南半球在冰川时期的高湿度
Rieneke Weij1,2, J M Kale Sniderman3, Jon D Woodhead4
1School of Geography, Earth and Atmospheric Sciences, University of Melbourne, Melbourne, Victoria, Australia. rieneke.weij@uct.ac.za.
Nature
|February 7, 2024
概括
与之前的看法相反, 晚期普莱斯托时代的冰期给澳大利亚带来了水分. 冰川时期是潮湿的,而温暖的间冰川时期是干燥的,挑战了已有的气候模型.
科学领域:
- 古气候学
- 四年纪地质
- 气候科学
背景情况:
- 晚期普莱斯托纪冰河时代的气候通常被认为是造成低至中度生态系统的潮湿压力.
- 这种假设主要是基于化石花粉数据,
- 冰川时期大气中低碳二氧化物 (CO2) 水平可以抑制木质植物的生长,需要植物独立的古气候指标.
研究的目的:
- 在南半球亚热带地区重建过去的气候湿度.
- 挑战冰川气候的传统观点,
- 开发一个新的古气候记录独立于植物.
主要方法:
- 分析南半球亚热带地区的洞穴生长时间.
- 一个独立于植被的古气候记录的发展.
- 在多个冰川间周期 (过去35万年) 中重建气候水分的可用性.
主要成果:
- 澳大利亚南部的气候湿度在冰川时期达到顶峰,包括最后的冰川最大期.
- 发现冰河间时期相对干燥.
- 在南方亚热带地区观察到持续的冷湿气候反应.
结论:
- 南半球亚热带地区的冰川气候并不均干燥,而是更加凉爽和潮湿.
- 由于冰川温度降低,蒸发的减少可能导致湿度增加.
- 冰川环境作为人口扩张的障碍需要重新评估.
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