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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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Related Experiment Video

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

Ross ice shelf sea temperatures.

A E Gilmour

    Science (New York, N.Y.)
    |February 2, 1979
    PubMed
    Summary
    This summary is machine-generated.

    Oceanographic data from the Ross Ice Shelf reveals that intermediate water inflow drives ice melting at 360 meters. This process sustains a basal ice layer temperature near the ambient freezing point, crucial for Antarctic ice shelf stability.

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    Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
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    Published on: June 8, 2015

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    Area of Science:

    • Oceanography
    • Glaciology
    • Antarctic Research

    Background:

    • The Ross Ice Shelf is a critical component of the Antarctic ice sheet.
    • Understanding basal ice-shelf processes is vital for predicting ice loss and sea-level rise.
    • Previous studies have suggested complex ocean-ice interactions beneath Antarctic ice shelves.

    Purpose of the Study:

    • To investigate the thermal regime and water mass characteristics beneath the Ross Ice Shelf.
    • To identify the heat source driving basal melting of the ice shelf.
    • To characterize the oceanographic conditions at the ice-ocean interface.

    Main Methods:

    • Deployment of a sensitive bathythermograph to record temperature profiles.
    • Analysis of temperature data to infer oceanographic conditions and heat transfer.
    • Site-specific measurements at the Ross Ice Shelf Project site (82°22.5′S, 168°37.5′W).

    Main Results:

    • Two distinct temperature profiles were recorded, indicating specific oceanographic conditions.
    • Evidence suggests an inflow of warmer water at intermediate depths.
    • Basal melting at 360 meters depth was identified as a key process, maintaining temperatures around -2.14°C.
    • A well-mixed layer approximately 35 meters thick was observed at the seabed.

    Conclusions:

    • Intermediate water inflow acts as a heat source, driving basal melting of the Ross Ice Shelf.
    • The observed melting regime is crucial for maintaining the thermal stability of the ice shelf base.
    • These findings enhance our understanding of ice-ocean interactions in Antarctica and their impact on ice shelf dynamics.