭谷地形波，形成明显的降水波状起伏分布曲线，气流越过山岭后下沉气流带来“焚风”效应，形成热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，在此次降水事件中一直维持，而且降水随的增强而加强，推动了降水区的东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水和潜水的流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处的残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用通法施工,利用井外降水井疏干降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

地形对降水空间分布的影响主要是通过宏观地形因素的性质和局地海拔高度不同而起作用的。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用雷达资料，采用一种改进后的叉相关法(COTREC)建立了一种降水临方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列的岭谷地形波，形成明显的降水波状起伏分布曲线，气流越过山岭后下沉气流带来“焚风”效应，形成干热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，干侵入在此次降水事件中一直维持，而且降水随干侵入的增强而加强，干侵入推动了降水区的东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水和潜水的入流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处的残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用普通法施工,利用井外降水井疏降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

地形对降水空间分布的影响主要是通过宏观地形因素的性质和局地海拔高度不同而起作用的。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用多普勒雷达资料，采用一种改进后的叉相关法(COTREC)建立了一种降水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列的岭谷地形波，形成明显的降水波状起伏分布曲线，气流越过山岭后下沉气流带来“焚风”效应，形成热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，入在此次降水事件中一直维持，而且降水入的增强而加强，入推动了降水区的东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水和潜水的入流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处的残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用普通法,利用井外降水井疏干降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

地形对降水空间分布的影响主要是通过宏观地形因素的性质和局地海拔高度不同而起作用的。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用多普勒雷达资料，采用一种改进后的叉相关法(COTREC)建立了一种降水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列的岭谷地形波，形成明显的降水波状起伏分布曲线，气流越过山岭后下沉气流带来“焚风”效应，形成干热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，干此次降水事件中一直维持，而且降水随干的增强而加强，干推动了降水区的东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水和潜水的流通道，尤其要潜水含水层底板低洼处设置降水井将低洼处的残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用普通法施工,利用井外降水井疏降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

地形对降水空间分布的影响主要是通过宏观地形因素的性质和局地海拔高度不同而起作用的。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用多普勒雷达资料，采用一种改进后的叉相关法(COTREC)建立了一种降水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列的岭谷地形波，形成明显的降水波状起伏分布曲线，气流越过山岭后下沉气流带来“焚风”效应，形成热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，侵入在此次降水事件中一直维持，而且降水随侵入的增而，侵入推动了降水区的东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增上层滞水和潜水的入流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处的残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采用普通法施工,利用井外降水井疏干降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

地形对降水空间分布影响主要是通过宏观地形因素性质和局地海拔高度不同而起作用。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

摘要利用多普勒雷达资料，采用一种改法(COTREC)建立了一种降水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵向排列岭谷地形波，形成明显降水波状起伏分布曲线，气流越过山岭下沉气流带来“焚风”效应，形成干热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，干侵入在此次降水事件中一直维持，而且降水随干侵入增强而加强，干侵入推动了降水区东南向移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水和潜水入流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处残留水引走。

The auxiliary shaft topsoil adopted ordinary construction and drainages in hygrometric well.

屯留煤矿副井井筒表土段采普通法施工,利井外降水井疏干降水。

The terrain affect Spatial Distribution of Precipitation by way of macroeconomics topographer and parcel height above sea level.

地形对降水空间分布影响主要是通过宏观地形因素性质和局地海拔高度不同而起作。

Using Doppler radar data, an algorithm for precipitation nowcast is set up by applying an improved cross-correlation extrapolation method (COTREC).

要利多普勒雷达资料，采一种改进后叉相关法(COTREC)建立了一种降水临近预报方法。

The wavy distribution curve of precipitation formed on the longitudinal-arranged underlying rangegorge landforms.At leeside of range, dry valley formed due to fohn effect.

纵岭谷地形波，形成明显降水波状起伏分布曲线，气流越过山岭后下沉气流带来“焚风”效应，形成干热河谷。

It is found that dry intrusion maintained during the precipitation periods.The intensity of precipitation increased with the increasing dry intrusion, which pushed the rainy region southeastwards.

分析发现，干侵入在此次降水事件中一直维持，而且降水随干侵入增强而加强，干侵入推动了降水区东南移动。

Minish the well space and increase transflux routeways upper backwater and driving, especially setup precipitation well and drain residual water at the bottom of diving layer.

减小井间距，增加上层滞水和潜水入流通道，尤其要在潜水含水层底板低洼处设置降水井将低洼处残留水引走。