4.7 Article

Extratropical Southern Hemisphere Synchronous Pressure Variability in the Early Twentieth Century

期刊

JOURNAL OF CLIMATE
卷 34, 期 14, 页码 5795-5811

出版社

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-20-0498.1

关键词

Antarctica; Pressure; Climate variability; Surface pressure; Decadal variability; Trends

资金

  1. National Science Foundation (NSF) [ANT-1744998]

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This study analyzes the spatial pattern of pressure variability across the Southern Hemisphere in the early twentieth century, revealing synchronous but opposite-signed pressure relationships between Antarctica and the midlatitudes in the Southern Hemisphere, especially in the summer and autumn. In addition to connections with the southern annular mode, regional and shorter duration pressure trends are found to be associated with influences from tropical variability and potentially the zonal wavenumber 3 pattern.
Because continuous meteorological observations across Antarctica did not start until the middle of the twentieth century, little is known about the full spatial pattern of pressure variability across the extratropical Southern Hemisphere (SH) in the early twentieth century, defined here as the period from 1905 to 1956. To fill this gap, this study analyzes pressure observations across the SH in conjunction with seasonal pressure reconstructions across Antarctica, which are based on observed station-to-station statistical relationships between pressure over Antarctica and the southern midlatitudes. Using this newly generated dataset, it is found that the early twentieth century is characterized by synchronous but opposite-signed pressure relationships between Antarctica and the SH midlatitudes, especially in austral summer and autumn. The synchronous pressure relationships are consistent with the southern annular mode, extending its well-known influence on SH extratropical pressure since 1957 into the early twentieth century. Apart from connections with the southern annular mode, regional and shorter-duration pressure trends are found to be associated with influences from tropical variability and potentially the zonal wavenumber 3 pattern. Although the reduced network of SH observations and Antarctic reconstruction captures the southern annular mode in the early twentieth century, reanalysis products show varying skill in reproducing trends and variability, especially over the oceans and high southern latitudes prior to 1957, which stresses the importance of continual efforts of historical data rescue in data-sparse regions to improve their quality.

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