The roles of imbalances for divergent and rotational modes in atmospheric flows
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The roles of imbalances for divergent and rotational modes in atmospheric flows
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The roles of imbalances for divergent and rotational modes in atmospheric flows

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CC Attribution 3.0 Germany:
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2019

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English

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Abstract 
A threedimensional general balanced solution to the governing equations of the atmosphere is given. The deviation from this balanced, or inactive, wind solution is called the active wind. For the horizontal components, this active wind is comparable to the ageostrophic wind. The vertical active wind component is similar to the isentropic displacement vertical wind. Transformed governing equations are derived as functions of the active wind components. This is also possible for the vorticity and divergence equations, respectively. It turns out that the classical balance equation is not part of the transformed divergence equation, but reflects the balanced part which had been removed. The terms on the right of the transformed equations can be scrutinized with respect to their effects on the evolution of the atmospheric state. Exemplarily, this is done for an idealized baroclinic wave in a dry atmosphere. The different terms on the right of the transformed equations and the active wind components are visualised and interpreted in their meaning. Most importantly, the newly introduced vertical active wind component allows for an analysis of the vertical motion of isentropes. The baroclinic wave development is discussed with focus on the fronts and the generation or depletion of kinetic energy. The new method allows for a unique separation of gravity waves and vortical modes. This facilitates the analysis of gravity wave generation and propagation from jets and fronts.

00:00
Presentation of a group
Numeral (linguistics)
00:15
Mass flow rate
Logic
Chemical equation
Divergence
Algebraic structure
Mach's principle
00:40
Dynamical system
Characteristic polynomial
Gradient
Chemical equation
Vector potential
Rotation
Wave
Divergence
Mathematics
Invariant (mathematics)
Gravitation
Vertical direction
Gravitation
Aerodynamics
Thermodynamics
02:02
Slide rule
Chemical equation
Multiplication sign
Price index
Food energy
Term (mathematics)
Vector potential
Friction
Function (mathematics)
Vector space
Nichtlineares Gleichungssystem
Iteration
Absolute value
Bernoulli number
Pressure
02:25
Slide rule
Functional (mathematics)
Dynamical system
Multiplication sign
Maxima and minima
Price index
8 (number)
Vector potential
Mach's principle
Plane (geometry)
Atomic number
Term (mathematics)
Vector space
Aerodynamics
Nichtlineares Gleichungssystem
Pressure
Mass flow rate
Chemical equation
Gradient
Food energy
Price index
Term (mathematics)
Measurement
Permutation
Vector potential
Function (mathematics)
Kinetische Gastheorie
Absolute value
Bernoulli number
Pressure
Daylight saving time
04:00
Mass flow rate
Closed set
Chemical equation
Multiplication sign
Price index
Food energy
Term (mathematics)
Vector potential
Pi
Function (mathematics)
Vector space
Phase transition
Kinetische Gastheorie
Absolute value
Aerodynamics
Pressure
04:40
Price index
Food energy
Term (mathematics)
Mereology
Vector potential
Equations of motion
Different (Kate Ryan album)
Term (mathematics)
Function (mathematics)
Vector space
Kinetische Gastheorie
Nichtlineares Gleichungssystem
Absolute value
Aerodynamics
Nichtlineares Gleichungssystem
Bernoulli number
Pressure
Daylight saving time
05:29
Momentum
Euclidean vector
Manysorted logic
Term (mathematics)
Mass flow rate
Vertical direction
Nichtlineares Gleichungssystem
Nichtlineares Gleichungssystem
Pressure
06:10
Standard deviation
Mass flow rate
Chemical equation
Multiplication sign
Connectivity (graph theory)
Physical law
Line (geometry)
Mereology
Wind wave
Graph coloring
Mach's principle
Different (Kate Ryan album)
Velocity
Phase transition
Vertex (graph theory)
Nichtlineares Gleichungssystem
Boundary value problem
Pressure
Physical system
08:59
Velocity
Vector space
Kinetische Gastheorie
Vertical direction
Aerodynamics
Food energy
Musical ensemble
Boundary value problem
Wind wave
Mach's principle
09:17
Multiplication sign
Algebraic structure
Mereology
Shift operator
Graph coloring
Mach's principle
Residual (numerical analysis)
Velocity
Average
Vector space
padische Zahl
Standard deviation
Distribution (mathematics)
