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Sea	
  Level	
  Rise:	
  Natural	
  Resource	
  
Impacts	
  and	
  Considera8ons	
  for	
  
Great	
  Marsh	
  Community	
  Resilience	
  

Julia	
  Knisel,	
  Coastal	
  Shoreline	
  and	
  Floodplain	
  Manager	
  
Kathryn	
  Glenn,	
  North	
  Shore	
  Regional	
  Coordinator	
  
Massachuse8s	
  Office	
  of	
  Coastal	
  Zone	
  Management	
  
Coastal	
  Inunda8on	
  Mapping	
  Elements	
  
•  Water	
  Level:	
  
–  Local	
  @de	
  ranges	
  
–  Sea	
  level	
  rise	
  data	
  &	
  projec@ons	
  
–  Flood	
  event	
  data	
  (surge	
  &	
  precipita@on)	
  

•  High	
  Resolu8on	
  Eleva8on	
  Data:	
  
–  Topographic	
  &	
  bathymetric	
  LIDAR	
  
–  Digital	
  eleva@on	
  models	
  referenced	
  to	
  
@dal	
  datums	
  	
  

•  Natural	
  &	
  Human	
  Responses:	
  
–  Current	
  ecosystems	
  (beaches	
  &	
  
wetlands)	
  
–  Landform	
  changes	
  (erosion	
  &	
  accre@on)	
  
–  Physical	
  barriers	
  to	
  migra@on	
  
(development,	
  seawalls,	
  culverts,	
  etc.)	
  
Cri8cal	
  Parameters	
  for	
  Modeling	
  Marsh	
  Migra8on	
  

Marshes	
  on	
  the	
  Move,	
  2011
	
  

•  If	
  sediment	
  accretes	
  (traps	
  on	
  surface	
  or	
  accumulates)	
  as	
  fast	
  as	
  
sea	
  level	
  rises,	
  then	
  marsh	
  may	
  avoid	
  being	
  converted	
  or	
  
submerged	
  
Mean	
  Higher	
  High	
  Water	
  Tidal	
  Datum	
  
Sea	
  Level	
  Rise	
  Scenarios	
  
Historic	
  Rate	
  of	
  Sea	
  Level	
  Rise	
  
(Boston	
  Tide	
  Gauge)	
  
•  Mean	
  range	
  (MHW-­‐MLW)	
  =	
  9.5	
  feet	
  
•  Record	
  =	
  1921-­‐2012	
  (91+	
  years)	
  
•  Sea	
  level	
  rise	
  =	
  0.9	
  feet/100	
  years	
  
Historic	
  Sea	
  Level	
  Trends	
  
from	
  1921	
  to	
  2006-­‐2012	
  (Boston)	
  

•  	
  Linear	
  mean	
  sea	
  level	
  rates	
  (	
  	
  	
  	
  )	
  &	
  95%	
  confidence	
  
intervals	
  (mm/yr)	
  calculated	
  from	
  1921	
  to	
  recent	
  years	
  
(2006-­‐2012)	
  at	
  the	
  NOAA	
  Boston	
  @de	
  gauge	
  sta@on	
  
•  Values	
  are	
  trend	
  of	
  en@re	
  data	
  period	
  up	
  to	
  that	
  year	
  
Great	
  Marsh	
  Sediment	
  Accre8on	
  
• 
• 

Marshes	
  accrete	
  by	
  trapping	
  sediment	
  &	
  by	
  organic	
  ma8er	
  
accumula@on	
  from	
  roots	
  &	
  rhizomes	
  
Maximum	
  accre@on	
  for	
  Great	
  Marsh	
  currently	
  recorded	
  ~	
  6	
  mm/yr	
  

Courtesy	
  of	
  Anne	
  Giblin,	
  Marine	
  Biological	
  Lab	
  
Wetland	
  Types	
  

Eleva@on	
  

66%	
  wetland	
  
Majority	
  
Mean	
  High	
  
Water	
  Spring	
  
Mean	
  High	
  
Water	
  
Mean	
  Tide	
  
Level	
  
Mean	
  Low	
  
Water	
  

Water	
  

Unconsolidated	
   Salt	
  
Shore*	
  
Marsh	
  

Brackish/	
  	
   Freshwater	
  
Transi@onal	
   Wetlands	
  

Dry	
  Lands	
  

*includes	
  silt,	
  sand,	
  or	
  gravel	
  that	
  is	
  subject	
  to	
  inunda@on	
  and	
  redistribu@on	
  due	
  to	
  the	
  ac@on	
  
of	
  water;	
  substrates	
  lack	
  vegeta@on	
  
Marsh	
  Migra8on	
  Limited	
  by
	
  
Development	
  &	
  Infrastructure	
  (Newbury)
	
