One of the ways to dissipate perspiration is by convection.

散发汗水的一种方法是通过对流作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法对流过环形后台阶通道内的层流分离和再附着进行了数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统角度,建立了广义对流扩散方程初边值问题所群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年的高空、地面，论了极地对流层顶与地面温度的关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

以水为工质,分别在过冷和饱和条件下对竖直窄环隙流道进行了自然对流沸腾流动不稳定性实验,观测到了窄隙流道饱和沸腾时所特有的蒸干型流动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有对流单体在原地维持成熟的结构，表现出较强的稳定性，而分裂出的新单体在移动过程中，逐渐向成熟位相发展，并且又分裂出新的单体。

One of the ways to dissipate perspiration is by convection.

汗水的一种方法是通过对流作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法对流过环形后台阶通道内的层流分离和再附着进行了数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统角度,建立了广义对流扩方程初边值问题所产生半群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年的高空、地面资料，讨论了极地对流层顶与地面温度的关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

以水为工质,分别在过冷和饱和条件下对竖直窄环隙流道进行了自然对流沸流动不稳定性实验,观测到了窄隙流道饱和沸所特有的蒸干型流动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有对流单体在原地维持成熟的结构，表现出较强的稳定性，而分裂出的新单体在移动过程中，逐渐向成熟位相展，并且又分裂出新的单体。

One of the ways to dissipate perspiration is by convection.

散发汗水的一种方法是通过对流作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法对流过形后台阶通道内的层流再附着进行了数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统角度,建立了广义对流扩散方程初边值问题所产生半群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年的高空、地面资料，讨论了极地对流层顶与地面温度的关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

以水为工质,别在过冷饱条件下对竖隙流道进行了自然对流沸腾流动不稳定性实验,观测到了隙流道饱沸腾时所特有的蒸干型流动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有对流单体在原地维持成熟的结构，表现出较强的稳定性，而裂出的新单体在移动过程中，逐渐向成熟位相发展，并且又裂出新的单体。

One of the ways to dissipate perspiration is by convection.

散发汗水的一种方法是通过对流作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法对流过环形后台阶通道内的层流分离和再附着进行数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力统角度,广义对流扩散方程初边值问题所产生半群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年的高空、地面资料，讨论极地对流层顶与地面温度的。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

水为工质,分别在过冷和饱和条件下对竖直窄环隙流道进行自然对流沸腾流动不稳定性实验,观测到窄隙流道饱和沸腾时所特有的蒸干型流动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有对流单体在原地维持成熟的结构，表现出较强的稳定性，而分裂出的新单体在移动过程中，逐渐向成熟位相发展，并且又分裂出新的单体。

One of the ways to dissipate perspiration is by convection.

散发汗水方法是通过对作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法对过环形后台阶通内层分离和再附着进行了数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统角度,建立了广义对扩散方程初边值问题所产生半群个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年高空、地面资料，讨论了极地对层顶与地面温度关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

以水为工质,分别在过冷和和条件下对竖直窄环隙进行了自然对沸腾动不稳定性实验,观测到了窄隙和沸腾时所特有蒸干型动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有对单体在原地维持成熟结构，表现出较强稳定性，而分裂出新单体在移动过程中，逐渐向成熟位相发展，并且又分裂出新单体。

One of the ways to dissipate perspiration is by convection.

散发汗水的一种方法是通过作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法过环形后台阶通道内的层分离和再附着进行了数模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统角度,建立了广义扩散方程问题所产生半群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京区1977—1990年的高空、面资料，讨论了极层顶与面温度的关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

以水为工质,分别在过冷和饱和条件下竖直窄环隙道进行了自然沸腾动不稳定性实验,观测到了窄隙道饱和沸腾时所特有的蒸干型动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有单体在原维持成熟的结构，表现出较强的稳定性，而分裂出的新单体在移动过程中，逐渐向成熟位相发展，并且又分裂出新的单体。

One of the ways to dissipate perspiration is by convection.

散发汗的一种方法是通过对流作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法对流过环形后台阶通道内的层流分离和再附着进行了数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统,立了广义对流扩散方程初边值问题所产生半群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年的高空、地面资料，讨论了极地对流层顶与地面温的关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

工质,分别在过冷和饱和条件下对竖直窄环隙流道进行了自然对流沸腾流动不稳定性实验,观测到了窄隙流道饱和沸腾时所特有的蒸干型流动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有对流单体在原地维持成熟的结构，表现出较强的稳定性，而分裂出的新单体在移动过程中，逐渐向成熟位相发展，并且又分裂出新的单体。

One of the ways to dissipate perspiration is by convection.

散发汗水的一种方法是通过对流作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER法对流过环形后台阶通道内的层流分离和再附着进行了数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统角度,建立了广义对流扩散方程初边值问题所产生半群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年的高空、地面资料，讨论了极地对流层顶与地面温度的关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

以水为工质,分别在过冷和饱和条件下对竖直窄环隙流道进行了自然对流沸腾流动不实验,观测到了窄隙流道饱和沸腾时所特有的蒸干型流动不。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有对流单体在原地维持成熟的结构，表现出较强的，而分裂出的新单体在移动过程中，逐渐向成熟位相发展，并且又分裂出新的单体。

One of the ways to dissipate perspiration is by convection.

散发汗水的一种方法是通过作。

Numerical simulations of laminar flow separation and reattachment occurred in an annular backstep passage are performed by the SIMPLER algorithm.

SIMPLER算法过环形后台阶通道内的分离和再附着进行了数值模拟。

This paper establishes a global attractor of hemigroup produced by the initial boundary value problem of generalized convection and expansion equation.

从动力系统角度,建立了广义扩散方值问题所产生半群的一个全局吸引子。

The relationship between arctic tropopause height and surface air temperature is discussed by using the aerological sounding and surface data during 1977-1990 in Beijing area.

利北京地区1977—1990年的高空、地面资料，讨论了极地顶与地面温度的关系。

Experimental study was performed using water as working medium to investigate the flow instability in a vertical narrow annuli with both subcooled and saturated boilings.

以水为工质,分别在过冷和饱和条件下竖直窄环隙道进行了自然沸腾动不稳定性实验,观测到了窄隙道饱和沸腾时所特有的蒸干型动不稳定性。

With the numerical simulated data of the storm, the structure and evolution of the helicity, superhelicity and their dynamical influences on the development of the storm are investigated.

原有单体在原地维持成熟的结构，表现出较强的稳定性，而分裂出的新单体在移动过中，逐渐向成熟位相发展，并且又分裂出新的单体。