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  • 8/6/2019 Lecture 04 Dynamic Modelling 2006

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    Financial Economics Lecture Ten

    Dynamic Modelling & the Circuit

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    Dynamic modellingan introduction

    Dynamic systems necessarilyinvolve time

    Simplest expression starts with definition of thepercentage rate of change of a variable:

    Population grows at 1% a year

    Percentage rate of change of a variable y is

    Slope of function w.r.t. time (dy/dt) Divided by current value of variable (y)

    So this is mathematically1

    .01dy

    y dt=

    This can be rearranged to .01dy

    ydt =

    Looks very similar to differentiation, which you havedone but essential difference: rate of change of yis some function of value of y itself.

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    Dynamic modellingan introduction

    Dependence of rate of change of variable on its current

    value makes solution of equation much more difficult thansolution of standard differentiation problem

    Differentiation also normally used by economists to findminima/maxima of some function

    Profit is maximised where the rate of change of totalrevenue equals the rate of change of total cost (blahblah blah)

    Take functions for TR, TC

    Differentiate Equate

    Easy! (also wrong, but thats another story)

    However differential equations

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    Dynamic modellingan introduction

    Simple model like this gives

    Exponential growth if a>0 Exponential decay if a

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    Dynamic modellingan introduction

    Simple example: relationship of fish and sharks.

    In the absence of sharks, assume fish population growssmoothly:

    The rate of growth of the fish population is a% p.a.1 dF

    a

    F dt

    = dF a dtF

    =

    dFadt

    F= ( ) 0ln F a F c= +

    ( ) 0 0a t c ca t a t F t e e e C e + = = =

    Rearrange

    Integrate

    Solve

    Expo

    nential

    s

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    Dynamic modellingan introduction

    Simulating gives exponential growth if a>0

    a .02:= F0 100:= F t( ) F0 ea t:=

    0 20 40 60 80 1000

    200

    400

    600

    800Fish population as a function of t ime

    Years

    F t( )

    t

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    Dynamic modellingan introduction

    Same thing can be done for sharks in the absence of fish:

    Rate of growth of shark population equals c% p.a. But here c is negative

    Sbadt

    dFF =1

    ( ) 2c tS t C e =

    c .01:= S0 50:= S t( ) S0 ec t

    :=

    0 20 40 60 80 10010

    20

    30

    40

    50Shark population as a function of time

    Years

    S t( )

    t

    But we know fish andsharks interact:

    The rate of change offish populations is alsosome (negative) functionof how many Sharks

    there are

    The rate of change ofshark population is alsosome (positive) function ofhow many Fish there are

    1 dS

    c d FS dt = +

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    Dynamic modellingan introduction

    Now we have a model where the rate of change of each

    variable (fish and sharks) depends on its own value andthe value of the other variable (sharks and fish):

    Sbadt

    dF

    F=

    1

    1 dSc d F

    S dt = +

    dFa F b S F

    dt=

    dSc S d F S

    dt= +

    This can still be solved, with more effort (dont worryabout the maths of this!):

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    Dynamic modellingan introduction

    But for technical reasons, this is

    the last level of complexity thatcan be solved

    Add an additional (nonlinearlyrelated) variablesay,seagrass levelsand modelcannot be solved

    But there are other ways

    Mathematicians have shownthat unstable processes canbe simulated

    Engineers have built tools forsimulating dynamic processes

    ( )lnd

    F a b S dt

    =

    ( )lnd F a b S dt =

    ( )lnd F a b S dt = ( ) ( )ln F a b S t c = +

    ( )( )1

    a b S t t F C e =

    ( )( )2

    c d F t t S C e + =

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    Dynamic modellingan introduction

    (1) Enter (preferably empirically derived!) parameters:

    Equilibrium values

    Fish Fec

    d:= Fe 10000=

    Sharks Se

    a

    b:= Se 10=

    (2) Calculate equilibrium values:

    (3) Rather than stopping there:

    Given

    t

    F t( )d

    d

    F t( ) a b S t( )( ) F 0( ) 8000

    tS t( )

    d

    dS t( ) c d F t( )+( ) S 0( ) 12

    F

    S

    Odesolve

    F

    S

    t, 10, 1000,

    :=

    Parameters

    a 1:= Annual population growth rate of fish in absence of sharks

    b .1:= Impact of each shark on fish population growth rate

    c 1:= Death rate of sharks in absence of fish

    d .0001:= Impact of each fish on survival of sharks

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    Dynamic modellingan introduction System is never in equilibrium

    Equilibrium unstablerepels as much as it attracts

    Commonplace in dynamic systems Systems are always far from equilibrium

    (What odds that the actual economy is inequilibrium?)

    0 2 4 6 8 107000

    8000

    9000

    1 .104

    1.1 .104

    1.2 .104

    1.3 .104

    1.4 .104

    7

    8

    9

    10

    11

    12

    13

    14

    Fish (LHS)

    Fish Equilibrium

    Sharks (RHS)

    Shark Equilibrium

    Fish (LHS)

    Fish Equilibrium

    Sharks (RHS)

    Shark Equilibrium

    Fish & Shark populations over time

    Years

    Numb

    er

    7 8 9 10 11 12 13 146000

    8000

    1 .104

    1.2 .104

    1.4 .104

    Time Path

    Equilibrium

    Time Path

    Equilibrium

    "Limit Cycle" of Fish & Sharks

    Sharks

    Fish

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    Dynamic modellingan introduction

    Thats the hard way; now for the easy way

    Differential equations can be simulated using flowcharts The basic idea Numerically integrate the rate of change of a

    function to work out its current value Tie together numerous variables for a dynamic

    system Consider simple population growth:

    Population grows at 2% per annum

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    Dynamic modellingan introduction

    Representing this as mathematics, we get1

    .02dP

    P dt

    =

    .02dP

    Pdt

    =

    .02 . P P dt =

    Next stage of a symbolic solution is

    Symbolically you would continue,putting dt on the RHS; butinstead, numerically, you integrate:

    As a flowchart, you get:

    Read it backwards, andits the same equation:

    Feed in an initial value (say, 18 million) and we cansimulate it (over, say, 100 years)

    Population

    * 1/S

    0.02

    Population

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    Dynamic modellingan introduction

    MUCH more complicated models than this can be built

    Population

    * 1/S

    0.02

    Population

    Plot

    Time (sec)

    0 10 20 30 40 50 60 70 80 90 1000

    20000000

    40000000

    60000000

    80000000

    100000000

    120000000

    140000000

    160000000

    180000000

    200000000

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    Dynamic modellingan introduction

    Models can have multiple interacting variables, multiplelayers; for example, a racing car simulation:

    Car Path and

    Vital ParametersSystem Dynamics

    LAPS

    LAPS

    LAPS

    ENGINE TORQUE

    LAPS

    LAPS

    TAU, MOD(Pi/2)

    0

    TAU, MOD(Pi)

    0

    1

    2TAU, MOD(Pi)

    ACCELERATION

    -

    -10

    0

    10

    20ACCELERATION

    ACCELR.

    ENGINE RPM

    LAPS

    0 .2 .4 .6 .8 15000

    6000

    7000

    8000ENGINE RPM

    Fc

    TORQUE AVA ILABLE

    LAPS

    0 .2 .4 .6 .8 1300

    350

    400

    450

    500ENGINE TORQUE, FT-#

    ENGINE TORQUE

    ENG.RPM

    DELTA "S" (PER STEP)

    LAPS

    0 .2 .4 .6 .8 1.4

    .5

    .6

    .7DELTA S

    NORMAL FORCE

    LATERAL FORCE LATERAL & NORM.FORCES

    LAPS

    0 .2 .4 .6 .8 10

    1000

    2000

    3000LATERAL FORCE

    TOT.TRACTION FORCE, Fc

    LAPS

    DELTA S

    INPUT PARAMETERS

    Automotive Dynamics:Simulation of Automobile RacingDynamics on a Race Track

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    Dynamic modellingan introduction

    System dynamics block has these components:

    TAU CONVERION.& DISPLAYS

    Acceleration andBraking Logic

    Normal andLateral Force

    Conversions Computations

    Rotating Mass

    Dynamics

    Car Mass

    Radius of Curvature Minimum Veloc ity

    LATERAL FORCE

    NORMAL FORCE

    MUACC-BRAKE FORCE & LOGIC

    Fx,BRAKING

    Fx, ACCEL.

