Remember all the way back to water year 2011 when Colorado’s reservoirs mostly filled to the brim? Here’s the Streamflow of 2011 — Water Year Summary from the United States Geological Survey (Xiaodong Jian/David M. Wolock/Harry F. Lins/Steve Brady).
For you numbers junkies the document should be a great read to take along next time you’re sitting under the cottonwoods by your favorite stream.
Here’s the introduction:
The maps and graph in this summary describe streamflow conditions for water year 2011 (October 1, 2010, to September 30, 2011) in the context of the 82-year period from 1930 through 2011, unless otherwise noted. The illustrations are based on observed data from the U.S. Geological Survey’s (USGS) National Streamflow Information Program (http://water.usgs.gov/nsip/). The period 1930–2010 was used because, prior to 1930, the number of streamgages was too small to provide representative data for computing statistics for most regions of the country.
In the summary, reference is made to the term “runoff,” which is the depth to which a river basin, State, or other geographic area would be covered with water if all the streamflow within the area during a single year was uniformly distributed upon it. Runoff quantifies the magnitude of water flowing through the Nation’s rivers and streams in measurement units that can be compared from one area to another. Each of the maps and graphs can be expanded to a larger view by clicking on the image. In all of the graphics, a rank of 1 indicates the highest flow of all years analyzed.
More USGS coverage here.