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.

在本世纪结束前，极地海水表层有可能变得对霰石不饱。

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

地区气候变化大，副极地气候湿润，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年高空、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.

南极的物种对极地生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、地资料，讨论了极地对流层顶与地的关系。

The Antarctic species have few special adaptations for polar life.

南的物种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，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.

这个区气候变化大，副气候的凉爽湿润，到南洲的冰天雪。

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年的高空、面资料，讨论了流层顶与面温度的。

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.

在本世纪结束前，极地海水表层有可能变得对霰石不饱。

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

地区气候变化大，副极地气候湿润，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年高空、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.

南极的物种对极生活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，副极气候的凉爽湿润，到南极洲的冰天雪。

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年的高空、资料，讨论了极对流层顶与度的关系。

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.

南极的物种对极生活几乎有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，副极气候的凉爽湿润，到南极洲的冰天雪。

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年的高空、面资料，讨论了极对流层面温度的关系。

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年、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、地面料，讨论了极地对流层顶与地面温度的关系。