Chlorophyll concentrations Productivity Carbon cycling Water clarity and suspended sediment Ocean color Fisheries management Currents Search and Rescue Deep sea drilling, etc.
Chlorophyll is used by plants to trap light energy which then drives photosynthesis Amount of chlorophyll related to amt. of photosynthesis Ocean productivity Carbon cycling Ocean ecology – food webs/fisheries Can estimate amount of chlorophyll in oceans using spectral data and models
Phytoplankton spectral reflectance similar to that of land plants in the visible part of the spectrum Chlorophyll reflects more green visible than blue or red Can 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
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 oceans Can’t be directly measured—must be modeled using remotely sensed data as inputs Function 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 Oct 2002 – note near-shore environments
Open ocean water nearly sediment free – perfectly clear Near-shore water holds variable sediment loads and is more turbid Turbid 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.
Turbidity near Mississippi delta in near-shore Louisiana
Turbid waters are more reflective than clear water Peaks in spectral response depend on: Amount of sediment Depth profile of sediment Type 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.
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 high High chlorophyll content relates to high productivity But…too much productivity or harmful blooms (e.g., red tides) can harm fisheries Ocean currents, climate change, nutrient inputs from land, etc. affect fisheries Pollution can harm fisheries especially near shore All of these things can be monitored with remote sensing and other geospatial tools
SeaWiFS (Sea-viewing Wide Field of view Sensor) Flies on the OrbView-2 platform Designed to monitor ocean color MODIS Flown on the Aqua and Terra platforms Photosynthetic activity of marine organisms Related to carbon cycle in oceans Some MODIS bands designed for ocean RS
SeaWiFS specifications Bands: Visible and NIR 1 km pixels Daily return
“…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
Airborne and satellite imagery used to: Monitor chlorophyll concentrations Monitor sediment loads Model ecosystems Model pollution Manage fishery Track coastal erosion Contribute to near shore land use planning