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addressing uncertainty in oil and natural gas industry greenhouse

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4.5.1 Round<strong>in</strong>g-off of Statistical Estimate<br />

Inappropriate round<strong>in</strong>g of the data can lead to errors <strong>in</strong> the f<strong>in</strong>al estimate. Us<strong>in</strong>g computer software, such<br />

as spreadsheets, helps the user avoid round<strong>in</strong>g dur<strong>in</strong>g <strong>in</strong>termediate steps. The estimate of emissions should<br />

be rounded to smallest unit of measure (API, 13.1.8.3, 1985). The <strong>uncerta<strong>in</strong>ty</strong> should be rounded to the<br />

same number of digits as the estimate.<br />

4.6 Assess<strong>in</strong>g Data Correlations<br />

As shown <strong>in</strong> Equations 4-5 <strong>and</strong> 4-7, the <strong>uncerta<strong>in</strong>ty</strong> propagation equation can be extended to account for<br />

<strong>uncerta<strong>in</strong>ty</strong> terms that are correlated or not <strong>in</strong>dependent. A simple way to assess if the uncerta<strong>in</strong>ties are<br />

correlated is to exam<strong>in</strong>e a graph of the uncerta<strong>in</strong>ties. If there is no pattern, the uncerta<strong>in</strong>ties are most likely<br />

<strong>in</strong>dependent. If there is a pattern to the uncerta<strong>in</strong>ties, they are not <strong>in</strong>dependent.<br />

The correlation between the uncerta<strong>in</strong>ties of two measured parameters can be calculated by apply<strong>in</strong>g the<br />

follow<strong>in</strong>g equation:<br />

r<br />

UX<br />

, UY<br />

=<br />

∑<br />

( UX − U ) ( )<br />

i X<br />

× UY −U<br />

i Y<br />

( n− 1) × s( U ) × s( U )<br />

X<br />

Y<br />

where<br />

r UxUy = the correlation coefficient of the uncerta<strong>in</strong>ties for X <strong>and</strong> Y;<br />

n = the sample size;<br />

Ux i = the uncerta<strong>in</strong>ties associated with sample po<strong>in</strong>ts from source X;<br />

U = the mean of the uncerta<strong>in</strong>ties from source X;<br />

X<br />

U = the mean of the uncerta<strong>in</strong>ties from source y;<br />

Y<br />

Uy i = the uncerta<strong>in</strong>ties associated with sample po<strong>in</strong>ts from source Y;<br />

s(U X ) = the st<strong>and</strong>ard deviation for the uncerta<strong>in</strong>ties of source X; <strong>and</strong><br />

s(U Y ) = the st<strong>and</strong>ard deviation for the uncerta<strong>in</strong>ties of source Y.<br />

(Equation 4-9)<br />

Before comb<strong>in</strong><strong>in</strong>g the data it is important to elim<strong>in</strong>ate the correlation of uncerta<strong>in</strong>ties, if possible. ISO<br />

5168:2005(E) Annex F discusses methods for mak<strong>in</strong>g measurement uncerta<strong>in</strong>ties <strong>in</strong>dependent, such as<br />

calibrat<strong>in</strong>g <strong>in</strong>struments aga<strong>in</strong>st different references <strong>and</strong> “redef<strong>in</strong><strong>in</strong>g mathematical relationships to elim<strong>in</strong>ate<br />

correlations” (ISO, 2005).<br />

Section A1.4.5 of the IPCC Good Practices document lists four sources for correlation:<br />

• Use of common activity data for several emissions estimates;<br />

• Mutual constra<strong>in</strong>ts on a group of emission estimates (such as a specified total fuel usage which<br />

provides <strong>in</strong>put to a number of processes);<br />

Pilot Version, September 2009 4-33

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