Not exact matches
The degradation of the historically
stable Filchner - Ronne
Ice Shelf would upset ice on land, triggering runaway melting over a vast region of the continent and accelerating global sea level ri
Ice Shelf would upset
ice on land, triggering runaway melting over a vast region of the continent and accelerating global sea level ri
ice on land, triggering runaway melting over a vast region of the continent and accelerating
global sea level rise.
The supposed
stable configuration of geography, with relatively predictable climate patterns, coastlines and icepacks in familiar locations, and clear demarcations of territorial control on land are increasingly dubious assumptions as weather patterns change,
sea levels rise and
ice packs disintegrate while technological innovations, communications and
global markets cause rapid fluctuations in the price in food and other essentials across boundaries.
The climate change had already affected the
seas around Antarctica and is warming some coastal waters.So now both Antarctic Peninsula and West Antarctica
Ice sheet are losing ice.For now, the East Antarctic Ice sheet is stable but it will influence on global climate change due to sea ice.In the future there is growing concern about the possible impact of climate change.Is Antarctica gaining ice that meant it will effect to climate change and the ecosystem of the regio
Ice sheet are losing
ice.For now, the East Antarctic Ice sheet is stable but it will influence on global climate change due to sea ice.In the future there is growing concern about the possible impact of climate change.Is Antarctica gaining ice that meant it will effect to climate change and the ecosystem of the regio
ice.For now, the East Antarctic
Ice sheet is stable but it will influence on global climate change due to sea ice.In the future there is growing concern about the possible impact of climate change.Is Antarctica gaining ice that meant it will effect to climate change and the ecosystem of the regio
Ice sheet is
stable but it will influence on
global climate change due to
sea ice.In the future there is growing concern about the possible impact of climate change.Is Antarctica gaining ice that meant it will effect to climate change and the ecosystem of the regio
ice.In the future there is growing concern about the possible impact of climate change.Is Antarctica gaining
ice that meant it will effect to climate change and the ecosystem of the regio
ice that meant it will effect to climate change and the ecosystem of the regions?
Normally you can run GCM for centuries with a
stable realistic surface temperature, but take the CO2 out, and in 5 - 10 years it has dropped 30 C in
global average temperature and is half - covered in
sea ice due to a powerful water vapor feedback in response to any
global temperature change.
But the real news here is that a human - forced warming of the globe has set a monstrous pile of
ice, once thought
stable, into a motion that will result in yet more
global sea level rise.
From 2006 to 2016,
global sea ice trends have also been remarkably
stable despite a massive increase in anthropogenic CO2 emissions during this period.
•
Global polar bear numbers have been
stable or risen slightly since 2005, despite the fact that summer
sea ice since 2007 hit levels not expected until mid-century: the predicted 67 % decline in polar bear numbers did not occur.
That settling down into a more
stable and truely predictable state will only ocme about by the overwhelming obviousness of the first hand experiences and events as they unfold and are once more creating louder headlines in the media than the so called scandals are now... i.e. new record lows in
sea ice, record highs in
global temps, and other extremes predicted by AGW models.
IMO, the strongest argument for
sea ice decline over the last decade for being unusual and at least in part attributable to
global warming is this (from Polyakov et al.): The severity of present
ice loss can be highlighted by the breakup of
ice shelves at the northern coast of Ellesmere Island, which have been
stable until recently for at least several thousand years based on geological data.