October 23rd, 2002, 2:21 pm
Firstly, if F(t,T) = E* [ S(T) ] , then you can still have peaks and troughs - the forwards will rise and fall in just the same way as we expect the spot to rise and fall.What I think you are referring to is the equation F(t,T)=S(t)e^(r(T-t))This only allows the sinusoidal behaviour of which you speak if you generalise to F(t,T)=S(t)e^(r-u+c)(T-t)where r is the interest rate, c is the cost of storage, and u is the convenience yield (defined as the benefit accruing to the holder of the asset but not to the holder of the forward). Although in reality all of r, u and c will be time dependent.In summer, all the gas is being stored, so the cost of storage goes up. Likewise, the convenience of having physical gas is pretty low - it isn't as if there is suddenly going to be a shortage. So c goes up and u goes down, and the forward price falls. So the forward price of gas at the start of winter (after the long summer) is higher than the spot price at the start of summer. Giving the desired result.At an extreme, think of electricity during a spike. The spot price is $10,000, while the forward price for the next day is $40. The reason for this is that the benefit of having electricity now (the convenience yield) is enormous, and the storage cost is virtually zero, as no one in their right mind would want to store it, rather than selling it now.In some ways, the convenience yield isn't quantifiable in itself - it is just a balancing entry to give the desired relationship between spot prices and forward prices at different times. If you take this view - well, then, you always get exactly the shape you want.