Logo
Unionpedia
Communication
Get it on Google Play
New! Download Unionpedia on your Android™ device!
Free
Faster access than browser!
 

Atmospheric thermodynamics

Index Atmospheric thermodynamics

Atmospheric thermodynamics is the study of heat-to-work transformations (and their reverse) that take place in the earth's atmosphere and manifest as weather or climate. [1]

47 relations: Adiabatic process, Alfred Wegener, Atmospheric temperature, Benoît Paul Émile Clapeyron, Chemical thermodynamics, Clausius–Clapeyron relation, Cloud, Cloud physics, Convection, Coriolis force, Density, Emagram, Entropy, Equilibrium thermodynamics, Exponential function, Fluid dynamics, Fluid parcel, Frank Washington Very, Greenhouse gas, Heat, Heinrich Hertz, Humidity, Ideal gas law, Isentropic process, Jacques Charles, James Pollard Espy, John Dalton, Joseph Louis Gay-Lussac, Josiah Willard Gibbs, Mass transfer, Nicolas Léonard Sadi Carnot, Non-equilibrium thermodynamics, Parametrization (atmospheric modeling), Pascal (unit), Phase transition, Pressure, Pressure gradient, Primitive equations, Relative humidity, Rudolf Clausius, Subsidence (atmosphere), Temperature, Thermodynamic diagrams, Thermodynamics, Vapor pressure, Water vapor, Wilhelm von Bezold.

Adiabatic process

In thermodynamics, an adiabatic process is one that occurs without transfer of heat or matter between a thermodynamic system and its surroundings.

New!!: Atmospheric thermodynamics and Adiabatic process · See more »

Alfred Wegener

Alfred Lothar Wegener (–) was a German polar researcher, geophysicist and meteorologist.

New!!: Atmospheric thermodynamics and Alfred Wegener · See more »

Atmospheric temperature

Atmospheric temperature is a measure of temperature at different levels of the Earth's atmosphere.

New!!: Atmospheric thermodynamics and Atmospheric temperature · See more »

Benoît Paul Émile Clapeyron

Benoît Paul Émile Clapeyron (26 February 1799 – 28 January 1864) was a French engineer and physicist, one of the founders of thermodynamics.

New!!: Atmospheric thermodynamics and Benoît Paul Émile Clapeyron · See more »

Chemical thermodynamics

Chemical thermodynamics is the study of the interrelation of heat and work with chemical reactions or with physical changes of state within the confines of the laws of thermodynamics.

New!!: Atmospheric thermodynamics and Chemical thermodynamics · See more »

Clausius–Clapeyron relation

The Clausius–Clapeyron relation, named after Rudolf Clausius and Benoît Paul Émile Clapeyron, is a way of characterizing a discontinuous phase transition between two phases of matter of a single constituent.

New!!: Atmospheric thermodynamics and Clausius–Clapeyron relation · See more »

Cloud

In meteorology, a cloud is an aerosol consisting of a visible mass of minute liquid droplets, frozen crystals, or other particles suspended in the atmosphere of a planetary body.

New!!: Atmospheric thermodynamics and Cloud · See more »

Cloud physics

Cloud physics is the study of the physical processes that lead to the formation, growth and precipitation of atmospheric clouds.

New!!: Atmospheric thermodynamics and Cloud physics · See more »

Convection

Convection is the heat transfer due to bulk movement of molecules within fluids such as gases and liquids, including molten rock (rheid).

New!!: Atmospheric thermodynamics and Convection · See more »

Coriolis force

In physics, the Coriolis force is an inertial force that acts on objects that are in motion relative to a rotating reference frame.

New!!: Atmospheric thermodynamics and Coriolis force · See more »

Density

The density, or more precisely, the volumetric mass density, of a substance is its mass per unit volume.

New!!: Atmospheric thermodynamics and Density · See more »

Emagram

An emagram is one of four thermodynamic diagrams used to display temperature lapse rate and moisture content profiles in the atmosphere.

