Esa12 extreme climatic events drive mammal irruptions

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Aaron C. Greenville, Glenda M. Wardle and Chris R. DickmanDesert Ecology Research Group

School of Biological SciencesUniversity of Sydney

Extreme climatic events drive mammal irruptions: 100-year trends in desert rainfall

and temperature

Extreme climatic events

Current

Climate parameter

Future

Extreme climate: spatial scale

IPCC (2007)

CSIRO & BOM (2012)

Global

Regional

Local

Aims

• To determine if extreme climate events have changed at similar rates to median events over local and regional scales.

• Determine if the frequency of large rainfall events increased.

• Are extreme climate events important for drive small mammal populations?

Methods: study region

• 11 weather stations for annual rainfall.• 4 weather stations for annual min and max

temperatures.• Small mammal trapping from Ethabuka Reserve.

Methods: climate

• Quantile regressions at 5,10, 50, 90 and 95th

• Poisson GLMM

Min Temp

1890 1920 1950 1980 2010

10

11

12

13

14

15

Alice Springs

Year

An

nu

al

min

imu

m t

emp

era

ture

C)

1890 1920 1950 1980 2010

14

15

16

17

18

19

Boulia

Year

An

nu

al

min

imu

m t

emp

era

ture

C)

1938 1962 1986 2010

13.5

14.0

14.5

15.0

15.5

16.0

Oodnadatta

Year

An

nu

al

min

imu

m t

emp

era

ture

C)

1965 1980 1995 2010

14

15

16

17

Birdsville

Year

An

nu

al

min

imu

m t

emp

era

ture

C)

P < 0.05

Max Temp

1885 1910 1935 1960 1985 2010

27

28

29

30

Alice Springs

Year

An

nu

al

ma

xim

um

tem

per

atu

re (

° C

)

1890 1910 1930 1950 1970 1990 2010

30

31

32

33

34

Boulia

Year

An

nu

al

ma

xim

um

tem

per

atu

re (

° C

)

1960 1970 1980 1990 2000 2010

29

30

31

32

Birdsville

Year

An

nu

al

ma

xim

um

tem

per

atu

re (

° C

)

1940 1950 1960 1970 1980 1990 2000 2010

27

28

29

30

31

Oodnadatta

Year

An

nu

al

ma

xim

um

tem

per

atu

re (

° C

)

P < 0.05

Rainfall

P < 0.05

1930 1950 1970 1990 2010

50

180

310

440

570

700

Bedourie

Year

An

nu

al

Ra

infa

ll (

mm

)

1890 1920 1950 1980 2010

50

180

310

440

570

700

Glenormiston

Year

An

nu

al

Ra

infa

ll (

mm

)

1905 1940 1975 2010

100

200

300

400

Oodnadatta

Year

An

nu

al

Ra

infa

ll (

mm

)

1870 1905 1940 1975 2010

200

400

600

800

Alice Springs

Year

An

nu

al

Ra

infa

ll (

mm

)

Extreme high eventsExtreme low eventsMedian events

Rainfall

Results: climate

• Decrease in years between extreme rainfall events (>95th quantile).

• GLMM estimate: -0.54, SE = 0.21, z value = -2.54, P = 0.01.

Methods: small mammals

• 22 years live-trapping data:

– rodents and dasyurids.

• Threshold relationship.

• Piecewise regression.

Results: small mammals

Rodents

Dasyurids

Summary• Extreme and median temperatures have

increased at both spatial scales.

• Magnitude of extreme rainfall events have increased, droughts getting drier, but variable across the region.

• Increased frequency of large rainfall events.

• Populations driven by extreme climate events.

Implications

• Increased wildfire.

• Establishment of introduced

species.

• Indirect effects and new

interactions.

• For more: Ecology and Evolution 2012; 2(11): 2645–2658.

Acknowledgements• Bobby Tamayo and the DERG team.• All our volunteers.• Bush Heritage Australia.• Bedourie Hotel.• ARC and APA.

Volunteer info at:http://sydney.edu.au/science/biology/sites/dickmanlab/index.shtml

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