06/09/2026
Late in the season many of the Sierra Nevada's automated snow sensors have melted out. Despite warm and dry conditions considerable amounts of snow remain at high elevations in complex terrain. Assessing the snow water equivalent of these areas is critical to understanding how much water remains above reservoirs across the state, even after snow sensors go offline.
Over the last month A*O field technicians were on the ground across the Sierras digging snow pits in support of our airborne surveys.
A*O depends on these measurements to support the remote sensing and data processing pipline that accurately and precisely estimates how much water is stored in the snowpack. Our field technicians collect snow density profiles from the snow surface down to the ground. Our team uses these measurements to assess and correct any bias in the isnobal model, combined with spatially complete, lidar-derived snow depths to measure SWE at the basin scale.
Unprecedented warm and dry conditions in 2026 have limited the insights available from point sensors. Our field measurements and basin-wide snow depths build a complete picture of SWE volume and distribution across the full extent of the basin.