Alternative Approaches to Estimating the Linear Propagator and Fi nite-time Growth Rates from Data

Similar documents
HEAT EXCHANGER OPERATING POINT DETERMINATION. Dušan D. GVOZDENAC

TT1300 Se ries. Low Noise Matched Transister Ar ray ICs DESCRIPTION APPLICATIONS FEATURES. Microphone Preamplifiers

TEST OF TOTAL HEAT FLUX FROM WOOD CRIB FIRE IN AND OUTSIDE COMPARTMENT

Ma trix re ar range ment

NUMERICAL INVESTIGATION OF FLUID FLOW AND HEAT TRANSFER CHARACTERISTICS IN SINE, TRIANGULAR, AND ARC-SHAPED CHANNELS

NUMERICAL STUDY OF A MODIFIED TROMBE WALL SOLAR COLLECTOR SYSTEM. Snežana M. DRAGI]EVI] and Miroslav R. LAMBI]

Gi ant Res o nance in 4d Photo-Ionization and -Ex ci ta tion of High Z Atoms and Ions; Sys tem atic Study of Dy namic Elec tron-correlation

V6309/V Pin Microprocessor Reset Circuit EM MICROELECTRONIC-MARIN SA. Fea tures. Typi cal Op er at ing Con figu ra tion.

TOTAL HEAT FLUX ON THE WALL: BENCH SCALE WOOD CRIB FIRES TESTS

EXPERIMENTAL INVESTIGATION OF A FLOW AROUND A SPHERE

Evaluation of Front Morphological Development of Reactive Solute Transport Using Behavior Diagrams

EFFECT OF CHAR LAYER ON TRANSIENT THERMAL OXIDATIVE DEGRADATION OF POLYETHYLENE

HEAT-BALANCE INTEGRAL METHOD FOR HEAT TRANSFER IN SUPERFLUID HELIUM. Bertrand BAUDOUY

FINITE TIME THERMODYNAMIC MODELING AND ANALYSIS FOR AN IRREVERSIBLE ATKINSON CYCLE

Density and Partial Mo lar Volumes of Binary Mixtures for the Dimethyl Ether of a Glycol + Eth a nol from T = K to T = 318.

Tie Bar Extension Measuring Chain

EMPIRICAL CORRELATIONS TO PREDICT THERMOPHYSICAL AND HEAT TRANSFER CHARACTERISTICS OF NANOFLUIDS

HOW GOOD IS GOODMAN S HEAT-BALANCE INTEGRAL METHOD FOR ANALYZING THE REWETTING OF HOT SURFACES?

RADIATION AND CHEMICAL REACTION EFFECTS ON ISOTHERMAL VERTICAL OSCILLATING PLATE WITH VARIABLE MASS DIFFUSION

One could hardly imag ine a wide va ri ety of pro cesses in the mod ern world with out ca tal y - sis. Many pro cesses in volved in fuel con ver

EXERGOECONOMIC OPTIMIZATION OF GAS TURBINE POWER PLANTS OPERATING PARAMETERS USING GENETIC ALGORITHMS: A CASE STUDY

NUMERICAL SIMULATION FOR THERMAL CONDUCTIVITY OF NANOGRAIN WITHIN THREE DIMENSIONS

APPLICATION OF INVERSE CONCEPTS TO DRYING

THEORETICAL ANALYSIS AND EXPERIMENTAL VERIFICATION OF PARABOLIC TROUGH SOLAR COLLECTOR WITH HOT WATER GENERATION SYSTEM

MODELING THE EFFECT OF THE INCLINATION ANGLE ON NATURAL CONVECTION FROM A FLAT PLATE The Case of a Pho to vol taic Mod ule

A NOVEL METHOD FOR ESTIMATING THE ENTROPY GENERATION RATE IN A HUMAN BODY

DISPERSION MODELING FOR REGULATORY APPLICATIONS

ul. Mokhovaya 11, k. 7, Moscow, Russia, b Hydrometeorological Research Center of the Russian Federation,

ANALYSIS OF PHOTOTHERMAL RESPONSE OF THIN SOLID FILMS BY ANALOGY WITH PASSIVE LINEAR ELECTRIC NETWORKS

VA LENCE XPS STRUC TURE AND CHEM I CAL BOND IN Cs 2 UO 2 Cl 4

MIXED CONVECTION FLOW OF JEFFREY FLUID ALONG AN INCLINED STRETCHING CYLINDER WITH DOUBLE STRATIFICATION EFFECT

MI LAN P. PEŠI] Sci en tific pa per DOI: /NTRP P

THE EFFECT OF SURFACE REGRESSION ON THE DOWNWARD FLAME SPREAD OVER A SOLID FUEL IN A QUIESCENT AMBIENT

Agnese Kukela, Valdis Seglins Uni ver sity of Lat via, 10 Al berta street, Riga, LV-1010, Lat via,

A MOD ERN MATH E MAT I CAL METHOD FOR FIL TER ING NOISE IN LOW COUNT EX PER I MENTS

EFFECT OF VARIABLE VISCOSITY AND SUCTION/INJECTION ON THERMAL BOUNDARY LAYER OF A NON-NEWTONIAN POWER-LAW FLUIDS PAST A POWER-LAW STRETCHED SURFACE

Molecular Distance-Edge Vec tor ( ) and Chro mato graphic Retention In dex of Alkanes

EMPIRICAL SOOT FORMATION AND OXIDATION MODEL. Karima BOUSSOUARA and Mahfoud KADJA

SOLAR EQUIPMENT FOR PREHEATING BITUMEN

A L A BA M A L A W R E V IE W

Sa lin ity Min i mum in the Up per Layer of the Sea of Ja pan

Im pact of GPS Ra dio Occultation Refractivity Soundings on a Sim u la tion of Ty phoon Bilis (2006) upon Land fall

FIRE SUPPRESSION STUDIES

A CFD ANALYSIS OF ROOM ASPECT RATIO ON THE EFFECT OF BUOYANCY AND ROOM AIR FLOW

THEORETICAL-EXPERIMENTAL DETERMINING OF COOLING TIME (t 8/5 ) IN HARD FACING OF STEELS FOR FORGING DIES

PRODUCTIVITY ENHANCEMENT OF STEPPED SOLAR STILL PERFORMANCE ANALYSIS. V. VELMURUGAN, S. SENTHIL KUMARAN, V. NIRANJAN PRABHU, and K.

