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TREES
THR O U G H T H E
                    THE STORY OF PRAIRIE DROUGHT TOLD BY TREE RINGS
Past dynamics ! Future behavior

                         PRESENT




         PAST                      FUTURE
         Precipitation             Drought risks
         Discharge                 Sustainable yield
         Lake level                Flood hazards
         Soil moisture
resource allocation
worst-case scenarios
Photograph: Manitoba Hydro
Photograph: Greg Brooks
Past dynamics ! Future behavior

                         PRESENT




         PAST                      FUTURE
         Precipitation             Drought risks
         Discharge                 Sustainable yield
         Lake level                Flood hazards
         Soil moisture
stationarity
A stationary time series is free of trends, shifts
or periodicity, and has statistical parameters that
remain constant through time.
Christopher Milly, Julio Betancourt, Malin Falkenmark, Robert
Hirsch, Zbigniew Kundzewicz, Dennis Lettenmaier, Ronald Stouffer

Stationarity is dead: whither
water management?
Science 319, 573-574, 2008
South Saskatchewan River at Saskatoon



relative change
in summer flow




Schindler and Donahue, 2006, PNAS
Annual discharge since 1924
                             + 58%
                                                                            NO TREND
                                          + 52%




                                                                  + 46%

                                                                      NO TREND
                                         NO TREND
                                                       NO TREND

                                                                          NO TREND
St. George, Journal of Hydrology, 2007
100
years of stream and lake gauging
CLIMATE HISTORY OF CANADA
                    Younger          Demise of Laurentide
                     Dryas                Ice Sheet

    20         16     12             8           4           0

                                                                 THOUSANDS OF
                                                                 YEARS AGO




                               Final Drainage
                              of Lake Agassiz
LAST GLACIAL                                              MODERN
  MAXIMUM                                               OBSERVATIONS
paleoclimatology
 the study of the Earth’s climate prior to the
 period of instrumental measurements
TREES AS BIOLOGICAL ARCHIVES
    How can records from the annual growth rings of trees be
1   interpreted as indicators of past environmental change?
TREES AS BIOLOGICAL ARCHIVES
    How can records from the annual growth rings of trees be
1   interpreted as indicators of past environmental change?

    PRAIRIE DROUGHTS SINCE AD 1500
    What tree rings tell us about severity, persistance and
2   dynamics of past droughts on the Prairies.
R ECO R D S F RO M ANCIEN T TR EES
Tree-ring display at elementary school




Photograph: Tom Swetnam
ARIZ
       ONA
A. E. Douglass
University of Arizona
The trees composing the forest rejoice
and lament with its successes and failures
and carry year by year something of its
story in their annual rings.

               A.E. DOUGLASS
Same environmental forcings




                            Similar
                    growth patterns
Photograph: Howard Arnott
North American
Tree-Ring
Chronologies
Western species
Ponderosa pine
Douglas-fir
Big cone douglas-fir
High elevation conifer
Mountain Hemlock
Other conifer


                         Eastern species
                           White oak group
                                   Hemlock
                                Baldcypress
                               Tulip poplar
                               Overcup oak
                           Northern red oak



Courtesy David Stahle
MEXICO
UNITED STATES
                Sonora
Arizona
                Baja California
California
Colorado
New Mexico
Nevada
Utah
Wyoming
~15
years of river gauge measurements
Colorado River Basin Water Management
National Academy of Sciences, 2007



     “... studies of past climate...[reveal] many periods
           when streamflow was lower than at any time
                in the past 100 years of recorded flows. ”
“rethink old assumptions”


       CHARLIE ESTER
       SALT RIVER PROJECT
Photograph: Tom Harlan
Photograph: Peter Kelly
Photograph: Kurt Kipfmueller
Photograph: Greg Pederson
Photograph: Erik Nielsen
Photograph: Erik Nielsen
53
Photograph: Erik Nielsen
Martin-Philippe Girardin
            Canadian Forest Service


                                                         Greg Pederson
                                                         United States Geological Survey




                                        David Sauchyn
Glen MacDonald                                                               Emma Watson
                                        University of Regina
         UCLA                                                          Environment Canada




           Erik Nielsen                       Jacques Tardif
           Manitoba Geological Survey         University of Winnipeg
Prairie tree-ring network
T R E E S A ND PRAI RI E DR OUGHT
Photograph: Dave Sauchyn
earlywood            latewood




                                cessation of growth
Photograph: Kevin Anchukaitis
“ The growth of trees is undoubtably controlled
  more by the movement of water than by the
  movement of any other single substance.”