    0

    0

    RADIUS OF CURVATURE

    And this block has the following components

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    Dynamic modellingan introduction

    Lets use it to build the Fish/Shark model

    Start with population model, only Change Population to Fish Alter design to allow different initial numbers

    This is equivalent to first half ofdF

    a F b S F dt

    =

    To add second half, have toalter part of model to LHS ofintegrator

    +

    +

    1/SFish

    Fish

    *0.02

    Plot

    Time sec

    0 10 20 30 40 50 60 70 80 90 1000

    5000

    10000

    15000

    20000

    25000

    30000

    1000

    Initial Fish Population

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    Dynamic modellingan introduction

    Sharks just shown

    as constant here

    Sharks substractfrom fish growth rate

    Now add shark dynamics

    Plot

    0 20 40 60 80 1001000

    2000

    3000

    4000

    5000

    6000

    7000

    8000

    *

    Sharks

    1e-006

    +

    -

    Initial Fish Population

    1000

    0.02*

    Fish

    Fish

    1/S

    +

    +

    Fish

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    Dynamic modellingan introduction

    Shark population

    declinesexponentially, justas fish populationrises

    (numbersobviouslyunrealistic)

    Now add interactionbetween two

    species

    Fish

    Initial Shark Population

    100

    -0.1*

    Sharks1/S

    ++

    Sharks

    Plot

    Time (years)0 20 40 60 80 100

    0

    20

    40

    60

    80

    100

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    Dynamic modellingan introduction

    Model now gives same cycles as seen in mathematicalsimulation.

    Now to apply this to endogenous money!

    Fish

    *

    Sharks

    2

    +

    -

    10*

    Fish

    1/S 1/S*

    1-

    +

    0.001Sharks

    *

    Fish

    Sharks

    Plot

    0 2 4 6 8 100

    1000

    2000

    3000

    4000

    50006000

    7000

    +

    +

    200010

    +

    +

    Plot

    0 2 4 6 8 100

    5

    10

    15

    20Plot

    0 5 10 15 200

    1000

    2000

    3000

    4000

    5000

    6000

    7000

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    Modelling endogenous money dynamically

    Remember our minimum 4 accounts?

    Capitalist Credit (KC

    ) Money paid in here

    Interest on balance

    Repayments out of here to Banker

    Capitalist Debt (KD) Repayment of debt recorded here

    Interest on balance

    Banker Principal Account (B

    P)

    Accepts repayment of debt by capitalist

    Banker Income Account (BY)

    Records incoming and outgoing interest payments

    Starting at the very simplest level: compound interest

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    Modelling endogenous money dynamically

    KD grows at rate of debt interest rd: =D Ddd

    K r Kdt

    KC grows at rate of credit interest rc: = cC Cd K r Kdt

    BY pockets the difference: = Y cD Cdd

    B r K r K dt

    As Circuitists feared, this is the road to ruin forcapitalists

    With Loan L=$100, rd=5%, rc=3%, after one year

    Simulating this with equations

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    Modelling endogenous money dynamicallyGiven

    KD 0( ) LCompound interest

    on both accounts tKD t( )

    d

    drd KD t( )Initial Loan

    recorded in bothdebt and creditaccount

    KC 0( ) LtKC t( )

    d

    drc KC t( )

    Bank comes outahead on the

    interest

    tBY t( )

    d

    drd KD t( ) rc KC t( ) BY 0( ) 0

    Simulate themodel and seewhat happens

    KD

    KC

    BY

    Odesolve

    KD

    KC

    BY

    t, 10, 1000,

    :=

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    Modelling endogenous money dynamically

