I used to BE Liability. Now I am but Ilar.
You are easily confused and massively misled.
I have not confused pollutants with toxins at all.
A lot of water vapor can impact the weather, too. It's still not a pollutant, you twit.
But then, water vapor has a very short residency in the atmosphere. Moreover, the concentration of water vapor in the atmosphere is also dependent on the concentrations of both aerosols and GHGs that reside in the atmosphere, both of which have a human component, components we can control.
Actually, there is a limit to which our global biosphere can sustain high levels of oxygen before serious damage occurs. Excess oxygen not only is damaging to the forests, it is also damaging to the oceans, and to vital anaerobic processes that break down organic compounds. Yes, dude, too much of a good thing is also a pollutant.
Ilar said:
And, of course, your false premise notwithstanding, a small and essentially insignificant additional release of CO2 into our atmosphere is not a pollutant, either, yo twit.
Demonstrating how little you understand about Earth processes. Congratulations.
Don't care what the atmos residency of water vapor is. Man's LAND USE and industries provide a NEW and INCREASING burden of water vapor into the atmos..
Right. That's why the Australian continent is 90% dry as a bone. That's why there is a long-term drought with no end in sight in the Western U.S. That is why the Gobi desert is growing by leaps and bounds. Because we are putting an "increasing water burden on the atmosphere". Perhaps you should restate your bullshite argument.
flacaltenn said:
Build a road or a parking lot and you've POLLUTED.. Because you've increased the atmos H20 vapor content. Insist on farming irrigation? You've polluted because you've provided a NEW steady supply of GHGas...
Roads increase run off. They do not increase the water vapor in the atmosphere.
You don't even KNOW what the atmos residency of CO2 really is..[/QUOTE]
CO2 has a short residence time
In the
IPCC 4th Assessment Report glossary, "lifetime" has several related meanings. The most relevant one is:
“Turnover time (T) (also called global atmospheric lifetime) is the ratio of the mass M of a reservoir (e.g., a gaseous compound in the atmosphere) and the total rate of removal S from the reservoir: T = M / S. For each removal process, separate turnover times can be defined. In soil carbon biology, this is referred to as Mean Residence Time.”
In other words, life time is the average time an individual particle spends in a given box. It is calculated as the size of box (reservoir) divided by the overall rate of flow into (or out of) a box. The
IPCC Third Assessment Report 4.1.4 gives more details.
In the carbon cycle diagram above, there are two sets of numbers. The black numbers are the size, in gigatonnes of carbon (GtC), of the box. The purple numbers are the fluxes (or rate of flow) to and from a box in gigatonnes of carbon per year (Gt/y).
A little quick counting shows that about 200 Gt C leaves and enters the atmosphere each year. As a first approximation then, given the reservoir size of 750 Gt, we can work out that the residence time of a given molecule of CO2 is 750 Gt C / 200 Gt C y-1 = about 3-4 years. (However, careful counting up of the sources (supply) and sinks (removal) shows that there is a net imbalance; carbon in the atmosphere is increasing by about 3.3 Gt per year).
It is true that an individual molecule of CO2 has a short residence time in the atmosphere. However, in most cases when a molecule of CO2 leaves the atmosphere it is simply swapping places with one in the ocean. Thus, the warming potential of CO2 has very little to do with the residence time of CO2.
What really governs the warming potential is how long the extra CO2 remains in the atmosphere. CO2 is essentially chemically inert in the atmosphere and is only removed by biological uptake and by
dissolving into the ocean. Biological uptake (with the exception of fossil fuel formation) is carbon neutral: Every tree that grows will eventually die and decompose, thereby releasing CO2. (Yes, there are maybe some gains to be made from reforestation but they are probably minor compared to fossil fuel releases).
Dissolution of CO2 into the oceans is fast but the problem is that the top of the ocean is “getting full” and the bottleneck is thus the transfer of carbon from surface waters to the deep ocean. This transfer largely occurs by the slow ocean basin circulation and turn over (*3). This turnover takes 500-1000ish years. Therefore a time scale for CO2 warming potential out as far as 500 years is entirely reasonable (See
IPCC 4th Assessment Report Section 2.10).