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相关概念视频

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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Radiation: Applications01:17

Radiation: Applications

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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
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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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Absorption of Radiation01:05

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The rate of heat transfer by emitted radiation is described by the Stefan-Boltzmann law of radiation:
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Atomic Emission Spectroscopy: Interference01:30

Atomic Emission Spectroscopy: Interference

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In atomic emission spectroscopy (AES), high-temperature atomizers excite a broad range of elements and molecules that generate complex emissions from sources such as oxides, hydroxides, and flame combustion products in the flame or plasma. Several strategies can be employed to minimize spectral interferences caused by overlapping emission lines or bands. These include increasing instrument resolution, choosing alternative emission lines, optimally placing the detector in low-background regions,...
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Attenuated Total Reflectance (ATR) Infrared Spectroscopy: Overview01:13

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Attenuated total reflectance (ATR) infrared spectroscopy is a powerful analytical technique used to study the composition of materials. It is widely employed in chemistry, materials science, forensic science, and other fields where sample characterization is required. ATR has several advantages over traditional transmission IR spectroscopy, including the requirement of little to no sample preparation and the ability to analyze a wide range of samples.
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相关实验视频

Updated: Jun 14, 2025

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
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表面的白色调节气溶直接影响气候.

Annan Chen1, Chuanfeng Zhao2,3, Haotian Zhang1

  • 1Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China.

Nature communications
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表面的白度变化对地球的能源预算有很大的影响. 这项研究揭示了不同表面白度如何影响气溶的直接辐射效应,这对气候变暖和变冷产生影响.

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科学领域:

  • 地球和大气科学 地球和大气科学
  • 气候科学 气候科学
  • 辐射转移是指辐射转移.

背景情况:

  • 气溶和表面白度 (SA) 是地球能量平衡的关键组成部分.
  • 最近表面类型和SA的变化引发了关于它们与气溶辐射效应的相互作用的问题.

研究的目的:

  • 调查气溶直接辐射效应 (ADRE) 从冷却到变暖的转变的关键SA值.
  • 分析SA变化对ADRE和气溶变暖效应 (AWE) 的影响.

主要方法:

  • 在不同的SA条件下分析ADRE和AWE.
  • 气溶特性 (厚度,吸收性) 的统计检查及其与AWE的关系.
  • 量化因SA趋势而发生的ADRE变化.

主要成果:

  • 气溶变暖效应 (AWE) 在中高度和吸收性气溶中普遍存在,临界SA值从0.18到0.96.
  • 较薄和更能吸收的气溶在统计学上与AWE增加有关.
  • 降低SA趋势 (-0.012/十年) 导致ADRE显著变化 (-0.2 ± 0.17W/m2/十年),特别是在夏季的北半球.

结论:

  • 降低SA增强ADRE冷却或减少AWE,这表明气溶的冷却效应更强,部分抵消了SA减少的变暖.
  • 了解这些相互作用对于准确的气候建模和能源预算评估至关重要.