Earth and Planetary Sciences ETDs
Publication Date
Summer 7-12-2017
Abstract
Observed streamflow and climate data are used to test the hypothesis that climate change is already affecting the streamflow volume derived from snow accumulation in ways consistent with climate model-based projections of 21st century streamflow. Annual and monthly changes in streamflow volume and surface climate variables on the upper Rio Grande (URG) near its headwaters in southern Colorado are assessed for water years 1958-2015. Trends in discharge are examined together with variations in snow water equivalent and surface climate variables. Results indicate that temperatures in the basin have increased significantly primarily in the winter and spring seasons, April 1 snow water equivalent has decreased by approximately 25%, and streamflow has declined in the runoff season, but small increases in precipitation have reduced the impact of declining snowpack on streamflow. Changes in the snowpack-runoff relationship are noticeable in hydrographs of mean monthly streamflow, but most apparent in the changing ratio of precipitation (rain+snow, and snow water equivalent) to streamflow and in regression statistics. The observed changes impact our ability to predict streamflow on a seasonal basis and affect long-term water management of the Rio Grande.
Degree Name
Earth and Planetary Sciences
Level of Degree
Masters
Department Name
Department of Earth and Planetary Sciences
First Committee Member (Chair)
David Gutzler
Second Committee Member
Grant Meyer
Third Committee Member
Peter Fawcett
Fourth Committee Member
Dagmar Llewellyn
Keywords
snowpack, Upper Rio Grande Basin, streamflow, climate change
Document Type
Thesis
Recommended Citation
Chavarria, Shaleene. "Observed Changes in Climate and Streamflow in the Upper Rio Grande Basin." (2017). https://digitalrepository.unm.edu/eps_etds/197
Included in
Environmental Monitoring Commons, Hydrology Commons, Other Earth Sciences Commons, Water Resource Management Commons