THE SPECTRAL RADIATIVE EFFECT OF Si/SiO 2 SUBSTRATE ON MONOLAYER ALUMINUM POROUS MICROSTRUCTURE

Con cen tra tion De pend ence of the Fifth-Order Two-Dimensional Raman Sig nal

Bimetal Industrial Thermometers

NUMERICAL ANALYSIS OF FORTH-ORDER BOUNDARY VALUE PROBLEMS IN FLUID MECHANICS AND MATHEMATICS

THE NATURE OF BIOLOGICAL SYSTEMS AS REVEALED BY THERMAL METHODS

Nikola V. ŽIVKOVI] *, Dejan B. CVETINOVI], Mili} D. ERI], and Zoran J. MARKOVI]

(NTS 092N; 093C, B, G, H),

AN INCREASE OF HYDRO-AGGREGATE'S INSTALLED POWER AND EFFICIENCY FACTOR BEFORE THE REVITALIZATION PHASE

1 Introduction. 2 The Problem and the present method. 2.1 The problem

Shal low S-Wave Ve loc ity Struc tures in the West ern Coastal Plain of Tai wan

The de sign and use of porous asphalt mixes

EXPERIMENTAL ANALYSIS OF FUZZY CONTROLLED ENERGY EFFICIENT DEMAND CONTROLLED VENTILATION ECONOMIZER CYCLE VARIABLE AIR VOLUME AIR CONDITIONING SYSTEM

PERSISTENCE OF THE LAMINAR REGIME IN A FLAT PLATE BOUNDARY LAYER AT VERY HIGH REYNOLDS NUMBER

THE EFECT OF POLYMERS ON THE DYNAMICS OF TURBULENCE IN A DRAG REDUCED FLOW

I/O7 I/O6 GND I/O5 I/O4. Pin Con fig u ra tion Pin Con fig u ra tion

EXPERIMENTAL INVESTIGATION OF TURBULENT STRUCTURES OF FLOW AROUND A SPHERE

Anal y sis of Tai pei Ba sin Re sponse for Earth quakes of Var i ous Depths and Locations Using Empirical Data

The Bonding Structure of Quadricyclanylidene Derivatives

EX PANDED AND COM BINED UN CER TAINTY IN MEA SURE MENTS BY GM COUN TERS

Micellar For ma tion Study of Crown Ether Surfactants

Vas cu lar elas tic ity from re gional dis place ment es ti mates

EFFECTS OF DIFFERENT MEAN VELOCITY RATIOS ON DYNAMICS CHARACTERISTICS OF A COAXIAL JET

RESEARCH IN SOLAR ENERGY AT THE POLITEHNICA UNIVERSITY OF TIMISOARA: STUDIES ON SOLAR RADIATION AND SOLAR COLLECTORS

GENERAL BUILDING HEIGHTS AND AREAS

(NTS 092N, O, 093B, C, F, G)

Geochemistry Projects of the British Columbia Geological Survey

NUMERICAL SIMULATION OF POROUS BURNERS AND HOLE PLATE SURFACE BURNERS

Cation Driven Charge Trans fer in (Co, Fe) Prus sian Blues

Laser Spectroscopic Studies of Tran si tion Metal Con taining Rad i cals

DETERMINATION OF THERMAL CONDUCTIVITY OF ROCKS SAMPLES USING FABRICATED EQUIPMENT

Introduction. Methodologies Receiver Function Analysis

For ma tion of Bacteriochlorophyll Anion Band at 1020 nm Produced by Nu clear Wavepacket Motion in Bacterial Reaction Cen ters

OH BOY! Story. N a r r a t iv e a n d o bj e c t s th ea t e r Fo r a l l a g e s, fr o m th e a ge of 9

OP TI MI ZA TION OF THE SELF-SUF FI CIENT THO RIUM FUEL CY CLE FOR CANDU POWER RE AC TORS

Velocity Models from Three-Dimensional Traveltime Tomography in the Nechako Basin, South-Central British Columbia (Parts of NTS 093B, C, F, G)

Solar Heat Worldwide Markets and Contribution to the Energy Supply 2006

Estimation of Permeability from Borehole Array Induction Measurements: Application to the Petrophysical Appraisal of Tight Gas Sands 1

BCFD a Visual Basic pro gram for cal cu la tion of the fractal di men sion of digitized geological image data using a box-counting technique

Solvent De pend ent Ultrafast Ground State Recovery Dynamics of Triphenylmethane Dyes

A new non li near DNA mo del. Un nue vo mo de lo no li neal del ADN

Evaluation of Mineral Inventories and Mineral Exploration Deficit of the Interior Plateau Beetle Infested Zone (BIZ), South-Central British Columbia

Jour nal of the Chi nese Chem i cal So ci ety, 2002, 49,

P a g e 5 1 of R e p o r t P B 4 / 0 9

SIMULATION ON MARINE CURRENTS AT MIDIA CAPE-CONSTANTA AREA USING COMPUTATIONAL FLUID DYNAMICS METHOD

Plurafac LF types. Technical Information

BUBBFIL ELECTROSPINNING OF PA66/Cu NANOFIBERS

OP TI MI ZA TION OF THE GAS FLOW IN A GEM CHAM BER AND DE VEL OP MENT OF THE GEM FOIL STRETCHER

FRAC TIONAL VARIATIONAL PROB LEMS AND PAR TI CLE IN CELL GYROKINETIC SIM U LA TIONS WITH FUZZY LOGIC AP PROACH FOR TOKA MAKS

Ap pli ca tion of Mo lec u lar Descriptors to the Pre dic tion of Re ten tion in Or ganic Sol vent Nanofiltration

Op ti mum Synthesis of Mesoporous Silica Ma te rials from Acidic Condition

Sim u la tion of Ice berg Drift as a Com po nent of Ice Mon i toring in the West Arc tic

Deep Aquifer Characterization in Support of Montney Gas Development, Northeastern British Columbia (Parts of NTS 093, 094): Progress Report

T h e C S E T I P r o j e c t

THE VEINING STRUCTURE METHOD, THE FINITE ELEMENT METHOD IN THERMAL DEFORMATION DETERMINATION FOR THE MAIN SPINDLE AT NUMERICAL CONTROL LATHES

Transcription:

Terr. Atmos. Ocean. Sci., Vol. 20, No. 2, 365-375, April 2009 doi: 10.3319/.2008.02.25.01(A) Alternative Approaches to Estimating the Linear Propagator and Fi nite-time Growth Rates from Data Yung-An Lee * and Zih-Ting Hung In sti tute of At mo spheric Phys ics, Na tional Cen tral Uni ver sity, Chung-Li, Taiwan, ROC Re ceived 3 September 2007, ac cepted 25 February 2008 AB STRACT The prop a ga tor of a lin ear model plays a cen tral role in em pir i cal nor mal mode and fi nite-time in sta bil ity prob lems. Its es ti ma tion will af fect whether the lin ear sta bil ity char ac ter is tics of the cor re spond ing dy namic sys tem can be prop erly ex tracted. In this study, we in tro duce two al ter na tive meth ods for es ti mat ing the lin ear prop a ga tor and fi nite-time growth rates from data. The first is the gen er al ized sin gu lar value de com po si tion (GSVD) and the sec ond is the sin gu lar value de com po si tion com bined with the co sine-sine de com po si tion (SVD-CSD). Both meth ods linearize the re la tion be tween the pre dic tor and the predictand by de com pos ing them to have a com mon evo lu tion struc ture and then make the es ti ma tions. Thus, the lin ear prop a ga tor and the as so ci ated sin gu lar vec tors can be si mul ta neously de rived. The GSVD clearly re veals the con nec tion be tween the fi nite-time am pli tude growth rates and the sin gu lar val ues of the prop a ga tor. How ever, it can only be ap plied in sit u a tions when given data have more state vari ables than ob ser va tions. Fur ther more, it gen er ally en coun ters an over-fit ting prob lem when data are con tam i nated by noise. To fix these two draw backs, the GSVD is gen er al ized to the SVD-CSD to in clude data fil ter ing ca pa bil ity. There fore, it has more flex i bil ity in deal ing with gen eral data sit u a tions. These two meth ods as well as the Yule-Walker equa tion were ap plied to two syn thetic datasets and the Kaplan s sea sur face tem per a ture anom a lies (SSTA) to eval u ate their per for mance. The re sults show that, be cause of linearization and flexible filtering capabilities, the propagator and its associated properties could be more accurately estimated with the SVD-CSD than other methods. Key words: Gen er al ized sin gu lar value de com po si tion, Fi nite-time in sta bil ity, Linearization Ci ta tion: Lee, Y. A. and Z. T. Hung, 2009: Al ter na tive ap proaches to es ti mat ing the lin ear prop a ga tor and fi nite-time growth rates from data. Terr. Atmos. Ocean. Sci., 20, 365-375, doi: 10.3319/.2008.02.25.01(A) 1. INTRODUCTION Waves are com mon phe nom ena in the at mo sphere and the ocean. The mech a nisms of the gen er a tion, evo lu tion, and pre dict abil ity of such phe nom ena are strongly de pend ent on the stability characteristics of these waves. Therefore, the ability to correctly extract wave stability characteristics from ob served data is very cru cial to our un der stand ing of the dynamics of the cor re spond ing sys tems. Cur rently, em - pirical sta bil ity stud ies are mainly car ried out through lin ear in verse mod el ing of the ob served spa tial-tem po ral data. In other words, one fits an ob served dataset that has m vari ables of n + tem po ral length to a dis crete form of the lin ear advection equa tion, * Cor re spond ing au thor E-mail: yalee@atm.ncu.edu.tw Y (t + ) = AY (t) (1) where Y (t) m n is the first n tem po ral length of the m vari ables (pre dic tor ma trix), Y (t + ) is the same vari ables at pe riod later (predictand ma trix), and A is the lin ear prop a ga tor. The prin ci pal os cil la tion pat tern anal y sis (POP; von Storch et al. 1995; von Storch and Zwiers 1998) ap - plies an eigenvalue-eigenfunction anal y sis to the lin ear prop a ga tor to ex tract the dom i nant nor mal mode os cil la - tions and the as so ci ated sta bil ity char ac ter is tics of the cor - re spond ing sys tem. How ever, nor mal mode in sta bil ity is not the only in sta bil ity mech a nism that op er ates in a fluid sys tem. The in ter ac tions among waves may also cause amplitudes of some per tur ba tions to growth tem po rarily even in a sys tem that is nor mal mode sta ble (Farrell and Ioannou 1996a, b). Be cause most ob ser va tional data are

366 Yung-An Lee & Zih-Ting Hung nearly sta tion ary, it is hard to as so ci ate any nor mal mode ex po nen tial growth be hav ior with them. There fore, the fi - nite-time in sta bil ity is widely ac cepted to play an equal or more im por tant role as the nor mal mode in sta bil ity in cy - clone gen e sis, pre dict abil ity, and data as sim i la tion stud ies. In such stud ies, the sin gu lar value de com po si tion (SVD; Golub and Van Loan 1996) is ap plied to the lin ear pro - pagator to ex tract the dom i nant sin gu lar vec tors and the associated fi nite-time growth rates. Be cause the lin ear pro - p a ga tor plays a cen tral role in em pir i cal nor mal mode and fi nite-time in sta bil ity prob lems, how to es ti mate it from the data will de ter mine whether the sta bil ity char ac ter is tics of the cor re spond ing sys tem can be prop erly ex tracted. Con ven tion ally, the lin ear prop a ga tor A is es ti mated using the Yule-Walker equa tion (Brockwell and Davies 1991): A = {Y (t + ) Y T (t)} {Y (t) Y T (t)} 1 (2) where su per scripts T and -1 de note the ma trix trans pose and ma trix in verse re spec tively. How ever, the pre dic tor and the predictand are gen er ally not per fectly lin early cor - re lated; i.e., their lag autocorrelations are al ways less than 1. Con se quently, the lin ear prop a ga tor so de rived gen er ally un der es ti mates the lin ear in sta bil ity of the cor re spond ing dy namic sys tem. For ex am ple, it is well known that POP anal y sis can yield only damped os cil la tion pat terns (von Storch et al. 1995). This means that us ing the Yule-Walker equa tion to es ti mate the prop a ga tor, the ob served vari abil - ity can not be fully main tained and Eq. (1) be comes a sta ble lin ear sys tem. Be cause of this, some kind of forc ing term must be added to Eq. (1) to main tain the ob served va ri - ability in the lin ear in verse model (Penland and Magorian 1993; Penland and Sardeshmukh 1995) and the Markov model (Xue et al. 1994; Xue et al. 2000). There fore, it is de - sir able to know whether an ini tial linearization of the orig i - nal data, be fore the es ti ma tion of the lin ear prop a ga tor, can al low the lin ear sta bil ity char ac ter is tics of the cor re spond - ing sys tem to be more prop erly ex tracted. Fur ther more, al - though it is well known that the sin gu lar val ues of a lin ear prop a ga tor rep re sent the non-modal av er aged am pli fi ca - tion or de cay ing rates (fi nite-time growth rates) of the cor - re spond ing lin ear dy namic sys tem in pe riod, the con nec - tion be tween them is gen er ally es tab lished through some pre de fined ma trix norms. Var i ous stud ies (Palmer et al. 1998; Kim and Mor gan 2002) have shown that dif fer ent choices of norms will yield quite dif fer ent sin gu lar vec tors. This seem ingly non-unique ness of sin gular vec tors has added con sid er ably com plex ity to the dynamic interpretation of the cor re spond ing sys tem. There fore, it is also de sir - able to es tab lish a more di rect and clearer con nec tion be - tween the sin gu lar val ues of a lin ear prop a ga tor and the fi - nite-time growth rates. In this study, we in tro duce two al ter na tive ap proaches, which orig i nate from the field of ma trix com pu ta tion, to es ti - mate the prop a ga tor, fi nite-time growth rates and the as - sociated sin gu lar vec tors from the data. Rather than us ing the autocovariance and the lag- covariance ma tri ces of the ob served data to es ti mate the prop a ga tor, these ap proaches first linearize the re la tion be tween the pre dic tor and the predictand by de com pos ing them to have the same com mon evo lu tion ma trix, and then make the es ti ma tions. Fur ther - more, these ap proaches es tab lish a di rect con nec tion be - tween the sin gu lar val ues of a lin ear prop a ga tor and the finite-time growth rates of the predictand sin gu lar vec tors. The re main der of this pa per is or ga nized as fol lows. Sec tion 2 de scribes the meth od ol ogy and prop er ties of the gen er al - ized sin gu lar value de com po si tion (GSVD; Golub and Van Loan 1996). Sec tion 3 de scribes the meth od ol ogy and pro - perties of the sin gu lar value de com po si tion (SVD) com - bined with the co sine-sine de com po si tion (CSD; Golub and Van Loan 1996). To com pare and eval u ate the rel a tive advantages of dif fer ent ap proaches, the Yule-Walker equa - tion, the GSVD and the SVD-CSD are ap plied to two syn - thetic datasets and an ob served dataset to es ti mate the cor - responding lin ear prop a ga tors and the as so ci ated prop er - ties. Sec tion 4 shows the re sults for two syn thetic datasets con sist ing of 10 nor mal mode os cil la tions plus two dif fer ent lev els of noise. Sec tion 5 shows re sults for the monthly mean sea sur face tem per a ture anom a lies (SSTA, Kaplan et al. 1998). Sec tion 6 dis cusses and sum ma rizes this study. 2. THE GENERALIZED SINGULAR VALUE DECOMPOSITION METHOD (GSVD) In the ma trix com pu ta tion field, there is a well-known the o rem called gen er al ized sin gu lar value de com po si tion (GSVD; the o rem 8.74 in Golub and Van Loan 1996). It states that, if F k q, G p q and k, p q, then there ex - ist two or thogo nal ma tri ces, U k k and V p p, and an invertible ma trix, X q q, such that: U T FX = C = diag (c 1,, c q ) 0 c 1 c 2 c q 1 (3) V T GX = S = diag (s 1,, s q ) 1 s 1 s 2 s q 0 (4) where C T C + S T S = I q and I q is a q q iden tity ma trix. There fore, a gen er al ized eigenvalue prob lem (i.e., Gx = Fx), can be di rectly solved with out the need for form ing G T G and F T F. Based on this the o rem, the pro posed GSVD method for es ti mat ing the lin ear prop a ga tor and the as so ci - ated prop er ties can be de scribed as fol lows. For the lin ear model of Eq. (1), if m n, the pre dic tor and the pre dictand ma tri ces can be de com posed us ing the GSVD as: Y (t) = UCX 1 (5) Y (t + ) = VSX 1 (6)

