As part of the regular operation of surface-water gaging stations in Arizona, photographs are taken to document channel conditions. The photographs show many features of the channel that are important to accurate streamflow gaging, including shifts in channel thalwegs or deepest point in the channel, changes in low-water controls, and changes in channel roughness. Photographs have been taken since gaging stations were first established in Arizona in the 1910s, and many photographs were taken in the 1920s and 1930s.
Now, these photographs provide an invaluable record for evaluating changes in the riverine environment of the major water courses in Arizona. Riparian vegetation in particular is highly valued, and its long-term status is much debated. Water development is frequently blamed for decimation or elimination of riparian ecosystems. Floods may damage or destroy vegetation within channels, and channel changes may cause damage to floodplain structures, agricultural fields, and water- and irrigation-supply systems. Increases in channel roughness may create higher stages during floods, raising the possibility of increased frequency of flood damage.
The photography at gaging stations documents long-term changes in the riverine environments of Arizona. The images shown here are selected to illustrate the range of changes, which include large increases in native and non-native vegetation at most sites, complete elimination of riparian vegetation at some sites, channel downcutting, lateral channel changes, and deposition of new fluvial terraces. The causes of many of the changes are not obvious; for example, at some sites, riparian vegetation has increased despite the occurrence of large floods or significant flow regulation. Despite the 20th century spread of tamarisk along the state's rivers, native species have increased as well.
If you have any technical questions on content or methods, you may direct them to Robert H. Webb or Diane E. Boyer.