Streamflow Permanence in Mount Rainier National Park, Washington

Fact Sheet 2023-3051
Prepared in cooperation with the U.S. National Park Service
By:

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Introduction

Streams that flow throughout summer (“permanent” streams) provide critical habitat for aquatic species and serve as an important water supply. Streams that go dry seasonally or only flow after rainfall or snowmelt are a natural feature of mountain systems, including Mount Rainier National Park. However, in years with substantially less than normal snowfall, like 2015, more streams go dry, resulting in less water for Mount Rainier National Park infrastructure and unknown consequences for stream ecology.

Suggested Citation

Jaeger, K.L., 2024, Streamflow permanence in Mount Rainier National Park, Washington: U.S. Geological Survey Fact Sheet 2023–3051, 2 p., https://doi.org/10.3133/fs20233051.

ISSN: 2327-6932 (online)

Study Area

Table of Contents

  • A Streamflow Permanence Model Calibrated to Simple Flow/No Flow Observations
  • Many Streams in Mount Rainier National Park are Estimated to Go Dry Each Summer
  • Stream Location Matters
  • What do More Dry Streams Mean?
Publication type Report
Publication Subtype USGS Numbered Series
Title Streamflow permanence in Mount Rainier National Park, Washington
Series title Fact Sheet
Series number 2023-3051
DOI 10.3133/fs20233051
Year Published 2024
Language English
Publisher U.S. Geological Survey
Publisher location Reston, VA
Contributing office(s) Washington Water Science Center
Description 2 p.
Country United States
State Washington
Other Geospatial Mount Rainier National Park
Online Only (Y/N) Y
Google Analytic Metrics Metrics page
Additional publication details