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相关概念视频

Radiation: Applications01:17

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...
Factors Affecting Body Temperature01:28

Factors Affecting Body Temperature

As a nurse, it is vital to understand the factors affecting body temperature to monitor variations and effectively evaluate deviations from regular.
Factors may  include:
What is Climate?01:16

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.
What is Weather?01:07

What is Weather?

Overview
Global Climate Change01:50

Global Climate Change

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.
Variation of Atmospheric Pressure01:18

Variation of Atmospheric Pressure

Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...

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Updated: Jul 12, 2026

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
06:27

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

Published on: May 29, 2019

控制热层平均温度的因素

R E Newell, B C Weare

    Science (New York, N.Y.)
    |December 24, 1976
    PubMed
    概括

    来自火山喷发的火山气溶,如Mt. 大山显著降低了热带热带层的温度. 大西洋海面温度对这些热带气候模式的影响很小.

    科学领域:

    • 气候学和大气科学 气候学和大气科学
    • 火山学 火山学是一门学科.
    • 海洋学 海洋学 海洋学

    背景情况:

    • 热带热带层温度受到各种气候因素的影响.
    • 太平洋海面温度是已知的热带气候变化的驱动因素.
    • 其他潜在因素的作用,如大西洋海面温度和火山气溶,需要进一步调查.

    研究的目的:

    • 研究大西洋海洋表面温度和火山气溶对热带热带层平均温度的影响.
    • 量化大火山喷发对热带热带层温度的影响.

    主要方法:

    • 分析历史气候数据,重点关注海面温度和大气温度.
    • 山峰的案例研究. 阿贡火山喷发对全球温度记录的影响.

    主要成果:

    • 这座山. 1963年3月的阿贡古喷发导致热带热带层的平均温度明显下降约0.5摄氏度.
    • 发现大西洋海面温度对热带热带层平均温度的影响微不足道.

    结论:

    • 火山气溶是影响热带热带层温度的重要因素.
    • 太平洋海面温度和火山活动是热带气候变化的关键驱动因素,而大西洋的影响是最小的.

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