The authors found that this small but diverse suite of evidence accurately reproduced
modern ocean chemistry and circulation patterns.
Not exact matches
By looking at the
chemistry of rocks deposited during that time period, specifically coupled carbon and sulfur isotope data, a research team led by University of California, Riverside biogeochemists reports that oxygen - free and hydrogen sulfide - rich waters extended across roughly five percent of the global
ocean during this major climatic perturbation — far more than the
modern ocean's 0.1 percent but much less than previous estimates for this event.
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.
-- Susan Solomon, Nature The Long Thaw is written for anyone who wishes to know what cutting - edge science tells us about the
modern issue of global warming and its effects on the pathways of atmospheric
chemistry, as well as global and regional temperatures, rainfall, sea level, Arctic sea - ice coverage, melting of the continental ice sheets, cyclonic storm frequency and intensity and
ocean acidification.