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相关概念视频

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.
Effects of Temperature on Free Energy02:11

Effects of Temperature on Free Energy

The spontaneity of a process depends upon the temperature of the system. Phase transitions, for example, will proceed spontaneously in one direction or the other depending upon the temperature of the substance in question. Likewise, some chemical reactions can also exhibit temperature-dependent spontaneities. To illustrate this concept, the equation relating free energy change to the enthalpy and entropy changes for the process is considered:
Mechanisms of Heat Transfer II01:20

Mechanisms of Heat Transfer II

In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
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...
Effect of Sea Water on Concrete01:22

Effect of Sea Water on Concrete

Concrete exposed to seawater can undergo degradation like the dissolution of ettringite and gypsum, increasing the material's porosity and decreasing its strength. In contrast, the crystallization of salts within the concrete's pores can cause expansion, particularly above the waterline where evaporation occurs. Nonetheless, this expansion only happens when seawater, enabled by the concrete's permeability, manages to infiltrate the structure.
Concrete in areas between tide marks, which undergo...
Marine Microbial Ecology01:30

Marine Microbial Ecology

Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...

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The effect of gestational age on neonatal outcome in low-risk singleton term deliveries.

The journal of maternal-fetal & neonatal medicine : the official journal of the European Association of Perinatal Medicine, the Federation of Asia and Oceania Perinatal Societies, the International Society of Perinatal Obstetricians·2014
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相关实验视频

Updated: Jul 7, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

热带超级温室效应在加热海洋表面中的作用

D Lubin

    Science (New York, N.Y.)
    |July 8, 1994
    PubMed
    概括

    水蒸气带来的超级温室效应使赤道海洋变暖. 测量显示,这种效应通过减少由水蒸气驱动的红外冷却来增加海面温度.

    科学领域:

    • 地球和大气科学 地球和大气科学
    • 海洋学 海洋学 海洋学
    • 气候科学 气候科学

    背景情况:

    • 卫星数据表明,一个
    • 超级温室效应是一种超级温室效应.
    • 在赤道海洋上,但其对海面温度的直接影响尚不清楚.

    研究的目的:

    • 通过使用地面测量来调查赤道海洋温室效应的规模和机制.
    • 为了确定水蒸气对该地区海面变暖的贡献.

    主要方法:

    • 使用富里叶变换红外 (FTIR) 光谱辐射仪测量中红外辐射 (520μm) 以1厘米-1的光谱分辨率.
    • 分析了表面净红外冷却的变化,以应对海面温度变化 (297303 K).

    主要成果:

    • FTIR数据显示,在赤道海洋上有一个异常大的水蒸气温室效应.
    • 由于海面温度上升,净红外冷却减少了3050W/m2.
    • 这种加热主要发生在中红外线中,通过水蒸气连续发射窗口.

    结论:

    • 超级温室效应直接导致海面辐射加热.

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  • 热带深层对流在推动这种增强的温室效应方面发挥着重要作用.
  • 水蒸气在中红外线中的作用对于了解海洋变暖至关重要.