The US CLIVAR PSMI Panel seeks new panelists with prior expertise in field / process studies or model development in one or more of the following areas: (a) clouds, (b) high - frequency ocean - atmosphere interaction (diurnal to sub-seasonal), (c)
coastal ocean processes, (d) high - latitude processes (i.e., Arctic, Antarctic, ocean - ice interactions), or (e) ocean biogeochemical cycles / ecosystem interactions.
By bringing together microbial ecologists, biogeochemists her group examines the influence of microbial communities on
coastal ocean processes, especially in light of a changing climate.
Not exact matches
The centre's research focuses on the mid-
ocean-ridges and plate tectonic
processes, the deep
ocean (emphasizing biological and geochemical
processes), the upper
ocean (emphasizing the chemical and biological
processes), and the management of the
coastal environment.
«A lot of what we are seeing right now in the
coastal regions is that warming
ocean waters are melting Antarctica's glaciers and ice shelves, but this
process may just be the beginning,» Shevenell said.
«This is because the
coastal ocean is shallower than the open ocean and can quickly transfer sequestered carbon dioxide to the deep ocean; this process creates an additional and effective pathway for the ocean to take up and store anthropogenic carbon dioxide,» said Cai, the Mary A.S. Lighthipe Professor in the College of Earth, Ocean, and Environ
ocean is shallower than the open
ocean and can quickly transfer sequestered carbon dioxide to the deep ocean; this process creates an additional and effective pathway for the ocean to take up and store anthropogenic carbon dioxide,» said Cai, the Mary A.S. Lighthipe Professor in the College of Earth, Ocean, and Environ
ocean and can quickly transfer sequestered carbon dioxide to the deep
ocean; this process creates an additional and effective pathway for the ocean to take up and store anthropogenic carbon dioxide,» said Cai, the Mary A.S. Lighthipe Professor in the College of Earth, Ocean, and Environ
ocean; this
process creates an additional and effective pathway for the
ocean to take up and store anthropogenic carbon dioxide,» said Cai, the Mary A.S. Lighthipe Professor in the College of Earth, Ocean, and Environ
ocean to take up and store anthropogenic carbon dioxide,» said Cai, the Mary A.S. Lighthipe Professor in the College of Earth,
Ocean, and Environ
Ocean, and Environment.
The Marine Sciences Laboratory's, Sequim Marine Research Operations is located on Sequim Bay in Washington's Puget Sound, offers various research capabilities in ecotoxicology, analytical chemistry, wetland and
coastal ecology, fisheries,
ocean processes, remote sensing, biotechnology and remediation.
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.
Our philosophy emphasizes the importance of understanding the
processes that govern change and sustainability in the world's
oceans to best use and protect our vital marine and
coastal resources.
My understanding of this
process is that it mostly occurs near
coastal upwellings which bring up nutrients from the deep and that it is responsible for a significant fraction of
ocean carbon sequestration.
All the
coastal oceans receive far more fixed nitrogen from humans than they can
process.
This WP aims to improve the resolution of
ocean models, as well as the representation of physical and biogeochemical processes, in key regions of the world's oceans (particularly tropical coastal regions, the Southern Ocean and high Northern latitudes) to reduce well known biases in
ocean models, as well as the representation of physical and biogeochemical
processes, in key regions of the world's
oceans (particularly tropical
coastal regions, the Southern
Ocean and high Northern latitudes) to reduce well known biases in
Ocean and high Northern latitudes) to reduce well known biases in ESMs.
increased CO -LCB- sub 2 -RCB- by using
ocean models that include realistic
processes such as horizontal heat transport, vertical mixing due to convection and small - scale
processes, and upwelling along
coastal regions and the equator.
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.
Employing these principles may help reduce impacts to
ocean recreation, nearshore ecology,
coastal processes, public safety, aesthetics, and fishing access.
Their safety and resilience depends on the effectiveness of natural and man - made
coastal flood protection, i.e. the capacity of the
coastal zone to act as a buffer and absorb
ocean energy through complex wave shoaling and breaking
processes.
Surfrider also recognizes that there are many questions and concerns about
ocean energy, including potential impacts to
ocean recreation, nearshore ecology,
coastal processes, public safety, aesthetics, and fishing access.
The strong controls that ecosystem metabolism and watershed
processes exert on the pH in
coastal ecosystems suggest that strategies based on the management of ecosystem components and watershed
processes may help buffer the impacts of OA by anthropogenic CO2 locally, an option not available for the open
ocean.
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.
This new concept of anthropogenic impacts on seawater pH formulated here accommodates the broad range of mechanisms involved in the anthropogenic forcing of pH in
coastal ecosystems, including changes in land use, nutrient inputs, ecosystem structure and net metabolism, and emissions of gases to the atmosphere affecting the carbon system and associated pH. The new paradigm is applicable across marine systems, from open -
ocean and
ocean - dominated
coastal systems, where OA by anthropogenic CO2 is the dominant mechanism of anthropogenic impacts on marine pH, to
coastal ecosystems where a range of natural and anthropogenic
processes may operate to affect pH.
River - dominated systems will reflect the dynamics of the freshwater end - member, and the deviation of
coastal ecosystems supporting intense metabolism from the conservative mixing lines delineated by the open -
ocean and freshwater end - members will depend on water residence time and mixing
processes (Anthony et al. 2011; Falter et al. 2013).
These models would be composed of regional oceanographic modelling systems, forced both by GCMs, capturing the transport of anthropogenic CO2 to the
coastal ocean and watershed
processes.
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.
Air - sea interaction, wave dynamics and wave breaking, effect of near - surface turbulence on heat, gas, and momentum transport, infrared remote sensing, upper -
ocean processes,
coastal and estuarine
processes.