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Extreme Times in Finance. J . Masoliver, M. Montero and J. Perelló Departament de Fisica Fonamental Universitat de Barcelona. Financial Makets: two levels of description. Tick-by-tick data. “Microscopic” description. Continuous Time Random Walk. “Mesoscopic” description.
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Extreme Times in Finance J. Masoliver, M. Montero and J. Perelló Departament de Fisica Fonamental Universitat de Barcelona
Financial Makets:two levels of description Tick-by-tick data • “Microscopic” description Continuous Time Random Walk • “Mesoscopic” description Daily, weekly... data Diffusion processes Stochastic Volatility Models
I - CTRW formalism • First developed by Montroll and Weiss (1965) • Aimed to study the microstructure of random processes • Applications: transport in random media, random networks, self-organized criticallity, earthquake modeling, and… now in financial markets
CTRW dynamics • The log-return and the zero-mean return: J. Masoliver, M. Montero, G.H. Weiss Phys. Rev E 67, 021112 (2003)
Return distribution • Objective • Renewal equation joint distribution of increments and waiting times • Formal solution
a) If they are independent: b) If they are positively correlated. Some choices: Are jumps and waiting times related to each other?
Approach to theGaussian density Long-tailed jump density: Lévy distribution At intermediate times: the tail behavior is given by extreme jumps General Results • Normal diffusion
Extreme Times • At which time the return leaves a given interval [a,b] for the first time? • Mean Exit Time (MET): J. Masoliver, M. Montero, J. Perelló Phys. Rev. E 71, 056130 (2005)
Integral Equation for the MET • is the mean time between jumps. • The MET does NOT depend on • the whole time distribution • the coupling between jumps and waiting times • Mean First Passage Time (MFPT) to a certain critical value:
An exact solution • Laplace(exponential) distribution: jump variance: • Exact solution: • Symmetrical interval It is also quadratic in L • For the Laplace pdf the approximate and • the exact MET coincide
Approximate solution • We need to specify the jump pdf • We want to get a solution as much general as possible • We get an approximate solution when: • the interval L is smaller than the jump variance • jump pdf is an even function and zero-mean with scaling:
Some Generalizations • Introduction of correlations by a Markov-chain model. • Assuming jumps are correlated: • Integral equation for the MET: M. Montero, J. Perelló, J. Masoliver, F. Lillo, S. Miccichè, R.N. Mantegna Phys. Rev. E, 72, 056101 (2005).
A two-state Markov chain model r = correlation between the magnitude of two consequtive jumps Integral equation Difference equations
Solution mid-point: • Scaling time Large values of L Stock independent
tick-by-tick data of 20 highly capita- lized stocks traded at the NYSE in the 4 year period 95-98; more than 12 milion transactions.
II – Stochastic Volatility models • “Low frequency” data (daily, weekly,...) Diffusion models Geometric Browinian Motion (Einstein-Bachelier model) • The assumption of constant volatility does not properly • account for important features of the market Stochastic Volatility Models
Two-dimensional diffusions Wiener processes
1. The Ornstein-Uhlenbeck model E. Stein and J. Stein, Rev. Fin. Studies 4, 727 (1991). J. Masoliver and J. Perelló, Int. J. Theor. Appl. Finance 5, 541 (2002).
2. The CIR-Heston model Cox, J., Ingersoll, J., and S. Ross, (1985a), Econometrica, 53, 385 (1985). S. Heston, Rev. Fin. Studies 6, 327 (1993). A. Dragulescu and V. Yakovenko, Quant. Finance 2, 443 (2002).
3. The Exponential Ornstein-Uhlenbeck model J.-P. Fouque, G. Papanicolau and K. R. Sircar, Int. J. Theor. Appl. Finance 3, 101 (2002). J. Masoliver and J. Perelló, Quant. Finance (2006).
In SV models the volatility proces is described by a one-dimensional diffusion • The OU model: • The CIR-Heston model: • The ExpOU model:
Extreme times for the volatility process • The MFPT to certain level ( reflecting) • Averaged MFPT
Scaling normal level of the volatility 1 - OU model 2 - CIR-Heston model 3- ExpOU model
Some analytical results 1 - OU model Assymptotics
2 - CIR-Heston model Kummer’s function of first kind Assymptotics
3 - ExpOU model Kummer’s function of second kind Assymptotics
Empirical Data Nomal Level (daily volatility) 1- DJIA: 0.71 % 2- S&P-500: 0.62 % 3- DAX: 0.84 % 4- NIKKEI: 0.96 % 5- NASDAQ: 0.78 % 6- FTSE-100: 0.77 % 7- IBEX-35: 0.96 % 8- CAC-40: 1.02 % Financial Indices 1- DJIA: 1900-2004 (28545 points) 2- S&P 500: 1943-2003 (15152 points) 3- DAX: 1959-2003 (11024 points) 4- NIKKEI: 1970-2003 (8359 points) 5- NASDAQ: 1971-2004 (8359 points) 6- FTSE-100: 1984-2004 (5191 points) 7- IBEX-35: 1987-2004 (4375 points) 8- CAC-40: 1983-2003 (4100 points)
Conclusions (I) • The CTRW provides insight relating the market microstructure with the distributions of intraday prices and even longer-time prices. • It is specially suited to treat high frequency data. • It allows a thorough description of extreme times under a very general setting. • MET’s do not depend on any potential coupling between waiting times and jumps. • Empirical verification of the analytical estimates using a very large time series of USD/DEM transaction data. • The formalism allows for generalizations to include price correlations.
Conclusions (II) • The “macroscopic” description of the market is quite well described by SV models. • Many SV models allow a analytical treatment of the MFPT. • The MFPT may help to determine a suitable SV model • OU and CIR-Heston models yield a quadratic behavior of the MFPT for small volatilities that is not conflicting with data. For large volatilities their exponential growth does not agree with data. • In a first approximation the ExpOU model seems to agree with data for both small and large volatilities.
Comparison with the Wiener Process • The Laplace MET is larger than the MET • when return follows a Wiener process: • We conjecture that this is true in any situation: • The Wiener process underestimates the MET. • Practical consequences for risk control and • pricing exotic derivatives.
The Wiener process underestimates the MET