  

Current	
  

75-­‐Year	
  Time	
  Horizon	
  (2080)	
  
	
  

Net	
  marsh	
  impact	
  =	
  MHHW	
  +	
  
4.5	
  l	
  sea	
  level	
  rise	
  –	
  1	
  l	
  accre@on	
  
Marsh	
  Migra8on	
  Limited	
  by
	
  
Development	
  &	
  Infrastructure	
  (Salisbury)
	
  

Current	
  

75-­‐Year	
  Time	
  Horizon	
  (2080)	
  
	
  

Net	
  marsh	
  impact	
  =	
  MHHW	
  +	
  
4.5	
  l	
  sea	
  level	
  rise	
  –	
  1	
  l	
  accre@on	
  
Marsh	
  Conversion	
  to	
  Unconsolidated	
  Shore	
  
(Gloucester)
	
  

Current	
  

75-­‐Year	
  Time	
  Horizon	
  (2080)	
  
	
  

Net	
  marsh	
  impact	
  =	
  MHHW	
  +	
  
4.5	
  l	
  sea	
  level	
  rise	
  –	
  1	
  l	
  accre@on	
  
Marsh	
  Conversion	
  to	
  Unconsolidated	
  Shore	
  
(Salisbury)
	
  

Current	
  

75-­‐Year	
  Time	
  Horizon	
  (2080)	
  
	
  

Net	
  marsh	
  impact	
  =	
  MHHW	
  +	
  
4.5	
  l	
  sea	
  level	
  rise	
  –	
  1	
  l	
  accre@on	
  
Marsh	
  Migra8on	
  Modeling	
  Resource	
  
www.csc.noaa.gov/digitalcoast/publica@ons/marshesonthemove	
  
Applying	
  SLR	
  Data/Mapping	
  
•  Great	
  Marsh	
  
communi@es	
  are	
  
currently	
  
grappling	
  with	
  
retrofinng	
  areas	
  
that	
  were	
  
developed	
  
before	
  SLR	
  and	
  
climate	
  change	
  
issues	
  were	
  
recognized	
  
Applying	
  SLR	
  Data/Mapping	
  
•  Past	
  
experience	
  
•  What	
  do	
  we	
  
know	
  now?	
  
•  What	
  can	
  we	
  
do	
  
differently?	
  
•  What	
  have	
  
we	
  learned?	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Development	
  in	
  flood	
  
prone	
  areas	
  
•  Impervious	
  floodplains	
  
•  Culverted	
  streams	
  and	
  
rivers	
  
•  Tidal	
  restric@ons	
  
•  Armored	
  river	
  and	
  coastal	
  
banks	
  
•  Hardened	
  shorelines	
  
•  Barriers	
  to	
  marsh	
  
migra@on	
  

NOAA	
  photo	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Development	
  in	
  flood	
  
prone	
  areas	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Impervious	
  
floodplains	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Confined	
  
stream	
  and	
  
river	
  beds	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Tidal	
  Restric@ons	
  
•  Causeways	
  
•  Low-­‐lying	
  roadways	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Armored	
  river	
  and	
  
coastal	
  banks	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Hardened	
  shorelines	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Barriers	
  to	
  marsh	
  
migra@on	
  

Photo:	
  Maine	
  Sea	
  Grant	
  
Altera8ons	
  that	
  Limit	
  Natural	
  Resilience	
  
•  Dams	
  
•  Culverts	
  
Sea	
  Level	
  Rising/Climate	
  Changing:	
  	
  
Key	
  Resource	
  Func8ons	
  to	
  Consider	
  
•  A8enua@on	
  of	
  	
  
	
  flood	
  waters	
  
•  Ability	
  of	
  storm/flood	
  
waters	
  to	
  recede	
  
•  Sediment	
  availability	
  
and	
  transport	
  
•  Energy	
  dissipa@on	
  
•  Natural	
  resource	
  
adapta@on	
  
•  Ecosystem	
  con@nuity	
  
AXenua8on	
  of	
  Flood	
  Waters	
  
•  Limit	
  impervious	
  areas	
  
•  Preserve	
  open	
  space	
  in	
  
developments	
  
•  Incorporate	
  LID	
  
•  Avoid	
  hardening	
  
stream	
  and	
  riverbanks	
  
•  Rethink	
  new	
  
development	
  in	
  flood	
  
prone	
  areas	
  
Ability	
  of	
  Storm/Floodwaters	
  to	
  Recede	
  
•  Limit	
  new	
  impervious/
incorporate	
  LID	
  and	
  
•  Address	
  restric@ons	
  and	
  
inappropriate	
  culvert	
  
designs	
  
•  Dam	
  removal	
  
•  Preserve	
  open	
  space	
  in	
  
developments	
  
•  Where	
  do	
  floodwaters	
  
go?	
  
