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CHANGES IN RIPARIAN VEGETATION IN THE SOUTHWESTERN UNITED STATES:
Repeat Photography at Streamflow Gaging Stations

 

GILA RIVER AT CALVA (09466500)

(March 6, 1932). The Gila River was ravaged by floods in the 1910s and 1920s, including one flood estimated at 100,000 ft³/s in 1916. This upstream view from the railroad bridge at Calva shows a wide, braided channel. An open cottonwood gallery forest appears in the midground at left (channel right), and the low shrubs at right appear to be native willows (W.E. Dickinson, #1053).
 
(June 18, 1964). In the intervening 32 years, the highest discharge through this reach was 27,900 ft³/s on October 1, 1941. Dense tamarisk has become established, creating a floodplain where the main channel once was. The channel has shifted to the right and is much smaller than it was in 1932 (Raymond M. Turner).
 
(October 17, 1973). To reduce evapotranspiration, phreatophytes (mostly tamarisk) were removed from this reach in 1970, and the floodplain was reseeded to native grasses. Those grasses are mostly gone at the time of this photograph, one year after a flood of 80,000 ft³/s passed through this reach. The small shrubs throughout the view are mostly tamarisks that are re-establishing in the reach (Raymond M. Turner).
 
(May 21, 1984). In October 1983, a flood of 150,000 ft³/s passed through this reach in the wake of Tropical Storm Octave. This flood followed one that peaked at 100,000 ft³/s in 1978. These floods shifted the channel back into the view, and driftwood racks appear throughout the foreground. Despite this flood, dense tamarisk appears on both floodplains (Raymond M. Turner).
 
(October 6, 2000). Except for withdrawals of domestic and irrigation water at low-head diversion dams, the Gila River is unregulated upstream from Calva. In January and February, 1993, three floods passed through this reach that exceeded 100,000 ft³/s. Despite these floods, tamarisk has grown considerably, blocking the view of the river channel from this camera station. Despite the enormous effort at tamarisk removal and river restoration, the tamarisk has attained a higher biomass than it had in 1964. The channel has shifted from the right side to the left side of this view (Dominic Oldershaw, Stake 331a).

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