The Ap pli ca tion of Linearization Pro ce dure in Data Anal y sis 367 Be cause Y (t) and Y (t + ) have been re ar ranged to have the same tem po ral evo lu tion struc ture, X 1 n n, the correlation co ef fi cient be tween the time se ries of each corresponding col umn vec tor of U m m and V m m beco mes unity. There fore, the use of GSVD linearizes the re la tion be tween the pre dic tor and the predictand. The sub sti tu tion of Eqs. (5) and (6) into Eq. (1) with some ma trix manipulations then yields: A = VSC 1 U T = V U T (7) where = diag ( 1,, n ) = SC 1 = diag (s1 c,, s c ) (8) 1 n n is a di ag o nal ma trix. From Eqs. (5), (6), and (7), it is clear that the lin ear propagator can be di rectly de rived from the GSVD de com - position of the pre dic tor and the predictand with out the need to form Y(t) Y T (t) and Y(t + )Y T (t) first. Fur ther more, it is noted that the left and right sin gu lar vec tors de rived from the SVD of a given ma trix are unique up to mul ti pli ca tion of a col umn of the left sin gu lar vec tors by a unit phase fac tor and simultaneous multiplication of the corresponding column of the right sin gu lar vec tors by the same unit phase fac tor if all the sin gu lar val ues are non-de gen er ate and non-zero. As Eq. (7) is also the SVD of A, there fore if the same con di tions are met, the use of GSVD de com po si tion al lows the sin gu lar val ues and the left and right sin gu lar vec tors of the prop a ga tor to be si mul ta neously de rived. Be cause all the sin gu lar val ues de rived from ob served data are gen er ally dis tinct and nonzero, therefore the linear propagator and the associated singular vec tors de rived from the GSVD are also gen er ally unique. The unique ness of the GSVD re sults can also be readily checked by di rect cal cu la tion. For ex am ple, one can randomly generate a linear propagator A, then use Eq. (1) and an ar bi trary ini tial con di tion to gen er ate the cor re spond ing Y(t) and Y(t + ). By ap ply ing the SVD to A and the GSVD to Y(t) and Y(t + ), one can eas ily see that the GSVD de - rived lin ear pro p a ga tor and sin gu lar val ues are the same as A and its as so ci ated sin gu lar val ues, while the GSVD de rived sin gu lar vec tors are also the same as those of A ex cept for pos si ble sign re ver sal among some of the vec tors. More over, we note in Eq. (8) that the i-th sin gu lar value i is ex pressed in terms of the ra tio be tween s i and c i, which are the nor mal ized am pli tude mea sures of the i-th sin gu lar vec tor of Y(t + ) and Y(t), respectively. Therefore, the i-th sin gu lar value of the prop a ga tor di rectly and clearly rep re - sents the non-modal av er aged am pli tude am pli fi ca tion or de cay rates of the cor re spond ing lin ear sys tem in pe riod in terms of the L2 norm of the state vec tor, Y(t). Be cause dif - ferent variables generally have different spectral character - is tics, it is likely that us ing dif fer ent state vari able to de scribe the same lin ear sys tem will yield some what dif fer ent lin ear prop a ga tors and as so ci ated sin gu lar vec tors. This fea ture may par tially ex plain why dif fer ent choices of norms in pre - vi ous stud ies yielded quite dif fer ent sin gu lar vec tors. An - other sig nif i cant fea ture of the method is the ex act equal ity between Y(t + ) and AY(t); i.e., Y(t + ) = VSX 1 = VSC 1 U T UCX 1 = AY(t). This im plies that the vari abil ity of Y(t + ) can be com pletely re pro duced by AY(t). Hence, when us ing the GSVD to es ti mate the lin ear prop a ga tor, there is no need to add any un known forc ing term to Eq. (1) to main tain the ob served vari abil ity. 3. THE SINGULAR VALUE DECOMPOSITION COM BINED WITH THE CO SINE-SINE DECOMPOSITION METHOD (SVD-CSD) The above der i va tion shows that, when data have more grid points than ob ser va tions, the GSVD pro vides a di rect way to estimate the linear propagator and its associated sin - gu lar vec tors. How ever, the GSVD the o rem re quires that k, p q, there fore it can not be ap plied to data with fewer vari - ables than ob ser va tions (i.e., m < n). More im por tantly, all data are more or less con tam i nated by noise. There fore, when m n, both the GSVD and the Yule-Walker equa tion are very likely to over-fit the lin ear re la tion be tween the predictor and the predictand and lead to wrong es ti ma tions. To pre vent such an over-fit ting prob lem, it is a com mon prac tice to use only the dom i nant prin ci pal com po nents (PCs) from the prin ci pal com po nent anal y sis (PCA; Preisen - dorfer and Mobley 1988) of the orig i nal data to es ti mate the lin ear prop a ga tor. In such cases, the num ber of re tained PCs will gen er ally be much less than the ob ser va tions. There fore, we need to de velop an other ap proach to es ti mate the lin ear prop a ga tor and the as so ci ated prop er ties for m < n cases. The SVD-CSD method is ba si cally an ex ten sion of the GSVD method. In line with the der i va tion of the GSVD theorem, we first linearize Y(t) and Y(t + ), by re quir ing that they have the same evo lu tion struc ture. Con se quently, the SVD is ap plied to their oint ma trix to yield: where Q 2m 2m and R n n are or thogo nal, = diag ( 1,, f ), and f min (2m, n). If m n, the co sine-sine decom po si tion (CSD; the o rem 2.6.2 in Golub and Van Loan 1996) can be used di rectly to de com pose Q, yield ing the same de com po si tions of Y(t) and Y(t + ) as those for Eqs. (5) and (6). How ever, the CSD can not be di rectly applied to Q when m < n. In such cases, Q,, and R need to be de - (9)

