Previous studies suggested impurities such as black carbon and dust drive melting of bare ice on
the lower part of the ice sheet.
Not exact matches
Any
parts of the bed this
low are easily exposed to ocean water, allowing the
ice sheet to weaken from below as the ocean water warms.
Based on the southern core we thought this was a localized
low heat - flux region — but our model shows that a much larger
part of the southern
ice sheet has
low heat flux.
Satellites detect a thinning
of parts of the Greenland
Ice Sheet at lower elevations, and glaciers are disgorging ice into the ocean more rapidly, adding 0.23 to 0.57 mm / yr to the sea within the last deca
Ice Sheet at
lower elevations, and glaciers are disgorging
ice into the ocean more rapidly, adding 0.23 to 0.57 mm / yr to the sea within the last deca
ice into the ocean more rapidly, adding 0.23 to 0.57 mm / yr to the sea within the last decade.
A massive
ice sheet almost completely covers Greenland, and as summertime temperatures climb and sunlight hours lengthen,
parts of the
ice sheet surface usually melt, especially at
lower elevations near the coast.
A CO2 pulse in the atmosphere will take centuries to finally return to original levels, and that is completely ignoring any potential feedbacks from other
parts of the system (ie temperatures raised for centuries could result in massve methane releases and loss
of signficant
low albedo
ice sheets etc.) The experiments I am aware
of that show improved plant growth in elevated CO2 levels require that all additional biological needs are amply provided for.