thoughts on assessing decadal precipitation variations as surrogate forecasts

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THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS Jeanne M. Schneider USDA Agricultural Research Service Grazinglands Research Laboratory El Reno, OK

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THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS. Jeanne M. Schneider USDA Agricultural Research Service Grazinglands Research Laboratory El Reno, OK. - PowerPoint PPT Presentation

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Page 1: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

THOUGHTS ON ASSESSING DECADAL PRECIPITATION

VARIATIONS AS SURROGATE FORECASTS

THOUGHTS ON ASSESSING DECADAL PRECIPITATION

VARIATIONS AS SURROGATE FORECASTS

Jeanne M. SchneiderUSDA Agricultural Research Service

Grazinglands Research Laboratory

El Reno, OK

Jeanne M. SchneiderUSDA Agricultural Research Service

Grazinglands Research Laboratory

El Reno, OK

Page 2: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

But first, a quick review/tutorial on probability of exceedance functions….which illustrates why someone might

want to use them.

But first, a quick review/tutorial on probability of exceedance functions….which illustrates why someone might

want to use them.

Page 3: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

0

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12

1970 1975 1980 1985 1990 1995 2000

May Precipitation at Kingfisher OK 1971-2000

Year

30 years of data

Page 4: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

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2

4

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1970 1975 1980 1985 1990 1995 2000

May Precipitation at Kingfisher OK 1971-2000

Year

30 years of data

average = 4.91"

Page 5: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

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Ranked May Precipitation at Kingfisher OK 1971-2000

"Below"Tercile

"Normal"Tercile

"Above"Tercile

33% 33% 33%Odds to be in tercile:

Page 6: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

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20

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50

60

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100

0 2 4 6 8 10 12

May Precipitation at Kingfisher OK 1971-2000

Probability of Exceedance (%)

Precipitation (inches)

Probability of Exceedance = 1 - (cumulative probability density function)

"a posteriori"

Page 7: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

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0 2 4 6 8 10 12

May Precipitation at Kingfisher OK 1971-2000

Precipitation (inches)

Probability of E

xceedance (%

)

67%

3.2”

“Two in three chance for more than 3.2 inches.”

Page 8: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

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0 2 4 6 8 10 12

May Precipitation at Kingfisher OK 1971-2000

Precipitation (inches)

Probability of E

xceedance (%

)

67%

3.2” 4.2”

50%

“Two in three chance for more than 3.2 inches.”

“Fifty-fifty chance for more than 4.2 inches.”

Page 9: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

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10

20

30

40

50

60

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0 2 4 6 8 10 12

May Precipitation at Kingfisher OK 1971-2000

Precipitation (inches)

Probability of E

xceedance (%

)

67%

33%

3.2” 6.1”4.2”

50%

“Two in three chance for more than 3.2 inches.”

“Fifty-fifty chance for more than 4.2 inches.”

“One in three chance for more than 6.1 inches.”

Page 10: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

0

10

20

30

40

50

60

70

80

90

100

0 2 4 6 8 10 12

May Precipitation at Kingfisher OK 1971-2000

Precipitation (inches)

Probability of E

xceedance (%

)

67%

33%

3.2” 6.1”4.2”

50%

“Two in three chance for more than 3.2 inches.”

“Fifty-fifty chance for more than 4.2 inches.”

“One in three chance for more than 6.1 inches.”

If you can associate a potential financial loss with each of these outcomes, then you have a definition of “risk”.

Page 11: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS
Page 12: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

So, what do we plan to do when the NOAA/CPC forecasts offer nothing beyond

the 30-year climatology ("EC")?

Or when the forecast skill is so low as to preclude practical use?

Do we have any other options for climate-conditioned decision support for agriculture in

areas where ENSO impacts are marginal?

So, what do we plan to do when the NOAA/CPC forecasts offer nothing beyond

the 30-year climatology ("EC")?

Or when the forecast skill is so low as to preclude practical use?

Do we have any other options for climate-conditioned decision support for agriculture in

areas where ENSO impacts are marginal?

Continuing where we left off last year….Continuing where we left off last year….