•  Consider	
  ousall	
  
loca@ons	
  

AP	
  photo	
  

Reuters	
  photo	
  
Sediment	
  Availability	
  and	
  Transport	
  
•  Unarmored	
  banks	
  
•  Bioengineering	
  
alterna@ves	
  
•  Re-­‐nourishment	
  
•  Open	
  pilings	
  for	
  
development	
  
•  Re-­‐vegeta@on	
  
Energy	
  Dissipa8on	
  
•  Protect	
  dune	
  stability	
  
•  Sediment	
  supply	
  
•  Maintain	
  floodplain	
  
func@on	
  
•  Sol	
  bank	
  stabiliza@on	
  
techniques	
  
Natural	
  Resource	
  Adapta8on	
  
•  Marsh	
  migra@on	
  and	
  
accre@on	
  
•  Barrier	
  beach	
  migra@on	
  
	
  
Ques8ons?	
  

Julia	
  Knisel	
  
CZM	
  Coastal	
  Shoreline	
  and	
  Floodplain	
  Manager	
  
617-­‐626-­‐1191;	
  julia.knisel@state.ma.us	
  
Kathryn	
  Glenn	
  
CZM	
  North	
  Shore	
  Regional	
  Coordinator	
  
978-­‐281-­‐3868;	
  kathryn.glenn@state.ma.us	
  

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Czm great marsh_20131114sm

  • 1. Sea  Level  Rise:  Natural  Resource   Impacts  and  Considera8ons  for   Great  Marsh  Community  Resilience   Julia  Knisel,  Coastal  Shoreline  and  Floodplain  Manager   Kathryn  Glenn,  North  Shore  Regional  Coordinator   Massachuse8s  Office  of  Coastal  Zone  Management  
  • 2. Coastal  Inunda8on  Mapping  Elements   •  Water  Level:   –  Local  @de  ranges   –  Sea  level  rise  data  &  projec@ons   –  Flood  event  data  (surge  &  precipita@on)   •  High  Resolu8on  Eleva8on  Data:   –  Topographic  &  bathymetric  LIDAR   –  Digital  eleva@on  models  referenced  to   @dal  datums     •  Natural  &  Human  Responses:   –  Current  ecosystems  (beaches  &   wetlands)   –  Landform  changes  (erosion  &  accre@on)   –  Physical  barriers  to  migra@on   (development,  seawalls,  culverts,  etc.)  
  • 3. Cri8cal  Parameters  for  Modeling  Marsh  Migra8on   Marshes  on  the  Move,  2011   •  If  sediment  accretes  (traps  on  surface  or  accumulates)  as  fast  as   sea  level  rises,  then  marsh  may  avoid  being  converted  or   submerged  
  • 4.
  • 5. Mean  Higher  High  Water  Tidal  Datum  
  • 6. Sea  Level  Rise  Scenarios  
  • 7. Historic  Rate  of  Sea  Level  Rise   (Boston  Tide  Gauge)   •  Mean  range  (MHW-­‐MLW)  =  9.5  feet   •  Record  =  1921-­‐2012  (91+  years)   •  Sea  level  rise  =  0.9  feet/100  years  
  • 8. Historic  Sea  Level  Trends   from  1921  to  2006-­‐2012  (Boston)   •   Linear  mean  sea  level  rates  (        )  &  95%  confidence   intervals  (mm/yr)  calculated  from  1921  to  recent  years   (2006-­‐2012)  at  the  NOAA  Boston  @de  gauge  sta@on   •  Values  are  trend  of  en@re  data  period  up  to  that  year  
  • 9. Great  Marsh  Sediment  Accre8on   •  •  Marshes  accrete  by  trapping  sediment  &  by  organic  ma8er   accumula@on  from  roots  &  rhizomes   Maximum  accre@on  for  Great  Marsh  currently  recorded  ~  6  mm/yr   Courtesy  of  Anne  Giblin,  Marine  Biological  Lab  
  • 10. Wetland  Types   Eleva@on   66%  wetland   Majority   Mean  High   Water  Spring   Mean  High   Water   Mean  Tide   Level   Mean  Low   Water   Water   Unconsolidated   Salt   Shore*   Marsh   Brackish/     Freshwater   Transi@onal   Wetlands   Dry  Lands   *includes  silt,  sand,  or  gravel  that  is  subject  to  inunda@on  and  redistribu@on  due  to  the  ac@on   of  water;  substrates  lack  vegeta@on  
  • 11.
  • 12.
  • 13.
  • 14.
  • 15.
  • 16.
  • 17.
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  • 19.
  • 20.
  • 21. Marsh  Migra8on  Limited  by   Development  &  Infrastructure  (Newbury)   Current   75-­‐Year  Time  Horizon  (2080)     Net  marsh  impact  =  MHHW  +   4.5  l  sea  level  rise  –  1  l  accre@on  
