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Atmosphere scientific expedition and research are one of the most important parts of Chinese Antarctic scientific research.

南极大气科学考察与研究是南极科学研究的重要组成部分。

China's 19th Antarctic expedition lasted 121 days, is China's previous Antarctic shortest time.

2002年,中国第19次南极考察历时121天,是中国历次南极考察时间最短的一次。

Poor southerners , there is no bright star near the south celestial pole .

可惜的是,天球南极附近没有光星,所以没有南极星为南半球居民引路。

We also isolated a structurally distinct 4-cysteine (4cys) hepcidin from an Antarctic eelpout that is unrelated to the notothenioids but inhabits the same freezing water.

利用基因组PCR和Southern杂交鉴定发现4cys_hepcidin只特异的存在于南极鱼中,而在非南极鱼(non-Antarctic taxa)中则没有发现,表明了这种分子内半胱氨酸残基数目的减少是对南极极端环境的一种适应机制。

The Japanese South Pole observation team "the Fuji dome" neighbor discovered in January 26, 2006 in the Japanese South Pole Observation station Base that according to Japanese State-run Polar region Research institute manager cane well principle line of expression, this is in the South Pole ice cap next 9994 feet place discoveries; Japan Science of education Department's official Mei Qiyou governs the expression, in the ice core air bubble includes many air bubbles, inside these air bubble's gas, very has the possibility is 1,000,000 years ago remains down, if after research, not only may understand the beforehand terrestrial environment, but may also use for to forecast the later climate.

日本南极观测队于2006年1月26日在日本南极观测站基地「富士圆顶」附近发现,据日本国立极地研究所所长藤井理行表示,这是在南极冰盖下9994英尺处发现;日本教育科学部门的官员梅崎友治表示,冰芯气泡中含有许多气泡,这些气泡里面的气体,很有可能是百万年前留下来的,如果经过研究,不但可以了解以前的地球环境,还可以用来预测以后的气候。

The obvious difference in the characteristics of AASW and SAMW may result in the formation of the Subantarctic Front.

在PF1以北,向北输送的南极表层水开始辐聚下沉,在下沉并北移的过程中与亚南极模态水相遇,SAMW与AASW之间温盐特征的巨大差异可能是导致亚南极锋形成的主要原因。

Antarctic sea-ice oscillation index with a seesaw pattern is defined Using NCEP/NCAR reanalysis girds data of monthly Antarctica sea-ice concentration from 1973 to 2002. The Relationships between the index of winter and the summer precipitations in China as well as the onset date of the summer East Asia monsoon are presented.

利用NCEP 1973-2002年逐月南极海冰密集度格点资料,定义了具有跷跷板式变化规律的南极海冰涛动指数,分析了冬季南极海冰涛动指数与我国夏季降水及东亚季风爆发时间的关系。

Coastal region at the Antarctic continent,where is under the influences both of ocean and ice sheet,as well as many humen activities,could be considered as a fragile zone in Antarctic ecological environment.

南极大陆沿海地带是南极海、陆、冰的交集带,它同时受到来自海洋、大陆冰以及人类活动的影响,因而成为南极生态环境最脆弱的环节。

Thereinto, the sea-ice extent of Weddell Sea and Ross Sea regions extends and area increases, while the sea-ice extent of the other three regions shrinks and area decreases.

南极海冰时空变化特征的研究对进一步认识南极地区海冰气相互作用的物理过程,讨论南极海冰变异与大气环流和天气气候的关系有重要意义

The maximum and the maximal variation of sea ice appear in Weddell Sea and Ross sea, while the minimum and the minimal variation of sea-ice appear inAntarctic Peninsula.

南极海冰最多和最少期分别出现在 9月和 2月;威德尔海和罗斯海地区海冰最多、变化最大,南极半岛地区海冰最少,变化也小;近 35年来环南极地区的海冰有明显的减少趋势。

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