                    HAL FRITTS
                    TREE RINGS AND CLIMATE
water stress

narrow ring    reduced photosynthesis



                 less cell expansion



                reduced cell division
never trust
   one tree
Prairie tree-ring network
2,860
   trees
889,862
    tree rings
Palmer
Drought
Severity
Index
69
755 m3/s

847 m3/s

809 m3/s

770 m3/s

823 m3/s

787 m3/s

901 m3/s
     3
“This
 must
  be
            ”
voodoo.
 Anonymous
water manager
good
  How            are
drought records from
     tree rings?
geography matters
southern Alberta
     10
                                                                              3

                                                                              2
       5
                                                                              1




                                                                                  Ringwidth
PDSI




       0                                                                      0

                                                                              -1
       -5
                                                                              -2

                                                                              -3
    -10
            1900              1920              1940     1960   1980   2000
                                                  Year (A.D.)
St. George et al., (2009), Journal of Climate
southern Alberta
     10
                                                                                 3

                                                                                 2
       5
                                                                                 1




                                                                                     Ringwidth
PDSI




       0                                                                         0

                                                                                 -1
       -5
                                                       r = 0.62                  -2

                                                                                 -3
    -10
            1900              1920              1940        1960   1980   2000
                                                  Year (A.D.)
St. George et al., (2009), Journal of Climate
755 m3/s

847 m3/s

809 m3/s

770 m3/s

823 m3/s

787 m3/s

901 m3/s
     3
DROUGHT HISTORY OF ALBERTA
     PDSI
6

4

2

0

-2

-4

-6

1500        1600   1700           1800   1900   2000

                          Year (AD)
DROUGHT HISTORY OF ALBERTA
     PDSI
6

4

2

0

-2

-4

-6

1500        1600   1700           1800   1900   2000

                          Year (AD)
bad
How        can
 drought get?
more persistent
more severe
more persistent
more severe
1720s
58 oN


                                                 1718 - 1722
         56 oN



        54 oN



   52 oN



 50 oN



48 oN


                                                                        oW
                                                                       90
                     114 oW                                     oW
                                                               96
                                    o              o
                                  108 W          102 W


                                                   Ringwidth anomaly
                                                       (deviations)
 !2                 !1        0         1    2
 -2                           0             +2
more persistent
more severe
1860s
1842 to 1876
                    Below average
Above average
CAPT. JOHN PALLISER
                88
“   The grass in this arid soil, always so scanty, was
    now actually swept away by the buffalo, who,
    assisted by the locusts had left the country as
    bare as if it had been overrun by fire; even at
    the edge of Sage Creek we could obtain but very


                               ”
    little water for our horses.

                          JOHN PALLISER, 1859




                                          89
Low reservoir




Photograph: Glen MacDonald
Prairie tree-ring network
NUMBER of tree ring records that track seasonal precipitation




 Autumn          Winter           Spring         Summer
    3              7                24             82


                                                  138 total
Medicine Hat, Alberta




Source: Environment Canada, Adjusted Historical Canadian Climate Data, 1895 – 2006
96
Past droughts and remote forcings
Janice Lough and Hal Fritts
The Southern Oscillation and tree rings: 1600 - 1961
Journal of Applied Meteorology 24, 1985




Roseanne D’Arrigo and Gordon Jacoby
A thousand year record of northwestern New
Mexico winter precipitation reconstructed from tree
rings and its relation to El Niño and the Southern
Oscillation
The Holocene 1, 1991




David Stahle and collaborators
Experimental dendroclimatic reconstruction of the
Southern Oscillation
Bulletin of the American Meteorological Society 79, 1998
ENSO and Prairie tree rings




                                                correlation with CTI
St. George et al., (2009), Journal of Climate
INSTRUMENTAL PDSI
                                      ENSO



+0.5




   0




       correlation coefficient
-0.5
St. George et al., (in preparation), Geophysical Research Letters
LE SS ONS L E A RNED
WORLD
DATA CENTER for
PALEOCLIMATOLOGY
Prairie tree-ring network
past
does the
 really matter?
climate change

YOU CAN TOUCH
100
years of stream and lake gauging
Common sense holds that what has really happened


CAN HAPPEN AGAIN

                             VIC BAKER
                 UNIVERSITY OF ARIZONA

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