  • 22. Marsh  Migra8on  Limited  by   Development  &  Infrastructure  (Salisbury)   Current   75-­‐Year  Time  Horizon  (2080)     Net  marsh  impact  =  MHHW  +   4.5  l  sea  level  rise  –  1  l  accre@on  
  • 23. Marsh  Conversion  to  Unconsolidated  Shore   (Gloucester)   Current   75-­‐Year  Time  Horizon  (2080)     Net  marsh  impact  =  MHHW  +   4.5  l  sea  level  rise  –  1  l  accre@on  
  • 24. Marsh  Conversion  to  Unconsolidated  Shore   (Salisbury)   Current   75-­‐Year  Time  Horizon  (2080)     Net  marsh  impact  =  MHHW  +   4.5  l  sea  level  rise  –  1  l  accre@on  
  • 25. Marsh  Migra8on  Modeling  Resource   www.csc.noaa.gov/digitalcoast/publica@ons/marshesonthemove  
  • 26. Applying  SLR  Data/Mapping   •  Great  Marsh   communi@es  are   currently   grappling  with   retrofinng  areas   that  were   developed   before  SLR  and   climate  change   issues  were   recognized  
  • 27. Applying  SLR  Data/Mapping   •  Past   experience   •  What  do  we   know  now?   •  What  can  we   do   differently?   •  What  have   we  learned?  
  • 28. Altera8ons  that  Limit  Natural  Resilience   •  Development  in  flood   prone  areas   •  Impervious  floodplains   •  Culverted  streams  and   rivers   •  Tidal  restric@ons   •  Armored  river  and  coastal   banks   •  Hardened  shorelines   •  Barriers  to  marsh   migra@on   NOAA  photo  
  • 29. Altera8ons  that  Limit  Natural  Resilience   •  Development  in  flood   prone  areas  
  • 30. Altera8ons  that  Limit  Natural  Resilience   •  Impervious   floodplains  
  • 31. Altera8ons  that  Limit  Natural  Resilience   •  Confined   stream  and   river  beds  
  • 32. Altera8ons  that  Limit  Natural  Resilience   •  Tidal  Restric@ons   •  Causeways   •  Low-­‐lying  roadways  
  • 33. Altera8ons  that  Limit  Natural  Resilience   •  Armored  river  and   coastal  banks  
  • 34. Altera8ons  that  Limit  Natural  Resilience   •  Hardened  shorelines  
  • 35. Altera8ons  that  Limit  Natural  Resilience   •  Barriers  to  marsh   migra@on   Photo:  Maine  Sea  Grant  
  • 36. Altera8ons  that  Limit  Natural  Resilience   •  Dams   •  Culverts  
  • 37. Sea  Level  Rising/Climate  Changing:     Key  Resource  Func8ons  to  Consider   •  A8enua@on  of      flood  waters   •  Ability  of  storm/flood   waters  to  recede   •  Sediment  availability   and  transport   •  Energy  dissipa@on   •  Natural  resource   adapta@on   •  Ecosystem  con@nuity  
  • 38. AXenua8on  of  Flood  Waters   •  Limit  impervious  areas   •  Preserve  open  space  in   developments   •  Incorporate  LID   •  Avoid  hardening   stream  and  riverbanks   •  Rethink  new   development  in  flood   prone  areas  
  • 39. Ability  of  Storm/Floodwaters  to  Recede   •  Limit  new  impervious/ incorporate  LID  and   •  Address  restric@ons  and   inappropriate  culvert   designs   •  Dam  removal   •  Preserve  open  space  in   developments   •  Where  do  floodwaters   go?   •  Consider  ousall   loca@ons   AP  photo   Reuters  photo  
  • 40. Sediment  Availability  and  Transport   •  Unarmored  banks   •  Bioengineering   alterna@ves   •  Re-­‐nourishment   •  Open  pilings  for   development   •  Re-­‐vegeta@on  
  • 41. Energy  Dissipa8on   •  Protect  dune  stability   •  Sediment  supply   •  Maintain  floodplain   func@on   •  Sol  bank  stabiliza@on   techniques  
  • 42. Natural  Resource  Adapta8on   •  Marsh  migra@on  and   accre@on   •  Barrier  beach  migra@on    
  • 43. Ques8ons?   Julia  Knisel   CZM  Coastal  Shoreline  and  Floodplain  Manager   617-­‐626-­‐1191;  julia.knisel@state.ma.us   Kathryn  Glenn   CZM  North  Shore  Regional  Coordinator   978-­‐281-­‐3868;  kathryn.glenn@state.ma.us