Finding a way to reverse climate change is the foremost challenge of our time and the first step is collecting ocean data in order to help us understand
how seawater chemistry is changing.
Years ago I read an article about
how seawater sprays are broken down into H2 and O2 by the interaction of salt and UV.
The detailed process will also give forensic scientists valuable insight into
how seawater affects deceased bodies, as they examine people of all ages and nationalities who died at the exact same moment under the same conditions.
Not exact matches
It's hard to articulate
how major a f — up this is, but Kyle Mizokami does a good job at Popular Mechanics: Indian authorities ordered the pipe replacement because they «likely felt that pipes exposed to corrosive
seawater couldn't be trusted again, particularly pipes that carry pressurized water coolant to and from the ship's 83 megawatt nuclear reactor.»
The team used samples of
seawater to determine
how nitrogen is removed from the oceans.
The researchers exposed baby corals from the Great Barrier Reef to acidified
seawater for varying lengths of time and investigated
how they responded at a molecular level.
Chemical clues in the mangroves and algae can also tell
how salty the water was, which shows whether or not El Niño was raising the local sea level and causing more
seawater to seep into the coastal wetlands.
The scientist describes
how thousands of years of soaking in
seawater have rendered the precious remains fragile.
By separating the different atomic masses («isotopes») of the element boron in the foraminifera shells, they tracked
how the pH of
seawater changed during the PETM.
«They hardly ever come onto land, and they don't swim in
seawater either,» he says, which helps explain
how a distinct species arose, in the case of the Suwannee alligator snapping turtle, in just one river.
Researchers put a number on
how much
seawater the world has, based on new data about the shape of the ocean floor.
Its goal is to find out where and
how fast
seawater is melting the glacial ice.
One question that has long and intensively been discussed in research is: Where and
how deep does
seawater penetrate into the seafloor to take up heat and minerals before it leaves the ocean floor at hydrothermal vents?
This guarantees further research into the topic, especially on the Mg - calcite solubility to further understand
how organisms cope with these
seawater conditions.
The scientists hope to gain more insight into this by exploring
how past changes in
seawater pH have impacted these organisms, but also through further field and laboratory studies testing the effect of ocean acidification on these calcifiers.
A new study led by The Australian National University (ANU) has found
seawater cycles throughout Earth's interior down to 2,900 km, much deeper than previously thought, reopening questions about
how the atmosphere and oceans formed.
«Once the ocean - atmosphere system was isolated, we could systematically probe
how changes in the
seawater due to biological activity affect the composition and climate properties of the sea spray aerosol,» said Prather, a professor in the Department of Chemistry and Biochemistry who holds a joint appointment at Scripps Institution of Oceanography.
The study examined 27 years worth of satellite data for sea surface temperatures, previous coral bleaching events, and studied
how corals responded to different
seawater warming conditions.
How the researchers determined this was a neat trick, involving balancing the vent site's CO2 budget by measuring the amount of CO2 in
seawater in the vent fluid; analyzing the isotopic makeup of the CO2; and radiocarbon dating the CO2.
The researchers knew
how much oxygen should have diffused down into each section of sediment from the
seawater, so any «missing» oxygen meant microbes had consumed it.
Seawater sulfate is a problem for methane in two ways: Sulfate destroys methane directly, which limits
how much of the gas can escape the oceans and accumulate in the atmosphere.
Kinetic studies uncovered factors that control
how fast uranium in
seawater binds to the adsorbent.
«Understanding
how the adsorbents perform under natural
seawater conditions is critical to reliably assessing
how well the uranium adsorbent materials work,» Gill said.
To measure the amount of salt in
seawater, for instance, they might measure
how well the solution conducts electricity, since the higher the level of dissolved salt, the higher the electrical conductivity of the water.
Scientists are studying this mound to gain an understanding of the interaction of crustal rocks and
seawater, and to learn
how sulfide mounds on land were formed millions of years ago.
How much salt is in
seawater?
How do communities in the nutrient - poor, so - called oligotrophic open ocean react, if the
seawater gradually acidifies due to the uptake of human - induced carbon dioxide (CO2)?
About BIOACID: Since 2009, more than 250 BIOACID scientists from 20 German research institutes have investigated
how different marine organisms respond to ocean acidification and increasing carbon dioxide concentrations in
seawater,
how their performance is affected during their various life stages,
how these reactions impact marine food webs and elemental cycles and whether they can be mitigated by evolutionary adaptation.
Learn
how to make your own
Seawater Lobster, and
how that lobster can quickly become a sumptuous Lobster Corn Chowder.
There is of course a lot of uncertainty about the details, that affect the melt rates, we just don't know
how quickly warmer
seawater will undercut floating glaciers, and buildup of darker older snow / ice layers will increase the amount of absorbed sun light.
All of these, as well as CO2 sequestration as is (just taking CO2 and burying it in old oil reservoirs, aquifers, etc.), would be attempts to grasp the «big control knob» (see Hank Roberts» 670), and in such a way as to have the same or nearly the same (depending on
seawater chemistry and
how carbonate dissolution works in buffering pH relative to sequestering CO2 from the atmosphere) effect as reducing anthropogenic CO2 emissions.
How dare you hunt such creatures to near extinction when no one needs to eat this meet that tastes like old steak soaked in
seawater for a hundred years anyway?»
In a report published in Scientific Reports, researchers describe
how they exposed herring and pink salmon embryos for a short period to levels of oil contaminants similar to the «safe» levels detected in samples of Prince William Sound
seawater after the spill cleanup.
Iris Hendriks of the Mediterranean Institute for Advanced Studies recently analyzed data from a wide sample of research into
how individual organisms respond to increased carbon dioxide in their
seawater.
Rain washes it into the
seawater = depends
how often rains.
The
seawater contains phytoplankton, which is the foundation of the food chain in the ocean and the catalyst that begins the process of
how sea spray aerosol particles can change global climate.
However, in the past measuring
how productive coral reefs are has been time - consuming and expensive, requiring ongoing measurement as scientists need to trace the changes in the dissolved oxygen of
seawater as it moves over the reef.
For example,
how is absorption of radiation in the atmosphere or evaporation of
seawater a cooling process?
I know, carbonate levels in
seawater probably were much higher too, but is remains to be seen in
how far the theory describes reality...