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相关概念视频

Global Climate Change01:50

Global Climate Change

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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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What is Climate?01:16

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Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
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The Water Cycle01:00

The Water Cycle

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The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
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Responses to Drought and Flooding02:41

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Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
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Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
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相关实验视频

Updated: Jul 4, 2025

Laser-Induced Fluorescence Emission L.I.F.E. as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
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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
PubMed
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.

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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.