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Brian Amiro - FluxNet-Canada - Drought Research Initiative

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FLUXNET-CANADA<br />

• University/government science network<br />

•Measurements of CO 2<br />

exchange between<br />

forests & peatlands and the atmosphere<br />

• Part of the international Fluxnet<br />

network (300+ sites internationally)<br />

•2002- 2007<br />

•Now: The Canadian Carbon Program


Canadian Carbon Program<br />

CFCAS Funded 2007-2010.<br />

$1.5 M/year<br />

Fundamental CCP Science Questions:<br />

What are the magnitudes and distributions of<br />

Canadian and North American carbon sources and<br />

sinks on monthly, seasonal, and inter-annual timescales<br />

How can we best estimate them<br />

What are the processes controlling their dynamics<br />

and can they be manipulated


Evapotranspiration is also measured at each flux tower<br />

BERMS (Boreal Ecosystem<br />

<strong>Research</strong> and Monitoring<br />

Sites)


Annual Precipitation 1999 to 2006<br />

(The horizontal lines show percentiles<br />

from Prince Albert, 1900-2000)<br />

Aspen<br />

Black Spruce<br />

Jack Pine<br />

← Deluge →<br />

← <strong>Drought</strong> →


Annual Evapotranspiration 1999 to 2006<br />

(adjusted by ~ +15% for energy-balance closure)<br />

Aspen (393 ± 80) Black Spruce (374 ± 33) Jack Pine (303 ± 21)<br />

<strong>Drought</strong>


Integrated Root-Zone Soil Water<br />

(dashed lines indicate frozen soil)<br />

Aspen (0-1.2m) Black Spruce (0-0.3m) Jack Pine (0-1.5m)


Young successional forests: mixed<br />

4<br />

Forest 1989<br />

Forest 1998<br />

Evapotranspiration (mm d -1 )<br />

3<br />

2<br />

1<br />

0<br />

2001 2002 2003 2004 2005<br />

Year


Summary of drought impacts<br />

• ET decreased in mature and young<br />

successional forests<br />

• ET less affected in very young forests<br />

(lower water demand)<br />

• Near surface soil moisture decreases<br />

variable, depending on site


SOIL MOISTURE 0-30 cm depth

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