极地研究 ›› 2017, Vol. 29 ›› Issue (3): 368-377.DOI: 10.13679/j.jdyj.2017.3.368

• 研究论文 • 上一篇    下一篇

普里兹湾区域风和温度资料对比分析: 以2007 年为例

谢泽林, 王召民   

  1. 南京信息工程大学极地气候系统与全球变化实验室, 江苏 南京 210044
  • 收稿日期:2016-07-26 修回日期:2016-08-30 出版日期:2017-09-30 发布日期:2017-09-30
  • 通讯作者: 王召民

Comparisons of wind and temperature in Prydz Bay, Antarctica

Xie Zelin, Wang Zhaomin   

  • Received:2016-07-26 Revised:2016-08-30 Online:2017-09-30 Published:2017-09-30

摘要:

通过分析再分析资料与站点观测资料的差异评估了普里兹湾区域5 套再分析资料的风速、风向以及
温度产品。这5 套再分析资料包括欧洲中心再分析资料(ERA-I)、日本25 年再分析资料(JRA-25)、日本55
年再分析资料(JRA-55)、美国国家环境预报中心再分析资料(CFSR)和美国国家航空航天局再分析资料
(MERRA)。采用的观测资料来自两个人工观测站和三个自动气象站。月平均和季节差异分析结果表明,
Mawson 站点再分析资料的风速一般小于站点风速, 其他站点再分析资料一般风速过大, 所有的站点风向与
再分析资料风向差异不大, 再分析资料的2 m 温度总体低于人工观测站的温度, 自动站和再分析资料的差
异则没有一致的差异特征。通过6 h 风速资料对比, 发现当Mawson 站点风速低于5 m·s–1 时, 再分析资料偏
高, 当站点风速高于15 m·s–1 时, 再分析资料偏低, 且该站点记录的极端强风次数远多于再分析资料。

关键词: 南极站点资料, 再分析资料, 风速, 风向, 温度

Abstract:

We evaluated the 10-m wind speed, wind direction, and 2-m temperature of the Prydz Bay region (Antarctica)
using five reanalysis products: the European Centre for Medium-Range Weather Forecasts Interim
Reanalysis, Japanese 25-year Reanalysis, Japanese 55-year Reanalysis, Climate Forecast System Reanalysis,
and Modern Era Retrospective-Analysis for Research and Application. The reanalysis products were compared
with observations acquired by two manual weather stations and three automatic weather stations during 2007.
Examination of the monthly mean and seasonal differences revealed that reanalysis wind speeds
were lower than station observations at Mawson but higher at the other stations. Discrepancies in wind direction
between the observations and the reanalysis datasets were small. The 2-m temperatures of the reanalysis
datasets were lower than observed at the manual weather stations. There was no consistent characteristic
in the differences between the 2-m temperatures from the reanalysis datasets and the data from the
automatic weather stations. We also evaluated 6-hourly data at Mawson. It was found that the reanalysis
datasets overestimated wind speed at low wind speeds (<5 m/s) and underestimated wind speed at high wind
speeds (>15 m/s). In addition, the number of strong wind events observed at Mawson was significantly
higher than indicated by the reanalysis datasets.

Key words: Antarctic station data, reanalysis datasets, wind speed, wind direction, temperature