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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

What is Climate?

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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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Phase Transitions: Sublimation and Deposition02:33

Phase Transitions: Sublimation and Deposition

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Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
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Phase Transitions: Melting and Freezing02:39

Phase Transitions: Melting and Freezing

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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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相关实验视频

Updated: Jun 15, 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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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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南极洲的冰崖难题是一个难题.

Alexander A Robel1

  • 1School of Earth and Atmospheric Sciences, Georgia Institute of Technology, 311 Ferst Drive, Atlanta, GA 30318, USA.

Science advances
|August 21, 2024
PubMed
概括

西南极洲高高的冰崖可能比以前认为的更加稳定. 研究表明,这些特征可能会抵抗快速的冰损失,为冰川动态提供新的见解.

科学领域:

  • 冰川学的冰川学
  • 气候科学 气候科学
  • 南极研究南极研究

背景情况:

  • 西南极洲冰川的迅速退却是全球海平面上升的一个重大问题.
  • 冰崖的不稳定性被认为是加速冰损失的主要机制.

研究的目的:

  • 为了评估南极快速收缩的冰川上高高的冰崖的稳定性.
  • 为了评估因冰崖破裂而导致失控的冰损失的潜力.

主要方法:

  • 利用了高分辨率卫星图像和数字海拔模型.
  • 分析了冰川流速和冰崖的几何形状.
  • 采用数值建模来模拟各种条件下的冰崖行为.

主要成果:

  • 观察到研究的冰川上的冰崖表现出比预期的更大的结构完整性.
  • 发现分娩过程并没有导致广泛,快速的悬崖撤退.
  • 模拟的场景表明,与以前的估计相比,对失控冰损失的敏感性较低.

结论:

  • 这个地区的高高的冰崖可能具有固有的稳定机制.
  • 这些特定的冰崖造成灾难性海平面上升的风险可能被高估了.

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LabVIEW-operated Novel Nanoliter Osmometer for Ice Binding Protein Investigations
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LabVIEW-operated Novel Nanoliter Osmometer for Ice Binding Protein Investigations

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Determining the Ice-binding Planes of Antifreeze Proteins by Fluorescence-based Ice Plane Affinity
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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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  • 需要进一步的研究,以了解对南极冰盖稳定的更广泛影响.