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Title: Preliminary Observations of Water


1
Preliminary Observations of Water Carbon
DioxideFluxes Across anAlpine Treeline
  • Peter Blanken, Mark Williams
  • Department of Geography, University of Colorado,
    Boulder, Colorado
  • Russ Monson, Sean Burns
  • Department of Ecology and Evolutionary Biology,
  • University of Colorado, Boulder, Colorado
  • Kurt Chowanski, Todd Ackerman
  • INSTAAR, University of Colorado, Boulder,
    Colorado
  • John Knowles, Adriana Bailey
  • Department of Geography, University of Colorado,
    Boulder, Colorado

2
Introduction Background Sites Methods
Results Summary
  • goals and objectives
  • Can eddy covariance (plot-scale) measurements be
    made in complex terrain (1/3 cont. US)?
  • Determine the magnitude/behavior of water/carbon
    cycling in two important alpine ecosystems
    (alpine tundra subalpine forest).
  • Compare/contrast the differences dynamics of
    water/carbon cycling across the alpine treeline.

3
Introduction Background Sites Methods
Results Summary
  • observed changes at treeline
  • Changes in species composition
  • (e.g. Keller et al. 2000 Pauli et al. 2001
    Walther et al. 2005)
  • Increased growth rates
  • (e.g. Paulson et al. 2000 Motta Nola 2001)
  • Increased tree
  • establishment
  • (e.g. Körner 2003)
  • Changes in land
  • use and climate
  • (e.g. Beniston et al. 1997
  • Gehrig-Fasel et al. 2007)

4
Introduction Background Sites Methods
Results Summary
  • causes climate
  • Major climate shifts?
  • European Alps
  • 2 oC increase annual min. temps. last century
    (Beniston et al. 1997)
  • Swiss Alps
  • 2.5 oC increase
  • mean annual temp.
  • last century
  • (Gehrig-Fasel et al. 2007)

5
Introduction Background Sites Methods
Results Summary
  • causes land use
  • Major changes in land use?
  • Swiss Alps Alpine farming decreased considerably
    since mid 19th century
  • (Mather Fairbairn 2000)
  • Rocky Mountains
  • urbanization
  • pollution fire
  • suppression
  • logging mining
  • mtn. pine beetle

6
Introduction Background Sites Methods
Results Summary
  • causes land use climate

Western Italian Alps (Motta et al. 2006) .tree
establishment, and more in general the forest
dynamic, has been mainly controlled by human
land-use and that the tree growth has been mainly
climatically controlled. Swiss Alps
(Gehrig-Fasel et al., 2007) 90 new forest was
invasion into abandoned grasslands 10 true
upward shifts of local treeline (4 attributed to
recent climate warming)
7
Introduction Background Sites Methods
Results Summary
  • location

Tundra
3.8 km
Forest
8
Introduction Background Sites Methods
Results Summary
  • alpine tundra
  • Elevation 3523 m asl
  • Relatively flat ridge
  • High solar radiation
  • Low air temps. (-3.7 oC mean annual at 3743 m)
  • Mean annual P 930 mm, most as snow
  • Sparse, low vegn
  • LAI lt 1 (lt 0.5?)

9
Introduction Background Sites Methods
Results Summary
  • subalpine forest
  • Elevation 3050 m asl
  • 2 km east of treeline
  • average annual P 800 mm
  • Mean annual air temp 4 oC
  • Subalpine fir, Engelmann spruce, lodgepole pine
  • LAI 4.2

10
Introduction Background Sites Methods
Results Summary
  • eddy covariance

High-frequency vertical wind speed (w), H2O /
CO2 density (scalar s). Covariance of deviation
(') from 30-min means (-). Std. corrections.
11
Introduction Background Sites Methods
Results Summary
  • energy balance closure

12
Introduction Background Sites Methods
Results Summary
  • General meteorology
  • air temperature

13
Introduction Background Sites Methods
Results Summary
  • General meteorology
  • relative humidity

14
Introduction Background Sites Methods
Results Summary
  • General meteorology
  • horizontal wind
  • speed

15
Introduction Background Sites Methods
Results Summary
  • General meteorology
  • wind direction

Night
Day
Tundra
Forest
16
Introduction Background Sites Methods
Results Summary
  • Non-turbulent fluxes
  • net radiation