Mass flow rate
Chemical equation
Food energy
Line (geometry)
Wind wave
Vector potential
Wave
Arithmetic mean
Velocity
Kinetische Gastheorie
Vertex (graph theory)
Vertical direction
Energy level
11:10
Standard deviation
Distribution (mathematics)
Chemical equation
Modulform
Algebraic structure
Algebraic structure
Term (mathematics)
Wind wave
Shift operator
Variable (mathematics)
Rotation
Mach's principle
Divergence
Residual (numerical analysis)
Velocity
Gravitation
Vertical direction
Nichtlineares Gleichungssystem
Aerodynamics
Energy level
Pressure
11:42
Momentum
Direction (geometry)
Modulform
Rotation
Variable (mathematics)
Mach's principle
Vortex
Mathematics
Manysorted logic
Term (mathematics)
Velocity
Vector space
Divergence
Gravitation
Aerodynamics
Nichtlineares Gleichungssystem
Pressure
Mass flow rate
Term (mathematics)
Divergence
Velocity
Vector space
IRIST
Vertex (graph theory)
Vertical direction
Nichtlineares Gleichungssystem
Turbulence
Flux
13:21
Modulform
Zeitdilatation
Term (mathematics)
Cartesian coordinate system
Mereology
Variable (mathematics)
Cartesian coordinate system
Divergence
Velocity
Vector space
Autoregressive conditional heteroskedasticity
Vector space
Divergence
Gravitation
Vertical direction
Gravitation
Nichtlineares Gleichungssystem
Aerodynamics
Pressure
14:15
Vector graphics
Mereology
Wind wave
Graph coloring
Order of magnitude
Rotation
Wave
Divergence
Complex number
Vector space
Order (biology)
Gravitation
Vertical direction
Gravitation
Nichtlineares Gleichungssystem
Nichtlineares Gleichungssystem
Block (periodic table)
15:29
Modulform
Likelihood function
Variable (mathematics)
Rotation
Vortex
Wave
Term (mathematics)
Gravitation
Physical law
Aerodynamics
Pressure
Mass flow rate
Projective plane
Vector graphics
Line (geometry)
Mortality rate
Price index
Term (mathematics)
Wind wave
Divergence
Velocity
Vertical direction
Gravitation
Nichtlineares Gleichungssystem
Flux
16:27
Wave
Divergence
Helmholtz decomposition
Gravitation
Nichtlineares Gleichungssystem
Mereology
Thermodynamics
Term (mathematics)
Force
Rotation
Flux
00:01
so the topic of my talk is not numerics but I think it is important to presenters here because Interscience to light on what we are doing and I a P and
00:12
it it also focuses on a on
00:15
the importance of what this balanced and what a smart arbitration molds and what are divergent mode in atmospheric flows and I think about what to see these structures familiar to true to and therefore I thought the I think is saying something about
00:33
balances and of logical modes and along this could be also interesting for people who are here so
00:43
we are on in atmospheric dynamics and which is a kind of threw it at room and guests which is on 1 of us and therefore we have to consider who we are as far as so we are on a specific and gravity and therefore we have to think about to good to we all enough we should not forget about gravity and then what we should not forget about is found with someone dynamics and these are the the principles to shape our atmospheric motions and and 2 disk I'd also a to flow which is balanced so what does balance in the atmosphere is the 1 of the questions we want to ask and this talk and the and then we want to ask the question what but people use if they are all at this balance the how does the what is it evolve holders' divergent evolve and how they'll they'll do vertical motions involved and and if we are in balance nothing that happened we will not have any changes and what is it no changes in the divergent and know changes in the heat of or in in temperature will no changes in temperature so and
02:04
what is the concept of to balance solution is that we are writing down or atmospheric iterations as we know them and then we say OK what is a balance we have put a very everything which is friction and heating and we say we want to be stationary and then all what this happens just does not change in
02:21
time all the slides here balanced and so we can have such a
02:27
solution and the solution is just this that the solution and this is given here it's a gradient of the potential temperature therefore day the 1st love summer dynamics or at least all off had to do was the temperature is important so it's a gradient of 2 potential temperature times in rated of Tibetan the function and a divided by the atoms potential what is achieved so that means and others potential what is it is the Coriolis force in depend on the function is the as the gravid he entered the 1st of summer than it is expressed by this term 10 town but so now we have to this kind of these kind of equations and this kind of steady solution for the wind and also for the pressure of I do not want to say something about this ideas I indexes is a general measure a whole to say how imbalanced as an atmospheric flow
