概括
根据13年的太阳辐射数据,人类活动似乎没有影响全球大气度. 自然气溶和火山尘埃的入侵显著影响大气不透明度和太阳辐射.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 环境监测 环境监测
背景情况:
- 大气度会影响到地球表面的太阳辐射.
- 了解影响度的因素对于气候建模和太阳能评估至关重要.
- 人类活动对全球大气度的潜在影响需要调查.
研究的目的:
- 评估人类活动对全球大气度的影响.
- 为了确定大气气溶的自然和人为来源.
- 分析气溶对太阳辐射的长期影响.
主要方法:
- 分析了13年的太阳辐射测量结果.
- 阳光照射数据与气溶度的相关性.
- 区分热层和平流层的气溶来源.
主要成果:
- 没有证据表明人类活动与大气度的全球变化有关.
- 短期太阳辐射波动与自然产生的热层气溶相关.
- 火山尘埃进入平流层会导致大气不透明度长期增加.
结论:
- 全球大气度主要受到自然过程的影响,而不是人类活动.
- 高层层气溶,特别是来自火山爆发的气溶,对大气不透明度有重大而持久的影响.
- 热层气溶有助于太阳辐射的短期变化.
相关概念视频
What is Weather?
Overview
What is Climate?
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.
Emission Spectra
When solids, liquids, or condensed gases are heated sufficiently, they radiate some of the excess energy as light. Photons produced in this manner have a range of energies, and thereby produce a continuous spectrum in which an unbroken series of wavelengths is present.
Radiation: Applications
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...
The average...
Absorption of Radiation
The rate of heat transfer by emitted radiation is described by the Stefan-Boltzmann law of radiation:
Radiation Pressure: Problem Solving
The radiation pressure applied by an electromagnetic wave on a perfectly absorbing surface equals the energy density of the wave. The wave's momentum also gets transferred to the surface when an electromagnetic wave is entirely absorbed by it. The rate at which momentum is transmitted to an absorbing surface perpendicular to the propagation direction equals the force on the surface.
The average value of the rate of momentum transfer divided by the absorbing area represents the average force per...
The average value of the rate of momentum transfer divided by the absorbing area represents the average force per...