17
Introduction Background Sites Methods
Results Summary
  • Turbulent fluxes
  • sensible heat flux

18
Introduction Background Sites Methods
Results Summary
  • Turbulent fluxes
  • latent heat flux

19
Introduction Background Sites Methods
Results Summary
  • Turbulent fluxes
  • evaporative fraction

20
Introduction Background Sites Methods
Results Summary
  • cumulative evaporative
  • water loss

21
Introduction Background Sites Methods
Results Summary
  • Turbulent fluxes
  • CO2 flux

22
Introduction Background Sites Methods
Results Summary
  • Turbulent fluxes
  • CO2 flux

23
Introduction Background Sites Methods
Results Summary
  • cumulative carbon
  • surface gain

24
Introduction Background Sites Methods
Results Summary
  • correlations

25
Introduction Background Sites Methods
Results Summary
The tundra ___ is ___ than that at the forest
  • comparisons

26
Preliminary Observations of Water Carbon
DioxideFluxes Across anAlpine Treeline
Peter Blanken, Mark Williams Department of
Geography, University of Colorado, Boulder,
Colorado Russ Monson, Sean Burns Department of
Ecology and Evolutionary Biology, University of
Colorado, Boulder, Colorado Kurt Chowanski, Todd
Ackerman INSTAAR, University of Colorado,
Boulder, Colorado John Knowles, Adriana
Bailey Department of Geography, University of
Colorado, Boulder, Colorado
27
References
  • Beniston, M., Diaz, H.F. Bradley, R.S. 1997.
    Climatic change at high elevation sites An
    overview. Clim. Change 36 233-251.
  • Bolli, JC, Rigling A, Bugmann H. 2007. The
    influence of changes in climate and land-use on
    regeneration dynamics of Norway Spruce at the
    treeline in the Swiss Alps. Silva Fennica 41(1)
    55-70.
  • Gehrig-Fasel J , Guisan A, Zimmermann NE. 2007.
    Tree line shifts in the Swiss Alps Climate
    change or land abandonment? J. Veg. Sci., 18(4),
    571-582.
  • Keller, F., Kienast, F. Beniston, M. 2000.
    Evidence of response of vegetation to
    environmental change on high-elevation sites in
    the Swiss Alps. Reg. Environ. Change 1 70-77.
  • Körner, C. 2003. Alpine plant life Functional
    plant ecology of High Mountain ecosystems. 2nd.
    ed. Springer, Berlin- Heidelberg, DE.
  • Motta R, Morales M, Nola P 2006 Human land-se,
    forest dynamics and tree growth at the treeline
    in the Western Italian Alps. Annals of Forest
    Science, 63(7) 739-747.
  • Mather, A.S. Fairbairn, J. 2000. From floods to
    reforestationThe Forest Transition in
    Switzerland. Environ. History 6399-421.
  • Motta, R. Nola, P. 2001. Growth trends and
    dynamics in subalpine forest stands in the
    Varaita Valley (Piedmont, Italy) and their
    relationships with human activities and global
    change. J. Veg. Sci. 12 219-230.

28
References
  • Pauli, H., Gottfried, M. Grabherr, G. 2001.
    High summits of the Alps in a changing climate.
    The oldest observation series on high mountain
    plant diversity in Europe. In Walther, G.R.,
    Burga, C.A. Edwards, P.J. (eds.) Fingerprints
    of climate change. Adapted behaviour and shifting
    species ranges, pp. 139-149. Kluwer
    Academic/Plenum Publishers, NY, US.
  • Paulsen, J., Weber, U.M. Körner, C. 2000. Tree
    growth near tree line Abrupt or gradual
    reduction with altitude? Arct. Antarct. Alp. Res.
    32 14-20.
  • Walther, G.-R., Beissner, S. Burga, C.A. 2005.
    Trends in the upward shift of alpine plants. J.
    Veg. Sci. 16 541-548.

29
Extras.
30
Introduction Background Sites Methods
Results Summary
  • causes land use climate
  • Swiss Alps (Gehrig-Fasel et al., 2007)
  • 90 new forests ingrowth (invasion into abandoned
    grasslands) 10 true upward shifts of local
    treeline
  • Small fraction (4) attributed to recent climate
    warming (but likely
  • to increase)
  • Land abandonment
  • most dominant
  • driver

31
Introduction Background Sites Methods
Results Summary
  • causes land use climate

Western Italian Alps (Motta et al. 2006) An
analysis of all the data taken together in the
present study argues in favor of the fact that
the tree establishment, and more in general the
forest dynamic, has been mainly controlled by
human land-use and that the tree growth has
been mainly climatically controlled. (dendroecol
ogical methods,1850-present)
32
Introduction Background Sites Methods
Results Summary
  • summary
  • Two anthropogenic disturbances closely related to
    changes in treeline ecotones
  • Land use changes
  • Rapid climate change
  • Combination of both
  • Warming agriculture
  • abandonment (e.g.
  • Swiss Alps
  • (Bolli et al. 2007)

33
Introduction Background Sites Methods
Results Summary
  • location

34
Introduction Background Sites Methods
Results Summary
  • Non-turbulent fluxes
  • ground heat flux
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