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Maturity Transformation and Interest Rate Risk in Large European ...

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Table 6: Percentage change <strong>in</strong> the value of an <strong>in</strong>dividual loan contract for various shock sizes, maturities<strong>and</strong> methods. Subtable (a) uses the Basel Committee guidel<strong>in</strong>e method, (b) uses the simplest flat yieldcurve loan pric<strong>in</strong>g model, (c) uses a model based on Nelson-Siegel forward rates calibrated to historicalparameters, <strong>and</strong> (d) uses Svensson forward rates also calibrated to historical parameter values. In eachsubtable the rows give the size of the shock, which is a parallel shift <strong>in</strong> the level of the forward curve,<strong>and</strong> the columns give the rema<strong>in</strong><strong>in</strong>g maturity of the loan contract.(a) Basel Committee guidel<strong>in</strong>e1 3 10 15 20 30-3.0% 2.1 6.8 19.9 26.8 33.6 39.0-2.0% 1.4 4.5 13.3 17.8 22.4 26.0-1.0% 0.7 2.2 6.6 8.9 11.2 13.0-0.5% 0.4 1.1 3.3 4.5 5.6 6.50.0% -0.0 -0.0 -0.0 -0.0 -0.0 -0.00.5% -0.4 -1.1 -3.3 -4.5 -5.6 -6.51.0% -0.7 -2.2 -6.6 -8.9 -11.2 -13.02.0% -1.4 -4.5 -13.3 -17.8 -22.4 -26.03.0% -2.1 -6.8 -19.9 -26.8 -33.6 -39.0(c) Nelson-Siegel (β 0 , β 1 , β 2 , τ 1 ) = (3.2, −.7, 4.5, 73)%1 3 10 15 20 30-3.0% 1.5 4.4 14.5 21.5 28.2 41.1-2.0% 1.0 3.0 9.6 14.1 18.5 26.7-1.0% 0.5 1.5 4.8 7.0 9.1 13.0-0.5% 0.2 0.7 2.4 3.5 4.5 6.40.0% 0.0 0.0 0.0 0.0 0.0 0.00.5% -0.2 -0.7 -2.3 -3.4 -4.4 -6.21.0% -0.5 -1.5 -4.7 -6.8 -8.8 -12.32.0% -1.0 -2.9 -9.3 -13.4 -17.2 -23.83.0% -1.5 -4.4 -13.8 -19.8 -25.3 -34.7(b) Flat rate δ = 3.2%1 3 10 15 20 30-3.0% 1.5 4.4 14.1 20.5 26.5 37.3-2.0% 1.0 2.9 9.3 13.5 17.4 24.1-1.0% 0.5 1.5 4.6 6.7 8.5 11.7-0.5% 0.2 0.7 2.3 3.3 4.2 5.80.0% 0.0 0.0 0.0 0.0 0.0 0.00.5% -0.2 -0.7 -2.3 -3.3 -4.1 -5.61.0% -0.5 -1.5 -4.5 -6.5 -8.2 -11.12.0% -1.0 -2.9 -9.0 -12.8 -16.1 -21.53.0% -1.5 -4.4 -13.4 -18.9 -23.7 -31.3(d) Svensson (β 0 , β 1 , β 2 , β 3 , τ 1 , τ 2 ) = (2.1, 1.1, 1.8, 5.5, 65, 855)%1 3 10 15 20 30-3.0% 1.5 4.6 18.7 29.2 38.0 49.9-2.0% 1.0 3.1 12.4 19.3 25.1 32.8-1.0% 0.5 1.5 6.2 9.6 12.4 16.1-0.5% 0.2 0.8 3.1 4.8 6.2 8.00.0% 0.0 0.0 0.0 0.0 0.0 0.00.5% -0.2 -0.8 -3.1 -4.7 -6.1 -7.91.0% -0.5 -1.5 -6.1 -9.4 -12.2 -15.62.0% -1.0 -3.1 -12.1 -18.7 -24.1 -30.83.0% -1.5 -4.6 -18.0 -27.9 -35.7 -45.44.2 How good is the Basel Committee <strong>in</strong>terest rate sensitivity guidel<strong>in</strong>efor loans?4.2.1 Effect of loan-specific pric<strong>in</strong>gThe Basel Committee guidel<strong>in</strong>es outl<strong>in</strong>ed <strong>in</strong> Section 1.1 do not take <strong>in</strong>to account the type of securityfor which an <strong>in</strong>terest rate risk assessment is be<strong>in</strong>g performed. In particular, the guidel<strong>in</strong>es may or maynot be suitable for typical loan contracts. We <strong>in</strong>vestigate the performance of the Basel Committeeguidel<strong>in</strong>e method for <strong>in</strong>terest rate revaluation sensitivity by compar<strong>in</strong>g it to our alternative simpleloan pric<strong>in</strong>g models of Section 3.2 with parametric forward curves specified <strong>in</strong> 3.3. The results aresummarised <strong>in</strong> Table 6. Under all methods, positive <strong>in</strong>terest rate shocks (<strong>in</strong>creases <strong>in</strong> the level of theforward curve) result <strong>in</strong> decreases <strong>in</strong> the value of a loan contract with any maturity, <strong>and</strong> decreases<strong>in</strong> <strong>in</strong>terest rates result <strong>in</strong> revaluation <strong>in</strong>creases. <strong>Large</strong>r absolute <strong>in</strong>terest rate shocks result <strong>in</strong> largeabsolute changes <strong>in</strong> value.The Basel Committee guidel<strong>in</strong>e method, like any duration-based sensitivity method 28 , producessensitivities that are symmetric about zero: positive <strong>and</strong> negative <strong>in</strong>terest rate shocks of equal absolutesize have an equal absolute revaluation effect; <strong>in</strong> other words, for any given loan maturity, thepercentage decrease <strong>in</strong> loan price from an <strong>in</strong>terest rate <strong>in</strong>crease is the same as the percentage <strong>in</strong>crease<strong>in</strong> loan price from an <strong>in</strong>terest rate decrease of equal absolute size. We can see that all the alternativesimple loan models, however, are able to capture the asymmetric revaluation effect of <strong>in</strong>terest ratechanges. At short maturities <strong>and</strong> for small shock sizes, these asymmetric effects are negligibly small,while at longer maturities <strong>and</strong> at larger shock sizes we note that loan prices are more sensitive todecreases <strong>in</strong> <strong>in</strong>terest rates. It is not surpris<strong>in</strong>g, therefore, that the Basel Committee guidel<strong>in</strong>e methodsometimes overstates, <strong>and</strong> at other times understates, the <strong>in</strong>terest rate sensitivity of loan prices.From the regulator’s po<strong>in</strong>t of view, we might be most concerned with situations where the Basel28 For an <strong>in</strong>troduction to duration-based sensitivity measurement, see Kaufman (1984).21

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