03:28
but I wanted to make you aware of and attentive to apply and of which is not quite known because usually if you talk about balances and yet was serious say OK again we have the geostrophic balance and we have to hydrostatic balance but what we are usually usually doing is we define the geostrophic balance on the plane all of which is the horizontal plane all which are you which which is actually there was something said plane but to dispel solution which I have written down on the previous slide here
04:03
but it also contains the fact that if house if we have a balanced solution then this balance solution must be found on an ISO attacked us face so on an idea about take of the on an idea about and this is in in in atmospheric close this is the potential temperature and ordered to Fayyad so phase of the same potential temperature so it means all flow is not balanced on the on the horizontal plane if if you have on the same time also the temperature in the play other
04:42
no defined transformed the creations in which we just and try to move a former late hour the equations of motion and the 1st of summer than makes independent on on the active wind which is the the difference between the actual wind and this a native all balanced solution and and this is what we get you that he that means we have removed all of the other parts of the equations which I balance so here we
05:19
have the 3 terms of which might have some parts which I balance so if you add them up they may add and up to serial
05:29
and here and these equations we have made this balanced part invisible and therefore all equations so do look a bit different especially in the momentum equation we have only Sweden instead of much more terms and this term here is so small that we can forget about and followers sort of motion so what it means to me draw the main driving term of all atmospheric motions as this the term which looks like a generalized core you as far as much as infect yup just 1 of the significant of forcing term in atmospheric flows of yeah and but as I said
06:11
the main difference of it is a balanced solution is that and has a vertical
06:18
component and this is what I wanted to show you here is the the color but the color shading is known a high at OFTA's isentropic so faced so do this through so face years no here and and plotted in the defined experiment of for the different types so the way you can see that that do balanced flawed part which is balanced that flows exactly on this black lines CEO which are depend really lines antecedent he's been really eyes lines go up and down and they do to laws and you go to the cells and so on and the interesting thing is no auditory see that this balance solution has a vertical component so was goes up and down but it cannot cool but down all the time even though it is barely eyes lines they crossed the so face you know at the end to end downfall to ideas fuel can no longer follow these generally eyes alliance because it hits the ground and they are the flow cannot be any longer balanced and what I have plotted in what it's like to call us Mr. of vertically in difference that means this is the balanced part off to the the balance part this is the Vedic part of this balanced solution here that would and if is negative out dispensed mint wants to go follow to what's the problem but this is not possible because at the who abundantly we have 2 vertical velocity secret to see what this means of while the active in solid deviation from the balance must be must going up here and it must going down here this and that and that means that the call as just a flashing over the so face and rising die Central and this is the whole of volcanic instability and it's actually working so all or where systems are just about trying to make to make does ISO so phase less steep as what it means our all our who color someone to flush intruders also so it wants to become less steep and at the same time that they have to rush over the ground and therefore a be shifted up and this is what we can see
09:01
here and this is the actual of the spectral band when where you mainly see that the idea of into goes up and down of you on the
09:16
size and trope them but did active
09:20
part which makes that makes that our atmosphere is evolving this is only governed by it is kind of a the black contour CEO pay you can see that upward movement this year and don't but movement is C and of what movement and if you think that it will fill is mainly going from west to east and you can see that the the green lines which are the ice and I central they just shift it here along by pushing them down on this eastern side and pushing them up wonders western side and therefore