368 Yung-An Lee & Zih-Ting Hung com posed into dom i nant (sub script d) and re main der (sub - script r) submatrices, based upon how many sin gu lar vec - tors need to be ex tracted or re tained. Be cause the num ber of re tained sin gu lar vec tors (N) can not ex ceed the num ber of state vari ables (m), for a given N m, then Q,, and R in Eq. (9) are fur ther de com posed into Q d1, Q d2 m N, Q r1, Q r2 m (2m N), d = diag ( 1, N ), r = diag ( N + 1,, f ), R d n N, and R r n (n N). In terms of these sub - matrices, Y(t) and Y(t + ) can also be sep a rated into Y d (t), Y r (t) and Y d (t + ), Y r (t + ), re spec tively. The or - thogonal re la tion be tween R d and R r im plies that Y d (t) and Y d (t + ) are also or thogo nal to Y r (t) and Y r (t + ). Hence, Eq. (1) can be di vided into a dom i nant equa tion and a re main der equa tion, i.e., Y d (t + ) = A d Y d (s) (10) Y r (t + ) = A r Y r (s) (11) Due to the fact that Y d (t) and Y d (t + ) rep re sent the do - minant lin ear covariability of Y(t) and Y(t + ), Eq. (10) can be viewed as a fil tered ver sion of Eq. (1). The CSD is then used to de com pose Q d1 and Q d2 to be come: (12) where U d1, U d2 m m, V d N N are or thogo nal ma tri - ces, C S and S S di ag o nal with C d T C d + S d T S d = I N. With these decom po si tions, Y d (t), Y d (t + ) and A d can be writ - ten, similar to Eqs. (5), (6), and (7), as: Y d (t) = U d1 C d V d T d R d T = U d1 C d X d 1 Y d (t + ) = U d2 S d V d T d R d T = U d2 S d X d 1 and A d = U d2 S d C d 1 U d1 T (13) (14) (15) Con se quently, when data have more state vari ables than ob ser va tions, the SVD-CSD still al lows for a di rect esti - mation of the lin ear prop a ga tor and the as so ci ated pro - perties from the fil tered pre dic tor [Y d (t)] and predictand [Y d (t + )]. Sim i larly, be cause the vari abil ity of Y d (t + ) can be com pletely re pro duced by A d Y d (t), one also does not need to add any un known forc ing term to Eq. (10) to main tain the ob served vari abil ity. The SVD-CSD can re cover the GSVD re sults when m > n and can be ap plied to m < n cases. There fore, al though slightly more com pli cated to im ple ment, the SVD-CSD has a wider range of ap pli ca bil ity. Fur ther more, if some kind of fil ter ing needs to be ap plied to the orig i nal data, the SVD-CSD has two op tions to choose from. The first is the num ber of re tained PCs (m); the sec ond is the num ber of retained sin gu lar vec tors (N). The use of a spe cific m to fil - ter data, as in the con ven tional data anal y sis, is based on the ex plained vari ance of the orig i nal data. How ever, this kind of data fil ter ing does not dif fer en ti ate whether the pre dic tor and the predictand are lin early re lated or not. There fore, some im por tant lin ear covariability be tween the pre dic tor and the predictand may be fil tered out. On the other hand, if all the PCs of the orig i nal data are re tained, the SVD-CSD can still al low data fil ter ing by se lect ing N < m. In such cases, one can as sure that the dom i nant lin ear covariability be tween the pre dic tor and the predictand will not be un - intentionally fil tered out. As for the Yule-Walker equa tion, because the re tained sin gu lar modes must be the same as the num ber of state vari ables, data fil ter ing can only be ap plied by choos ing a sub set of PCs (i.e., choos ing a spec i fied m and N = m). There fore, the SVD-CSD of fers a more se lec tive data fil ter ing mech a nism for the es ti ma tion of the lin ear prop a ga tor and the as so ci ated prop er ties. 4. THE SYN THETIC NOR MAL MODE OSCILLATIONS In the above der i va tions, we learned that both the GSVD and the SVD-CSD are ca pa ble of de riv ing the lin ear pro - pagator and the as so ci ated prop er ties di rectly from the pre - dictor and the predictand ma tri ces. How ever, their per for - mance in estimating the linear propagator and the associated sin gu lar val ues should be com pared with the con ven tional Yule-Walker equa tion to eval u ate their use ful ness. In this sec tion, we ap ply all these meth ods to two syn thetic datasets with known nor mal mode growth rates to see if they can faithfully extract the stability characteristics from the data. These syn thetic datasets are con structed as a su per po si tion of 10 nor mal mode os cil la tions con tam i nated by two dif - ferent lev els of ran dom noise on the global trop ics be tween 30 S - 30 N with 5 5 resolution, that is: 10 z( x, y, t ) cos( k x l y t ) e N ( 0, ) 1 (16) where N (0, ) de notes ran dom noise with zero mean and stan dard de vi a tion = 0.1 or = 1, k 180, l = [( 1 2( 1)] [ 1 3( 1)], with = 1,, 180 600 10, = -0, -0.001,, -0.009 is the growth rate of the th nor mal mode, x = 0, 5,, 350, 355, y = -30, -25,, 25, 30 and t = 1, 2,, 600. It is noted that each of the dataset con - sists of 936 time se ries (m = 936), with 600 time steps (n = 600) in each se ries, there fore the GSVD re stric tion is sat is - fied (i.e., m n). Fur ther more, be cause these 10 modes are t

