Remotely Sensed Reflectance over the Heuksan Mud Belt, Korea
Transcript of Remotely Sensed Reflectance over the Heuksan Mud Belt, Korea
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Remotely Sensed Reflectance over the Heuksan Mud Belt, Korea
Catherine Evans
Supervisor: Dr. Paul Hill
AGS Colloquium 2019
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Introduction to the Project
• Remote sensing can give surfacepatterns of ocean color.
• Sediment changes the ocean color.
• Can we infer subsurfacesedimentary processes with satellite images?
Image Source: Chardon (2008)
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Suspended Particulate Matter Matters?• Visibility hazards
• Navigation
• Affects productivity
• Transports pollutants
How do we study Suspended Sediment?
• In Situ Measurements• Landsat 8 - Bands 4 and 5
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Primary Study Site • Heuksan Mud Belt (HMB)
• Southeastern Yellow Sea.
• Mud and silt.
• Macrotidal environment.
• Peak flow speed of 1.5 m/s.
Lee, Yong (2001)
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Field Results
• Stratified at peak flow
• Very high concentration
Sediment Concentration Vs. Depth
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Project Goals• Determine reflectance patterns over channel
and ridge.
• Explore reasons for variability.
• Link to subsurface mechanisms.
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Hypothesis
• Banded pattern matches bathymetry.
• Tidal current creates lutocline.
• Remote sensing can determine subsurface process with surface SPM.
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Methods
Environmental Variables
Ridge and Channel Reflectance
Statistical Tests and
Interpretations
Results
Landsat Bands 4 and 5 (B4, B5)
Image source: https://earthexplorer.usgs.gov/
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Heuksan Mud Belt (HMB)
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Channel Reflectance Levels: Bathymetry• Bathymetry vs reflectance
demonstrates a negative trend.
• Due to tidal current, lutocline.
• Subsurface processes resolved from space.
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Why do we see these patterns?
• Channel has a lower reflectance than ridge.
• What causes variability?• Environmental variables
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Correlation Results: HMB
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Sites
https://commons.wikimedia.org/wiki/Maps_of_the_world#/media/File:BlankMap-World-v2.png
Heuksan Mud Belt (HMB) Gyeonggi Bay (GB) Gulf of Khambhat (GOK)1 2 3
N = 15 N = 46N = 15
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Gyeonggi Bay (GB)
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Gulf of Khambhat (GOK)
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Channel Reflectance Levels: Bathymetry
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Conclusions
• Surface reflectance correlates with depth in all three sites.
• Supports hypothesis of suspended sediment stratification at depth.
• Subsurface process resolved with remote sensing of surface.
• Method for identifying other areas for suspended sediment stratification in tidal seas.
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Acknowledgements
• Dr. Paul Hill
• Dalhousie University Faculties of Earth Sciences & Oceanography
• Department of The Navy Office of Naval Research
• Fisheries and Oceans Canada
• Coordinators and hosts of AGS
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Sources
• Hill, P. (TBA).• Lee, H. J. (2001). Origin of Inner-Shelf Mud Deposit in the Southeastern
Yellow Sea: Huksan Mud Belt. Journal of Sedimentary Research, 144-154.• Lee, H. J. (2015). A Review on the Holocene evolution of an Inner-shelf
Mud Deposit in the Southeastern Yellow Sea: the Huksan Mud Belt. Ocean Science Journal, 615-621.
• Park S. C., L. H. (2000). Evolution of late Quaternary mud deposits and recent sediment budget in the southeastern Yellow Sea. Marine geology, 271-288.
• WorldMap. https://commons.wikimedia.org/wiki/Maps_of_the_world#/media/File:BlankMap-World-v2.png