🗊 Презентация Moist adiabatic processes

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Moist adiabatic processes, слайд №1 Moist adiabatic processes, слайд №2 Moist adiabatic processes, слайд №3 Moist adiabatic processes, слайд №4 Moist adiabatic processes, слайд №5 Moist adiabatic processes, слайд №6 Moist adiabatic processes, слайд №7 Moist adiabatic processes, слайд №8 Moist adiabatic processes, слайд №9 Moist adiabatic processes, слайд №10 Moist adiabatic processes, слайд №11 Moist adiabatic processes, слайд №12
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Moist adiabatic processes An adiabatic process in moist, saturated air is called MOIST ADIABATIC PROCESS This process is significantly different form...
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Moist adiabatic processes An adiabatic process in moist, saturated air is called MOIST ADIABATIC PROCESS This process is significantly different form that in the dry or non-saturated air

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Moist adiabatic processes, слайд №2
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Moist adiabatic processes, слайд №3
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First law of thermodynamics for the moist, saturated air Suppose a parcel of the saturated air has got some amount of heat dq. This heat will be laid...
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First law of thermodynamics for the moist, saturated air Suppose a parcel of the saturated air has got some amount of heat dq. This heat will be laid out for: Inner energy increase Expansion work Evaporation of some amount of water Reason for evaporation

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Moist adiabatic processes, слайд №5
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Moist adiabatic processes, слайд №6
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Moist adiabatic processes, слайд №7
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Moist adiabatic processes, слайд №8
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Criterion of instability for the moist air
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Criterion of instability for the moist air

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Some additional information Equivalent-potential temperature is the potential temperature of an air parcel, the water vapor containing in it had been...
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Some additional information Equivalent-potential temperature is the potential temperature of an air parcel, the water vapor containing in it had been condensed due to adiabatic ascent and the heat obtained has been laid out to rise up the air parcel temperature,

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Some additional information The pseudopotential temperature(Θp.p) is a combination of the air temperature and the humidity. Θp.p is the temperature...
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Some additional information The pseudopotential temperature(Θp.p) is a combination of the air temperature and the humidity. Θp.p is the temperature that an air mass package will have after condensation and falling out of all water vapour due to upward motion followed by dry adiabatic downward motion to the starting position. In practise the combination of Θp.p and the wind barbs should be used.

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If we have a convergence in an area with relatively high tpspot we should be aware to convection or even severe thunderstorms.Although we have that...
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If we have a convergence in an area with relatively high tpspot we should be aware to convection or even severe thunderstorms.Although we have that parameter only for 2m-values the following thresholds can be used as guidlines: - tpspot < 50°C: thunderstorms not likely, - 50°C > tpspot < 60°C: thunderstorms possible, - 60°C > tpspot < 70°C: thunderstorms likely (partly severe), - 70°C > tpspot < 80°C: severe thunderstorms, - tpsopot > 80°C: extreme thunderstorms

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