Using Webcam Technology for Measuring and Scaling Phenology of Tamarisk (Tamarix ramosissima) Infested with the Biocontrol Beetle (Diorhabda carinulata) on the Dolores River, Utah

Tamarisk is an introduced shrub/tree that is now widespread in western U.S. riparian corridors. There is concern that tamarisk displaces native vegetation and consumes large amounts of water from riparian aquifers. Consequently, the saltcedar leaf beetle (Diorhabda carinulata) has been introduced into the western US to control the spread of tamarisk. We studied the phenology and water use of tamarisk in two adjacent, beetle infested stands on the Dolores River, in southeastern Utah. A 10 m tower was erected in each tamarisk stand (“orchard” and “gauge”) prior to the 2008 growing season. Beetle damage was measured using fractional cover from images taken from the tower-mounted visible and infrared cameras (“phenocams”) starting in mid-May 2008 and again in mid-May 2009 through the growing season of each year. Tamarisk plants developed fresh leaves ca. mid-April and dense canopies by late-May. In 2008, defoliation became significant by June, whereas in 2009, defoliation became significant by mid-July (orchard) to late-July (gauge). In 2007, cameras were not installed, however defoliation occurred in July. Partial refoliation occurred approximately six weeks after the tamarisk trees were completely defoliated. Time-lapse image sets from the cameras were compared with fine-scale estimates of water use using stem sap flow measurements conducted over three growing seasons (2007-2009). Damage at an intermediate scale was measured with Aster imagery (15 m resolution) and at a coarse scale with MODIS imagery (250 m resolution). Vegetation indices (VIs) from the fine scale (tower phenocams) were comparable to VIs from satellite imagery at the intermediate and coarse scale. Plant transpiration fell dramatically during or shortly after the defoliated period, but recovered when new leaves were produced each year. Potential water salvage was constrained to the relatively brief period of defoliation. At the intermediate scale of measurement, beetle damage was seen to be spotty and localized among plant stands. Furthermore, at the coarse scale, beetle damage was not readily apparent. Because defoliation by the beetle is new to the ecosystem (~ 5 years), relative to the presence of tamarisk (>100 years), the long-term effect of the defoliation on water salvage is unknown. Our preliminary findings and assessment of these defoliation effects show that beetle damage is transient and damage tends to be localized, and thus, the prospects for water salvage over large areas of river so far appear to be limited as beetle - tamarisk interactions have not yet stabilized on western rivers.