Simulations with general
circulation ocean models do not fully support the gas exchange - sea ice hypothesis.
Modelling of the biological system, however, has been more challenging, and it has only been recently that primitive ecosystem models have been incorporated in global general
circulation ocean models.
Not exact matches
The
models did not show as strong a shift as the observations, Frierson said, suggesting that
ocean circulation also played a role in the drought.
Greatly improved computer
models began to suggest how such jumps could happen, for example through a change in the
circulation of
ocean currents.
This is according to emergency
ocean model simulations run by scientists at the National Oceanography Centre (NOC) and The University of Southampton to assess the potential impact of local
ocean circulation on the spread of pollutants.
These simulations were run using the leading - edge, high - resolution global
ocean circulation model, NEMO.
This
model is widely used by both UK and international groups for research into
ocean circulation, climate and marine ecosystems, and operationally as part of the UK Met Office's weather forecasting.
The results provide new information about the significant dispersion patterns currently un-accounted for in
ocean circulation models, according to the authors.
«We ran five years of
ocean circulation in the
model, and we measured the damping of energy at every grid point to see what the statistics are,» Fox - Kemper said.
The higher resolution
model better reflects the
ocean circulation and sea floor bathymetry in smaller, complex areas like the Gulf of Maine and the U.S. Northeast Shelf.
«Northwest Atlantic
Ocean may get warmer, sooner: High resolution global climate model shows much faster warming and changing ocean circulation.&r
Ocean may get warmer, sooner: High resolution global climate
model shows much faster warming and changing
ocean circulation.&r
ocean circulation.»
Using this
model, it took the researchers two months using 1,000 processors to simulate just five years of
ocean circulation.
«Formation of coastal sea ice in North Pacific drives
ocean circulation, climate: New understanding of changes in North Pacific
ocean circulation over the past 1.2 million years could lead to better global climate
models.»
By incorporating these data into an M.I.T.
model, the result is «realistic descriptions of how
ocean circulation evolves over time,» according to the press release.
Salinity of the surface waters can be influenced by the amount of river water flowing into the
oceans, yet no computer
models of ancient
ocean circulation had included this variable.
CMIP was established as a resource for climate modelers, providing a standard protocol for studying the output of coupled atmosphere -
ocean general
circulation models so that these
models can be compared and validated.
Some of the variables controlling the
models are not all that well known,» he adds, including forces such as winds,
ocean circulation, and how icebergs calve.
They used a
model of
ocean circulation to estimate where the young turtles would be carried from natal beaches in the Atlantic, Mediterranean and Indian
oceans.
They then analyzed
ocean - atmosphere carbon exchange and
ocean carbon cycling within their
circulation model.
Climate
models show the absence of a global atmospheric
circulation pattern which bolsters high
ocean temperatures key to coral bleaching
The researchers plugged that trash census data into
ocean models, which simulate the
circulation of the world's waters.
They were Jorge Sarmiento, an oceanographer at Princeton University who constructs
ocean -
circulation models that calculate how much atmospheric carbon dioxide eventually goes into the world's
oceans; Eileen Claussen, executive director of the Pew Center for Global Climate Change in Washington, D.C.; and David Keith, a physicist with the University of Calgary in Alberta who designs technological solutions to the global warming problem.
Its number - crunching capabilities are used to study ship hydrodynamics and air turbulence, to probe industrial combustion turbines to create cleaner engines, and to understand global
ocean circulation, as well as for earthquake simulations and aircraft noise - reduction
modeling.
The researchers paired MIT's global
circulation model — which simulates physical phenomena such as
ocean currents, temperatures, and salinity — with an ecosystem
model that simulates the behavior of 96 species of phytoplankton.
New understanding of changes in North Pacific
ocean circulation over the past 1.2 million years could lead to better global climate
models
Using multiple climate
models from around the world, Clement's research team removed the
ocean circulation from the analysis to reveal that variations in the Atlantic climate were generally the same.
Our study compares climate
models that include
ocean circulation (top right) with climate
models that have no
ocean circulation (bottom right).
«This study confirmed that
ocean circulation physics and K. brevis biology are equally important and that both immediate and short term prediction may be achieved using a combination of
circulation models supported by in situ observations of physical, biological and chemical variables and satellite imagery,» concluded the researchers.
Your statement that «Thus it is natural to look at the real world and see whether there is evidence that it behaves in the same way (and it appears to, since
model hindcasts of past changes match observations very well)» seems to indicate that you think there will be no changes in
ocean circulation or land use trends, nor any subsequent changes in cloud responses thereto or other atmospheric
circulation.
I'd love to know what they did take into account in attempting to
model that period — must include astronomical location, sun's behavior, best estimates about a lot of different conditions — where the continents were, what the
ocean circulation was doing, whether there had been a recent geological period that laid down a lot of methane hydrates available to be tipped by Pliocene warming into bubbling out rapidly.
