But scientists gathered valuable data on
coastal ocean currents before instruments went offline
Not exact matches
An initial high - resolution study shows that off Peru the
ocean layer called «oxygen minimum» where life is limited is sensitive to the intensity of the seasonal
current from the equator that brings water containing little oxygen to the
coastal ecosystem.
Pushed by the natural motion of wind and
ocean currents — often over long distances — the litter is present in
oceans worldwide, as well as in sea floor sediment and
coastal sands.
The waters probed during this study, known as the California
Current, are a hot spot of
ocean acidification because of
coastal upwelling, which brings naturally acidic waters to the surface, where they are made even more acidic by greenhouse gas pollution.
Greenland's ice sheet melts and sends large amounts of fresh water into the
coastal waters, where it is of major importance for local production but potentially also for global
ocean currents.
Unexpectedly, this more detailed approach suggests changes in Antarctic
coastal winds due to climate change and their impact on
coastal currents could be even more important on melting of the ice shelves than the broader warming of the
ocean.
That's because a
current of cold
ocean water moves from north to south along the West Coast, cooling the
coastal Pacific and removing the threat of hurricanes, which form only when low pressure systems siphon off the energy from warm
ocean water.
That may mean making politically unpalatable choices like retreat from
current ocean shorelines, an effort actually under way in New York via buyouts of some
coastal residents.
Coastal and boundary
current systems with a focus on processes that link the nearshore and continental shelf to the open
ocean, such as along - and across - shore transport processes, stirring and mixing of water masses, and the
coastal response to larger - scale forcing events; long - duration, high - resolution observations using autonomous underwater gliders.
Fewer predators (do not need the protection of a pod) in the
current habitat - most lone dolphins are observed in
coastal habitats, whereas when found in the open
ocean lone dolphins will swim with other species of cetaceans
Kenya's coastline offers 500 kilometres of tranquil Indian
Ocean beaches and the announcement expands the
current coastal product offering.
-- Climate impacts: global temperatures, ice cap melting,
ocean currents, ENSO, volcanic impacts, tipping points, severe weather events — Environment impacts: ecosystem changes, disease vectors,
coastal flooding, marine ecosystem, agricultural system — Government actions: US political views, world - wide political views, carbon tax / cap - and - trade restrictions, state and city efforts — Reducing GHGs: + electric power systems: fossil fuel use, conservation, solar, wind, geothermal, nuclear, tidal, other + transportation sector: conservation, mass transit, high speed rail, air travel, auto / truck (mileage issues, PHEVs, EVs, biofuels, hydrogen) + architectural structure design: home / office energy use, home / office conservation, passive solar, other
Such as wildfire feedback,
coastal erosion, weather / atmospheric anomalies, seasonal changes, species adaptation,
ocean currents etc..
Using an
ocean circulation model for the shelf, the authors find that surface temperatures may increase by 0.5 to 2.0 °C, seasonal surface salinity may drop by up to 2 PSS in some areas, and that Haida Eddies will strengthen, as will the Vancouver Island
Coastal Current and freshwater discharges into
coastal waters.
Extension of the
current synoptic capacity of 6 - 7 days to 14 days would be a great start, but the lack of sufficient weather in the
oceans would make this difficult to achieve for vulnerable
coastal communities.
This policy document aims to provide context for Rio +20 discussions through analysis of
current challenges in
ocean and
coastal management around the world, assessment of how well the multiple goals and objectives of previous international efforts have been met, and building on recent dialogue and inputs including the meeting of the UN Informal Consultative Process on
Oceans and the Law of the Sea (UNICPOLOS) and the Secretary General's report on
Oceans and Law of the Sea.
(Sec. 479) Requires each state to prepare a natural resources adaptation plan detailing the state's
current and projected efforts to address the potential impacts of climate change and
ocean acidification on natural resources and
coastal areas in order to be eligible for funds under this subpart.