The Ap pli ca tion of Linearization Pro ce dure in Data Anal y sis 369 or thogo nal and each is small, the fi nite-time growth rate can be ap proximately taken as 1 + if is also small. There fore, the estimated fi nite-time growth rates from the GSVD, the SVD-CSD and the Yule-Walker equa tion can be com pared to these known val ues to eval u ate their va lid ity. Re sults from the weakly ran dom noise con tam i nated syn thetic dataset (i.e., = 0.1) are shown in Figs. 1 and 2. In Fig. 1a, one clearly notes that the ex plained vari ance of the first 20 PCs are well above those of the rest of PCs. Be cause the sig nal part of the syn thetic time se ries con sti tutes 10 normal mode os cil la tions and each nor mal mode can be decomposed into a pair of equal vari ance PCs, this re sult indicates that the PCA is very ef fec tive in dif fer en ti at ing sig nal from noise in the weakly ran dom noise con tam i nated data. Fig ure 1b shows the es ti mated lag-1 ( = 1) fi nite-time growth rates us ing both the GSVD and the Yule-Walker equa tion meth ods. Be cause the GSVD and the Yule-Walker equa tion yield A 600 600 and A 936 936, respectively, the max i mum num ber of sin gu lar vec tors can be ex tracted from them are 600 and 936, re spec tively. How ever, the Yule-Walker equa tion needs to cal cu late the in verse of the auto covariance ma trix. When data have fewer ob ser va tions than grid points, the re sul tant auto covariance ma trix is singular. Hence, with the Yule-Walker equa tion, one en - counters the rank de fi ciency prob lem in ma trix in ver sion and yields un re al is ti cally large fi nite-time growth rates com - pared to the GSVD. Con versely, re sults from the GSVD showed a nearly anti-symmetrical distribution between the grow ing and de cay ing modes. Be cause C and S, as shown in Eqs. (5) and (6), are ar ranged in as cend ing and de scend ing or der be tween 0 and 1, re spec tively, this anti-sym met ri cal distribution is what one would ex pect when the vari abil ity of Y(t + 1) can be faith fully re pro duced by AY(t). Never - theless, be cause the GSVD does not have any data fil ter ing mechanism to differentiate signal from noise, it inevitably overestimates the linear relation between the predictor and the predictand. There fore it is also in ca pa ble of yield ing the cor rect re sults (i.e., the solid line sig nif i cantly de vi ates from the di a mond sym bols). Fig ure 2 shows the SVD-CSD and the Yule-Walker equa tion es ti mated lag-1 growth rates for PCA fil tered data. The SVD-CSD re sults are cal cu lated us ing 20 re tained PCs (m = 20) and re tained sin gu lar vec tors, N = 5, 10, 15, 20, respectively. The Yule-Walker equa tion re sults are cal cu - lated us ing re tained PCs m = 5, 10, 15, 20, re spec tively. One ob serves clearly that the Yule-Walker equa tion al ways over - es ti mates the de cay rates, while the SVD-CSD yields re sults over all quite sim i lar to the true de cay rates. How ever, when Fig. 1. The PCA and the es ti mated lag-1 ( = 1) fi nite-time growth rates re sults of the weakly ran dom noise con tam i nated syn thetic dataset (stan dard de vi a tion = 0.1). is the ex plained vari ance as a func tion of PC modes from PCA of the data. is the es ti mated fi nite-time growth rates as a func - tion of the sin gu lar vec tors us ing the Yule-Walker equa tion (dashed line) and the GSVD (thick solid line), re spec tively. The di a mond sym bols rep re - sent the lag-1 fi nite-time growth rates de rived from the nor mal mode growth rates of the syn thetic data (i.e., 1 + ).

370 Yung-An Lee & Zih-Ting Hung (c) (d) Fig. 2. The es ti mated lag-1 fi nite-time growth rates re sults of the weakly ran dom noise con tam i nated syn thetic dataset us ing both the SVD-CSD (thick solid line) and the Yule-Walker equa tion (dashed line) meth ods.,, (c), and (d) cor re spond to re sults from the SVD-CSD us ing 20 PCs (m = 20) and re tained sin gu lar vec tors N = 5, 10, 15, 20 and re sults from the Yule-Walker equa tion us ing 5, 10, 15, and 20 PCs (m = 5, 10, 15, 20), re spec tively. Sim i larly, The di a mond sym bols in each panel rep re sent the lag-1 fi nite-time growth rates de rived from the nor mal mode growth rates of the syn thetic data (i.e., 1 + ). the re tained sin gu lar vec tors are equal to the re tained PCs (i.e., m = N = 20), the growth rates of the first few sin gu lar vec tors tend to be over es ti mated. Note that the re tained PCs, al though be ing PCA fil tered, are still not noise-free. When m = N, be cause the SVD-CSD is un able to ap ply fur ther fil - ter ing to the data, the over es ti ma tion of the lin ear re la tion be tween the pre dic tor and the predictand in ev i ta bly leads to the over es ti ma tion of the growth rates. Fig ures 3 and 4 show re sults from the mod er ately ran - dom noise con tam i nated syn thetic dataset (i.e., = 1). In Fig. 3a, one notes that all PCs of the = 1 data have greater ex plained vari ance than those of the = 0.1 data. Fur ther - more, sig nal and noise parts of the spec tra are not as clearly sep a rated as those of the = 0.1 case. These re sults in di cate that the PCA is ineffective in differentiating signal from noise in mod er ately ran dom noise con tam i nated data. Sim i - lar to Fig. 1b, Fig. 3b also shows clearly that both the GSVD and the Yule-Walker equa tion meth ods are un able to es ti - mate the fi nite-time growth rates cor rectly from orig i nal data. These re sults strongly sug gest that one al ways needs to ap ply some kinds of data fil ter ing to cor rectly es ti mate the lin ear prop a ga tor and the as so ci ated prop er ties. Fig ure 4 shows the same as Fig. 2, ex cept for re sults of the = 1 case. One notes that the over es ti ma tion of the de cay rates by the Yule-Walker equa tion is more se ri ous than that in the = 0.1 case. On the other hand, the SVD-CSD still yields re sults quite sim i lar to the true de cay rates for re tained sin gu lar vec tors up to 15. When m = N = 20, be cause the noise level is rel a tively high and the SVD-CSD is un able to ap ply fur ther fil ter ing to the data, the over es ti ma tion of the lin ear re la tion be tween the pre dic tor and the predictand then leads to a more se ri ous over es ti ma tion of the growth rates for the first few sin gu lar vec tors. These re sults clearly sug - gest that the se lec tive data fil ter ing ca pa bil ity of SVD-CSD can yield a more cor rect es ti ma tion of the prop a ga tor and the as so ci ated fi nite-time growth rates than can the Yule-Walker equa tion. It is noted that sim i lar anal y ses were also ap plied to var i ous val ues of. Their re sults (not shown) are quite sim i lar to those of = 1. There fore, the above con clu sions are valid not ust for = 1 only. 5. SEA SURFACE TEMPERATURE ANOMALIES In this sec tion, all three meth ods are ap plied to Kaplan s SSTA data (Kaplan et al. 1998) to eval u ate their per for - mance. Kaplan s SSTA data con sist of the global gridded (5 5 ) monthly mean SSTA from Jan u ary 1856 to March 2003 (they can be found in http://ing rid.ldeo.co lum bia.edu /SOURCES/.KAPLAN/.EX TENDED). It was con structed us ing op ti mal es ti ma tion in the space of 80 PCs to in ter po -

The Ap pli ca tion of Linearization Pro ce dure in Data Anal y sis 371 Fig. 3. The same as Fig. 1, ex cept for re sults of the mod er ately ran dom noise con tam i nated syn thetic data (stan dard de vi a tion = 1). For com par i son, the PCA re sult of the = 0.1 (dashed line) is also shown in. (c) (d) Fig. 4. The same as Fig. 2, ex cept for re sults of the mod er ately ran dom noise con tam i nated syn thetic data (stan dard de vi a tion = 1).

