🗊Презентация Thermodynamics of the atmosphere

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Thermodynamics of the atmosphere The atmosphere is a medium where transition of energy from one form to another constantly occurs. The branch of meteorology dealing with the general regularities of energy transformation and variation of the state of the atmosphere under influence of heat influxes is called THERMODYNAMICS OF THE ATMOSPHERE
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Thermodynamics of the atmosphere The atmosphere is a medium where transition of energy from one form to another constantly occurs. The branch of meteorology dealing with the general regularities of energy transformation and variation of the state of the atmosphere under influence of heat influxes is called THERMODYNAMICS OF THE ATMOSPHERE

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This law is also known as the law of energy conservation. It is widely used in the thermodynamics of the atmosphere. The first law of thermodynamics holds: the total amount of energy remains constant or is conserved. It is not possible for the energy to be destroyed or to arise. It can only be transformed from one form to another. For instance:
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This law is also known as the law of energy conservation. It is widely used in the thermodynamics of the atmosphere. The first law of thermodynamics holds: the total amount of energy remains constant or is conserved. It is not possible for the energy to be destroyed or to arise. It can only be transformed from one form to another. For instance:

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Thermodynamics of the atmosphere, слайд №3
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Ideal Gas An ideal gas is a theoretical gas composed of a set of randomly-moving, non-interacting point particles. The ideal gas concept is useful because it obeys the ideal gas law, a simplified equation of state
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Ideal Gas An ideal gas is a theoretical gas composed of a set of randomly-moving, non-interacting point particles. The ideal gas concept is useful because it obeys the ideal gas law, a simplified equation of state

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Thermodynamics of the atmosphere, слайд №5
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Adiabatic process Thermo dynamical process going on without energy income or outflow to a body ( )is called adiabatic process.
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Adiabatic process Thermo dynamical process going on without energy income or outflow to a body ( )is called adiabatic process.

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Thermodynamics of the atmosphere, слайд №7
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Dry adiabatic lapse rate
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Dry adiabatic lapse rate

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Thermodynamics of the atmosphere, слайд №9
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Polytropic processes Along with adiabatic processes there are more general ones known as polytropic processes. The process is called polytropic in the case as a heat influx to an air parcel is proportional to the parcel temperature variation.
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Polytropic processes Along with adiabatic processes there are more general ones known as polytropic processes. The process is called polytropic in the case as a heat influx to an air parcel is proportional to the parcel temperature variation.

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Thermodynamics of the atmosphere, слайд №11
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Thermodynamics of the atmosphere, слайд №12
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Thermodynamics of the atmosphere, слайд №13
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Thermodynamics of the atmosphere, слайд №14
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Thermodynamics of the atmosphere, слайд №15
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Criterion of the atmosphere stability
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Criterion of the atmosphere stability

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Thermodynamics of the atmosphere, слайд №17
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Thermodynamics of the atmosphere, слайд №18
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Thermodynamics of the atmosphere, слайд №19
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Thermodynamics of the atmosphere, слайд №20
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Adiabatic processes in moist but non-saturated air Suppose, a unit of non-saturated mass of air get some amount of energy dq.
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Adiabatic processes in moist but non-saturated air Suppose, a unit of non-saturated mass of air get some amount of energy dq.

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Thermodynamics of the atmosphere, слайд №22
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