From Atmospheric Rivers to Rivers Of Debris: Coupling Extreme Precipitation Events, Glacial Retreat, Debris Flows, And Channel Changes On Mount Rainier, Washington [Gordon Grant]
From Atmospheric Rivers to Rivers Of Debris: Coupling Extreme Precipitation Events, Glacial Retreat, Debris Flows, And Channel Changes On Mount Rainier, Washington. Presented by Gordon Grant at the "Perth II: Global Change and the World's Mountains" conference in Perth, Scotland in September 2010.
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From Atmospheric Rivers to Rivers Of Debris: Coupling Extreme Precipitation Events, Glacial Retreat, Debris Flows, And Channel Changes On Mount Rainier, Washington [Gordon Grant]
1. From atmospheric rivers…
to rivers of debris.
Gordon Grant
PNW Research Station
USDA Forest Service
Anne Nolin, Lauren Parker, Beth Copeland
Stephen Lancaster, Jonathan Ellinger
Oregon State University
Paul Kennard, Erin Tainer Ian Delaney
Mt Rainier National Park Whitman College
Coupling extreme precipitation events, glacial retreat, debris
flows and channel changes on Mount Rainier, Washington
2. November 7, 2006
was a dark, stormy,
and very wet night...
Pineapple Express /
Atmospheric River
November 6, 2006
14. PE/AR event non PE/AR event
A debris flow was considered PE/AR related if a PE/AR event occurred
on the same day as a debris flow, or on the day prior.
15. Mount Hood
Classification of storms proceeding debris flows
Mount Rainier
Classification of storms proceeding debris flows
Pineapple Express (PE) events (Dettinger, 2004) and Atmospheric Rivers (AR) (Neiman et al., 2008);
Debris flow data from Driedger, Walder, Kennard
16. …and 3) Little snow cover
100
90 Mount Rainier
80 Antecedent SWE
70
SWE (mm)
60
50
40
30
20
10
0
86 88 89 90 91 92 92 03 05 06
26/ 0/15/ 11/8/ 10/2/ 11/4/ 9/7/ 9/19/ 0/19/ 9/28/ 11/5/
10/ 1 1
One Day Prior to Debris Flow Event Date
18. Geomorphic
factors associated
with debris flow
initiation
All recent initiation sites are:
• In areas exposed by recent
(5-10 year) glacier retreat
• Near glacier termini or
debris-mantled stagnant ice
• At heads of steep-walled
gullies flanked by steep
debris-mantled slopes
21. Fire Hose Effect?
Photo: NPS
• water concentrated in sub- or supra-glacial channels.
• flow directed toward unstable, sediment mantled slopes
below/adjacent to glaciers.
22. Source areas
• Moraines
• Ice-cored debris
• Debris mantled
slopes
Runout
Zone
Deposition in larger channels
Downstream
channel response?
23. Aggradation rates within Mount Rainier National Park
1000.0
Recent Aggradataion Rates (cm/yr)
1) Evidence for
widespread
100.0 aggradation
(not incision)
Sunshine
Point
Lower Van
10.0 Trump
2) Higher than
White long-term
River average in last
decade
1.0 Longmire
1997-2006 2006
0.1
0.1 1.0 10.0 100.0 1000.0
Long term (1910-2006) Aggradation Rates (cm/yr)
26. Effects of climate change?
• Change in • Continued
intensity/frequency of glacial
PE/AR events retreat /
fragmentation
• Increased
length of
snow free
period
• Downstream
signal?
27. No smoking gun yet…
• Atmospheric events producing
debris flows come in different
flavors
• Apparent recent increase in
debris flows, but record is
incomplete and potentially
biased
• Consistent pattern of
aggradation within Mt Rainier
National park itself
• No consistent aggradation in
larger rivers