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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.
Isothermal Processes01:21

Isothermal Processes

A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
Thermal Stress01:09

Thermal Stress

If the temperature of an object is changed while it is prevented from expanding or contracting, the object is subjected to stress. The stress is compressive if the object expands in the absence of constraint and tensile if it contracts. This stress resulting from temperature change is known as thermal stress. It can be quite large and can cause damage. To avoid this stress, engineers may design components so they can expand and contract freely. For instance, on highways, gaps are deliberately...
Thermal Strain01:19

Thermal Strain

Thermal strain is a concept that arises when we consider how temperature changes affect structures. Unlike the conventional assumption that structures remain constant under load, real-world scenarios often involve temperature fluctuations that can significantly impact these structures. Consider a homogeneous rod with a uniform cross-section resting freely on a flat horizontal surface. If the rod's temperature increases, the rod elongates. This elongation is proportional to the temperature...
Temperature and Thermal Equilibrium01:11

Temperature and Thermal Equilibrium

Heat and temperature are essential concepts for everyone every day. The study of heat and temperature is part of an area of physics known as thermodynamics. It is not always easy to distinguish heat and temperature.
The concept of temperature has evolved from the common concepts of hot and cold. The scientific definition of temperature explains more than just our sense of hot and cold. Temperature is operationally defined as the quantity measured with a thermometer. Furthermore, temperature is...
Thermal expansion and Thermal stress: Problem Solving01:27

Thermal expansion and Thermal stress: Problem Solving

San Francisco's Golden Gate Bridge is exposed to temperatures ranging from -15 °C to 40 °C. At its coldest, the main span of the bridge is 1275 m long. Assuming that the bridge is made entirely of steel, what is the change in its length between these temperatures?
To solve the problem, first, identify the known and unknown quantities. The initial length (L) of the bridge is 1275 m, the coefficient of linear expansion (α) for steel is 12 x 10-6/°C, and the change in temperature (ΔT) is 55 °C.

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相关实验视频

Updated: Jul 12, 2026

Thermal Limits Determination for Zooplankton Using a Heat Block
07:16

Thermal Limits Determination for Zooplankton Using a Heat Block

Published on: November 18, 2022

在全新世纪期间,多个热最大值.

O K Davis

    Science (New York, N.Y.)
    |August 10, 1984
    PubMed
    概括

    气候变化的天文学理论表明,与传统观点不同的是,Holocene的多个热最大值. 生态系统的反应揭示了基于气候变量和季节的不同温度最大时间.

    科学领域:

    • 古气候学 古气候学
    • 气候变化的天文学理论
    • 全新纪的气候动力学.

    背景情况:

    • 传统的全新纪气候变化模型认为,大约在6000年前,单一的热极限发生了.
    • 气候变化的天文学理论假设周期性热最大值与季节性阳光照射变化有关.
    • 地球的轨道参数,特别是近日-平日关系,在22000年的周期中影响季节性日照.

    研究的目的:

    • 评估气候变化的天文学理论,作为传统的全新纪时间表的替代方案.
    • 用生态系统对不同季节气候的反应来研究全新纪热量最大的时间.
    • 将敏感于夏季初的古气候数据与反映夏季后期条件的重建进行比较.

    主要方法:

    • 分析地球轨道周期 (周日同) 和全新世纪日照模式之间的关系.
    • 利用从生态系统反应,特别是植被类型,到夏末气候的气候重建.
    • 将这些重建与敏感于初夏气候的古气候数据进行比较.

    主要成果:

    • 晚夏的阳光照射在大约5000年前达到峰值,而早夏的阳光照射在大约13,000年前达到峰值.
    • 基于生态系统的气候重建表明,与夏季初气候敏感数据相比,后期的全新世热量最大值.
    • 在爱达荷州南部,不同的植被类型在不同的全新世纪时期显示出热极值,这取决于控制的气候变量.

    更多相关视频

    Field-Based Thermal Physiology Assay: Cold Shock Recovery under Ambient Conditions
    07:54

    Field-Based Thermal Physiology Assay: Cold Shock Recovery under Ambient Conditions

    Published on: March 9, 2021

    High-Throughput Assays of Critical Thermal Limits in Insects
    06:58

    High-Throughput Assays of Critical Thermal Limits in Insects

    Published on: June 15, 2020

    相关实验视频

    Last Updated: Jul 12, 2026

    Thermal Limits Determination for Zooplankton Using a Heat Block
    07:16

    Thermal Limits Determination for Zooplankton Using a Heat Block

    Published on: November 18, 2022

    Field-Based Thermal Physiology Assay: Cold Shock Recovery under Ambient Conditions
    07:54

    Field-Based Thermal Physiology Assay: Cold Shock Recovery under Ambient Conditions

    Published on: March 9, 2021

    High-Throughput Assays of Critical Thermal Limits in Insects
    06:58

    High-Throughput Assays of Critical Thermal Limits in Insects

    Published on: June 15, 2020

    结论:

    • 天文学理论为理解多个Holocene热最大值提供了一个框架.
    • 生态系统对气候的反应对特定的季节性阳光变化敏感,导致热量最大的时间变化.
    • 在爱达荷州南部重建的全新纪气候动态支持天文气候变化理论的季节性预测.