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。

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置降水井将低的残留水引走。

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。

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

屯留煤矿副井井筒表土段普通法施工,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).

摘要利多普勒雷达资料，种改进后的叉相关法(COTREC)建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。

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。

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直维持，而且降水随干侵入的增强而加强，干侵入推动降水区的东南向移动。

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

屯留煤矿筒表土段采用普法施工,利用外降水疏干降水。

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，气越过山岭后下沉气带来“焚风”效应，形成干热河谷。

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.

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

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。

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

屯留煤矿副筒表土段采用普通法施工,利用外疏干。

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

地形对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.

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

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.

小间距，增加上层滞和潜的入流通道，尤其要在潜含层底板低洼处设置将低洼处的残留引走。

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，干侵入在此次事件中一直维持，而且随干侵入的增强而加强，干侵入推动了区的东南向移动。

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

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的影响主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。

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，增加上层滞水和水的入流通道，尤其水含水层底板低洼处设置降水井将低洼处的残水引走。

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。

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

屯留煤矿副井井段采用普通法施工,利用井外降井疏干降。

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

地形对降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，采用一种改进后叉相关法(COTREC)建立了一种降临近预报方法。

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。

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，增加上层滞和潜流通道，尤其要在潜含层底板低洼处设置降井将低洼处残留引走。

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，干侵在此次降事件中一直维持，而且降随干侵增强而加强，干侵推动了降区东南向移动。

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。

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处设置降水井将处的残留水引走。

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。

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,利用井外井疏干。

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

地形对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).

摘要利用多普勒料，采用一种改进后的叉相关法(COTREC)建立了一种近预报方法。

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。

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，增加上层滞和潜的入流通道，尤其要在潜含层底板低洼处设置井将低洼处的残留引走。

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，干侵入在此次事件中一直维持，而且随干侵入的增强而加强，干侵入推动了区的东南向移动。

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,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的。

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

摘要多普勒雷达资料，采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。

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，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。

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强而加强，干侵入推动了降水区的东南向移动。