Researchers carry out innovative basic and applied research programs in coral reef biology, ecology, and geology; fish biology, ecology, and conservation; shark and billfish ecology; fisheries science; deep - sea organismal biology and ecology; invertebrate and vertebrate genomics, genetics, molecular ecology, and evolution; microbiology; biodiversity; observation and
modeling of large - scale
ocean circulation, coastal dynamics, and
ocean atmosphere coupling; benthic habitat mapping; biodiversity; histology; and calcification.
I would agree that unforeseen changes in
ocean circulation could throw off
model predictions, there are surely other wildcards too, but uncertainty like that is not your friend if you want to argue against avoiding climate change.
This corresponds in scope (not un-coincidentally) to the atmospheric component of General
Circulation Models (GCMs) coupled to (at least) a mixed - layer
ocean.
Our general
circulation model simulations, which take into account the recently observed widespread occurrence of vertically extended atmospheric brown clouds over the Indian
Ocean and Asia3, suggest that atmospheric brown clouds contribute as much as the recent increase in anthropogenic greenhouse gases to regional lower atmospheric warming trends.
It should also be noted that the authors examined whether the large - scale
ocean circulation, the Meridional Overturning Circulation (MOC), and two other ocean phenomena - the Pacific Decadal Oscillation (PDO) and Atlantic Meridional Oscillation (AMO)- could explain the warming in the 20th century simulations, but found no evidence in
circulation, the Meridional Overturning
Circulation (MOC), and two other ocean phenomena - the Pacific Decadal Oscillation (PDO) and Atlantic Meridional Oscillation (AMO)- could explain the warming in the 20th century simulations, but found no evidence in
Circulation (MOC), and two other
ocean phenomena - the Pacific Decadal Oscillation (PDO) and Atlantic Meridional Oscillation (AMO)- could explain the warming in the 20th century simulations, but found no evidence in the
models.
Suppose also that — DESPITE THIS STABILIZING MECHANISM some as - yet unknown
ocean circulation cycle operates that is the sole cause of the Holocene centennial scale fluctuations, and that this cycle has reversed and is operating today, yielding a temperature change that happens to mimic what
models give in response to radiative forcing changes.
Influence of physical forcing on planktonic ecosystems and elemental cycling; mesoscale
ocean dynamics; primary production; coastal
circulation; zooplankton population dynamics; harmful algal blooms; numerical
modeling and data assimilation.
(Top left) Global annual mean radiative influences (W m — 2) of LGM climate change agents, generally feedbacks in glacial - interglacial cycles, but also specified in most Atmosphere -
Ocean General
Circulation Model (AOGCM) simulations for the LGM.
Marine planktonic ecosystem dynamics, biogeochemical cycling and
ocean - atmosphere - land carbon system,
ocean acidification, climate change and
ocean circulation, satellite
ocean color, air - sea gas exchange, numerical
modeling, data analysis, and data assimilation
Broecker's articulation of likely effects of freshwater outbursts in the North Atlantic on
ocean circulation and global climate (Broecker, 1990; Broecker et al., 1990) spurred quantitative studies with idealized
ocean models (Stocker and Wright, 1991) and global atmosphere —
ocean models (Manabe and Stouffer, 1995; Rahmstorf 1995, 1996).
Computer
models reveal that exoplanets with very saline
oceans could have
circulation patterns opposite to that on Earth, resulting in dramatic warming of their polar regions, possibly extending their range of habitability.
A number of recent studies linking changes in the North Atlantic
ocean circulation to sea ice extent led Yeager to think that it would also be possible to make decadal predictions for Arctic winter sea ice cover using the NCAR - based Community Earth System
Model...
Coastal
circulation dynamics, numerical
modeling and data assimilation, biophysical interaction, air - sea interaction, coastal
ocean observing system
Observation and
modeling of large scale
ocean circulation, bio-geo-chemical tracer distributions.
i would much rather discuss and learn about cloud
models,
ocean circulation, ice sheet stability than repeatedly counter ignorant arguments by innumerate dunces.
Jin, X.Z., X.H. Zhang, and T.J. Zhou, 1999: Fundamental framework and experiments of the third generation of the IAP / LASG World
Ocean General
Circulation Model.
Six, K.D., and E. Maier - Reimer, 1996: Effects of plankton dynamics on seasonal carbon fluxes in an
ocean general
circulation model.
This year we received 14 June SIO submissions from dynamical
models, of which 3 were from ice -
ocean models forced by atmospheric reanalysis or other atmospheric
model output and 12 were from fully - coupled general
circulation models.
In an ensemble of fully coupled atmosphere -
ocean general
circulation model (AOGCM) simulations of the late Paleocene and early Eocene, we identify such a
circulation - driven enhanced intermediate - water warming.
Gent, P.R., J. Willebrand, T.J. McDougall, and J.C. McWilliams, 1995: Parameterizing eddy - induced tracer transports in
ocean circulation models.