372 Yung-An Lee & Zih-Ting Hung late ship ob ser va tions from the UK Met Of fice da ta base (Parker et al. 1994). The data af ter 1981 rep re sents the pro - ec tion of the NCEP OI anal y sis (which com bines ship ob - ser va tions with re mote sens ing data) by Reynolds and Smith (1994) on the same set of 80 PCs. In this study, only trop i cal ocean (27.5 S - 27.5 N) data be tween the years 1950 and 2002 are used. The re sults (not shown) from ap ply ing the GSVD and the Yule-Walker equa tion to the orig i nal data are sim i lar to those in Fig. 1 and still are un able to yield cor rect esti - mations. The es ti mated max i mum lag-1 fi nite-time growth rates for the PCA fil tered Kaplan s SSTA from both the SVD-CSD (m = 80) and the Yule-Walker equa tion as a function of the re tained sin gu lar modes are shown in Fig. 5. Results from both the Yule-Walker equa tion and the SVD- CSD show monotonically in creas ing growth rates with re - tained sin gu lar vec tors. Nev er the less, those from the Yule- Walker equa tion have lower growth rates than those for the SVD-CSD. As can be seen in Fig. 5b, no in sta bil ity can be found in the re sults from the Yule-Walker equa tion for re - tained sin gu lar vec tors less than 4. Does the Yule-Walker equa tion un der es ti mate the growth rates? Fig ure 6 shows the es ti mated fi nite-time growth rates for the PCA fil tered Ka - plan s SSTA from both the SVD-CSD and the Yule-Walker equa tion as a func tion of the sin gu lar vec tors for 5, 10, (c) 15, and (d) 20 re tained sin gu lar vec tors, re spec tively. Note that the growth rate curves from the Yule-Walker equa tion are pre dom i nantly asym met ri cal to wards the decay states (growth rates < 1), while those from the SVD-CSD are more anti-sym met ri cal about the neu tral state (growth rate = 1). The re sults of the Yule-Walker equa tion in di cate that the vari abil ity of Y(t + 1) can not be well main tained by AY(t). To show this is in deed the case, the ra tios be tween the total variance of AY(t) and Y(t + 1) are cal cu lated. They are 0.96, 0.94, 0.93, and 0.92, re spec tively. These re sults show the variability of Y(t + 1) is not fully re cov ered by AY(t) when the Yule-Walker equa tion is used to es ti mate A. Fur - ther more, the damp ing of the vari abil ity of Y(t + 1) in - creases as more PCs are used. Con versely, the anti-sym met - rical distribution re sults of the SVD-CSD are what one would ex pect when the vari abil ity of Y d (t + 1) can be faith - fully repro duced by A d Y d (t). These re sults clearly sug gest that, due to the incapability of differentiating linear related and un re lated vari abil ity be tween the pre dic tor and the pre - Fig. 5. The es ti mated max i mum lag-1 fi nite-time growth rates for the PCA fil tered Kaplan SSTA as a func tion of the re tained sin gu lar vec tors us ing both the SVD-CSD and the Yule-Walker equa tion meth ods. The thick solid line cor re sponds to the re sults ob tained by ap ply ing the SVD-CSD to the first 80 PCs. The dashed line cor re sponds to the re sults ob tained by ap ply ing the Yule-Walker equa tion to the same num ber of PCs as used for the re - tained sin gu lar vec tors. shows re sults for all re tained sin gu lar vec tors. shows a blown-up view of, for the first 20 re tained sin gu lar vec tors.

The Ap pli ca tion of Linearization Pro ce dure in Data Anal y sis 373 (c) (d) Fig. 6. The es ti mated fi nite-time growth rates for the PCA fil tered Kaplan SSTA as a func tion of the sin gu lar vec tors for: 5, 10, (c) 15, and (d) 20 re tained sin gu lar vec tors, re spec tively. The thick solid and dashed lines cor re spond to the re sults ob tained by ap ply ing the SVD-CSD to the first 80 PCs, and from the Yule-Walker equa tion. dictand, the Yule-Walker equa tion may overly un der es ti - mate the growth rates. As for dif fer ent choice of (re sults are not shown), al though the es ti mated growth rates are generally larger than those of = 1, the con clu sions are sim i lar. The dif fer ences be tween these two ap proaches are shown not only in the growth rates but also in the sin gu lar vec tors. Be cause the orig i nal data has been PCA fil tered, the sin gu lar vec tors so de rived are lin ear com bi na tions of the retained PC modes. Fig ure 7 shows the op ti mal sin gu lar vectors (the most un sta ble sin gu lar vec tors) de rived by the Yule-Walker equa tion as a func tion of the re tained PC modes for m = N = 2, 4,, 20, re spec tively. As all the cor re - sponding op ti mal growth rates are close to unity, the pat - terns between the pre dic tor and the predictand are very sim i - lar for each given m. Fur ther more, the op ti mal mode con - stituents in crease as more PCs are re tained. How ever, the relative con tri bu tion of each PC mode to the op ti mal mode does not show a dra matic change with the in crease of the retained PCs. This is be cause the Yule-Walker equa tion is covariance based. The sin gu lar vec tors so de rived not only de pend on the lin ear re la tion be tween the pre dic tor and the predictand but also on their vari ance. Since most vari ance of the pre dic tor and the predictand is ex plained by the first few PCs, the covariance struc ture be tween the pre dic tor and the predictand is also pri mar ily con trolled by these few PCs. There fore, even though the lin ear re la tion ship may change if more PCs are re tained, the op ti mal modes so de rived are relatively in sen si tive to the vari a tion of the re tained PCs. Fig ure 8 shows the same plots as Fig. 7, ex cept for re - sults from the SVD-CSD with m = 80. The re sem blance between pat terns of the pre dic tor and the predictand can still be clearly ob served. How ever, be cause they are de rived us ing 80 re tained PCs, the op ti mal mode con stit u ents are no lon ger re stricted only to PC modes less than the re tained singular vec tors. Fur ther more, the rel a tive con tri bu tion of each PC mode to the op ti mal mode grad u ally shifts to ward higher PC modes, as more sin gu lar vec tors are re tained (i.e., N in creases). Be cause the SVD-CSD has linearized the re - lation be tween the pre dic tor and the predictand be fore estimating the lin ear prop a ga tor, the op ti mal modes thus derived are cho sen solely ac cord ing to which com bi na tion of the em pir i cal or thogo nal func tions [EOFs, i.e., col umn vec tors of Q in Eq. (9)] of the oint pre dic tor and the pre - dictand ma tri ces will yield the larg est sin gu lar value. There - fore, the struc tures of the SVD-CSD de rived op ti mal modes de pend strongly on how many sin gu lar vec tors (or equiv a - lently, how many col umn vec tors of Q) are re tained. 6. SUM MARY AND DIS CUS SION The prop a ga tor of a lin ear model plays a very im por tant

374 Yung-An Lee & Zih-Ting Hung Fig. 7. The optimal singular vectors for the Kaplan s SSTA derived from the Yule-Walker equation as a function of PC modes, from top to bottom, for 2, 4,, 20 and retained singular vectors, respectively. and show results for the predictor and the predictand, respectively. Fig. 8. The same as Fig. 5, except for results obtained by applying the SVD-CSD to the first 80 PCs of the Kaplan s SSTA.

