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Kachemak Bay
National Estuarine Research Reserve System    Research Reserve


60 years of change in Kachemak Bay
     Changing shorelines, salt marshes and glaciers




          Steve Baird, Kachemak Bay Research Reserve
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



                     Coastal Erosion
     Why are people interested in coastal erosion?
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



                  Shoreline Change
Kachemak Bay
National Estuarine Research Reserve System       Research Reserve



                         Erosion Rates
• Overall average – 0.7 m/yr (2.3 ft/yr)
• West of Spit – 0.8 m/yr (2.6 ft/yr)
• East of Spit – 0.6 m/yr (2.0 ft/yr)

•   1951-1961        –   1.04 m/yr (3.4 ft/yr)
•   1961-1968        –   0.78 m/yr (2.6 ft/yr)
•   1968-1975        –   1.49 m/yr (4.9 ft/yr)
•   1975-1996        –   0.46 m/yr (1.5 ft/yr)
•   1996-2003        –   0.57 m/yr (1.9 ft/yr)
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



                                 Parcels
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve




                                              2003
                                              2008
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



                                  LiDAR
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve




     LiDAR Difference Grids
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve


  Coastal Erosion and Climate Change




     • Erosion rates will be affected by frequency of
            waves impacting bluff
     • Frequency, intensity, and direction of storms
     • Relative sea-level
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



                   Relative Sea-Level
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



                   Relative Sea-Level
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



                       Coastal Uplift
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve


         Changes in Salt Marshes
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



               Shifting Salt Marshes
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve



               Shifting Salt Marshes




     • Sensitive to changes in elevation / sea-level
     • Affected by sedimentation rates
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve
Grewingk Glacier
Doroshin Glacier
Glacier
Kachemak Bay
National Estuarine Research Reserve System       Research Reserve



                       Rates of retreat
  Glacier                        Rate (ft/yr)   Miles/56 yrs
  Grewingk                              92             0.97
  Portlock                              100            1.06
  Dixon                                 105            1.11
  Halibut Creek                         41             0.43
  Woznesenski                           115            1.22
  Doroshin                              100            1.06
  Doroshin South                        107            1.14
  Goat                                  56             0.59
  Dinglestadt                           220            2.34
Kachemak Bay
National Estuarine Research Reserve System   Research Reserve


                      Glacial Thinning




                                                VanLooy et. al. 2006
Kachemak Bay
National Estuarine Research Reserve System                  Research Reserve


                      Glacial Thinning




                                             Chris Larsen, Geophysical Institute, UAF
Kachemak Bay
National Estuarine Research Reserve System         Research Reserve


                              Summary
• Erosion along Homer shoreline an ongoing concern
• Salt marshes are sensitive to changes in elevation & sedimentation
• Glaciers are receding and thinning, at an accelerating rate
• To predict climate-change impacts, we need to understand:
    • Balance between coastal uplift rates and sea-level rise
    • Whether uplift rates are uniform; relation to underlying geology
    • Changes in frequency, intensity, and direction of storm events
    • Changes in glacial melt and sedimentation rates
    • For salt marsh habitats, the importance of these habitats to a
         wide range of species

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