南极平流层变暖可能导致南方的消极环状模式,改变全球天气模式,影响澳大利亚的气候。 Antarctic stratospheric warming may lead to a negative Southern Annular Mode, altering global weather patterns and affecting Australia's climate.
南极洲平流层变暖,可能由热浪引发,可能导致持续的消极南方环形模式,影响全球天气模式。 Antarctica's stratospheric warming, potentially triggered by a heatwave, could lead to a persistent negative Southern Annular Mode, affecting global weather patterns. 极地旋涡变弱可能会在澳大利亚东南部造成更温暖、更干燥的条件,同时南部地区降雨量增加,高山地区降雪。 The weakening polar vortex may cause warmer, drier conditions in southeastern Australia, while increasing rainfall in southern regions and snowfall in alpine areas. 影响取决于气候系统向北推进的时间和程度,以及厄尔尼诺和印度洋分极等其他影响因素。 The impact depends on the duration and extent of weather systems being pushed northward, as well as other influencers like El Niño and the Indian Ocean Dipole.