The Ap pli ca tion of Linearization Pro ce dure in Data Anal y sis 375 role in nor mal mode and fi nite-time in sta bil ity prob lems. Its estimation will affect whether the linear stability characteristics of the cor re spond ing dy namic sys tem can be prop erly ex tracted. Con ven tion ally, the prop a ga tor is es ti mated us ing the Yule-Walker equa tion with the auto and lag covariance ma tri ces of the pre dic tor and the predictand. How ever, be - cause non lin ear and noise in for ma tion of the pre dic tor and the predictand may also be in cluded in form ing these co - variance matrices, the linear propagator thereby derived is likely to underestimate the linear relationship between them. There fore, in this study the GSVD and SVD-CSD meth ods have been in tro duced as al ter na tives to the Yule-Walker equa tion to es ti mate the lin ear prop a ga tor and its as so ci ated prop er ties for a lin ear model. In ac cord with the ba sic con - cept of a lin ear model, both meth ods linearize the re la tion be tween the pre dic tor and the predictand by de com pos ing them to have a com mon evo lu tion struc ture and then make the es ti ma tions. With these de com po si tions, the lin ear pro - pagator and the as so ci ated sin gu lar vec tors can be si mul - taneously de rived. Fur ther more, the con nec tion be tween the fi nite-time am pli tude growth rates and the sin gu lar val ues of the prop a ga tor are clearly es tab lished. Both the GSVD and the SVD-CSD, to gether with the Yule-Walker equa tion, are ap plied to two syn thetic datasets and Kaplan s SSTA data - sets to eval u ate their re spec tive per for mances. The re sults show that, be cause of the linearization and flex i ble fil ter ing capabilities, the SVD-CSD allows the propagator, the fi - nite-time growth rates, and the as so ci ated sin gu lar vec tors to be more appropriately estimated. It is noted that the ap pli ca tion of the SVD-CSD is not re - stricted to lin ear mod els where the pre dic tor and the pre - dictand use the same field vari ables. There fore, it can be ap - plied not only to linear statistical prediction problem, but also to bias cor rec tion or sta tis ti cal downscaling prob lems. As for data as sim i la tion and re lated prob lems in nu mer i cal weather prediction, because the linear propagator is time de - pend ent, the ap pli ca bil ity of the SVD- CSD to these pro b - lems is not clear and needs fur ther stud ies. Ac knowl edge ments I would like to thank the anon y mous re view ers and the ed i tor for their crit i cal re view of this pa - per. Their com ments were es sen tial to im prov ing the fi nal ver sion of this pa per. This study was sup ported by the Na - tional Sci ence Coun cil of Tai wan through grants NSC 90-2111-M-008-061 and NSC91-2111- M- 008-011. REFERENCES Brockwell, P. J. and R. A. Da vis, 1991: Time Se ries: The ory and Meth ods, Sec ond edi tion, Springer-Verlag, 577 pp. Farrell, B. F. and P. J. Ioannou, 1996a: Gen er al ized sta bil ity theory. Part I: Au ton o mous op er a tors. J. Atmos. Sci., 53, 2025-2040, doi: 10.1175/1520-0469(1996)053<2025: GSTPIA>2.0.CO;2. [Link] Farrell, B. F. and P. J. Ioannou, 1996b: Gen er al ized sta bil ity theory. Part II: Nonautonomous op er a tors. J. Atmos. Sci., 53, 2041-2053, doi: 10.1175/1520-0469(1996)053<2041: GSTPIN>2.0.CO;2. [Link] Golub, G. H. and C. F. Van Loan, 1996: Ma trix Com pu ta tions, Johns Hopkins Univ. Press, Bal ti more, 694 pp. Kaplan, A., M. Cane, Y. Kushnir, A. Clem ent, M. Blumenthal, and B. Raagopalan, 1998: Anal y ses of global sea sur face tem per a ture 1856-1991. J. Geophys. Res., 103, 18567-18589, doi: 10.1029/97JC01736. [Link] Kim, H. M. and M. C. Mor gan, 2002: De pend ence of sin gu lar vec tor struc ture and evo lu tion on the choice of norm. J. Atmos. Sci., 59, 3099-3116, doi: 10.1175/1520-0469(2002) 059<3099:DOSVSA>2.0.CO;2. [Link] Palmer, T. N., R. Gelaro, J. Barkmeuer, and R. Buizza, 1998: Sin gu lar vec tors, met rics, and adap tive ob ser va tions. J. Atmos. Sci., 55, 633-653, doi: 10.1175/1520-0469(1998) 055<0633:SVMAAO>2.0.CO;2. [Link] Parker, D. E., P. D. Jones, C. K. Folland, and A. Bevan, 1994: Interdecadal changes of sur face tem per a ture since the late nine teenth cen tury. J. Geophys. Res., 99, 14373-14399, doi: 10.1029/94JD00548. [Link] Penland, C. and T. Magorian, 1993: Pre dic tion of Niño 3 sea sur face tem per a tures us ing lin ear in verse mod el ing. J. Climate, 6, 1067-1076, doi: 10.1175/1520-0442(1993)006 <1067:PONSST>2.0.CO;2. [Link] Penland, C. and P. D. Sardeshmukh, 1995: The op ti mal growth of tropical sea surface temperature anomalies. J. Cli mate, 8, 1999-2024, doi: 10.1175/1520-0442(1995)008<1999: TOGOTS>2.0.CO;2. [Link] Preisendorfer, R. W. and C. D. Mobley, 1988: Prin ci pal Com - ponent Anal y sis in Me te o rol ogy and Ocean og ra phy. El - sevier, 425 pp. Reynolds, R. W. and T. M. Smith, 1994: Im proved global sea sur face tem per a ture anal y sis us ing op ti mum in ter po la tion. J. Cli mate, 7, 929-948, doi: 10.1175/1520-0442(1994)007 <0929:IGSSTA>2.0.CO;2. [Link] von Storch, H. and F. W. Zwiers, 1998: Sta tis ti cal anal y sis in cli mate re search, Cam bridge Uni ver sity Press, 484 pp. von Storch, H., G. Bürger, R. Schnur, and J. S. von Storch, 1995: Prin ci pal os cil la tion pat terns: A re view. J. Cli mate, 8, 377-400, doi: 10.1175/1520-0442(1995)008<0377: POPAR>2.0.CO;2. [Link] Xue, Y., M. A. Cane, S. E. Zebiak, and M. B. Blumenthal, 1994: On the pre dic tion of ENSO: A study with a low-or der Markov model. Tellus, 46A, 512-528, doi: 10.1034/.1600-0870.1994.00013.x. [Link] Xue, Y., A. Leetmaa, and M. Ji, 2000: ENSO pre dic tion with Markov mod els: The im pact of sea level. J. Cli mate, 13, 849-871, doi: 10.1175/1520-0442(2000)013<0849:EPWMMT> 2.0.CO;2. [Link]