Colorado River Flows Reduced by Warmer Spring Temps

Although climate models have suggested that spring temperatures affect streamflow, this study is the first to examine the instrumental historical record to see if a temperature effect could be detected, said lead author Connie Woodhouse, a UA professor of geography and development and of dendrochronology.

"Forecasts of streamflow are largely based on precipitation," Woodhouse said. "What we’re seeing since the 1980s is that temperature plays a larger role in streamflow and in exacerbating drought."

The bulk of streamflow in the upper Colorado comes from snowpack. However, temperatures during the "runoff season" of March-July can have a significant impact on the amount of water that ends up in the river, the researchers found. The team studied the records of temperature, cool-season precipitation and streamflow for the years 1906 to 2012.

"In certain years temperature became a very strong influence. It was a bit of a surprise," Woodhouse said. "If we have a warmer spring, we anticipate that the river flows will be less relative to the amount of snowpack." 

Seven Western states and Mexico use water from the Colorado River for agriculture and for cities. Major U.S. cities that use Colorado River water include Denver, Albuquerque, Salt Lake City, Phoenix, Tucson, Las Vegas, Los Angeles and San Diego.

Woodhouse’s co-authors are Gregory Pederson of the U.S. Geological Survey in Bozeman, Montana;  Kiyomi Morino  of the UA Laboratory of Tree-Ring Research; Stephanie McAfee of the University of Nevada, Reno; and Gregory McCabe of the USGS in Denver. The U.S. Department of the Interior’s Southwest Climate Science Center funded the research.

From her previous work with water managers in the region, Woodhouse knows they are interested in how temperature affects streamflow in the Colorado River.

She and her colleagues wanted to determine how Upper Colorado River Basin winter precipitation, March-July temperatures and November soil moisture levels influence annual streamflow at Lees Ferry, Arizona.

For each year from 1906 to 2012, the U.S. Bureau of Reclamation estimates natural upper Colorado River flow based on data recorded from streamgages at Lees Ferry. At that location, Colorado River streamflow reflects water that has drained from the upper basin, which includes Colorado, Wyoming, Utah and New Mexico.

Using the streamflow data, the researchers identified six droughts that occurred in the Upper Colorado River Basin from 1906 to 2012. A drought was defined by consecutive years with below-average streamflow punctuated by no more than one year of normal or above-average flow.

The drought periods were: 1931-1940, 1950-1956, 1959-1969, 1972-1977, 1988-1996 and 2000-2012.

For average winter precipitation and March-July temperatures for the Upper Colorado River Basin, the research team turned to a database that provides climatological data at very high spatial resolution for locations all over the U.S. The database goes back more than 100 years.

Soil moisture records don’t exist very back far into the 20th century. Therefore, the team used a hydrologic model, which is based on modern observations, to generate annual averages for November soil moisture going back to 1906.

The team found November soil moisture had only a small effect on streamflow.

The researchers found that winter precipitation and average runoff-season temperatures varied from drought to drought.

"The 1950s was the driest period, but also the coolest," Woodhouse said. "In contrast, the most recent drought of 2000 to 2012 was the warmest, but only moderately dry."

If the temperatures during the runoff season — March to July — were cooler than average, streamflow was higher than expected on the basis of winter precipitation alone, the team found. However, when runoff-season temperatures were above average, streamflow was less than expected on the basis of winter precipitation. 

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