Biorthogonal decomposition: Difference between revisions
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This is not always the most appropriate assumption: | This is not always the most appropriate assumption: | ||
e.g., travelling waves have a structure such as ''cos(kx-ωt)''; however, most propagating waves can still be recognised clearly by their distinct footprint in the biorthogonal modes (provided there are not too many): a travelling wave will produce a pair of modes with similar amplitude and a 90° phase difference. | e.g., travelling waves have a structure such as ''cos(kx-ωt)''; however, most propagating waves can still be recognised clearly by their distinct footprint in the biorthogonal modes (provided there are not too many): a travelling wave will produce a pair of modes with similar amplitude and a 90° phase difference. | ||
== Relation with signal correlation == | |||
The correlation between signals ''j<sub>1</sub>'' and ''j<sub>2</sub>'' is defined as: | |||
:<math>C(j_1,j_2) = \sum_i {Y(i,j_1)Y(i,j_2)},\!</math> | |||
Using the above expansion of ''Y'' and the orthogonality relations, it is easy to show that the topos ''φ<sub>k</sub>'' are the eigenvectors of the correlation matrix ''C'', and ''λ<sub>k</sub><sup>2</sup>'' the corresponding eigenvalues. | |||
== See also == | == See also == |
Revision as of 19:58, 19 March 2010
The Biorthogonal Decomposition (BOD, also known as Proper Orthogonal Decomposition, POD) applies to the analysis of multipoint measurements
where i=1,...,N is a temporal index and j=1,...,M a spatial index (typically). The time traces Y(i,j) for fixed j are usually sampled at a fixed rate; however the measurement locations x(j) need not be ordered in any specific way.
The BOD decomposes the data matrix as follows:
where ψk is a 'chrono' (a temporal function) and φk a 'topo' (a spatial or detector-dependent function), such that the chronos and topos satisfy the following orthogonality relation
The combination chrono/topo at a given k, ψk(i) φk(j), is called a spatio-temporal 'mode' of the fluctuating system, and is constructed from the data matrix without any prejudice regarding the mode shape. The λk are the eigenvalues (sorted in decreasing order), where k=1,...,min(N,M), and directly represent the square root of the fluctuation energy contained in the corresponding mode. This decomposition is achieved using a standard Singular value decomposition of the data matrix Y(i,j). Thus, the oscillations of the spatiotemporal fluctuating field are represented by means of a very small number of spatio-temporal modes that are constructed from the data themselves, without prejudice regarding the mode shape. [1]
A limitation of the technique is that it assumes space-time separability. This is not always the most appropriate assumption: e.g., travelling waves have a structure such as cos(kx-ωt); however, most propagating waves can still be recognised clearly by their distinct footprint in the biorthogonal modes (provided there are not too many): a travelling wave will produce a pair of modes with similar amplitude and a 90° phase difference.
Relation with signal correlation
The correlation between signals j1 and j2 is defined as:
Using the above expansion of Y and the orthogonality relations, it is easy to show that the topos φk are the eigenvectors of the correlation matrix C, and λk2 the corresponding eigenvalues.