New!!: Atmospheric thermodynamics and Emagram · See more »

Entropy

In statistical mechanics, entropy is an extensive property of a thermodynamic system.

New!!: Atmospheric thermodynamics and Entropy · See more »

Equilibrium thermodynamics

Equilibrium Thermodynamics is the systematic study of transformations of matter and energy in systems in terms of a concept called thermodynamic equilibrium.

New!!: Atmospheric thermodynamics and Equilibrium thermodynamics · See more »

Exponential function

In mathematics, an exponential function is a function of the form in which the argument occurs as an exponent.

New!!: Atmospheric thermodynamics and Exponential function · See more »

Fluid dynamics

In physics and engineering, fluid dynamics is a subdiscipline of fluid mechanics that describes the flow of fluids - liquids and gases.

New!!: Atmospheric thermodynamics and Fluid dynamics · See more »

Fluid parcel

In fluid dynamics, within the framework of continuum mechanics, a fluid parcel is a very small amount of fluid, identifiable throughout its dynamic history while moving with the fluid flow.

New!!: Atmospheric thermodynamics and Fluid parcel · See more »

Frank Washington Very

Frank Washington Very (1852 – November 23, 1927) was a U.S. astronomer.

New!!: Atmospheric thermodynamics and Frank Washington Very · See more »

Greenhouse gas

A greenhouse gas is a gas in an atmosphere that absorbs and emits radiant energy within the thermal infrared range.

New!!: Atmospheric thermodynamics and Greenhouse gas · See more »

Heat

In thermodynamics, heat is energy transferred from one system to another as a result of thermal interactions.

New!!: Atmospheric thermodynamics and Heat · See more »

Heinrich Hertz

Heinrich Rudolf Hertz (22 February 1857 – 1 January 1894) was a German physicist who first conclusively proved the existence of the electromagnetic waves theorized by James Clerk Maxwell's electromagnetic theory of light.

New!!: Atmospheric thermodynamics and Heinrich Hertz · See more »

Humidity

Humidity is the amount of water vapor present in the air.

New!!: Atmospheric thermodynamics and Humidity · See more »

Ideal gas law

The ideal gas law, also called the general gas equation, is the equation of state of a hypothetical ideal gas.

New!!: Atmospheric thermodynamics and Ideal gas law · See more »

Isentropic process

In thermodynamics, an isentropic process is an idealized thermodynamic process that is both adiabatic and reversible.

New!!: Atmospheric thermodynamics and Isentropic process · See more »

Jacques Charles

Jacques Alexandre César Charles (November 12, 1746 – April 7, 1823) was a French inventor, scientist, mathematician, and balloonist.

New!!: Atmospheric thermodynamics and Jacques Charles · See more »

James Pollard Espy

James Pollard Espy (or the Storm King) (May 9, 1785 – January 24, 1860) was a U.S. meteorologist.

New!!: Atmospheric thermodynamics and James Pollard Espy · See more »

John Dalton

John Dalton FRS (6 September 1766 – 27 July 1844) was an English chemist, physicist, and meteorologist.

New!!: Atmospheric thermodynamics and John Dalton · See more »

Joseph Louis Gay-Lussac

Joseph Louis Gay-Lussac (also Louis Joseph Gay-Lussac; 6 December 1778 – 9 May 1850) was a French chemist and physicist.

New!!: Atmospheric thermodynamics and Joseph Louis Gay-Lussac · See more »

Josiah Willard Gibbs

Josiah Willard Gibbs (February 11, 1839 – April 28, 1903) was an American scientist who made important theoretical contributions to physics, chemistry, and mathematics.

New!!: Atmospheric thermodynamics and Josiah Willard Gibbs · See more »

Mass transfer

Mass transfer is the net movement of mass from one location, usually meaning stream, phase, fraction or component, to another.

New!!: Atmospheric thermodynamics and Mass transfer · See more »

Nicolas Léonard Sadi Carnot

Nicolas Léonard Sadi Carnot (1 June 1796 – 24 August 1832) was a French military engineer and physicist, often described as the "father of thermodynamics".

