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Wonders of Wetlands

COESSING Regional Maritime UniversityAugust 9, 2019

Wonders of Wetlands(& coastal ecosystems)

COESSING Regional Maritime UniversityAugust 9, 2019

Coastal Zone

Coastal Zone

Coastal Zone

Three main classifications

Wave dominated

Three main classifications

Tidally dominated

Wave dominated

Three main classifications

Tidally dominated River

dominated

Wave dominated

Three main classifications

Tidally dominated River

dominated

Wave dominated

Parameters and processes of interest

Wave-dominated Coasts

• Fetch = the distance over which wind blows on the sea surface, generating and propagating waves

Wave-dominated coasts

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• Wave height (H) = distance from crest to trough

Wave-dominated coasts

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• Wave height (H) = distance from crest to trough

Wave-dominated coasts

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Wave height

• Significant wave height (HS) = average height of the largest 1/3 of waves

Wave-dominated coasts

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Rayleigh Distribution:

NOAA

• Significant wave height (HS) = average height of the largest 1/3 of waves

Wave-dominated coasts

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Rayleigh Distribution:

NOAA

Atlantic Ocean Æ HS is about 2 m

Tidally-dominated coasts

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Tidally-dominated coasts

18NOS Tidal Datums pub

Tidally-dominated coasts

19NOS Tidal Datums pub

Tidally-dominated coasts

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High in the tidal frame

NOS Tidal Datums pub

Tidally-dominated coasts

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High in the tidal frame

Low in the tidal frame

NOS Tidal Datums pub

Vegetation is influenced by the tide range

Flemming, Siliciclastic Back-Barrier Tidal Flats

Size of the tide range: Macro-, Meso-, Microtidal

Vegetation is influenced by the tide range

Flemming, Siliciclastic Back-Barrier Tidal Flats

Size of the tide range: Macro-, Meso-, Microtidal

Vegetation and landform are influenced by the tide range

Adopted from Haslett, Coastal Systems

Microtidal Mesotidal Macrotidal

Salt marshes

Mudflats

Funnel Estuaries

Tidal Deltas

Barrier Islands

River Deltas

River-dominated coasts

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River-dominated coasts

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Seybold et al. 2007

http://www.seddepseq.co.uk/depositional_env/deltas/deltas.htm

http://www.seddepseq.co.uk/depositional_env/deltas/deltas.htm

http://www.seddepseq.co.uk/depositional_env/deltas/deltas.htm

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Sweet et al. 2017

Causes of sea level change

Can deltas keep pace with sea-level rise?

42Giosan et al. 2014

Can deltas keep pace with sea-level rise?

43Giosan et al. 2014

no net emissions Æ sea-level rise = 0.3 m by 2100high emissions Æ sea-level rise = 2.5 m by 2100

(Sweet et al. 2017)

Mangroves around the world

Source: Giri, 2016

Ecosystem Services from salt marshes and mangroves

1. Habitat2. Carbon sequestration 3. Water treatment4. Wave attenuation/erosion control 5. Valuable goods 6. Flood reduction

1. Habitat2. Carbon sequestration 3. Water treatment4. Wave attenuation/erosion control 5. Valuable goods 6. Flood reduction

Ecosystem Services from salt marshes and mangroves

Carbon Sequestration

Mangroves among the most carbon-rich forests in the tropics

Donato et al 2011

Carbon Sequestration

“Blue Carbon” is carbon stored in wet environments (marshes, sea grass, mangroves)

Carbon Sequestration

“Blue Carbon” is carbon stored in wet environments (marshes, sea grass, mangroves)

Occurs via sedimentation and biomass burial

Sediment Capture

Suspended Sediment

Sediment Capture

SSC =Suspended SedimentConcentration

Sediment Capture

Sediment Capture

Sediment Capture

Sediment Capture

Sediment Capture

Accretion

Sediment Capture

Burial of Biomass

Burial of Biomass

Burial of Biomass

Anaerobic Decomposition

verrryyyyyyy sloooowwAnd can be smelly

Burial of Biomass

Burial of Biomass

Burial of Biomass

ErosionAccretion

ErosionAccretion

• Greater biomass• High SSC• Inundation time• Desiccation time

Case Study: Spatial Mapping of Carbon Stock

• Field Measurement

Diameter Tape

Lily Lisa YevugahKNUST

Classified Landsat Image

• Insert: images

Lily Lisa YevugahKNUST

Results on Carbon Map

Lily Lisa YevugahKNUST

Mangroves can keep pace with sea level rise

Mangroves can keep pace withsea level rise

Mangroves can keep pace with sea level rise

Mangroves can keep pace with sea level rise

Mangroves can keep pace with sea level rise

Important! Rate of sea level rise is increasing

Mangroves can keep pace with sea level rise

Ecosystem Services from salt marshes and mangroves

1. Habitat2. Carbon sequestration 3. Water treatment4. Wave attenuation/erosion control 5. Valuable goods 6. Flood reduction

Water Treatment

http://www.wetlands-initiative.org/nutrient-removal/

Water Treatment

Ecosystem Services from salt marshes and mangroves

1. Habitat2. Carbon sequestration 3. Water treatment4. Wave attenuation/erosion control 5. Valuable goods 6. Flood reduction

Case Study: Wave Attenuation

Loss of wave energy (Æcalculate from wave height)

Case Study: Wave Attenuation

Loss of wave energy (Æcalculate from wave height)

Case Study: Wave Attenuation

Loss of wave energy (Æcalculate from wave height)

Smaller Larger

H H

Case Study: Wave Attenuation

Why do we care?

Smaller Larger

H H

1. Storm Protection2. Geomorphology3. Modelling

Case Study: Wave Attenuation

How do we measure it?

Case Study: Wave Attenuation

How do we measure it?

High-Frequency Pressure Sensors

Case Study: Wave Attenuation

How do we measure it?

Time [sec]

Dept

h [m

]

Case Study: Wave Attenuation

How do we measure it?

Time [sec]

Dept

h [m

]

Case Study: Wave Attenuation

How do we measure it?

Time [sec]

Dept

h [m

]

Case Study: Wave Attenuation

How do we measure it?

Time [sec]

Dept

h [m

]

Case Study: Wave Attenuation

How do we measure it?

Time [sec]

Dept

h [m

]Case Study: Wave Attenuation

Measured the depth every 8 sec → 8 Hz

Case Study: Wave Attenuation

Compare the waves at each station

Wave Attenuation C D

Calm Turbulent Pinsky et al. 2013

Wave Attenuation C D

Function of the local conditions

Pinsky et al. 2013

Conservation > Restoration

Conservation > Restoration

• Less resilient to sea level rise•More prone to erosion • Less belowground biomass

Salt ponds

Salt ponds

Conservation > Restoration

Hardened Shorelines

Hardened Shorelines

1. Need to plan for sea level rise for our future generations2. Consider how coastal development changes the natural coastal processes

Main Takeaways

Thank you! Medaase!