The title of my talk directly addresses one of the top four objectives for hydrology, “Quantify rates of snow accumulation, snowmelt, ice melt, and sublimation from snow and ice worldwide at scales driven by topographic variability.” Remote sensing of snow water equivalent has posed a difficult problem for four decades, so perhaps a more likely approach will be through measurement of depth and modeling of snow density.
SEMINARS IN CHEMICAL AND BIOMOLECULAR ENGINEERING Friday, Nov. 09, 2018 | 10:00am-11:00am Boelter Hall 3400 Presented By: Mark A. Barteau Vice President for Research, Texas [...]
Civil and Environmental Engineering Graduate students and faculty are formally invited to attend the Final Defense Exam Earthquake Ground Motion and Site Amplification Modeling in [...]
Civil and Environmental Engineering Graduate students and faculty are formally invited to attend the Final Defense Exam An Improved Framework for the Analysis and Dissemination [...]
Civil and Environmental Engineering Graduate students and faculty are formally invited to attend the Final Defense Exam Characterizing Seismic Performance of Levees on Peat from [...]
Civil & Environmental Engineering Graduate Admission & ESAP Information Session Tuesday, November 27 11:00am – 12:00pm Boelter Hall 4275RSVP by 11/21: http://www.cee.ucla.edu/esaprsvp/ This information session [...]
Civil and Environmental Engineering Graduate students and faculty are formally invited to attend the Final Defense Exam Resilience-Based Seismic Evaluation and Design of Reinforced Concrete [...]