Page 13: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Annual Precipitation in Central Oklahoma

Year

Precipitation [in] Annual Precipitation

5-yr weighted average

Dry PeriodsWet Periods

CD3405; 1895-200415

25

35

45

55

1895 1915 1935 1955 1975 1995

Page 14: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

0

0.2

0.4

0.6

0.8

1

0 1 2 3 4 5 6 7 8 9 10 11

Dry periods1900-19041909-19171936-19391952-19561963-19721976-1980

Wet periods1905-19081941-19451957-19611982-2000

Probability of Exceedance of September PrecipitationClimate Division 3405; Central Oklahoma; 1895-2005

Pro

b.

of

Exc

eed

ance

Precipitation [in/mo]

Dry PeriodsMean = 3.2 [in]

38 Years

Wet PeriodsMean = 4.6 [in]

33 Years

1895-2005Mean = 3.7 [in]

111 Years

Preliminary data, subject to revision

USDA-ARS-GRL

Page 15: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Assume that the earth/ocean/atmosphere

system behaves as a chaotic system with a

very large number of degrees of freedom, but

that the net expression of that chaos on the

precipitation processes at any location can be

usefully described as a small collection of

states (dry, wet, perhaps transition), where

each state persists for several years.

Assume that the earth/ocean/atmosphere

system behaves as a chaotic system with a

very large number of degrees of freedom, but

that the net expression of that chaos on the

precipitation processes at any location can be

usefully described as a small collection of

states (dry, wet, perhaps transition), where

each state persists for several years.

A faint flavor of chaotic dynamics:A faint flavor of chaotic dynamics:

Page 16: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Climate changes:

To what degree does the past predict the future?

Data is incomplete and imperfect:

if a predictive signal exists in the phenomena,

can we discern it in the record?

Where, when, and how do we search for the signal?

And on and on, ad nauseum….

Climate changes:

To what degree does the past predict the future?

Data is incomplete and imperfect:

if a predictive signal exists in the phenomena,

can we discern it in the record?

Where, when, and how do we search for the signal?

And on and on, ad nauseum….

But there are problems with statistical approaches to climate forecasts:

But there are problems with statistical approaches to climate forecasts:

Page 17: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

However, as has been noted by several presenters already:

"….decisions have to be made".

However, as has been noted by several presenters already:

"….decisions have to be made".

Page 18: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

We need monthly, location specific guidance relative to precipitation for producers,

agricultural extension agents, and others involved with small to medium scale

agriculture.

To be useful in the near term, that guidance needs to be built using existing data and tools.

We need monthly, location specific guidance relative to precipitation for producers,

agricultural extension agents, and others involved with small to medium scale

agriculture.

To be useful in the near term, that guidance needs to be built using existing data and tools.

The good news is that we have a couple of simplifying constraints:The good news is that we have a couple of simplifying constraints:

Page 19: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Can we, or can we not, produce probabilistic

monthly precipitation guidance for specific

locations that is more reliable than the

standard 30-year climatology,

given data and tools currently in hand?

Can we, or can we not, produce probabilistic

monthly precipitation guidance for specific

locations that is more reliable than the

standard 30-year climatology,

given data and tools currently in hand?

The Acid Test:The Acid Test:

Page 20: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Klaus Wolter'sExperimental Climate Divisions

Klaus Wolter'sExperimental Climate Divisions

http://www.cdc.noaa.gov/people/klaus.wolter/ClimateDivisions/http://www.cdc.noaa.gov/people/klaus.wolter/ClimateDivisions/

Page 21: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Klaus Wolter'sExperimental Climate Divisions

Klaus Wolter'sExperimental Climate Divisions

http://www.cdc.noaa.gov/people/klaus.wolter/ClimateDivisions/http://www.cdc.noaa.gov/people/klaus.wolter/ClimateDivisions/

Because these are based on precipitation variability, I will use these experimental climate divisions to define

"location specific".

Page 22: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Century-scale monthly data from PRISMCentury-scale monthly data from PRISM

http://www.prism.oregonstate.edu/http://www.prism.oregonstate.edu/

Select a grid point near the center of each experimental forecast division, and use the 103-year long PRISM

time series data to define the decadal variations in precipitation.

I will test different lengths of base record, de-trending options, and

definitions of state and persistence.

Page 23: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Use individual station data to test the reliability

of both the decadal and 30-year climatology

as probabilistic forecasts over the last decade.

Given the short period, use as many stations

as possible within each experimental forecast

division for the assessment.

Use individual station data to test the reliability

of both the decadal and 30-year climatology

as probabilistic forecasts over the last decade.

Given the short period, use as many stations

as possible within each experimental forecast

division for the assessment.

NOAA/NCDC Coop Station DataNOAA/NCDC Coop Station Data

Page 24: THOUGHTS ON ASSESSING DECADAL PRECIPITATION VARIATIONS AS SURROGATE FORECASTS

Conceptually, this is so simple it can be done graphically for each month and

experimental forecast division.But realistically,

we will build assessment PoEsfrom the station data, and adapt or

develop measures of relative reliability.

Conceptually, this is so simple it can be done graphically for each month and

experimental forecast division.But realistically,

we will build assessment PoEsfrom the station data, and adapt or

develop measures of relative reliability.

More next year….