Gavin, it might be worth a mention in the FAQ of how climate models overlap
with ocean chemistry models.
«There were big things going on
with ocean chemistry,» he said.
Not exact matches
Foraminifera, small single - celled marine organisms, form their shells in concert
with the
ocean's temperature and
chemistry.
Forams form their shells in concert
with ocean temperatures and
chemistry, acting as miniscule time capsules, each containing a precise record of the temperature and
ocean chemistry during its lifetime.
Researchers endowed the observatory's six nodes
with instruments that measure the
ocean's changing temperature and
chemistry, cameras that spy underwater creatures, hydrophones that listen to passing whales and seismometers and tsunami detectors that measure hazards as they happen.
Because such
chemistry provides energy for microbial life on Earth, the discovery makes Enceladus the top candidate for hosting life elsewhere in the solar system — besting even Jupiter's Europa, another icy moon
with an
ocean.
Scientists conducting fieldwork in the region are reporting massive chick die - offs and nests
with abandoned eggs, reports National Geographic's Winged Warnings series, which lays out the many threats facing the island's seabirds: warming
oceans, earlier thaws, changing
ocean chemistry and food webs, and increasing levels of
ocean pollutants from PCBs to mercury.
Calcium carbonate has great scientific relevance in biomineralization and geosciences, forming enormous scales of biological (reefs and
ocean sediments) and geological origin, which bind a huge amount of CO2 and affect the
chemistry of
ocean water (1) and,
with it, Earth's atmosphere and climate.
Titan's surface seems to be covered
with ethane
oceans and an organic goo that may resemble the Earth's early surface
chemistry, but nobody knows for sure, because astronomers can't see through the moon's maddeningly opaque orange fog.
The
chemistry in the growth rings in the shells of the clam — which occur much like the annual growth rings in the centre of trees — can act as a proxy for the chemical make - up of the
oceans, enabling researchers to reconstruct a history of how the
oceans have changed over the past 1000 years
with unprecedented dating precision.
Satkoski, who is first author of a new report on
ocean chemistry from this remote period, says the conventional wisdom of geology has envisioned an oceanic planet,
with little or no land above the waves.
When I discovered that the university offered courses in marine
chemistry, I decided to try to combine a love for the
ocean with an interesting
chemistry career.
Previous CO2 rises on Earth happened so slowly that the accompanying
ocean acidification was relatively minor, and ammonites and other planktonic calcifiers were able to cope
with the changing
ocean chemistry.
While biology and
chemistry control the growth of the blooms, it is
ocean circulation that unites the nutrients
with sunlight to facilitate photosynthesis, said Weisberg.
«The other carbon dioxide problem», «the evil twin of global warming», or part of a «deadly trio», together
with increasing temperatures and loss of oxygen: Many names have been coined to describe the problem of
ocean acidification — a change in the
ocean chemistry that occurs when carbon dioxide (CO2) from the atmosphere dissolves in seawater.
development of a regional scale earth system model that includes coupling WRF
with other earth system components such as
ocean, sea ice, land surface hydrology, ecosystem, and
chemistry; and
As the science develops, it is important for managers to design select examples of coral reef areas in a variety of
ocean chemistry and oceanographic regimes (e.g., high and low pH and aragonite saturation state; areas
with high and low variability of these parameters) for inclusion in MPAs.
You probably won't notice changes to the water's
chemistry with a trip to the beach and a dip in the
ocean — even wearing your snorkel mask.
Never mind that this would be easily traceable by
ocean carbon
chemistry,
with low pH water plumes streaming from the ridge crests.
Prior films like «Ex Machina» and «The Light Between
Oceans» showed what
chemistry she could have
with her co-stars.
This setup consists of an atmospheric model
with a simple mixed - layer
ocean model, but that doesn't include
chemistry, aerosol vegetation or dynamic ice sheet modules.
The
ocean takes up some,
with no biology involved, just
chemistry, and forests apparently take up the rest.
The review, which is being published in the journal Science on Friday, concludes that the human - driven buildup of carbon dioxide under way now appears to be far outpacing past natural events, meaning that, for
ocean chemistry particularly, the biological implications are potentially enormous — and laden
with the kind of uncertainty that is hard to see as a source of comfort.
While it is a very important point for the lay person to know that the acidification of the
ocean by CO2 (it combines
with water to produce dilute Carbonic Acid) can reduce the effectiveness of the Calcium Carbonate processes at sequestering Carbon (and can even reverse it, by dissolving Calcium Carbonate), your model
chemistry seems quite simplistic.
The
ocean model I used does carbon
chemistry,
with plankton and gas exchange and all that.
The workshop summarized the state of understanding, key uncertainties and next research steps on the shifting
chemistry of the
oceans and the impacts on species and ecosystems,
with a focus on ecosystems of particular interest to humans.
The most indirect impact of all is coming through the global buildup of carbon dioxide and other greenhouse gases, which are altering the climate and
ocean chemistry with long - lasting repercussions.
I know nothing about this issue, but I just came across a reference to Jacobson, Mark Z., «Studying
ocean acidification
with conservative, stable numerical schemes for nonequilibrium air -
ocean exchange and
ocean equilibrium
chemistry.»
