The recentlyreleased 2016 NOAA-funded forecast calls for an about average dead zone in theChesapeake Bay this summer. Scientists are predicting that the dead zone in
the nation's largest estuary will cover a volume of 1.58 cubic miles, just
about the long term average since 1950. The University of Maryland Center for
Environmental Science and University of Michigan scientists who developed the
model that forecast the: midsummer low-oxygen hypoxic zone, early-summer
oxygen-free anoxic zone, and late-summer oxygen-free anoxic zone that we call
the dead zone. The scientists to the
cool and relatively dry spring in Pennsylvania followed by late arriving rains
the same thing that happened in 2013 and 2015. The spring load of nutrients
into the bay was light and locked in a lighter load of nutrients in the water
layers within the Chesapeake Bay for the summer.
The forecast is based to a large extent on the quantity and timing of rainfall in the Chesapeake Bay watershed, but there is hope that this also reflects that the overall condition of the bay may be improving in response to the mandated U.S. Environmental Protection Agency TMDL coordinated by the Chesapeake Bay Program. "There has been a recent trend toward less hypoxia later in the summer that may signal an emerging response to actual reductions in nutrient pollution," said Donald Boesch, Ph.D., president of the University of Maryland Center for Environmental Science. It is difficult to know if this is the proof that the Watershed improvement plans are working.
The predicted “dead zone” size is based on models that forecast the zone based on midsummer volume of the low-oxygen hypoxic zone, early-summer oxygen-free anoxic zone, and late-summer oxygen-free anoxic zone. The models were developed by NOAA-sponsored research at the University of Maryland Center for Environmental Science and the University ofMichigan. They rely on nutrient loading estimates supplied by the U. S. Geological Survey. USGS provides nutrient runoff and river stream data used in the forecast models. USGS estimates that the Susquehanna River delivered 66.2 million pounds of nitrogen to the Bay from January to May 2016, which is 17% below average.
Later this year researchers will measure oxygen levels in the Chesapeake Bay. The model forecasts are then combined with the oxygen measurements taken during summer monitoring cruises to improve our understanding of how nutrients, hydrology, and other factors affect the size of the hypoxic zone. Improved understanding will result in improved the models which are used in turn to develop effective strategies for reducing dead zones.
Dead zones have become a yearly occurrence in the Chesapeake Bay and other estuaries. Dead zones form in summers when higher temperatures reduce the oxygen holding capacity of the water, the air is still and especially in years of heavy rains that carry excess nutrient pollution from cities and farms. The excess nutrient pollution combined with mild weather encourages the explosive growth of phytoplankton, which is a single-celled algae. While the phytoplankton produces oxygen during photosynthesis, when there is excessive growth of algae the light is chocked out and the algae die and fall from the warmer fresh water into the colder sea water. The phytoplankton is decomposed by bacteria, which consumes the already depleted oxygen in the lower salt level, leaving dead oysters, clams, fish and crabs in their wake.
In a wedge shaped estuary such as Chesapeake Bay where the layers of fresh and salt water are not well mixed, there are several sources of dissolved oxygen. The most important is the atmosphere. At sea level, air contains about 21% oxygen, while the Bay’s waters contain only a small fraction of a percent. This large difference between the amount of oxygen results in oxygen naturally dissolving into the water. This process is further enhanced by the wind, which mixes the surface of the water. The other important sources of oxygen in the water are phytoplankton and aquatic grasses which produce oxygen during photosynthesis, but when they die consume oxygen during decomposition by bacteria. Finally, dissolved oxygen flows into the Bay with the water coming from streams, rivers, and the Atlantic Ocean.
The forecast is based to a large extent on the quantity and timing of rainfall in the Chesapeake Bay watershed, but there is hope that this also reflects that the overall condition of the bay may be improving in response to the mandated U.S. Environmental Protection Agency TMDL coordinated by the Chesapeake Bay Program. "There has been a recent trend toward less hypoxia later in the summer that may signal an emerging response to actual reductions in nutrient pollution," said Donald Boesch, Ph.D., president of the University of Maryland Center for Environmental Science. It is difficult to know if this is the proof that the Watershed improvement plans are working.
The predicted “dead zone” size is based on models that forecast the zone based on midsummer volume of the low-oxygen hypoxic zone, early-summer oxygen-free anoxic zone, and late-summer oxygen-free anoxic zone. The models were developed by NOAA-sponsored research at the University of Maryland Center for Environmental Science and the University ofMichigan. They rely on nutrient loading estimates supplied by the U. S. Geological Survey. USGS provides nutrient runoff and river stream data used in the forecast models. USGS estimates that the Susquehanna River delivered 66.2 million pounds of nitrogen to the Bay from January to May 2016, which is 17% below average.
Later this year researchers will measure oxygen levels in the Chesapeake Bay. The model forecasts are then combined with the oxygen measurements taken during summer monitoring cruises to improve our understanding of how nutrients, hydrology, and other factors affect the size of the hypoxic zone. Improved understanding will result in improved the models which are used in turn to develop effective strategies for reducing dead zones.
Dead zones have become a yearly occurrence in the Chesapeake Bay and other estuaries. Dead zones form in summers when higher temperatures reduce the oxygen holding capacity of the water, the air is still and especially in years of heavy rains that carry excess nutrient pollution from cities and farms. The excess nutrient pollution combined with mild weather encourages the explosive growth of phytoplankton, which is a single-celled algae. While the phytoplankton produces oxygen during photosynthesis, when there is excessive growth of algae the light is chocked out and the algae die and fall from the warmer fresh water into the colder sea water. The phytoplankton is decomposed by bacteria, which consumes the already depleted oxygen in the lower salt level, leaving dead oysters, clams, fish and crabs in their wake.
In a wedge shaped estuary such as Chesapeake Bay where the layers of fresh and salt water are not well mixed, there are several sources of dissolved oxygen. The most important is the atmosphere. At sea level, air contains about 21% oxygen, while the Bay’s waters contain only a small fraction of a percent. This large difference between the amount of oxygen results in oxygen naturally dissolving into the water. This process is further enhanced by the wind, which mixes the surface of the water. The other important sources of oxygen in the water are phytoplankton and aquatic grasses which produce oxygen during photosynthesis, but when they die consume oxygen during decomposition by bacteria. Finally, dissolved oxygen flows into the Bay with the water coming from streams, rivers, and the Atlantic Ocean.
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