    0 2 4 6 8 10100

    120

    140

    160

    180

    0

    10

    20

    30

    Capitalist Debt

    Capitalist Credit

    Bank Income (RHS)

    Capitalist Debt

    Capitalist Credit

    Bank Income (RHS)

    Bank Balances over time: no repayment

    Years

    $

    KD t( )

    KC t( )BY t( )

    t

    KD 1( ) 105.127= KC 1( ) 103.045= KC 1( ) KD 1( ) 2.082= BY 1( ) 2 .082=

    Whod be a capitalist?

    But model isnt complete yet: no repayment

    First, same model as a flowchart

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    Modelling endogenous money dynamically

    In flowchart format, equations

    =D Ddd K r Kdt =cC C

    dK r Kdt = Y cD Cd

    dB r K r K dt

    Become

    KD1/S

    Capitalist Debt

    +

    +

    *rd

    L

    Bank Accounts

    No repayment

    Time (Years)0 2 4 6 8 10

    0

    20

    40

    60

    80

    100

    120

    140

    160

    180

    200Capitalist Debt

    Capitalist Credit

    Bank Income

    Parameters

    rc *

    ++

    1/S

    Capitalist CreditKC

    rd*

    KD

    KC

    *rc

    +-

    1/SBank Income

    BY

    100

    Initial Loan

    KD

    KC

    Simulating this in realtime

    01Norepayment.vsm

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    Modelling endogenous money dynamically

    Tidied up using compound blocks:

    L

    Bank AccountsNo repayment

    Time (Years)

    0 2 4 6 8 100

    20

    40

    60

    80

    100

    120

    140

    160

    180

    200Capitalist Debt

    Bank IncomeCapitalist Credit

    Parameters

    BY100Initial Loan

    KC

    Capitalist

    DebtKD

    CapitalistCredit

    BankIncome

    01Norepayment02.vsm

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    Modelling endogenous money dynamically

    How to model repayment? Standard home loan styleregular payments over term

    of loan? OK at micro level, but at macro:

    Lots of loans, starting different times, endingdifferent times, some extended, others paid off

    early Aggregate outcome very different to each

    individual loan Fixed repayment commitment?

    Like exponential decay: = 1

    PDD

    dK RK dt

    Debt would fall towards zero as t Sensible objective for capitalist borrowers;

    How to achieve it?

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    Modelling endogenous money dynamically

    Currently debt has dynamics: =D Ddd

    K r Kdt

    To convert this to = 1 PDD

    d K RK dt Need to add:

    Repayment of interest( )= D D Dd d

    dK r K r K

    dt

    & Repayment of principal ( )= + pD D D D d dd

    K r K r K R K dt Both amounts have to come out of

    capitalist credit account KC(capitalists only source of funds)

    ( )= +c pC C D D dd

    K r K r K R K dt

    Interest to banker income account BY(already shown)

    Repayment of principal to bankerprincipal account BP

    =P P Dd

    B R Kdt

    ll

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    Modelling endogenous money dynamically

    So (still incomplete) system is: ( )= + pD D D D d dd

    K r K r K R K dt

    ( )= +c pC C D D dd K r K r K R K dt

    =P P Dd

    B R Kdt

    = Y cD Cdd B r K r K dt

    How does this behave? Simulate and find out

    Try R=1Given

    t

    KD t( )d

    d

    rd KD t( ) rd KD t( ) RP KD t( )+( ) KD 0( ) L

    KC 0( ) L

    tKC t( )

    d

    drc KC t( ) rd KD t( ) RP KD t( )+( )

    BY 0( ) 0

    tBY t( )

    d

    drd KD t( ) rc KC t( )

    BP 0( ) 0

    t

    B

    P

    t( )d

    d

    R

    P

    K

    D

    t( )

    KD

    KC

    BY

    BP

    Odesolve

    KD

    KC

    BY

    BP

    t, 10, 1000,

    :=

    Picture looks a lot better forcapitalists than withoutrepayment

    d ll d d ll

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    Modelling endogenous money dynamically