This study shows that a weaker surface
ocean current system produces colder
coastal SST's along the Atlantic coast of Florida, thereby reducing the length and the total seasonal accumulation of rainfall in the wet season of Peninsular Florida relative to the simulation in which these
currents are stronger.
The results also highlight
coastal regions that are well - represented in
current generation climate models (and those that are not) and the time periods over which
coastal sea level may be used as a proxy for the large - scale
ocean circulation.
-- In order to be eligible for funds under section 480, not later than 1 year after the development of a Natural Resources Climate Change Adaptation Strategy required under section 476 each State shall prepare a State natural resources adaptation plan detailing the State's
current and projected efforts to address the potential impacts of climate change and
ocean acidification on natural resources and
coastal areas within the State's jurisdiction.
The complicated
currents within the
ocean slosh the growing heat around, in 2D (ENSO, PDO, NAO, AO, AAO) and 3D (thermohaline conveyor belt,
coastal upwellings,
ocean terrain dependent vertical
currents, etc).
Nevertheless, if El Niño comes on as strong as
current projections seem to indicate, we can say with some level of confidence that
coastal South American countries will see above average rainfall and flooding in the coming months, while countries on the other side of the
ocean like Australia and Indonesia will likely see drought.
In Washington and Oregon, oysters farms are in
coastal Pacific waters where upwelling
currents are bringing up cold, deep water with higher amounts of CO2 and a more acidic pH. Watch and listen to two oyster farmers from Taylor Shellfish Farms in Washington state talk how about
ocean acidification is impacting their young oysters.
Tide heights near ice shelves can be measured using traditional
coastal tide gauges and bottom pressure recorders, while
currents can be measured with meters on moorings in the open
ocean or deployed through boreholes drilled through ice shelves, which are the floating portions of ice sheets.
What about earthquake - induced elevation change,
coastal erosion change following a cliff fall, temperature and precipitation change from variation in
ocean currents, effects of ENSO, PDO and AMO, etc..?
Lansner and Pepke Pedersen (2018) point out that, due to the divergent rates of warming and cooling for land vs.
ocean water, there is a significant difference in the range of temperature for the regions of the world influenced by their close proximity to
oceans and
coastal wind
currents (
ocean air affected, or OAA) and the inland regions of the world that are unaffected by
ocean air effects and
coastal wind because they are sheltered by hills and mountains or located in valleys (
ocean air sheltered, or OAS).
Whether it's the threat of dramatic sea level rise to
coastal areas or
current climate change refugees from low - lying islands, the effects of climate change and global warming on the world's
oceans are both real and imminent.
As I understand it central Greenland varied 2.5 C over the last 2000 years but the
coastal slopes varied as much as 5 - 7C due to changes in
ocean currents.
Threats to marine biodiversity in the U.S. are the same as those for most of the world: overexploitation of living resources; reduced water quality;
coastal development; shipping; invasive species; rising temperature and concentrations of carbon dioxide in the surface
ocean, and other changes that may be consequences of global change, including shifting
currents; increased number and size of hypoxic or anoxic areas; and increased number and duration of harmful algal blooms.
Hence, how the pH of
coastal ecosystems in year 2100 will differ from
current ones is difficult to predict due to lack of understanding of the average values and their variability in
current environments and of the future trajectories of the multiple factors affecting
coastal pH compared to the open
ocean.
Hence, the
current narrative of OA as an anthropogenic process driven by increased CO2 emissions to the atmosphere and subsequent dissolution in the
ocean is only applicable partially to the
coastal ocean where anthropogenic impacts on pH have multiple sources and vary in intensity and direction.
The California
Current System (CCS) contains one of the five major
coastal upwelling zones in the world's
oceans, and hosts a great diversity and abundance of marine life [1].
Airborne Researchers Measure Greenland's Ice (Reporter package) View Animation Greenland's
coastal ice is disappearing fast enough that at its
current rate of decline it will contribute to a rise in the world's
oceans of a little less than a centimeter in the space of a single human lifetime.