reference : Changes in snowmelt runoff timing in western North America under a "business as usual" climate change scenario

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/reference/52c72f28-b78c-4a82-9ca6-df2bbb15ef58
Bibliographic fields
reftype Journal Article
Abstract Spring snowmelt is the most important contribution of many rivers in western North America. If climate changes, this contribution may change. A shift in the timing of springtime snowmelt towards earlier in the year already is observed during 1948–2000 in many western rivers. Streamflow timingchanges for the 1995–2099 period are projected using regression relationsbetween observed streamflow-timing responses in each river, measured by the temporal centroid of streamflow (CT) each year, and local temperature (TI) and precipitation (PI) indices. Under 21st century warming trends predicted by the Parallel Climate Model (PCM) under business-as-usual greenhouse-gas emissions, streamflow timing trends across much of western North America suggest even earlier springtime snowmelt than observed to date. Projected CT changes are consistent with observed rates and directions of change during the past five decades, and are strongest in the Pacific Northwest, Sierra Nevada, and Rocky Mountains, where many rivers eventually run 30–40 daysearlier. The modest PI changes projected by PCM yield minimal CT changes. The responses of CT to the simultaneous effects of projected TI and PI trends are dominated by the TI changes. Regression-based CT projections agree with those from physically-based simulations of rivers in the Pacific Northwest and Sierra Nevada.
Author Stewart, Iris T.; Cayan, Daniel R.; Dettinger, Michael D.
DOI 10.1023/B:CLIM.0000013702.22656.e8
Date January 01
ISSN 1573-1480
Issue 1
Journal Climatic Change
Pages 217-232
Title Changes in snowmelt runoff timing in western North America under a "business as usual" climate change scenario
Type of Article journal article
Volume 62
Year 2004
Bibliographic identifiers
_record_number 21535
_uuid 52c72f28-b78c-4a82-9ca6-df2bbb15ef58