It is more than just age. Surface melting will decrease albedo dramatically as well.
Actually, it has. With all the melting of ice, the albedo has been decreasing dramatically even though all the ice hasn't melted yet.
Do you really think humans were not putting out soot before the industrial revolution? I hate to break it to ya but man has been producing soot for thousands of years. Hell... we have been putting out soot ever since man learned to control fire.
Nope. Wrong again.
Here is that article again. I think this is like the 6th time I have shown it to you. Here are a couple of quotes:
and:
Looks to me like you don't know what you are talking about. As usual.
It is a hell of a lot more than you have. At least I can cite numerous examples of me proving you wrong. And I could cite plenty more if I wanted to. But you have yet to cite even one single example of you proving me wrong.
Not even once!!
But you go ahead and keep deluding yourself. That seems to be all you are really good at anyway.
Your article support the soot on ice.
The soot amounts inferred by CN85 were mostly in the
range 5–50 nanograms of carbon per gram of snow (ng g−1,
or ppb by mass), which could reduce the broadband (0.3–
2.8 μm) albedo of snow by as much as 0.04, depending on
snow grain size (Warren and Wiscombe, 1985). CN85 suggested
a mean value of 25 ng g−1 for the Arctic, and a corresponding
albedo reduction of 0.02 (CN85; Warren and
Clarke, 1986). An albedo reduction of this magnitude is
not detectable by eye and is below the accuracy of satellite
observations, but it is significant for climate (Hansen and
Nazarenko, 2004; Jacobson et al., 2004; Hansen et al., 2005;
Flanner et al., 2007).
---
There are several possible reasons: (1) the
peak of soot fallout in the Arctic occurs in spring, coinciding
with the onset of snowmelt; (2) melting (coarse-grained)
snow has lower albedo than cold (fine-grained) snow; (3) earlier
melt exposes a dark underlying surface; and (4) the stable
atmospheric boundary layer over snow prevents rapid heat
exchange with the free troposphere, concentrating the warming
at the surface. For a specified radiative forcing, sootin-
snow had 1.8 times the climatic warming effect of anthropogenic
CO2, giving soot-in-snow an “efficacy” of 1.8
(Hansen et al., 2005). Subsequent climate modeling by Flanner
et al. (2007), incorporating snow processes into a GCM,
found an even higher efficacy of 3.2, because of several additional
considerations: (5) an initial albedo reduction causes
a temperature increase and therefore growth of snow grain
size, even before the onset of melting (LaChapelle, 1969;
Flanner and Zender, 2006) and further reducing albedo;
(6) soot causes greater albedo reduction in coarse-grained
snow than in fine-grained snow (Fig. 7 of Warren and Wiscombe,
1980); and (7) it has been hypothesized that melting
may tend to concentrate soot at the top surface (e.g. in the
modeling study of Flanner al., 2007), where it is exposed to
more sunlight. The radiative effects of BC in snow are now
the subject of several additional modeling efforts (Jacobson,
2004; Koch and Hansen, 2005; Koch et al., 2009) and summary
assessments (Quinn et al., 2008).
OK, the first passage says the average 25 nanogram/gram corresponds to an albedo decrease of 2%. The second passage gives possible reasons, which are now have greater evidence of being true. It suggests that soot increases this snow melt which farther decreases abedo even more. It also says the effect is greater than antropogenic CO2.