stochastic climate model

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tochastic climate model dy ' dt + y ' τ = ν ( t) y’ = some climate variable (PERTURBATION) characteristic timescale (“MEMORY”) t “noise” forcing lest way of representing a system with memory and r g . a first-order autoregressive process, or AR(1) red noise”

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Stochastic climate model. a.k.a. a first-order autoregressive process, or AR(1) or “red noise”. y’ = some climate variable (PERTURBATION) t = characteristic timescale (“MEMORY”) n( t )= “noise” forcing. Simplest way of representing a system with memory and random - PowerPoint PPT Presentation

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Page 1: Stochastic climate model

Stochastic climate model

dy'

dt+y '

τ= ν (t)

y’ = some climate variable (PERTURBATION) characteristic timescale

(“MEMORY”)t “noise” forcing

• Simplest way of representing a system with memory and random forcing

• a.k.a. a first-order autoregressive process, or AR(1) or “red noise”

Page 2: Stochastic climate model

But can write:

dy

dt=y t − y t−1

Δt

So:

y t+1 − y tΔt

+y tτ

= a0υ t

Page 3: Stochastic climate model

In discretized form (i.e., time stepping in increments of t):

y't = a1y 't−Δt +a0ν ta1 = 1- t/t = noise - a random event, (normalized)a0 = amplitude of noise.

memory randomforcing

currentstate

This is called a first order autoregressive process , or AR(1)Also known as ‘red noise’ process

The element of random noise makes it a stochastic process

Page 4: Stochastic climate model

What is noise?

Ex: Daily maximum temperature at SeaTac airport in 2002:

Page 5: Stochastic climate model

Anomalous temperature

• Now consider departure from normal (i.e., remove the annual cycle)

Page 6: Stochastic climate model

Histogram of anomalies

• Temperatures are most likely to be near normal, but there are a few days with extreme departures from normal.

Page 7: Stochastic climate model

No memory (uncorrelated)

= 5 yrs

= 1 yrs

= 25 yrs

= 0 yrs

Time (yrs) Long memory

Stochastic models with different characteristic timescales

• The greater the memory, the longer the timescale of the variability (i.e., length of interval above or below average).

Page 8: Stochastic climate model

What does the spectrum of variability look like?How does the power (or energy) in the time series vary as a function of frequency (or period)?

Period in years (i.e. 1/frequency) note the log scale.

Pow

erPower spectrum

Time Series

= 0 yrs (no memory)

Time (yrs)

For no memory, energyIs the same at all periods (frequencies). Hence ‘white noise’.

Page 9: Stochastic climate model

What does the spectrum of variability look like?How does the power (or energy) in the time series vary as a function of frequency (or period)?

Period in years (i.e. 1/frequency) note the log scale.

Pow

erPower spectrum

Time Series

= 1 yrs

Time (yrs)

Increased memoryincreases powerat longer periods:hence “red” noise

Page 10: Stochastic climate model

What does the spectrum of variability look like?How does the power (or energy) in the time series vary as a function of frequency (or period)?

Period in years (i.e. 1/frequency) note the log scale.

Pow

erPower spectrum

Time Series

= 5 yrs

Time (yrs)

Increased memoryincreases powerat longer periods:hence “red” noise

Page 11: Stochastic climate model

What does the spectrum of variability look like?How does the power (or energy) in the time series vary as a function of frequency (or period)?

Period in years (i.e. 1/frequency) note the log scale.

Pow

erPower spectrum

Time Series

= 25 yrs

Time (yrs)

Increased memoryincreases powerat longer periods:hence “red” noise

Page 12: Stochastic climate model

P( f ) =ao

2

1+ (2πfτ )2

Equation for power spectrum of a red noise process

P(f) = power per unit frequency, f

• Can also show (how?) that half the energy in the time seriesoccurs at periods which are 2 or longer.

See, e.g., Jenkins and Watts, 1968

By analogy: Pendulum time constant =

l

gl = length of stringg = gravity

Period of oscillation =

2πl

g

Page 13: Stochastic climate model

Example from last time: Pacific Decadal Oscillation. Even though variability is decadal, time series consistent with a red noise processwith a timescale of ~1 yr.

Because any geophysical system at all will always have random noise, and some inertia (a tendency to remember previous states), red noiseshould always be the default expectation

Page 14: Stochastic climate model

PDO index (top panel) compared to 2 random realizations of a an AR(1) process with a characteristic time scale of 1.2 years

-note the apparent cycles

Page 15: Stochastic climate model