    0 2 4 6 8 1050

    0

    50

    100

    0

    1

    2

    3

    Capitalist Debt

    Capitalist CreditBank Income (RHS)

    Capitalist Debt

    Capitalist CreditBank Income (RHS)

    Bank Balances over time: repayment

    Years

    $

    KD t( )

    KC t( )BY t( )

    t

    KD 1( ) 36.788= KC 1( ) 35.501= KC 1( ) KD 1( ) 1.287= BY 1( ) 1.287=

    But being a capitalist still a losing proposition

    Because production isnt yet modelled

    Capitalists borrow to produce, sell, & make a profit

    M d ll d d ll

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    Modelling endogenous money dynamically

    Observations on Circuitists vs Keynes

    Graziani: As soon as firms repay their debt to thebanks, the money initially created is destroyed.

    Keynes: Credit, in the sense of finance, looks after aflow of investment. It is a revolving fund which can beused over and over again. It does not absorb orexhaust any resources. The same finance can tackleone investment after another. (247)

    Keynes is right: the money created by the loan continuesto exist & circulate as an asset of the banks. It is either

    The outstanding debt of capitalists to banks; or

    The balance in bankers principal account:

    M d lli d d i ll

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    Modelling endogenous money dynamically Sum of capitalist debit account KD + banker principal account

    BP always equals value of initial loan L:

    0 2 4 6 8 100

    50

    100

    150

    Bankers Principal

    Capitalist Debt

    Sum

    Bankers Principal

    Capitalist Debt

    Sum

    Money, Credit & Debt

    Years

    $

    Debt destroyed by repayment; money is conserved as a revolving

    fund of finance

    M d lli d d i ll

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    Modelling endogenous money dynamically

    Final step to close (simple) model: production How to model?

    Complicated! Input-output issues, pricing, stocks Leave till later & take essence:

    Whole purpose of production to make $ profit Must spend $ to make $: outflow from KC Production requires workers

    Must be paid wages (into new account WY)

    Products sold to capitalists, workers, bankers Transactions from sale flow to capitalist credit

    account (out of BY, WY) Net revenue generated resolves into either

    profits orwages in proportions of flow of income from

    production, wage share + profit share = 1

    M d lli d d i ll

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    Modelling endogenous money dynamically

    Call proportion of outflowthat finances production P:

    ( )= + c pC C D D Cdd

    K r K r K R K PK dt

    Fraction (1 ) of this flows toworkers as wages:

    ( )= 1Y Cd

    W PKdt

    Workers earn interest too: ( )= +1Y c YCdW PK rW dt

    Paid by bankers from BY: = Y c c Y D Cdd

    B r K r K rW dt

    Fraction flows back to

    capitalists as profits:

    ( ) = + +c pC C D D C Cdd

    K r K r K R K PK PK dt

    Workers & bankers consume:( ) = + 1Y c Y Y C

    dW PK rW W

    dt= Y c c Y Y D Cd

    dB r K r K rW B

    dt

    ( ) = + + + +c p Y Y C C D D C C dd

    K r K r K R K PK PK W B

    dt

    & pay $ to KC account

    M d lli d d i ll

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    L

    Bank AccountsNo repayment

    Time (Years)

    0 2 4 6 8 10-100

    -50

    0

    50

    100Capitalist Debt

    Bank PrincipalCapitalist Credit

    Parameters

    BY

    100Initial Loan

    KC

    CapitalistDebt

    KD

    CapitalistCredit

    BankIncome

    KD

    Bank Accounts

    No repayment

    Time (Years)0 2 4 6 8 10

    0

    5

    10

    15

    20Bank Income

    Workers Income

    KC

    BankPrincipal

    BP

    WY

    WYBY

    WorkerIncome

    Modelling endogenous money dynamically

    So the first complete (but still simple!) system is:

