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#1
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Does anyone know the answer to the following?
http://actuary.ca/phpBB/viewtopic.php?t=40523 Your help would be much appreciated! Thank you! |
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#2
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Quote:
dx = a(x, t)dt + b(x, t)dz then an application of Ito's Lemma proves that: dy = y [(a(ln y, t) + 1/2 b^2(ln y, t))dt + b(ln y, t)dz]. While exactuary is correct about terminology (geometric brownian motion is defined to have constant drift and volatility), the above SDE for y is certainly a generalization of GBM. Working from the other direction, if x = ln y, and: dy = a(y, t)dt + b(y, t)dz, then: dx = (a(e^x, t) - 1/2 b^2(e^x, t))dt + b(e^x, t)dz]. The confusing thing about this is the fact that, for SDEs, dy / y != d ln y; those expressions are equivalent only for ODEs. In general, exponentiating a general Ito process results in something that looks like a generalized GBM with an upward drift adjustment, while taking the log of a general Ito process results in another general Ito process (which looks nothing like a GBM) with a downward drift adjustment. And, yes, there are interest rate models in use which assume time varying drift and volatility.
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