Glacier monitoring at Mount Rainier gives insight to summer stream flows.
Every year crews from the North Coast & Cascades Inventory & Monitoring Network track glacier health at Mount Rainier. In the spring, crews visit Nisqually and Emmons glaciers to measure how much new snow has accumulated on the glacier surface during the winter. Snow depth and density measurements determine how much water is held in that snowpack (snow water equivalent). Measurement rods are also installed to track snow and ice melt over the coming summer. This allows us to track accumulation (snow that becomes added ice) and melt (lost ice) over the long term.
NPS/S.Hagen Photo: Glacier monitoring lead smiles at the success of the spring glacier trip on the lower Nisqually, 4/22/24.
In the short term, the snow depth measurements, along with data contributed from climate stations, can help us anticipate melt water availability in the summer.
Graph of SWE at two locations on the Nisqually Glacier during drought years compared to average.
Results of the snow water equivalent (SWE), or how much water would result if all the snow melted, at two different elevations on the Nisqually Glacier are displayed in the graph. Notably, the results from a 4/22/24 survey on the Nisqually Glacier are below the average. In 2024, SWE at these elevations is higher than the drought year of 2005 but below the drought year of 2015 at both elevations.
Snow is not the only contribution to water in streams, but in our region it’s an important source.










