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Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

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Page 1: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

Water Resources: Hydroclimatic Forensics Through Reanalysis

Bryson C. BatesLeader, Pathways to Adaptation Theme 24th June 2008

Climate Adaptation

Page 2: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

● Colleagues● Steve Charles (CSIRO)

● Richard Chandler (University College London)

● James Hughes (University of Washington)

● Eddy Campbell (CSIRO)

● Funding● Australian Climate Change Science Program

● Indian Ocean Climate Initiative

● South Eastern Australian Climate Initiative

Acknowledgments

Page 3: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

● The problem ● characteristics of multi-year drought

● short hydrologic record lengths < 100 years

● reliability of water supply systems – over-rated &/or over-allocation?

● ACRE applications● deriving the ‘recent’ envelope of natural climate

variability

● documenting atmospheric circulation changes that caused droughts prior to middle of 20th Century?

● putting anthropogenic climate change in context

● stochastic assessments of system reliability

Why ACRE & Water Resources?

Page 4: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

IWSS Dam Inflow Series

Cost of system expansion: 2 billion AUD spent over last decade

Page 5: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

Rules; What Rules?

● Traditional water planning based on assumption of stationarity (constant mean, variance & autocorrelation)

● Observed changes in means, variance & extremes – old rules are breaking down

● Trends or shifts: if, when & why?

● Regimes (periods exhibiting stationarity)?

● Use all of the record; or which part?

Page 6: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

● Dam inflow series● trend?

● change points & regimes?

● Stochastic downscaling● changes in atmospheric circulation variables?

● changes in frequencies of synoptic types?

● At-site precipitation● changes in occurrence?

● changes in amounts?

Experimental Design

Page 7: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

IWSS Inflows

Year

Inflo

w (

Gl)

1920 1960 2000

10

10

01

00

0 a

h

Pro

ba

bili

ty v

alu

e

2 6 10

0.0

00

.01

0.0

20

.03 b

h

p-v

alu

e

6 8 10 12

0.1

0.2

0.3

Page 8: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

Site Map

Page 9: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

Nonhomogeneous Hidden Markov Model

● Observed process: sequence of regional precipitation occurrence patterns Rt: t = 1, …, T

● Hidden discrete-valued process: sequence of weather types (or states) St

● State to state transitions driven by atmospheric information (predictors) Xt

Page 10: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

● Season: May to October

● Period of interest: 1958 – 2007

● Fitting: sequential estimation – BIC

● Number of weather states: 6

● Atmospheric predictors:● mean MSLP

● N-S MSLP gradient

● DTd850 = T850 – Td850

● 1st canonical variate

● Testing: split sample & physical scrutiny

NHMM Details

Page 11: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

Interannual & Split Sample Validation

Fitting Validation

Fitting Validation

Dryspell

Wetspell

Validation Fitting

Observed daily rainfall

Sim

ula

ted

da

ily

ra

infa

ll

Page 12: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

Atmospheric Predictors

(1983:2007)

versus

(1958:1982)

Page 13: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

Synoptic Typing & Frequency

199819781958

00.

20.

4

1958 19981978

00.

20.

4

Pro

bab

ility

Pro

bab

ility

Type 3: Wet West & Central Type 5: Dry Everywhere

Southwest Australia

Page 14: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

● Overall reduction in precipitation occurrence – changes most notable in west of the region

● Most sites exhibit reductions in mean wet-day precipitation amounts

● Some indication of increase in precipitation intensity in SW corner of the region

At-Site Precipitation

1958 to 2007

Page 15: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

SE Australia

Total River Murray System Inflows (including Darling River)Modelled Annual Inflows - current conditions

0

5 000

10 000

15 000

20 000

25 000

30 000

1892 1902 1912 1922 1932 1942 1952 1962 1972 1982 1992 2002

Ann

ual I

nflo

w (

GL)

Long-term Average Inflow (11 200 GL/yr)

Average Inflows during Drought Periods

5 400 GL/yr4 150 GL/yr

6 300 GL/yr

Drivers of Federation, WWII & current droughts?

Page 16: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

Water planners confronting historically-unprecedented drought non-stationarity in dam inflow series apparent increase in climatic risk due to

anthropogenic climate change

ACRE can assist water planners by providing additional information about envelope of

natural climate variability – system reliability providing explanations for the causes of major

droughts prior to middle of 20th century putting anthropogenic climate change in context –

if & when will the envelope of natural climate variability be breached (approximately)?

Concluding Remarks

Page 17: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

NHMM vs. Null Model

Occurrence Amounts

Period SSM SSE Er SSM SSE Er

1958-77 10306 15567 0.398 919753 2198732 0.295

1978-92 7712 10084 0.433 687208 1640354 0.295

1993-98 3197 4187 0.433 280207 727790 0.278

Page 18: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

SW Australia

0

20

40

60

80

100

120

Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov DecMonth

mm

1925-1975

1976-2003

Indian Ocean Climate Initiative

Informed Adaptation

Page 19: Water Resources: Hydroclimatic Forensics Through Reanalysis Bryson C. Bates Leader, Pathways to Adaptation Theme 24 th June 2008 Climate Adaptation

ACRE Workshop 2008

"Dry Everywhere" "Wet Everywhere"

Weather Type Probabilities: SE MDB

SEACI