rotary spectra

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Rotary Spectra Separate vector time series (e.g., current or wind data) into clockwise and counter-clockwise rotating circular components. Instead of having two Cartesian components (u, v) we have two circular components (A - , - ; A + , + ) Suppose we have de-meaned u and v components of velocity, represented by Fourier Series (one coefficient for each frequency): These can be written in complex form (dropping subindices and summation) as: n n n n n n n n n n ) t sin( d ) t cos( c ) t ( v ) t sin( b ) t cos( a ) t ( u ) t sin( d ) t cos( c i ) t sin( b ) t cos( a iv u w ) t sin( ) id b ( ) t cos( ) ic a (

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Rotary Spectra. Separate vector time series (e.g., current or wind data) into clockwise and counter-clockwise rotating circular components . Instead of having two Cartesian components ( u , v ) we have two circular components ( A - ,  - ; A + ,  + ) - PowerPoint PPT Presentation

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Page 1: Rotary  Spectra

Rotary SpectraSeparate vector time series (e.g., current or wind data) into clockwise and counter-clockwise rotating circular components.

Instead of having two Cartesian components (u, v) we have two circular components (A-, - ; A+, + )

Suppose we have de-meaned u and v components of velocity, represented by Fourier Series (one coefficient for each frequency):

These can be written in complex form (dropping subindices and summation) as:

nnnnn

nnnnn

)tsin(d)tcos(c)t(v

)tsin(b)tcos(a)t(u

)tsin(d)tcos(ci)tsin(b)tcos(a ivuw

)tsin()idb()tcos()ica(

Page 2: Rotary  Spectra

Now write w as a sum of clockwise and counter-clockwise rotating components:

Remember: e i t = cos(t) + i sin( t) rotates counter-clockwise in the complex plane, and e -i t = cos( t) – i sin( t) rotates clockwise.

Equating the coefficients of the cosine and sine parts, we find:

)tsin(i)AA()tcos()AA(

)tsin(i)tcos(A)tsin(i)tcos(A eAeAw titi

idbAAiicaAA

)bc(idaA

)bc(idaA

2121

dibAAicaAA

)tsin()idb()tcos()ica(w

dibAAicaAA

A- A+

Page 3: Rotary  Spectra

Magnitudes of the rotary components :

The - and + components rotate at the same frequency but in opposite directions.

→ Sometimes they will reinforce each other (pointing in the same direction) and sometimes they will oppose each other (pointing in opposite direction) tending to cancel each other.

2

122

2122

2121

bcdaA

bcdaA

Major axis = (A++ A-)

minor axis = (A+- A-)

)bc(idaA

)bc(idaA

2121

Page 4: Rotary  Spectra

21

21

:phase

:norientatio

dabctan

dabctan

1

1

where:

Major axis = (A++ A-)

minor axis = (A+- A-)

tN

AS

tNAS

2

2

and the components of the rotary spectrum:

Page 5: Rotary  Spectra

La Paz Lagoon, Gulf of California

Small minor axisOriented ~40º from EastSlope ~ 0.84

uv

Page 6: Rotary  Spectra

abcd

nnnnn

nnnnn

)tsin(d)tcos(c)t(v

)tsin(b)tcos(a)t(u

2/2/

2/2/

)/2sin(2)/2cos(2

)/2cos(2)/2cos(2

N

nn

N

nn

N

nn

N

nn

NnjvN

dNnjuN

b

NnjvN

cNnjuN

a

Page 7: Rotary  Spectra

22

22

dc

ba

Fourier Coefficients

Page 8: Rotary  Spectra

tN

AS

tNAS

2

2

2

122

2122

2121

bcdaA

bcdaA

S+ S-

Page 9: Rotary  Spectra

S+

S-

Fortnightly(0.068 cpd)

Page 10: Rotary  Spectra

S+S-

Page 11: Rotary  Spectra

21 :norientatio

dabctan

dabctan

1

1

where:

Page 12: Rotary  Spectra

Major axis = (A++ A-)

minor axis = (A+- A-)

Page 13: Rotary  Spectra

SSSSr

Ellipticity = minor / major

Page 14: Rotary  Spectra

Examples:

Miles Sundermeyer notes (U MASS)

Page 15: Rotary  Spectra

Examples:

Miles Sundermeyer notes (U MASS)

Page 16: Rotary  Spectra

Examples:

Miles Sundermeyer notes (U MASS)

Page 17: Rotary  Spectra

Examples:

Miles Sundermeyer notes (U MASS)