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where R = p and p = [ 1 , x2 , x3 ] x If G, p, p, and p are each represented along the geographic frame north, east, and down axes, then pn = [0, 0, R] (1119)

111 GRAVITATION AND SPECIFIC FORCE and eqn (1118) reduces to Gn pn 1 0 GM 0 1 R3 0 0 0 0 2

When the Oracle Database receives a SQL statement that can be executed in parallel, and when parallelism is enabled for that instance, the parallel execution process begins, as shown in Figure 2-11 In first step of parallel processing, the server process running the statement becomes the parallel query coordinator, shown as QC in the diagram The QC is responsible for distributing and coordinating work among the parallel server processes, shown as PX in the diagram The query coordinator communicates with the parallel servers through a pair of buffers and, in most cases, the parallel servers communicate with each other through another set of buffers

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Continuing to neglect the ie ie p term from eqn (1114), we have 1 0 0 g 0 1 0 pn (1121) gn = R 0 0 2 where g = GM and gn = [ gn , ge , gd ] R2 The e ect of the gravity error on the velocity error dynamics is considered in detail in Section 1143 In that section, the vertical component of the position error is height above the ellipse h, not error in the down component d of the geodetic vector The fact that h = d inserts one extra negative sign in the error analysis of that section 1 0 0 n g 0 1 0 e (1122) gn = R 0 0 2 h The following two paragraphs brie y discuss simple models for the horizontal and vertical error dynamics The purpose is to introduce the important e ects that gravity has on the inertial system navigation systems In the navigation frame, the lateral position error di erential equations can be represented as = gn + n n = ge + e e where all error sources other than those due to gravity are combined into the terms n and e The full error model that de nes n and e will be discussed in Section 1141 From eqn (1122), gn = g n and ge = R g R e; therefore, the dependence of the lateral position error on the gravity error has the form + n g n R g + e e R = n = e

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Now that you know the basics of parallelism in Oracle, we can walk through a couple of examples of parallelism in action The first example is a simple table scan, as shown in this SQL statement:

which are forced harmonic oscillators with natural frequency equal to the g Schuler frequency s = R If the gravity error terms were absent, then the lateral position errors would be the pure integral of the errors n and

e We see that the gravity error terms in the lateral dynamics have a stabilizing e ect Because they are small and stable, they are often dropped in the error analysis For the vertical error dynamics, the situation is di erent The vertical position error di erential equation can be written as d = gd + d

SELECT * FROM customers;

where d represent all other error sources except for those due to gravity g and from eqn (1121) we have gd = 2 R d Therefore, the vertical position error model is g d 2 d = d R

g This system has eigenvalues at 2 R where the positive eigenvalue shows that the vertical error dynamics due to gravity error are unstable Even though this eigenvalue is small, because the e ect of the gravity error on the system is destabilizing, the e ect of gravity error on the vertical dynamics cannot be neglected in the overall error analysis in Section 1143

100,000 C$5,000,000 500,000 S$1,000,000 $100,000 100,000 100,000 500,000 200,000 $100,000 $100,000 $200,000 $100,000

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