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Ecology, Climate, Physical Oceanography
Multi and Hyperspectral Remote Sensing for Marine and Coastal
Applications
Bering Sea, AlaskaSeaWifs Image (Norman Kuring image, NASA, April 25, 1998)
Turquoise = phytoplankton bloom
Chlorophyll concentrationsProductivityCarbon cyclingWater clarity and suspended sedimentOcean colorFisheries managementCurrentsSearch and RescueDeep sea drilling, etc.
Some marine applications
Chlorophyll is used by plants to trap light energy which then drives photosynthesis
Amount of chlorophyll related to amt. of photosynthesisOcean productivityCarbon cyclingOcean ecology – food webs/fisheries
Can estimate amount of chlorophyll in oceans using spectral data and models
Ocean chlorophyll concentrations
Upwelling off coast of California
Phytoplankton spectral reflectance similar to that of land plants in the visible part of the spectrumChlorophyll reflects more green visible than
blue or redCan also measure amount of fluorescence with
some sensors (e.g., MODIS)IR light almost all absorbed by water and not
a strong part of the ocean phytoplankton signature
Spectral properties of ocean phytoplankton
Visible Wavelengths NIR Wavelengths
2004 “Red Tide” off coast of Florida with SeaWiFS chlorophyll and MODIS flourescence
Red Tide – La Jolla, California (from Wikipedia)
Measured by the net amount of carbon “fixed” by biota in the oceansCan’t be directly measured—must be modeled
using remotely sensed data as inputsFunction of amount of chlorophyll, ocean
temperature, amount of incoming solar radiation, and mixing models to deal with 3-dimensional ocean (it has depth)
Oceans are net sinks for carbon – remove SOME carbon from the atmosphere each year (but less than enters the atmosphere).
Ocean productivity
From IPCC AR4 (2007)
Ocean plants need sunlight as do land plants – productivity drops off with depth. So does our ability to remotely sense chlorophyll.
Ocean productivity Oct 2002 – note near-shore environments
Open ocean water nearly sediment free – perfectly clear
Near-shore water holds variable sediment loads and is more turbidTurbid water coincides with more productive
parts of ocean near shore due to input of sediment by rivers and shallower water
Turbidity can cause erroneous chlorophyll (and productivity) measurements from RS
Important to know where ocean is turbid so that you can be careful about predicting chlorophyll there.
Water clarity and suspended sediment
Turbidity near Mississippi delta in near-shore Louisiana
Turbid waters are more reflective than clear water
Peaks in spectral response depend on:Amount of sedimentDepth profile of sedimentType of sediment (mineralogy, etc.)
Turbidity can be a temporal phenomenon – sediment input by rivers after floods, stirred up by hurricanes and other wind events, etc.
Spectral properties of turbid water
Change in spectral curves with time in turbid water during settling: 575 nm spectral peak declines with reduced turbidity
Ocean fisheries are most productive where ocean productivity is highHigh chlorophyll content relates to high
productivityBut…too much productivity or harmful blooms
(e.g., red tides) can harm fisheriesOcean currents, climate change, nutrient
inputs from land, etc. affect fisheriesPollution can harm fisheries especially near
shoreAll of these things can be monitored with
remote sensing and other geospatial tools
Fisheries
Global FisheriesTheglobaleducationproject.org
SeaWiFS (Sea-viewing Wide Field of view Sensor)Flies on the OrbView-2 platformDesigned to monitor ocean color
MODISFlown on the Aqua and Terra platformsPhotosynthetic activity of marine organisms
Related to carbon cycle in oceansSome MODIS bands designed for ocean RS
Satellites for Marine Remote Sensing
SeaWiFS specifications
Bands: Visible and NIR1 km pixelsDaily return
Coastal erosion monitoring
Hurricane damage assessment
Estuarine ecologyCoastal geomorphologyCoastal ecologyHuman impacts
Coastal applications of optical RS
“…to detect, assess, and predict the effects of weather, climate, natural hazards, and human activities on the state of the coastal ocean, its ecosystems and living resources, and the U.S. economy. It consists of both a national backbone and regional coastal ocean observing systems…”
Coastal Monitoring Goals…
Chesapeake Bay is the largest estuary in the U.S.
Important fishery (fish, crabs, oysters, etc.)Hammered by pollution from major East Coast
rivers and urban inputs E.g., Susquehanna River, Potomac River,
Washington/Baltimore, etc.Nutrient inputs, pesticides, industrial chemicals, etc.
Very populated coastal zone with vulnerability to erosion, sea level rise, hurricanes, etc.
Many issues common to coastal zones globally
Case Study: Chesapeake Bay
Airborne and satellite imagery used to:
Monitor chlorophyll concentrationsMonitor sediment loadsModel ecosystemsModel pollutionManage fisheryTrack coastal erosionContribute to near shore land use
planning
Remote sensing in Chesapeake Bay
Hurricane Isabel 2003Extensive damage to human structures, coastal erosion and temporary changes in water quality
Ganges Delta, Bangladesh. Coastal zones are often densely populated and vulnerable. Will be a focus of remote sensing for years to come.
Most Chesapeake Bay slides/figures from presentations at a Smithsonian Environmental Research Center symposium.
Acknowledgements