Marshall Gareth J, Thompson David W J, van den Broeke Michiel R
British Antarctic Survey Natural Environment Research Council Cambridge UK.
Department of Atmospheric Science Colorado State University Fort Collins CO USA.
Geophys Res Lett. 2017 Nov 28;44(22):11580-11589. doi: 10.1002/2017GL075998. Epub 2017 Nov 18.
We provide the first comprehensive analysis of the relationships between large-scale patterns of Southern Hemisphere climate variability and the detailed structure of Antarctic precipitation. We examine linkages between the high spatial resolution precipitation from a regional atmospheric model and four patterns of large-scale Southern Hemisphere climate variability: the southern baroclinic annular mode, the southern annular mode, and the two Pacific-South American teleconnection patterns. Variations in all four patterns influence the spatial configuration of precipitation over Antarctica, consistent with their signatures in high-latitude meridional moisture fluxes. They impact not only the mean but also the incidence of extreme precipitation events. Current coupled-climate models are able to reproduce all four patterns of atmospheric variability but struggle to correctly replicate their regional impacts on Antarctic climate. Thus, linking these patterns directly to Antarctic precipitation variability may allow a better estimate of future changes in precipitation than using model output alone.
我们首次全面分析了南半球气候变化的大尺度模式与南极降水详细结构之间的关系。我们研究了区域大气模型的高空间分辨率降水与南半球气候变化的四种大尺度模式之间的联系:南斜压环形模态、南极环形模态以及两种太平洋-南美洲遥相关型。所有这四种模式的变化都会影响南极地区降水的空间格局,这与它们在高纬度经向水汽通量中的特征一致。它们不仅影响平均降水量,还影响极端降水事件的发生率。当前的耦合气候模型能够再现大气变化的所有四种模式,但难以正确复制它们对南极气候的区域影响。因此,将这些模式直接与南极降水变化联系起来,可能比仅使用模型输出能更好地估计未来降水的变化。