Living Estuaries Estuaries, the vital
coastal zones where rivers and streams meet the oceans.
Not exact matches
Though relatively small in comparison to the open ocean, the
coastal zones are
where an extremely large amount of the carbon dioxide is exchanged between air and water.
The researchers compiled urban development, flood hazard and census data and overlaid it on a map of the U.S.. Although their analysis shows that Americans in general have become more aware of the risk of floods over the 10 - year study period, the researchers identified several U.S. hot spots
where urban development has grown in
coastal flood
zones including New York City and Miami.
«However, combined effects of nutrient loading and climate change are greatly increasing the number and size of «dead
zones» in the open ocean and
coastal waters,
where oxygen is too low to support most marine life.»
The eddies also supply nutrients to
coastal zones and the surface ocean
where plankton blooms may result.
For centuries Kenya was part of a
coastal trading
zone along the Indian Ocean
where.
Such knowledge is important in a warming world
where water column deoxygenation in the
coastal zone is becoming more and more common.Link
Areas of the
coastal ocean
where oxygen is low or absent in bottom waters, so - called dead
zones, are expanding worldwide (Diaz and Rosenberg, 2008).
And excess nitrogen fertilizer applied to the fields of feed corn grown to satisfy the world's livestock runs off into streams and rivers, sometimes flowing to
coastal waters
where it creates large algal blooms and low - oxygen «dead
zones»
where fish can not survive.
Sea - level changes are of special significance, not only for the low - lying atoll islands but for many high islands
where settlements, infrastructure and facilities are concentrated in the
coastal zone.
Dead
zones are caused by several factors, particularly eutrophication
where too many nutrients run off
coastal cities and agricultural areas into rivers that carry these materials out to sea.
The
coastal islands off the west of Ireland are known for ancient soil - building,
where beach sand and seaweed were transported — sometimes miles — to allow agriculture in barren rocky
zones.
However, the conditions predicted for the open ocean may not reflect the future conditions in the
coastal zone,
where many of these organisms live (Hendriks et al. 2010a, b; Hofmann et al. 2011; Kelly and Hofmann 2012), and results derived from changes in pH in
coastal ecosystems often include processes other than OA, such as emissions from volcanic vents, eutrophication, upwelling and long - term changes in the geological cycle of CO2, which commonly involve simultaneous changes in other key factors affecting the performance of calcifiers, thereby confounding the response expected from OA by anthropogenic CO2 alone.
Calculations to resolve the anthropogenic component of CO2 are remarkably difficult for the
coastal ocean,
where the assumptions of the various methods (Sabine and Tanhua 2010) are not met, thereby precluding a direct calculation of the effect of anthropogenic CO2 on observed trends in
coastal pH. Calculations based on mixing between an open - ocean end - member displaying the trajectories predicted from OA and the freshwater end - member are also unreliable because pH and the carbon system do not necessarily behave conservatively within the
coastal zone and because the freshwater end - member may also shift into the future.
Such knowledge is important in a warming world
where water column deoxygenation in the
coastal zone is becoming more and more common.
The expected outputs range from integrating climate change risks into development planning and
coastal zoning regulation to diversifying livelihoods to finding more secure sources of water in communities
where saline intrusion is a problem (Community Based Adaptation to Climate Change through
Coastal Afforestation).
Additionally, there is a designated
coastal zone of varying width in which
where all proposed development must be reviewed and approved by the California
Coastal Commission.