New!!: Atmospheric thermodynamics and Nicolas Léonard Sadi Carnot · See more »

Non-equilibrium thermodynamics

Non-equilibrium thermodynamics is a branch of thermodynamics that deals with physical systems that are not in thermodynamic equilibrium but can be described in terms of variables (non-equilibrium state variables) that represent an extrapolation of the variables used to specify the system in thermodynamic equilibrium.

New!!: Atmospheric thermodynamics and Non-equilibrium thermodynamics · See more »

Parametrization (atmospheric modeling)

Parameterization in a weather or climate model within numerical weather prediction is a method of replacing processes that are too small-scale or complex to be physically represented in the model by a simplified process.

New!!: Atmospheric thermodynamics and Parametrization (atmospheric modeling) · See more »

Pascal (unit)

The pascal (symbol: Pa) is the SI derived unit of pressure used to quantify internal pressure, stress, Young's modulus and ultimate tensile strength.

New!!: Atmospheric thermodynamics and Pascal (unit) · See more »

Phase transition

The term phase transition (or phase change) is most commonly used to describe transitions between solid, liquid and gaseous states of matter, and, in rare cases, plasma.

New!!: Atmospheric thermodynamics and Phase transition · See more »

Pressure

Pressure (symbol: p or P) is the force applied perpendicular to the surface of an object per unit area over which that force is distributed.

New!!: Atmospheric thermodynamics and Pressure · See more »

Pressure gradient

In atmospheric science (meteorology, climatology and related fields), the pressure gradient (typically of air, more generally of any fluid) is a physical quantity that describes in which direction and at what rate the pressure increases the most rapidly around a particular location.

New!!: Atmospheric thermodynamics and Pressure gradient · See more »

Primitive equations

The primitive equations are a set of nonlinear differential equations that are used to approximate global atmospheric flow and are used in most atmospheric models.

New!!: Atmospheric thermodynamics and Primitive equations · See more »

Relative humidity

Relative humidity (RH) is the ratio of the partial pressure of water vapor to the equilibrium vapor pressure of water at a given temperature.

New!!: Atmospheric thermodynamics and Relative humidity · See more »

Rudolf Clausius

Rudolf Julius Emanuel Clausius (2 January 1822 – 24 August 1888) was a German physicist and mathematician and is considered one of the central founders of the science of thermodynamics.

New!!: Atmospheric thermodynamics and Rudolf Clausius · See more »

Subsidence (atmosphere)

Subsidence, in the Earth's atmosphere, is most commonly caused by a low temperature.

New!!: Atmospheric thermodynamics and Subsidence (atmosphere) · See more »

Temperature

Temperature is a physical quantity expressing hot and cold.

New!!: Atmospheric thermodynamics and Temperature · See more »

Thermodynamic diagrams

Thermodynamic diagrams are diagrams used to represent the thermodynamic states of a material (typically fluid) and the consequences of manipulating this material.

New!!: Atmospheric thermodynamics and Thermodynamic diagrams · See more »

Thermodynamics

Thermodynamics is the branch of physics concerned with heat and temperature and their relation to energy and work.

New!!: Atmospheric thermodynamics and Thermodynamics · See more »

Vapor pressure

Vapor pressure or equilibrium vapor pressure is defined as the pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases (solid or liquid) at a given temperature in a closed system.

New!!: Atmospheric thermodynamics and Vapor pressure · See more »

Water vapor

No description.

New!!: Atmospheric thermodynamics and Water vapor · See more »

Wilhelm von Bezold

Johann Friedrich Wilhelm von Bezold (June 21, 1837 – February 17, 1907) was a German physicist and meteorologist born in Munich, Kingdom of Bavaria.

New!!: Atmospheric thermodynamics and Wilhelm von Bezold · See more »

References

[1] https://en.wikipedia.org/wiki/Atmospheric_thermodynamics

OutgoingIncoming
Hey! We are on Facebook now! »