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北半球500 hPa高度场趋势变化与突变

陈辉 施能 王永波

陈辉, 施能, 王永波. 北半球500 hPa高度场趋势变化与突变[J]. 热带气象学报, 2000, (3): 272-281.
引用本文: 陈辉, 施能, 王永波. 北半球500 hPa高度场趋势变化与突变[J]. 热带气象学报, 2000, (3): 272-281.
CHEN Hui, SHI Neng, WANG Yong-bo. THE SECULAR TREND VARIATIONS AND ABRUPT CHANGE OF NORTHERN 500 hPa GEOPOTENTIAL HEIGHT[J]. Journal of Tropical Meteorology, 2000, (3): 272-281.
Citation: CHEN Hui, SHI Neng, WANG Yong-bo. THE SECULAR TREND VARIATIONS AND ABRUPT CHANGE OF NORTHERN 500 hPa GEOPOTENTIAL HEIGHT[J]. Journal of Tropical Meteorology, 2000, (3): 272-281.

北半球500 hPa高度场趋势变化与突变

基金项目: 国家自然科学基金(No:49875019)资助

THE SECULAR TREND VARIATIONS AND ABRUPT CHANGE OF NORTHERN 500 hPa GEOPOTENTIAL HEIGHT

  • 摘要: 用1951~1998年的资料研究了北半球500 hPa四季高度场的长期趋势变化。结果表明, 48年来低纬度 500 hPa高度场多为正趋势而高纬度则多为负趋势。近 48年低纬的西北非洲、地中海及以西的北非北部,低纬度的中太平洋、贝加尔湖及以东地区,西北北美的高度呈持续正趋势;而阿留申及北太平洋、格林兰以南及东北北美、阿拉伯海以北高度明显降低。突变分析表明,大约60年代初及1976年,500 hPa发生明显的环流突变。这两次变化在两大洋上的 500 hPa有明显不同,第 1次表现为低纬中大西洋高度降低,西北非洲高度增加。第2次则表现为低纬中太平洋、贝加尔湖地区高度增加,北太平洋高度降低。统计检验表明第2次突变,低纬的正突变比北太平洋负突变更明显,是一次北半球的大尺度跃变事件。

     

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出版历程
  • 收稿日期:  1999-07-05
  • 修回日期:  1999-10-15

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