Physical
chemistry is a combination of
chemistry and physics, it is fine that you derived the equation, but it relates to thermodynamics just the same; chemists make those lasers work, those DVD's play, and I have taken calculus physics, modern physics, (multi variable calculus physics) which means technically I too have a degree in physics, but my focus has been
chemistry, biology, and I took a few graduate courses dealing
with meteorology,
ocean dynamics, geology, atmospheric science and my undergraduate courses were filled
with earth science related material and after all the math needed for Pchem engineering mathematics is not difficult nor is graduate physics:) so the derivation you just made is discussed in math classes before, even calculus one, so I am not sure what you are trying to prove.
There have been many explanations put borth inlcluding deep
ocean heating, ozone
chemistry, volcanoes reducing incident energy, trade winds and, of course, Cowtan and Way along
with this latest data set that shows the energy imbalance is still tracking CO2.
We have enough problems
with over fishing, mercury contamination, nitrates, and plastics without climate change altering
ocean chemistry as well.
Even
with almost no chance of the high end of climate sensitivity estimates being right, the odds of substantial, prolonged and disruptive climate change (and changes in
ocean chemistry) are still plenty high enough to justify a sustained push toward an energy menu that works for the long haul.
Further increased efforts will be needed in linking terrestrial ecosystems
with the atmosphere, the land
with the
ocean, the
ocean (and its ecosystems)
with the atmosphere, the
chemistry of the atmosphere
with the physics of the atmosphere, and finally linking the human system to them all.
It turns out that like all tightly coupled systems, the
ocean and the atmosphere like to be in equilibrium
with each other, which means that the
chemistry of the
ocean is affected by the
chemistry of the atmosphere.
Combining that
with theoretical knowledge on
ocean chemistry and on known sources of carbon from burning fossil fuels and other human activities is enough to give a clear picture on main trends.
Freshman
chemistry, the partial pressure of CO2 in the
ocean, 50,000 Gtons dissolved, 100,000 Gtons precipitate, varies
with temperature.
«We knew there were changes in carbonate
chemistry of the surface
ocean associated
with the large - scale glacial - interglacial cycles in CO2 [levels], and that these past changes were of similar magnitude to the anthropogenic changes we are seeing now,» says study co-author William Howard, a marine geologist at ACE.
One part of that argument is based on the depth of mixed layer in the
oceans in combination
with the known
chemistry of CO2 and carbonates.
The physical components of the earth, from its atmosphere to its
oceans, closely integrate
with all of its living organisms to maintain climatic
chemistry in a self - regulating balance ideal for the maintenance and propagation of life.
The details of the
ocean and atmospheric links are fascinating — it is postulated that it starts
with solar uv / ozone
chemistry modulating
ocean and atmospheric circulation throughout the system.
For instance,
oceans absorb heat from the atmosphere and mix
with freshwater run - off from melting glaciers and ice caps, which changes
ocean chemistry and puts stress on
ocean ecosystems.
Keeping in mind, the model is greatly simplified at only 3 bodies from our own actual system of interacting
ocean oscillations and
ocean life and
ocean chemistry, terrestrial conditions and terrestrial life, solar variability, orbital variability, land use, anthropogenic aerosols, and GHGs, any of which might suffer the eventual fate of a body in the 3 Body problem: ejection or collision more rapidly
with larger perturbation, and all of which are more certain to follow irregular and extreme paths.
But as for
ocean chemistry and heat, the
oceans are really big and really deep
with enormous thermal and buffering capacity.
Because the
chemistry of the
ocean equilibrates
with that of the atmosphere (on time scales of decades to centuries), methane oxidized to CO2 in the water column will eventually increase the atmospheric CO2 burden (Archer and Buffett, 2005).
The HadGEM3 family includes a coupled atmosphere -
ocean configuration,
with or without a vertical extension in the atmosphere to include a well - resolved stratosphere, and an Earth - System configuration which includes dynamic vegetation,
ocean biology and atmospheric
chemistry.
Warming of sea surface temperatures and alteration of
ocean chemistry associated
with anthropogenic increases in atmospheric carbon dioxide will have profound consequences for a broad range of species, but the potential for seasonal variation to modify species and ecosystem responses to these stressors has received little attention.
Topics that I work on or plan to work in the future include studies of: + missing aerosol species and sources, such as the primary oceanic aerosols and their importance on the remote marine atmosphere, the in - cloud and aerosol water aqueous formation of organic aerosols that can lead to brown carbon formation, the primary terrestrial biological particles, and the organic nitrogen + missing aerosol parameterizations, such as the effect of aerosol mixing on cloud condensation nuclei and aerosol absorption, the semi-volatility of primary organic aerosols, the importance of in - canopy processes on natural terrestrial aerosol and aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of aerosol burden and its spatiotemporal distribution, especially
with regard to its role and importance on gas - phase
chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect on key gas - phase species like ozone + the physical and optical properties of aerosols, which affect aerosol transport, lifetime, and light scattering and absorption,
with the latter being very sensitive to the vertical distribution of absorbing aerosols + aerosol - cloud interactions, which include cloud activation, the aerosol indirect effect and the impact of clouds on aerosol removal + changes on climate and feedbacks related
with all these topics In order to understand the climate system as a whole, improve the aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic aerosol changes in the atmosphere on the terrestrial biosphere, the
ocean and climate.
What had not been studied before was how climate change, in concert
with higher concentrations of carbon dioxide, would affect
ocean chemistry and biology.