All time components of the perturbation vanish. For this immediately givesFor a spatial index ,by the stated property. Thus the perturbation is transverse.
Its Minkowski trace is purely spatial:Adding the displayed components and collecting the coefficients of the independent functions , , and makes each coefficient vanish separately, soTogether with and , this proves that the wave is in transverse-traceless gauge.
On the positive axis, and . Taking this limit in the spatial components giveswith evaluated at retarded time . A wave propagating toward the observer along the direction has polarization matrixConsequently the observed gravitational wave polarization amplitudes areThe mode and the orthogonal combination of do not contribute on this symmetry axis. The observer therefore sees a purely plus-polarized wave; a rotation of the transverse axes would represent the same physical polarization as the corresponding spin-two mixture of plus and cross.
Articles by others on the same topic
There are currently no matching articles.