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関連する概念動画

Maxwell-Boltzmann Distribution: Problem Solving01:20

Maxwell-Boltzmann Distribution: Problem Solving

Individual molecules in a gas move in random directions, but a gas containing numerous molecules has a predictable distribution of molecular speeds, which is known as the Maxwell-Boltzmann distribution, f(v).
This distribution function f(v) is defined by saying that the expected number N (v1,v2) of particles with speeds between v1 and v2 is given by
Heat Flow and Specific Heat01:12

Heat Flow and Specific Heat

Heat is a type of energy transfer that is caused by a temperature difference, and it can change the temperature of an object. Since heat is a form of energy, its SI unit is the joule (J). Another common unit of energy often used for heat is the calorie (cal), which is defined as the energy needed to change the temperature of 1 g of water by 1 °C, specifically between 14.5 °C and 15.5 °C, since the energy needed shows a slight temperature dependence. Another commonly used unit is the kilocalorie...
Conduction, Convection and Radiation: Problem Solving01:20

Conduction, Convection and Radiation: Problem Solving

There are three methods by which heat transfer can take place: conduction, convection, and radiation. Each method has unique and interesting characteristics, but all three have two things in common: they transfer heat solely because of a temperature difference; and the greater the temperature difference, the faster the heat transfer.
In order to solve a problem related to heat transfer, first of all, the situation needs to be examined to determine the type of heat transfer involved. This could...
Heat Capacities of an Ideal Gas III01:25

Heat Capacities of an Ideal Gas III

The number of independent ways a gas molecule can move along straight line, rotate, and vibrate is called its degrees of freedom. Supposing d represents the number of degrees of freedom of an ideal gas, the molar heat capacity at constant volume of an ideal gas in terms of d is
Heat Capacities of an Ideal Gas II01:23

Heat Capacities of an Ideal Gas II

For a system that undergoes a thermodynamic process at a constant volume condition, the heat absorbed is used only to increase the system's internal energy and not for doing any kind of work. While for a system undergoing a thermodynamic process under a constant pressure condition, the amount of heat absorbed is used not only for increasing the internal energy (as a function of temperature) but also for doing some work. The molar heat capacity is the amount of heat required to increase the...
Heating and Cooling Curves02:44

Heating and Cooling Curves

When a substance—isolated from its environment—is subjected to heat changes, corresponding changes in temperature and phase of the substance is observed; this is graphically represented by heating and cooling curves.
For instance, the addition of heat raises the temperature of a solid; the amount of heat absorbed depends on the heat capacity of the solid (q = mcsolidΔT). According to thermochemistry, the relation between the amount of heat absorbed or released by a substance, q, and its...

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関連する実験動画

Updated: Jul 12, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

温かいプール・ヒート・予算とショートウェーブ・クラウド・フォッシング: 物理学が欠けているのか?

V Ramanathan, B Subasilar, G J Zhang

    Science (New York, N.Y.)
    |January 27, 1995
    PubMed
    まとめ

    西太平洋の暖かいプール上の雲は,熱を反射し,閉じ込めることによって,海面の太陽放射線を大幅に減少させます. この発見は気候変動に大きな影響を及ぼし,既存の海洋熱伝送モデルに挑戦しています.

    科学分野:

    • 海洋学 海洋学 海洋学
    • 大気科学 大気科学
    • 気候科学 気候科学

    背景:

    • 船の観測と海洋モデルの調査は,西太平洋の温水池の混合層 (<20 W/m2) から発生する熱の輸出が最小であることを明らかにしています.
    • 雲の放射性効果を理解することは,正確な気候モデリングに不可欠です.

    研究 の 目的:

    • 西太平洋の暖かいプールにおける海面での太陽放射線の純量に対する雲の影響を推論する.
    • 推論されたと観測されたショートウェーブクラウドフォースの間の不一致を調査するために.

    主な方法:

    • 船舶の観測データと海洋モデルのデータを熱輸出計算に活用した.
    • 海面エネルギーバランスに基づく推論された短波雲強制.

    主要な成果:

    • 推論されたショートウェーブ雲の強制力は相当 (~ -100 W/m2),大気の上部で観測された値の1.5倍でした.
    • 雲は,反射と有意な大気吸収の両方によって,海面の太陽放射線を減らすように見える.

    結論:

    • 暖かいプールの上の雲の放射性特性は,典型的なモデル仮定とは異なる.
    • 過剰な雲の吸収は,熱帯から熱帯外への海洋熱伝送に重大な影響を及ぼします.

    さらに関連する動画

    Pool-Boiling Heat-Transfer Enhancement on Cylindrical Surfaces with Hybrid Wettable Patterns
    07:32

    Pool-Boiling Heat-Transfer Enhancement on Cylindrical Surfaces with Hybrid Wettable Patterns

    Published on: April 10, 2017

    関連する実験動画

    Last Updated: Jul 12, 2026

    Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
    13:27

    Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

    Published on: June 8, 2015

    Pool-Boiling Heat-Transfer Enhancement on Cylindrical Surfaces with Hybrid Wettable Patterns
    07:32

    Pool-Boiling Heat-Transfer Enhancement on Cylindrical Surfaces with Hybrid Wettable Patterns

    Published on: April 10, 2017