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Drought, restoration, and evapotranspiration in the Middle<br />

Rio Grande riparian corridor, New Mexico<br />

James Cleverly, Michael Slusher, James Thibault, Jennifer Schuetz,<br />

and Clifford Dahm<br />

*UNM Hydrogeoecology, http://sevilleta.unm.edu<br />

sevilleta.unm.edu/~cleverly


Populus deltoides ssp. wislizenii<br />

(Rio Grande Cottonwood)<br />

Native<br />

Exotic<br />

Elæagnus angustifolia (Russian Olive)<br />

Tamarix chinensis (Tamarisk)


Evapotranspiration<br />

Atmosphere<br />

Sensors<br />

Phreatophytes<br />

Shallow Aquifer<br />

Floodwater and soil water evaporation (exposed & shaded, sand & clay)


Video: P Sprott<br />

3-D Eddy Covariance<br />

R n : Net Radiation (incoming energy flux)<br />

λET: Latent Heat Flux (evapotranspiration energy flux)<br />

H: Sensible Heat Flux (temperature gradient flux)<br />

G: Ground Heat Flux (soil heat flux)<br />

R n - λET -H -G = closure*


Tower-equipped<br />

Sites<br />

Flooding Russian-olive<br />

Nonflooding Tamarisk<br />

Flooding<br />

Cottonwood<br />

Nonflooding<br />

Cottonwood<br />

Flooding Tamarisk


Seasonal Drought<br />

Year<br />

Winter/Spring Summer<br />

2000 normal-dry very dry<br />

2001 normal-wet normal<br />

2002 dry very dry<br />

2003 very dry very dry<br />

2004 normal-dry normal-dry<br />

2005 record wet very dry


Annual ET<br />

ET<br />

150<br />

130<br />

110<br />

90<br />

70<br />

50<br />

2000 2001 2002 2003 2004 2005<br />

Cottonwood/Saltcedar/Russian Olive<br />

Cottonwood/Willow/(Alfalfa)<br />

Russian Olive/Willow<br />

Monospecific Tamarisk<br />

Tamarisk/Saltgrass<br />

Year<br />

• Drought is associated with ET decline in all but invaded cottonwood forest<br />