    ( )= + pD D D D d dd

    K r K r K R K dt

    ( ) = + + + +c p Y Y C C D D C C dd

    K r K r K R K PK PK W B dt

    =P P Dd

    B R Kdt

    ( ) = + 1Y c Y Y CdW PK rW W dt

    = Y c c Y Y D Cdd

    B r K r K rW B dt 06Production02.vsm

    M d lli d d i ll

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    Modelling endogenous money dynamically

    Almostobvious why capitalists go into debt:

    0 2 4 6 8 100

    5

    10

    15

    0

    5

    10

    15

    20

    Capitalist Debt

    Capitalist Credit

    Bank Income (RHS)

    Worker Credit

    Capitalist Debt

    Capitalist Credit

    Bank Income (RHS)

    Worker Credit

    Bank Account Balances over time: production

    Years

    $

    KD t( )

    KC t( )

    BY t( )

    WY t( )

    t

    KD 1( ) 36.788= KC 1( ) 27.452= KC 1( ) KD 1( ) 9.336= BY 1( ) 0 .747= WY 1( ) 8.589=

    Does it matter that capitalists are in net debt?

    M d lli d d i ll

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    Modelling endogenous money dynamically

    No:

    Capitalist entrepreneurs are the debtors parexcellence in capitalism:

    becoming a debtor arises from the necessity ofthe case and is not something abnormal, anaccidental event to be explained by particularcircumstances. What he first wants is credit.Before he requires any goods whatever, herequires purchasing power. He is the typicaldebtor in capitalist society. (Schumpeter, Theory

    of Capitalist Development: 102) Net debt tapers to zero over time:

    M d lli d d i ll

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    Modelling endogenous money dynamically

    After ten years

    Capitalist net debt position negligible Almost all net money in BP account:

    0 2 4 6 8 100

    50

    100

    150

    Bankers Principal

    Capitalist Debt

    Sum

    Bankers Principal

    Capitalist Debt

    Sum

    Money, Credit & Debt

    Years

    $

    KD 10( ) 4.54 103

    = KC 10( ) KD 10( ) 1.89 103

    = WY 10( ) 8.306 104

    =

    KC 10( ) 2.65 103

    = BY 10( ) 1.059 103

    = BP 10( ) 99.995=

    What about incomes?

    KD, KC, WY, etc. record

    bank balances

    Entries WY, BY,

    etc. recordtransactionsbetweenaccounts

    Incomes are subset oftransactions

    M d lli d s d mi ll

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    Modelling endogenous money dynamically

    Workers: wages + interest =

    + cC C DdPK r K r K

    ( ) +1 c YCPK rW

    c c YD Cdr K r K rW Bankers: net interest =

    Capitalists: profit + net interest =

    These are flows

    Aggregateincomegenerated byinitial loanL=$100 is stock:

    Integral of theseover time:

    Profit t( )

    0

    t

    t P KC t( ) rd KD t( )

    d:= Profit 10( ) 86.754=

    CapInc t( )

    0

    t

    t P KC t( ) rc KC t( ) rd KD t( )( )+

    d:= CapInc 10( ) 89.048=

    BankInc t( )

    0

    t

    trd KD t( ) rc KC t( ) rc WY t( )

    d:= BankInc 10( ) 2.062=

    WorkInc t( )

    0

    t

    t1 ( ) P KC t( ) rc WY t( )+

    d:= WorkInc 10( ) 214.736=

    M d llin nd n us m n d n mic ll

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    Modelling endogenous money dynamically

    So initial loan of $100 can generate:

    $89 income to capitalists; $2 to bankers; and

    $215 to workers

    (with example parameters)

    Withoutrelending All money eventually accumulates in BP & activity

    ceases

    Next extension: with re-lending so that we model

    credit as a revolving fund which can be used over andover again. (Keynes)

    Bankers re-lend proportion B of existing BP

    Amount paid into KC; recorded in KD:

    Modelling endogenous money dynamically

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    Modelling endogenous money dynamically

    Final system is:

