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Rainfall reductions over Southern Hemisphere semi-arid regions: the role of subtropical dry zone expansion

机译:南半球半干旱地区降雨减少:亚热带干旱区扩张的作用

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摘要

Since the late 1970s, Southern Hemisphere semi-arid regions such as southern-coastal Chile, southern Africa, and southeastern Australia have experienced a drying trend in austral autumn, predominantly during April and May. The rainfall reduction coincides with a poleward expansion of the tropical belt and subtropical dry zone by around 2°–3° in the same season. This has raised questions as to whether the regional rainfall reductions are attributable to this poleward expansion. Here we show that the impact of the poleward subtropical dry-zone shift is not longitudinally uniform: a clear shift occurs south of Africa and across southern Australia, but there is no evidence of a poleward shift in the southern Chilean sector. As such, a poleward shift of climatological April-May rainfall can explain most of the southeastern Australia rainfall decline, a small portion of the southern Africa rainfall trend, but not the autumn drying over southern Chile.
机译:自1970年代后期以来,南半球半干旱地区,如智利南部沿海,南部非洲和澳大利亚东南部,在南方秋季经历了干旱的趋势,主要是在4月和5月。在同一季节,降雨减少与热带带和亚热带干旱区向极扩张约2°–3°相吻合。这引起了有关区域降雨减少是否归因于这种极度扩张的质疑。在这里,我们表明,极地亚热带干旱区移动的影响在纵向上并不均匀:非洲南部和澳大利亚南部地区发生了明显的移动,但是没有证据表明智利南部地区发生极地移动。因此,4月至5月气候变化的极点变化可以解释澳大利亚东南部的大部分降雨下降,南部非洲降雨趋势的一小部分,但不能解释智利南部的秋季干旱。

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