The Antarctic species have few special adaptations for polar life.

南的物地生活几乎没有什么特别的适应性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪结束前，地海水表层有可能变得霰石不饱和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候变化大，副地气候的凉爽湿润，到南洲的冰天雪地。

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.

利用北京地区1977—1990年的高空、地面资料，讨论了地流层顶与地面温度的关。

The Antarctic species have few special adaptations for polar life.

南极的物种对极地生活几乎没有什么特别的适应性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪结束前，极地海水表层有可能变得对霰石。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候变化大，副极地气候的凉，到南极洲的冰天雪地。

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.

利用北京地区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。

The Antarctic species have few special adaptations for polar life.

南极的物种对极地生活几乎没有什么特别的适应性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪结束前，极地海水表层有可能变得对霰和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候变化大，副极地气候的凉爽，南极洲的冰天雪地。

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.

利用北京地区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。

The Antarctic species have few special adaptations for polar life.

南极物种对极地生活几乎没有什么特别适应性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪，极地海水表层有可能变得对霰石不饱和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候变化大，副极地气候凉爽湿润，到南极洲冰天雪地。

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.

利用北京地区1977—1990空、地面资料，讨论了极地对流层顶与地面温度关系。

The Antarctic species have few special adaptations for polar life.

南物种对生活几乎没有什么特别性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪结束前，海水表层有可能变得对霰石不饱和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个区气候变化大，副气候凉爽湿润，到南洲冰天雪。

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.

利用北京区1977—1990年高空、面资料，讨论对流层顶与面温度关系。

The Antarctic species have few special adaptations for polar life.

南极的物种对极地生活几乎没有什么特别的适应性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪结束前，极地海水表层有可能变得对霰石不饱和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候变化大，副极地气候的凉爽湿润，到南极洲的冰天雪地。

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.

利用北京地区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。

The Antarctic species have few special adaptations for polar life.

南极的物种对极地生活几乎没有什么特别的适应性。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

本世纪结束前，极地海水表层有可能得对霰石不饱和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候化大，副极地气候的凉爽湿润，到南极洲的冰天雪地。

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.

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

The Antarctic species have few special adaptations for polar life.

南极的物种对极地生活几乎没有什么特别的适应性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪结束前，极地海水表层有可能变得对霰和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候变化大，副极地气候的凉爽，南极洲的冰天雪地。

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.

利用北京地区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。

The Antarctic species have few special adaptations for polar life.

的物种地生活几乎没有什么特别的适应性改变。

Polar surface waters most likely will become undersaturated for aragonite before the end of this century.

在本世纪结束前，地海水表层有可能变得不饱和。

In this area the climate changes from cool, humid, and subpolar to the frozen conditions of Antarctica.

这个地区气候变化大，副地气候的凉爽湿润，洲的冰天雪地。

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.

利用北京地区1977—1990年的高空、地面资料，讨论了地流层顶与地面温度的关系。