    ( )= + +p PD D D D d dd

    K r K r K R K BB dt

    ( ) = + + + + +c p Y Y P C C D D C C dd

    K r K r K R K PK PK W B BB dt

    = P P PDd

    B R K BB dt

    ( ) = + 1Y c Y Y CdW PK rW W dt

    = Y c c Y Y D Cdd

    B r K r K rW B dt

    Initial loan L can now fund oneinvestment after another, as

    Keynes argued:

    L

    Bank Accounts

    No repayment

    Time (Years)

    0 2 4 6 8 100

    20

    40

    60

    80

    100Capitalist Debt

    Bank PrincipalCapitalist Credit

    Parameters

    BY

    100Initial Loan

    KC

    CapitalistDebt KD

    CapitalistCredit

    BankIncome

    KD

    Bank AccountsNo repayment

    Time (Years)

    0 2 4 6 8 100

    5

    10

    15

    20

    25

    30Bank Income

    Workers Income

    KC

    BankPrincipal

    BP

    WY

    WYBY

    WorkerIncome

    BP

    BP

    07Relending02.vsm

    Modelling endogenous money dynamically

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    Modelling endogenous money dynamically

    All accounts stabilise at constant level:

    0 2 4 6 8 10

    20

    40

    60

    80

    100 Capitalist DebtCapitalist Credit

    Bank Principal

    BP+KD

    Capitalist DebtCapitalist Credit

    Bank Principal

    BP+KD

    Bank Account Balances over time: relending

    Years

    $

    KD t( )

    KC t( )

    BP t( )

    BP t( ) KD t( )+

    t

    0 2 4 6 8 100

    5

    10

    15

    20

    Workers Account

    Bankers Income Account

    Workers Account

    Bankers Income Account

    Bank Account Balances over time: relending

    Years

    $

    WY t( )

    BY t( )

    t

    Flow of revolving fund

    through accountsgenerates sustainedstream of income for all 3classes from single initial

    loan:

    Modelling endogenous money dynamically

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    Modelling endogenous money dynamically

    With parameter values used, $100 initial loan can finance:

    $61 of profit $143 of wages; and

    $1 of bank income per year

    CapInc t( )t 1

    t

    t P KC t( ) rc KC t( ) rd KD t( )( )+

    d:= CapInc 10( ) 59.367=

    BankInc t( )

    t 1

    t

    trd KD t( ) rc KC t( ) rc WY t( )

    d:= BankInc 10( ) 1.375=

    WorkInc t( )

    t 1

    t

    t1 ( ) P KC t( ) rc WY t( )+

    d:= WorkInc 10( ) 143.162=

    TotalInc t( ) CapInc t( ) BankInc t( )+ WorkInc t( )+:= TotalInc 10( ) 203.904=

    Modelling endogenous money dynamically

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    InterestInterest

    on debton debt

    Modelling endogenous money dynamically

    How can capitalists borrow money & make a profit?dilemma easily solved:

    So long as income from production exceeds interestpayments on borrowed money!:

    IncomeIncomefromfrom

    productionproduction

    Profits t( )

    t 1

    t

    t P KC t( ) rd KD t( )( )

    d:= Profits 10( ) 57.838=

    Circuitist how can Mbecome M`? dilemma a case ofconfusing stocks(initial loan) and flows(incomes,including profits)

    Additional insights from model

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    Additional insights from model

    Endogenous money works

    Dont need deposits to make loans (exogenous moneyperspective)

    instead loans create deposits

    Loans(t) = KD(t)

    Deposits(t) = KC(t)+WY(t)+BY(t) Amounts identically equal over time

    Bank creates money ab initio

    No need for it to have any assets

    Just need acceptance of its IOUs as money by thirdparties

    Additional insights from model

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    Additional insights from model

    0 2 4 6 8 100

    20

    40

    60

    80

    100

    5 .104

    0

    5 .104

    Deposits

    Loans

    Loans-Deposits (RHS)

    Deposits

    Loans

    Loans-Deposits (RHS)

