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Ry (t1 , t2 ) = =

104 120 #

h(t1 )

80 # #

.

E w( )w( )

21 45 24 21 45 24 21 45 24

104 120 16 104 120 16 104 120 16

h(t1 )Rwy ( , t2 )d h( )Rwy (t1 , t2 )d (443)

80 # #

the space environment between the Sun and the Earth and also about Earth s magnetosphere The causes of whistlers are generally well known today though not yet completely understood What is clear is that whistlers owe their existence to lightning storms Lightning stroke energy happens at all electromagnetic frequencies simultaneously The Earth is literally bathed in lightning-stroke radio energy from an estimated 1500 to 2000 lightning storms in progress at any given time, triggering over a million lightning strikes daily The total energy output of lightning storms far exceeds the combined power output of all man-made radio signals and electric power generated from power plants Whistlers also owe their existence to Earth s magnetic field (magnetosphere), which surrounds the planet like an enormous glove, and also to the Sun Streaming from the Sun is the Solar Wind, which consists of energy and charged particles, called ions And so, the combination of the Sun s Solar Wind, the Earth s magnetosphere surrounding the entire planet, and lightning storms all interact to create the intriguing sounds and great varieties of whistlers How do whistlers occur from this combination of natural solar-terrestrial forces Some of the radio energy bursts from lightning strokes travel into space beyond Earth s ionosphere layers and into the magnetosphere, where they follow approximately the lines-of-force of the Earth s magnetic field to the opposite polar hemisphere along ducts formed by ions streaming toward Earth from the Sun s Solar Wind Solar-Wind ions get trapped in and aligned with Earth s magnetic field As the lightning energy travels along a fieldaligned duct, its radio frequencies become spread out (dispersed) in a similar fashion to light shining into a glass prism The higher radio frequencies arrive before the lower frequencies, resulting in a downward falling tone of varying purity A whistler will often be heard many thousands of miles from its initiating lightning stroke and in the opposite polar hemisphere! Lightning storms in British Columbia and Alaska may produce whistlers that are heard in New Zealand Likewise, lightning storms in eastern North America may produce whistlers that are heard in southern Argentina or even Antarctica Even more remarkably, whistler energy can also be bounced back through the magnetosphere near.

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Rwy ( ) = Ry ( ) =

9 9

(444) (445)

80 80 # 80 80 0

.

9 9

The Fourier transforms of eqns (444-445) provide the cross power spectral density of y and w and the power spectral density of y Swy (j ) Sy (j ) = Sw (j )H(j ) = H(j )Swy (j ) = H(j )Sw (j )H(j ) (446) (447) (448)

We get a remainder of 0, so we know that x = 5 is a real root of the original cubic 9 We can write the cubic presented in Prob 8 in binomial-trinomial form on the basis of the results of the synthetic division Because x = 5 is a real root of the cubic, we know that it has a binomial factor of (x 5) In the trinomial factor, the coefficient of x 2 is 9, the coefficient of x is 24, and the stand-alone constant is 16, because those three numbers appear, in that order, in the bottom row before the remainder 0 We can now write down the entire binomial-trinomial cubic equation: (x 5)( 9x 2 24x 16) = 0 To figure out whether there are any other roots besides x = 5, we must find the discriminant of the trinomial factor If we let a2 = 9, b2 = 24, and c = 16, we can find the discriminant, d, as follows: d = b22 4a2c = ( 24)2 4 ( 9) ( 16) = 576 576 =0

In the single-input, single-output case where y and w are both scalar random variables, eqn (448) reduces to Sy (j ) = |H(j )|2 Sw (j ) (449)

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