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関連する概念動画

Specific Heat01:16

Specific Heat

The specific heat capacity of a substance refers to the energy required to increase the temperature of one gram of that substance by one degree Celcius. Specific heat capacity is often represented in calories (cal), grams (g), and degrees Celsius (oC), but can also be expressed in joules (J), kilograms (kg), and Kelvin (K), among other units.
For example, increasing the temperature of one gram of water by 1°C requires one calorie of heat energy and can be written as 1 cal/g-°C, or 4186 J/kg/K.
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...
Thermometers and Temperature Scales01:22

Thermometers and Temperature Scales

Any physical property that depends consistently and reproducibly on temperature can be used as the basis of a thermometer. For example, volume increases with temperature for most substances. This property is the basis for the common alcohol thermometer and the original mercury thermometers. Other properties used to measure temperature include electrical resistance, color, and the emission of infrared radiation.
As many physical properties depend on temperature, the variety of thermometers is...
Thermal Expansion01:22

Thermal Expansion

The expansion of alcohol in a thermometer is one of many commonly encountered examples of thermal expansion, which is the change in size or volume of a given system as its temperature changes. The most visible example is the expansion of hot air. When air is heated, it expands and becomes less dense than the surrounding air, which then exerts an upward force on the hot air to, for example, make steam and smoke rise, and hot air balloons float. The same behavior happens in all liquids and gases,...
Requirements for Human Life01:26

Requirements for Human Life

The Earth and its atmosphere have provided humans with air, water, and food, but these are not the only requirements for survival. Humans also require a specific range of temperature and pressure that the Earth and its atmosphere provides.
Oxygen
Atmospheric air is only about 20 percent oxygen, but that oxygen is a key component of the chemical reactions that keep the body alive, including the reactions that produce ATP. Brain cells are susceptible to a lack of oxygen because they require a...
Gas Solubility01:31

Gas Solubility

Gas solubility in liquids forms liquid-gas solutions, such as soft drinks, where carbon dioxide is dissolved in water, and the ocean, where the solubility of oxygen and carbon dioxide supports marine life. The ability of oceans to dissolve gases impacts weather conditions in the troposphere.However, gas-liquid interactions vary. For instance, hydrogen chloride gas is highly soluble in water, while oxygen's solubility is much lower. Because these solutions are non-ideal, Raoult’s law, which...

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関連する実験動画

Updated: Jun 29, 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

ロッスの氷棚 海温 海温

A E Gilmour

    Science (New York, N.Y.)
    |February 2, 1979
    PubMed
    まとめ

    ロス・アイスシェルフの海洋学的なデータは,中間的な水流入が360メートルの氷の融解を促していることを示しています. このプロセスは,南極の氷棚の安定性にとって極めて重要な環境凍結点に近い基礎氷層の温度を維持します.

    科学分野:

    • 海洋学 海洋学 海洋学
    • 氷河学 氷河学とは
    • 南極研究南極研究

    背景:

    • ロス氷床は,南極の氷床の重要な構成要素です.
    • 基礎氷床のプロセスを理解することは,氷の消失と海面上昇を予測するために不可欠です.
    • 過去の研究では,南極の氷棚の下には複雑な海洋氷の相互作用が示唆されている.

    研究 の 目的:

    • ロス氷床の下の熱状態と水質の特徴を調査する.
    • 氷床の基礎融解を推進する熱源を特定するために.
    • 氷と海の界面における海洋学的条件を特徴づけるために.

    主な方法:

    • 温度プロフィールを記録するために,敏感なバチサーモグラフを展開する.
    • 海洋学的な条件と熱伝導を推論するために,温度データを分析する.
    • ロス・アイスシェルフ・プロジェクト・サイト (82°22.5′S, 168°37.5′W) のサイト特有の測定.

    主要な成果:

    • 2つの異なる温度プロファイルが記録され,特定の海洋学的条件を示しました.
    • 証拠は,中間の深さでより暖かい水の流入を示唆しています.
    • 360メートルの深さでの基礎融解は, -2.14°Cの温度を維持する重要なプロセスとして特定されました.

    さらに関連する動画

    Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
    08:16

    Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine

    Published on: March 13, 2017

    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

    関連する実験動画

    Last Updated: Jun 29, 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

    Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine
    08:16

    Ice Generation and the Heat and Mass Transfer Phenomena of Introducing Water to a Cold Bath of Brine

    Published on: March 13, 2017

    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

  • 海底では,厚さ約35メートルのよく混ざった層が観察されました.
  • 結論:

    • 中間流入の水は熱源として作用し,ロス氷床の基礎融解を引き起こしている.
    • 観測された融解状態は,氷床の底部の熱安定性を維持するために極めて重要です.
    • これらの発見は,南極の氷と海洋の相互作用,そして氷床のダイナミクスへの影響に関する私たちの理解を深めています.