In the first category, physically plausible mechanisms have been proposed that link human
activities associated with the creation of the ozone hole1 and increased runoff from the Antarctic
ice sheets2 (
land ice) to increased sea
ice.
Using the figurines and builds included in the kit, photographer Markus
Land constructed a series of photos showcasing the characters as they engage in
activities like
ice hockey or just surveying the icy planet.
Other factors would include: — albedo shifts (both from
ice > water, and from increased biological
activity, and from edge melt revealing more
land, and from more old dust coming to the surface...); — direct effect of CO2 on
ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on
ice; — «stuck» weather systems bringing more and more warm tropical air ever further toward the poles; — melting of sea
ice shelf increasing mobility of glaciers; — sea water getting under parts of the
ice sheets where the base is below sea level; — melt water lubricating the
ice sheet base; — changes in ocean currents -LRB-?)
I also believe that soot and all the other aerosols that combine and rain out has contributed to significant albedo changes and is food for localized warming from biochemical
activity in the boreal north that has significantly contributed to the melting of
land and sea
ice.