10:00
in the end if you're looking but what our atmosphere padic flow is doing this even in the initial time the half the size and troops which others shit to this the dashed lines you know there are quite steeped in the poem in the mid latitudes and after the passage of a Bauer Clinic wave d use I send troops have a different shape with those of the solid line and they are both shifted up what's you know and shifted downwards here and this is indicated by the mean the deviation from this and in actively and if you would just plot the actual average after vertical velocity we would get this those color shading here and you would see that the wind is going down here and going up here but it does all in balance and therefore it does not change and the distribution of to potential temperature or anything else and then I have also I
11:15
wanted to say is this is what I wanted to say about its temperature structure which is governed by the deviation of off to of what good to do what I have
11:28
discussed here was the the related to the deviation of the vertical wind from the balanced amend and and distribution of about a given from the balance and go governs the temperature distribution in
11:43
atmosphere and no we are interested also in what governs the vorticity and what governs the divergencies and atmosphere and we can rewrite that Our transformed equations in terms of the vorticity and a divergency creation and we see that we have only about 1 forcing terms for both the what is it the equation and a divergent exploration and D forcing terms the vorticity flux yeah the horizontal vorticity flux and a vertical advection term for momentum and this this this seat age as the voice the vector what his city and this is mainly EU or DVD over the set so it's a a change in the velocity so that means they have mainly true only to drive us for the was sort of velocity equation and if if this vector here is divergent then it would drive toward his city and if this vector here is quotation and ended with a drive the divergent and so you can discriminate so you can see that the same vector governs both the what is a and 2 directions and today you can imagine and strongly turbulent fluid flow have an imprint on both the vorticity and divergent now let's look on
13:19
a DEC of the divergent
13:24
and what is achieved that the divergent and dilatation of this G. back of this vector here here you
13:33
see it but I of quotation is part of the spectra and which is the application of part of this vector at the end of the wood Haitian of this and you see that as an imprint of the of the gravity vase which you can see here and here you see the divergency of this vector and the red and the divergent part of Office vector and you see that is it forces the what is city and yeah that and so you can see that the same vector governs bolus the what is achieved and divergent of and you you can
14:17
see this in the different tied you see gravity waves are moving up it onto the stratosphere and also order what is it passed the book sold of what is it did that part which was is the what is it equation has also an imprint on the same scale as and 2 divergent part has so that means the order of magnitude is a bit smaller for the what is a key part but it does that at the same the locations s in the real parts the what is it you forcing is still not drawn so therefore we can
14:58
also received now dear movement of a gravity base which are divergent part of 2 forcing into the Borgia part of the phones imposing isn't colors and you can see that the relative base and move up into the stratosphere or they can also move against the vendor along of fronts so you have different and no you can ask yourself because this of forcing to here this
15:33
vorticity flux term projects on both the vorticity and divergent so can I ask
15:38
perhaps if Duflo is strongly nonlinear den the likelihood that it forces of bowl was the what is it and a divergent is large and this is what you for instance here the the shaded black con here did the black dashed lines day indicator forcing for the vorticity and a callout our indicator forcing for the divergent and to see whether what is city forcing is large at the front and you also that he checked that gravity rates and this is what we want to know and all of research we want to know where the gravity vase to come from and obviously the nonlinearity of to flow is the most important aspect they have yeah it's
16:30
thank
16:33
you you know