
- APRIL 2004 327L U N D Q U I S T E T A L . 2004 American Meteorological Society
- Volume 26, Number 1, Spring 2009 Published: 10 July 2009
- Use of spatially distributed stream stage recorders to augment rain gages by identifying locations of thunderstorm precipitation
- 2 Automated algorithm for mapping regions of cold-air pooling in 3 complex terrain
- Evergreen trees as inexpensive radiation shields for temperature sensors
- Relationships between Barrier Jet Heights, Orographic Precipitation Gradients, and Streamflow in the Northern Sierra Nevada
- Using inexpensive temperature sensors to monitor the duration and heterogeneity
- Temperature trends at high elevations: Patterns across the globe N. C. Pepin1
- Rain versus Snow in the Sierra Nevada, California: Comparing Doppler Profiling Radar and Surface Observations of Melting Level
- Surface temperature patterns in complex terrain: Daily variations and long-term change in the central Sierra Nevada, California
- Onset of Snowmelt and Streamflow in 2004 in the Western United States: How Shading May Affect Spring Streamflow Timing in a Warmer World
- How snowpack heterogeneity affects diurnal streamflow timing Jessica D. Lundquist1
- F. Zhao and L. Guibas (Eds.): IPSN 2003, LNCS 2634, pp. 518528, 2003. Springer-Verlag Berlin Heidelberg 2003
- OCTOBER 2002 591L U N D Q U I S T A N D C A Y A N 2002 American Meteorological Society
- Variability and Trends in Spring Runoff in the Western United States Jessica D. Lundquist 1
- Evaluation of Precipitation Scaling Using the Observed Snow CoveEvaluation of Precipitation Scaling Using the Observed Snow Cover Disappearance Date for Snow Modelsr Disappearance Date for Snow Models Mark S. Raleigh, Frederic C. Lott, and Jessica D. Lund
- Lundquist et al., Online supplement for Measurement Paper, page 1 Electronic Supplement to: Strategic use of stream stage recorders as proxy rain
- Snow-fed streamflow timing at different basin scales: Case study of the Tuolumne River above Hetch Hetchy,
- Lundquist and Loheide, Sierra ET vs. Elevation page 1 of 46 How evaporative water losses vary between wet and dry water years as a function of
- Assistant Professor, Civil and Environmental Engineering University of Washington