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相关概念视频

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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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Phase Transitions: Melting and Freezing02:39

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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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Concrete structures in cold climates, such as those along roadsides, can retain moisture. This moisture makes them susceptible to frost-related damage when temperatures fall below freezing. Adding moisture worsens the damage during temperature fluctuations, leading to repeated freezing and thawing. De-icing salts, spread over these structures to melt ice, add to the freeze-thaw cycle, and draw even more moisture into the concrete.
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In a nonhomogeneous rod made up of steel and brass, restrained at both ends and subjected to a temperature change, several steps are involved in calculating the stress and compressive load. Due to the problem's static indeterminacy, one end support is disconnected, allowing the rod to experience the temperature change freely. Next, an unknown force is applied at the free end, triggering deformations in the rod's steel and brass portions. These deformations are then calculated and added...
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In the site survey of a four-sided traverse, internal angles are essential to ensure geometric accuracy. The survey revealed that the sum of the measured internal angles was 359 degrees and 48 minutes, which is 12 minutes less than the expected 360 degrees. This discrepancy signals an error likely arising from measurement inaccuracies during the fieldwork.To rectify this error, the adjustment process involved distributing the 12-minute shortfall equally across the four internal angles. By...
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在全球变暖下,绘制地图显示了南极冰川盆地的倾斜风险.

Ricarda Winkelmann1,2,3, Julius Garbe1,3, Jonathan F Donges1,2,4

  • 1Earth Resilience Science Unit, Potsdam Institute for Climate Impact Research (PIK), Member of the Leibniz Association, Potsdam, Germany.

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南极冰盖面临着由于变暖而不可逆转的冰损失. 不同地区都有临界点,西南极洲面临1-2°C升温的风险,东南极洲面临2-5°C升温的风险,威胁到海平面的大幅上升.

关键词:
气候变化的影响 气候变化的影响冰层科学 冰层科学预测和预测的投影和预测.

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科学领域:

  • 冰川学的冰川学
  • 气候科学 气候科学
  • 地球系统科学 地球系统科学

背景情况:

  • 南极冰盖容易受到放大反的影响,从而加速冰的流失.
  • 冰的消失可能导致实际上不可逆转的退缩,对全球海平面构成重大风险.

研究的目的:

  • 分析南极单个排水盆地的独特性质和长期冰损失的风险.
  • 在不同的全球变暖情景下评估这些风险.

主要方法:

  • 分析各个排水盆地的冰损失动态.
  • 评估影响冰盖稳定的地形和气候条件.
  • 确定不同南极地区的临界变暖值.

主要成果:

  • 一些南极盆地随着变暖而呈现逐渐的冰损失,而另一些则具有导致解体的关键值.
  • 在工业化前的水平上升1-2°C可能会导致西南极洲40%的冰体积崩.
  • 东南极洲的海洋基础部门,海平面潜在上升约5米,在2-5°C的变暖下风险不稳定.

结论:

  • 南极冰盖包括多个相互作用的倾斜系统,而不是一个单一的单质系统.
  • 了解盆地特定的脆弱性对于预测未来海平面上升至关重要.
  • 南极冰层损失的早期预警值是可以识别的,对减缓气候变化的努力至关重要.