Max Fajardo

Max Hawthorne Bucci Fajardo – 322 Wellesley Dr SE Albuquerque, NM 87108 – mbucci@unm.edu

Climate models continue to illustrate a future with lesser water flux in the Southwestern United States. Along with diminishing reservoirs of water and anomalous fluxes in precipitation, the southwest is experiencing sooner than expected peak snowmelt runoff on the order of days. With the sooner snowmelt runoff peak, the less time the snowpack has to accumulate over the cold winter months. Hence we seek to demonstrate the relationship between global air temperature and receding peak runoff values. The data used are from the Rio Grande Headwaters stream flux provided by NOAA. Through the research we seek to present numerically modelled recessions in peak snowmelt runoff; moreover, we find that peak runoff timing is getting earlier in the year and it’s not clear that there is a direct relationship with global air temperature models. Thus, there is currently research in progress on the principle causes of the shifting peak snow runoff date. The methods of research are nonlinear algorithm writing and k-clustering machine learning using Python and its accompanying libraries.

2019 New Mexico Geological Society Annual Spring Meeting April 12, 2019, Macey Center, New Mexico Tech campus, Socorro, NM Online ISSN: 2834-5800

Pages: 20