极地研究

极地研究 ›› 2013, Vol. 25 ›› Issue (3): 268-277.DOI: 10.3724/SP.J.2013.00268

• 研究论文 • 上一篇    下一篇

2012年南极长城站气象和海冰特征分析

杨清华1  张本正2  李明1  孟上1   

  1. 1国家海洋环境预报中心，北京100081； 2武汉市气象局，湖北 武汉430040
  • 收稿日期:2013-01-10 修回日期:2013-04-25 出版日期:2013-09-30 发布日期:2013-09-30
  • 通讯作者: 杨清华

ANALYSIS OF WEATHER AND SEA ICE AT THE ANTARCTIC GREAT WALL STATION IN 2012

Yang Qinghua1，Zhang Benzheng2，Li Ming1，Meng Shang1   

  1. 1National Marine Environmental Forecasting Center, Beijing 100081, China; 2Wuhan Meteorological Service, Wuhan 430040, China
  • Received:2013-01-10 Revised:2013-04-25 Online:2013-09-30 Published:2013-09-30
  • Contact: Yang Qinghua

PDF (PC)

1489

被引次数

7

摘要： 基于中国第28次南极科学考察长城站越冬期间获取的常规气象和海冰观测资料，结合统计的1985—2010年气候值，对比分析了长城站2012年的气象及海冰特征。气象分析表明，该年平均气压和气温偏低，N—W风向频率显著偏低，E—SE风向频率显著偏高；雾日偏少，降雪量、吹雪及雪暴显著偏多；针对观测期间某些月份比较明显的气象要素和天气现象异常，从大气环流角度进行了分析解释。海冰观测表明，长城湾冰情变化受大气动力作用影响大，冰情稳定性差，外围海域海冰极不稳定，2012年4月至2012年11月冰情几经进退，先后交替出现3个完全冰冻和3个部分冰冻期。

关键词: 南极长城站, 气象, 异常, 大气环流, 海冰

Abstract: Based on the observation at Great Wall Station (GWS) in 2012, the meteorology and sea ice parameters are analyzed compared with the climate statistics from 1985 to 2010. Firstly, the annual air pressure and temperature are lower, the N-W wind is less frequent while the E-SE wind is much more frequent than the climatic mean. The fog occurs significantly less, while the falling snow and blowing snow is significantly higher than the normal level. Secondly, the Antarctic atmospheric circulation is analyzed to explain the GWS weather anomalies happened in 2012. Finally, it shows that the sea ice in the Great Wall Bay is in an instability status which is more likely affected by the atmospheric dynamics. Three frozen periods and three partial frozen periods occurred in 2012.

Key words: Antarctic Great Wall station, weather, anomaly, atmospheric circulation, sea ice