Luyện nghe bài hát At The Cyclone

Hey

At The
Two of Air
Hot and
Quik

At The
We a hit
Soda bank is not
it smells
We at the cyclone

(Hey Marian) One
Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low pressure area).[9] Cyclogenesis is an umbrella term for several different processes, all of which result in the development of sort of cyclone. It can occur at various scales, from the microscale to the synoptic scale. Extratropical cyclones form as waves along weather fronts before occluding later in their life cycle as cold core cyclones.

At The
Two of Air
Hot and
Really

At The
We a hit
bank is not scent
it badly
We Refresh at the

(Hey Marian) Two
Tropical cyclones form due to latent heat driven by significant thunderstorm activity, and are core.
[10] Mesocyclones form as warm core cyclones over land, and can lead to tornado formation.[11] Waterspouts can also from mesocyclones, but more often develop from environments of high instability and low vertical wind shear.[12] Cyclogenesis is the opposite of cyclolysis, and has an anticyclonic (high pressure system) equivalent which deals with the formation of high pressure areasAnticyclogenesis.[17]

At The
Two of Air
Hot and
Really

At The
We a hit
Soda bank is not
it smells
We Refresh at the

(Joanne Bananas) Three
The surface low has a variety of ways of forming. Topography can force a surface low when dense low-level high pressure system ridges in east of a north-south mountain barrier.[18] convective systems can spawn surface lows which are initially warm core.[19] The disturbance can grow into a wave-like formation along the front and the low will be positioned at the crest. Around the low, flow will become cyclonic, by definition.

I am
We are
My kiss the original way!

At The
Two of Air
Hot and
Really

At The
We a hit
Soda bank is not
it smells
We at the cyclone

At The
Two of Air
Hot and
Really

At The
We a hit
Soda is not scent
it badly
We at the cyclone