《Table 3 Regional correlation coeffi cients between the monthly fi elds of the SAT and SIC for the p
提示：宽带有限、当前游客访问压缩模式
本系列图表出处文件名：随高清版一同展现
《Satellite-observed trends in the Arctic sea ice concentration for the period 1979–2016》
The impacts of the SAT on the SIC are variable depending on the area.In-phase correlations between the monthly fi elds of the SAT and SIC are generally low（-0.16）to moderate（-0.57）（Table 3） .Nevertheless，a lagged correlation analysis ahead by one to three months suggests that SAT variations can explain a fraction of the SIC changes in the Central Arctic Ocean，Barents Sea，Bering Sea，and Greenland Sea（Table 4）.Recent observations have revealed thinner sea ice in the Arctic Ocean sea ice cover，which can be partly attributed to warmer surface air temperatures together with a shortened freezing period during the cold seasons.Thinner ice is usually a prerequisite during the spring for the substantial sea ice loss in the following summer.Therefore，the decreases in SIC within the Arctic Ocean shelf seas during the summer（Fig.3c）and autumn（Fig.3d）are most vulnerable to the rising surface temperatures during autumn through to spring（Fig.10d，a，and b）.
| 图表编号 | XD0034428400 严禁用于非法目的 |
|---|---|
| 绘制时间 | 2019.01.01 |
| 作者 | WANG Yunhe、BI Haibo、HUANG Haijun、LIU Yanxia、LIU Yilin、LIANG Xi、FU Min、ZHANG Zehua |
| 绘制单位 | CAS Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences、University of Chinese Academy of Sciences、CAS Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences |
| 更多格式 | 高清、无水印（增值服务） |
