Brian Amiro - FluxNet-Canada - Drought Research Initiative
Brian Amiro - FluxNet-Canada - Drought Research Initiative
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