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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
November 7, 2006
                      was a dark, stormy,
                      and very wet night...




Pineapple Express /
 Atmospheric River




                            November 6, 2006
Mount Rainier




Oct 31-Nov 7, 2006

                                     NASA Earth Observatory
> 100yr Flood
Tahoma Creek, Washington
West Fork Middle Fork Hood




              Mount Hood Debris Flows




Eliot Creek                                            Hwy 35
8
                                      7      Mount Hood

            # of debris flows
                                      6
                                      5
                                      4
                                      3
                                      2
                                      1
                                      0
                                          1947 1952 1957 1962 1967 1972 1977 1982 1987 1992 1997 2002 2007


                                      8
                                      7      Mount Rainier
                  # of debris flows




                                      6
                                      5
                                      4
                                      3
                                      2
                                      1
                                      0
                                          1947 1952 1957 1962 1967 1972 1977 1982 1987 1992 1997 2002 2007

Debris flow data from Driedger, Walder, Kennard
Cascadian Periglacial Debris Flow Project


1) Atmospheric
  rivers
                                  2) Initiation
                                    of debris
                                    flows


                          3) Downstream
   Climate                  consequences

   Change?
Are debris flows correlated with Pineapple Express and
         Atmospheric River (PE/AR) events?
PE/AR = Lots of rain




        Pineapple Express event of November 5 and 6, 2006
+ High Freezing levels
                         Mount Rainier Freezing Altitudes
     Mt Rainier
     peak elevation




       Mountain peak elevations                       Rainier
                                                      Hood
Associated with strong southwest flow




    Dettinger, 2004
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.
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
…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
RAIN
SNOW DEPTH




             Iverson, pers comm.
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
2001-2006
   debris flow
   initiation sites
Glacier Extent
    1913

    2008
Ellinger, 2010
Fire Hose Effect?




                                           Photo: NPS
• water concentrated in sub- or supra-glacial channels.
• flow directed toward unstable, sediment mantled slopes
  below/adjacent to glaciers.
Source areas
                                        • Moraines
                                        • Ice-cored debris
                                        • Debris mantled
                                          slopes


                             Runout
                             Zone

                     Deposition in larger channels



Downstream
 channel response?
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)
1951




1960




1978




1989
                  post 2006 storm
       Tahoma Creek
Aggradation rates
 downstream of
 Mount Rainier
  National Park




                    Christopher Magirl, USGS
Effects of climate change?
• Change in                      • Continued
  intensity/frequency of           glacial
  PE/AR events                     retreat /
                                     fragmentation

                                 • Increased
                                   length of
                                   snow free
                                   period

            • Downstream
              signal?
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

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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
  • 3. Mount Rainier Oct 31-Nov 7, 2006 NASA Earth Observatory
  • 6. West Fork Middle Fork Hood Mount Hood Debris Flows Eliot Creek Hwy 35
  • 7.
  • 8. 8 7 Mount Hood # of debris flows 6 5 4 3 2 1 0 1947 1952 1957 1962 1967 1972 1977 1982 1987 1992 1997 2002 2007 8 7 Mount Rainier # of debris flows 6 5 4 3 2 1 0 1947 1952 1957 1962 1967 1972 1977 1982 1987 1992 1997 2002 2007 Debris flow data from Driedger, Walder, Kennard
  • 9. Cascadian Periglacial Debris Flow Project 1) Atmospheric rivers 2) Initiation of debris flows 3) Downstream Climate consequences Change?
  • 10. Are debris flows correlated with Pineapple Express and Atmospheric River (PE/AR) events?
  • 11. PE/AR = Lots of rain Pineapple Express event of November 5 and 6, 2006
  • 12. + High Freezing levels Mount Rainier Freezing Altitudes Mt Rainier peak elevation Mountain peak elevations Rainier Hood
  • 13. Associated with strong southwest flow Dettinger, 2004
  • 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
  • 17. RAIN SNOW DEPTH Iverson, pers comm.
  • 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
  • 19. 2001-2006 debris flow initiation sites Glacier Extent 1913 2008
  • 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)
  • 24. 1951 1960 1978 1989 post 2006 storm Tahoma Creek
  • 25. Aggradation rates downstream of Mount Rainier National Park Christopher Magirl, USGS
  • 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