    Loans & Deposits: No relending

    Years

    $

    0 2 4 6 8 1060

    70

    80

    90

    100

    5 .104

    0

    5 .104

    Deposits

    Loans

    Loans-Deposits (RHS)

    Deposits

    Loans

    Loans-Deposits (RHS)

    Loans & Deposits: Relending

    Years

    $

    Deposits destroyed as Loans repaid, not Moneywhich isconserved

    Money a bank asset: Money(t) = KD(t) + BP(t)

    Technically, Loans destroyed by returning Deposits to Banks

    Additional insights from model

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    Additional insights from model

    Form of money is either

    Debt by other parties to banks (loans=deposits); or Banks unencumbered asset in BP account (reserves)

    Reserves created byrepayments of loans

    Reverse of exogenous money perspective

    (loans made possible by reserves)

    0 2 4 6 8 100

    50

    100

    150

    Bankers Principal

    Capitalist Debt

    Sum (=Money)

    Bankers Principal

    Capitalist Debt

    Sum (=Money)

    Money: no relending

    Years

    $

    0 2 4 6 8 100

    50

    100

    Bankers Principal

    Capitalist Debt

    Sum (=Money)

    Bankers Principal

    Capitalist Debt

    Sum (=Money)

    Money: relending

    Years

    $

    Next extension: creation of new money

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    Next extension: creation of new money

    Model so far has single injection of money KD(0)

    In actual economy, new money created endogenously allthe time

    How to model here?

    Simplest step: banks create new money at rate nm%

    p.a. New money generated in Bank Principal account1

    P m P m P P

    d dB n B n B

    B dt dt = =

    New money then loaned to firms

    Recorded as positive entry in credit (money) and debtaccount

    Subtracted from Bankers Principal account once paidto capitalists

    Creation of new money

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    Creation of new money

    Final model is:

    ( )p PD D D m PDd dd

    K r K r K R K BB dt n B= + + +

    ( )c p Y Y P C C D D C C m Pdd

    K r K r K R K PK PK W B B nt

    BBd

    = + + ++ + +

    ( )mD mP P P Pd

    B R K B dt n n BB + =

    ( ) = + 1Y c Y Y CdW PK rW W dt

    = Y c c Y Y D Cdd

    B r K r K rW B dt

    Model now has growing levels of income over time

    Creation of new money

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    Creation of new money

    All account balances grow over time

    0 20 40 60 80 1000

    1 106

    ?

    2 106

    ?

    3 106

    ?

    0

    5 104

    ?

    1 105

    ?

    1.5 105

    ?

    Capitalist DebtBankers Principal

    Bankers Income (RHS)

    Workers Income (RHS)

    Transaction account balances

    Year

    $

    As do incomes, etc.

    0 10 20 30 40 500

    2 106

    ?

    4 106?

    6 106

    ?

    0

    1 108

    ?

    2 108

    ?

    3 108

    ?

    4 108

    ?

    Flow of net profit

    Flow of wages

    Aggregate profit (RHS)

    Aggregate wages (RHS)

    Profit & wage flows and aggregates

    $

    But things arentquite this stable inthe real world

    Creation of new money

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    Creation of new money Components of US Money Supply 1959-2006:

    1955 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010

    0

    1000

    2000

    3000

    4000

    5000

    6000

    7000

    Money Stock

    M2-M1

    M1-Currency

    Currency

    US Money Stock & Components

    Year (Source: US Federal Reserve H6Hist1,2,5)

    US

    $

    Billions

    Latest data confirms Kydland-Prescott stats, endogenousmoney theory: credit drives Base Money

    But system very cyclical

    Conclusion

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    Conclusion

    Circuitists/Keynes/Schumpeter correct:

    Loan in pure credit system initiates sustainedeconomic activity

    Money in economy endogenously determined

    Debt an essential aspect of capitalist economy

    This simple linear model reaches equilibrium But with endogenous money, debt an essential aspect

    of capitalism

    Behavioural dynamics of capitalism can lead to cycles &

    excessive debt levels Next lecture

    The nonlinear, disequilibriumdynamics of debt