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Decadal Signals In Precipitation
Graphics supporting a February 20 lecture at the University of Arizona's Laboratory of Tree-Ring Research.
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- Slide 1: The prominence of decadal variability
in North American precipitation
S c ott St. G eorge
Geological Survey of Canada
Toby A ult
University of Arizona
- Slide 3: Greg McCabe, Michael Palecki, and
Julio Betancourt, 2004:
Pacific and Atlantic Ocean
influences on multidecadal
drought frequency in the
United States
PNAS 12, 4136 - 4141
- Slide 4: Here be
decadal variability
Decadal variability in precipitation or
drought as a signal detection problem
Terrestrial climate records often
processed to emphasize D2M timescales4
- Slide 5: Does it matter at the regional scale?
5
- Slide 6: 1920 1940 1960 1980 2000
Decadal variance
30%
Decadal variance
5%
1920 1940 1960 1980 2000
- Slide 7: Where is decadal variability
in precipitation strong?
- Slide 8: Dan Cayan, Michael Dettinger,
Henry Diaz, and Nick Graham,1998:
Decadal variability of
precipitation over
western North America.
Journal of Climate 11, 3148-3166
- Slide 9: Methods
Photo: Christos_m2001
- Slide 10: PDSI
Temperature
Precipitation Streamflow
Storms
Rain/snow
- Slide 11: Gridded (0.5 deg) monthly
precipitation, Climate Research
Unit, University of East Anglia
Period of record: 1901 - 2002
- Slide 12: Decadal variability
Decadal variabil
Decadal varia
Decadal v
- Slide 15: Noise
Interannual
Trend
Multidecadal
Decadal
- Slide 17: What did we find?
Photo: futureshape
- Slide 18: Slides missing*
* Thank goodness
- Slide 19: Winter decadal
0% 10% 20% 30% variance
- Slide 20: Autumn decadal
0% 10% 20% 30% variance
- Slide 21: Annual multidecadal
0% 10% 20% 30% variance
- Slide 22: Northern California precipitation
- Slide 23: Northern California precipitation
Decadal variance = ~30 percent
- Slide 24: D2M ‘hotspots’
- Slide 25: “Decadal-scale fluctuations are
crucial because they control water
supplies, affect biota, and may
modulate higher-frequency events
such as floods and drought.”
Dan Cayan and colleagues [1998]
- Slide 26: Decadal hotspot - Oregon/California
- Slide 27: Northern California
- Slide 28: Sacramento River
Photo: Patty Colmer
- Slide 29: Northern California
- Slide 30: Northern California
- Slide 31: Photo: California Department of Water Resources
Levee break, Sacramento basin
- Slide 32: 1915 levee break
Photo: California Department of Public Works
Courtesy Joan Florsheim
- Slide 33: Northern California
- Slide 34: Northern California
- Slide 35: Decadal hotspot - Minnesota
- Slide 36: Minnesota
- Slide 37: Mississippi River at Minneapolis
Photo: Mulad
- Slide 38: Minnesota
- Slide 39: Minnesota
- Slide 40: Minnesota
- Slide 41: Mech et al. (1987):
Does high snow over
consecutive winters have a
cumulative, negative, effect
on the viability of moose
offspring?
- Slide 42: Minnesota
- Slide 43: Minnesota
- Slide 44: Minnesota
- Slide 45: Associations with
major climate modes
- Slide 46: It’s complicated.
46
- Slide 47: Winter precipitation and
the PDO
- Slide 48: Winter precipitation and
the PDO
- Slide 49: Three main points
49
- Slide 50: location and
seasonality
make a big difference
50
- Slide 51: D2M propagates into
hydrology* and
ecology**
* clearly
** maybe
51
- Slide 52: Is it a coincidence that D2M
variability is strongest in
the ENSO-PDO
null?
52
- Slide 53: Thank you
Julio Betancourt Dave Meko
Julia Cole Joellen Russell
Susan Pullan Mike Wallace
Mike Mann Connie Woodhouse
Support
Manitoba Hydro
Natural Resources Canada
National Science Foundation
- Slide 54: S co t t St. G e o r g e Toby Au lt
Geological Survey of Canada University of Arizona
sstgeorg@nrcan.gc.ca tault@email.arizona.edu