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From page 8...
... 2-1 CHAPTER 2. Technical Reference 2.1.
From page 9...
... 2.1.1. Sou The the rocket 2.1.1 for the sou its total th Ridge Re between f 2014]
From page 10...
... 2.1.1 a static en of the rela 2012; Buc rocket exh airflow. C descendin velocity d the differe which red typically g a forward 2.1.1 specific d receiver.
From page 11...
... 2.1.1 observer m by the m frequency identical During a sound as explained crest is em slightly le successive source of from the reducing t where a) moving a frequency sound lev frequencie FIGURE for highe velocity < 2.1.2.
From page 12...
... procedure standard. 2.1.2 provide a accurately to ground receiver a ground m energy to Embleton wind and included i ground wh FIGURE 2.1.2.4.
From page 13...
... FIGURE set distan 2-6 Measu ces from th FIGURE red versus p e launch pad 2-7 Measur redicted laun - (right) Ma ed versus pr ch vehicle n ximum OAS edicted laun oise exposur PL at set di ch vehicle no e levels - (le stances from ise time hist ft)
From page 14...
... 2.2. Soni The [Plotkin e model inc operations  C  A  H  B F An e tourism th ship at sl descends down" mo powered a flight dur SpaceShip characteri FIGURE The includes b presented and signa metrics ca 2.2.1.
From page 15...
... the length sketched recompres between. Figu shown at perspectiv perspectiv later time always as associated azimuths.
From page 16...
... Follo crossing a the associ the focus Focal zon properly r booms, bu FIGURE Figu associated moderate steep dive elliptical where des ray cone h vertical la ground un FIGU wing rays is nd tracing o ated isopemp region. Ther es are genera epresent.
From page 17...
... 2-10 2.2.1.2. Vehicle Source Characteristics Sonic booms are the wave field of a supersonic vehicle, as heard on the ground.
From page 18...
... 2-11 FIGURE 2-17 Logical flow of sonic boom calculations. There are additional elements to sonic boom computation which must be considered under certain circumstances: Prediction and Computation of Focal Zone Signatures.
From page 19...
... 2-12 in PCBoom. The main ray tracing and signature aging module, FOBoom, calculates signatures with thin shocks.
From page 20...
... FIGURE N-wav Laun As underexpa F-function parameter 1975] the universal parameter Hyp The Tiegerman It is best u weight an assumes a did not ge 2.2.2.2 P Soni signature propagate is based orthogona tracing yi 2-18 F-fun e, based on s ch Vehicle M part of the nded rocket for the veh s are based ory with dra plume mod s.
From page 21...
... Figu cone that independe interest on plane con 1972] calc Acou Cons where P sound spe assumptio The amplitude including substitute phase fun FIGUR re 2-21 illustr is orthogona nt variables: that ray con taining the fl ulated boom stics and th ider a sound  trp , r is a spati ed.
From page 22...
... 2-15 however, the limit  is taken, such that the acoustic wavelength is small compared to the gradient scales of unperturbed flow quantities, the following two equations are obtained [Blokhintzev, 1946]
From page 23...
... The diagonally a quantity local unit sectional a Ellip Trad flat Earth where pro gradients. boom car distances examples capability section an scheme th al., 2010]
From page 24...
... point of t sketched i x,y that c offset to t an initial r Schu Beca There are trajectorie Schulten relation fo where q i somewhat and the ra Equa natural ch integratio derivative layered sc surface. G easy to ex he x axis is n Figure 2-2 an be related he ellipsoid)
From page 25...
... routines a are compu Prov origins an step sizes Later ellipses si the spatia Admittanc sample ra types of o 2.2.2.3 S As a signatures rather tha the local s Prop where p waveform Figu When a p become si The wave. Wh for weak shock.
From page 26...
... 2-19 implemented in two steps: an "age parameter" that defines how much the wave has steepened, and a general area balance procedure. The Age Parameter Sonic boom propagation may be summarized by the linear solution [Witham, 1956]
From page 27...
... Area A ge [Middleto The key to balance o handling process fo Figu integral o regions. points of o complex Equation equal that shocks wi similar m iterating t Midd integral o where  shocks fo it can evo between s intersectio coalescen Haye piecewise the differe Balance an neral signatu n et al., 196 this method f the F-funct multiple cros r its applicat re 2-25 illus f the F-funct Each region verlapping f signatures is (14)
From page 28...
... 2-21     Fs1 (17) The equivalent of Equation (16)
From page 29...
... 2-22 point will thus move in space, and in two dimensions will trace out a line. This line (or surface in three dimensions)
From page 30...
... 2-23 As noted, Pmax is the traditional measure of the amplitude of N-wave booms. CSEL is specified by standards [ANSI, 1996]

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