• ET increased before cessation of drought at two sites<br />

• Following drought, ET at all mesic riparian sites were equivalent


Wait a minute, isn’t Tamarisk<br />

supposed to be drought tolerant<br />

ET<br />

150<br />

130<br />

110<br />

90<br />

70<br />

50<br />

2000 2001 2002 2003 2004 2005<br />

Year<br />

ET<br />

(mm/day)<br />

6.2<br />

5.7<br />

5.2<br />

4.7<br />

4.2<br />

3.7<br />

3.2<br />

2000 2001 2002 2003 2004 2005<br />

Dense Tamarisk<br />

Tamarisk/Saltgrass<br />

Season length (days):<br />

Year<br />

2000 2001 2002 2003 2004 2005<br />

T 211 198 181 209 192 209<br />

T+SG 202 193 181 196 206 198


Why did ET remain stable at the<br />

invaded cottonwood site<br />

ET<br />

150<br />

130<br />

110<br />

90<br />

70<br />

50<br />

-2<br />

Leaf Chlorophyll Content (mg m )<br />

P. deltoides<br />

T. chinensis<br />

E. angustifolia<br />

Depth to Groundwater (cm)<br />

700<br />

600<br />

500<br />

400<br />

300<br />

200<br />

100<br />

0<br />

125<br />

150<br />

175<br />

200<br />

225<br />

250<br />

275<br />

300<br />

325<br />

350<br />

375<br />

a<br />

ad<br />

cd<br />

bc<br />

bc<br />

b<br />

b b<br />

e<br />

Albuquerque Belen Bosque del Apache<br />

2000 2001 2002 2003 2004 2005<br />

Year


Understory Restoration<br />

150<br />

130<br />

ET<br />

110<br />

90<br />

70<br />

50<br />

2000 2001 2002 2003 2004 2005<br />

Year


Restoration water salvage<br />

♦ Understory Russian olive and<br />

saltcedar removed from South<br />

Valley Albuquerque cottonwood<br />

forest between 2003 and 2004<br />

growing seasons<br />

♦ First year reduction in ET of 9%<br />

while other sites increasing by 12%<br />

(total = -21% or -26 cm/yr)<br />

♦ Second year increase matched<br />

increase at other sites: 0 cm/yr<br />

140<br />

120<br />

Albuquerque's South Valley: cottonwood<br />

La Joya: Russian olive/coyote willow<br />

San Acacia: saltcedar/saltgrass<br />

Bosque del Apache: monospecific saltcedar thicket<br />

Non-native native understory cleared<br />

ET (cm/yr)<br />

100<br />

80<br />

60<br />

2003 2004 2005<br />

Year


Increased Tamarisk ET during<br />

150<br />

drought<br />

130<br />

ET<br />

110<br />

90<br />

70<br />

12<br />

Depth to Groundwater (cm)<br />

BDAS 2003<br />

ET (mm/day)<br />

50<br />

2000 2001 2002 2003 2004 2005<br />

Year<br />

30<br />

10<br />

-50<br />

0<br />

25<br />

8<br />

50<br />

PPT (mm/day)<br />

ET<br />

20<br />

6<br />

15<br />

4<br />

100<br />

150<br />

200<br />

GW<br />

10<br />

250<br />

2<br />

300<br />

5<br />

0<br />

350<br />

50 100 150 200 250 300 350<br />

Day of Year


Tamarisk and Groundwater<br />

♦ Depth to groundwater does not limit<br />

transpiration:<br />

♦ when the water table is 10-m below the surface<br />

(Horton et al 2001)<br />

♦ when the water table is 25-m below the<br />

surface (Gries et al 2003)<br />

♦ Tamarisk found in sites with seasonally<br />

variable depth to groundwater<br />

(Lite & Stromberg 2005)


Groundwater recession<br />

1 Draining begins, soil too<br />

saturated for taproot<br />

elongation, uptake continues<br />

at original capillary fringe<br />

Falling<br />

2<br />

1<br />

Rising<br />

-7.5 -5 -2.5 0 2.5 5<br />

dWT/dt (9-day average, cm/day)<br />

3<br />

9<br />

8<br />

7<br />

6<br />

5<br />

4<br />

ET (9-day average, mm/day)<br />

3 Uptake continues at<br />

deeper water table, uptake<br />

at original water table<br />

curtailed by soil drying<br />

2 Taproot growth exploits<br />

deeper water table, uptake<br />

continues at or near original<br />

capillary fringe<br />

(Cleverly et al 2006)


Conclusions<br />

120<br />

ET (cm/yr)<br />

100<br />

80<br />

Cottonwood,<br />

Tamarisk, &<br />

Russian olive<br />

CW<br />

Monospecific<br />

Tamarisk<br />

RO<br />

Tamarisk<br />

&<br />

Saltgrass


Acknowledgements<br />

♦<br />

NASA award NAG5-6999<br />

♦ Bosque Initiative/Bosque<br />

Improvement Grant<br />

♦ Interstate Stream Commission<br />

♦ US Bureau of<br />

Reclamation/Endangered<br />

Species Workgroup<br />

♦ US Army Corps of Engineers<br />

♦ US Fish and Wildlife<br />

Service/Bosque del Apache<br />

NWR<br />

♦ NM House Bill 2<br />

♦ NSF/EPSCoR RII-2<br />

♦<br />

♦<br />

♦<br />

♦<br />

♦<br />

♦<br />

♦<br />

♦<br />

♦<br />

♦<br />

UNM Hydrogeoecology<br />

UNM Sevilleta LTER<br />

NM ET Workgroup<br />

NM Bosque Hydrology Group<br />

City of Albuquerque Open<br />

Spaces Division<br />

Middle Rio Grande Conservancy<br />

District<br />

NM State Land Office<br />

Bosque del Apache NWR<br />

Sevilleta NWR<br />

Rio Grande Nature Center

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