I can sum up most of my frustration with Volchaos with one line: it's a game entirely set in a volcano that plays like
an extended ice level.
Not exact matches
It had much higher sea
levels, forests
extended all the way to the Arctic Ocean, and there was almost certainly a lot less sea
ice.
Two
levels of terraces
extending upstream indicated a wall of
ice and mud had dammed the river, backing up a lake that filled the valley.
The potential for unstable
ice sheet disintegration is controversial, with opinion varying from likely stability of even the (marine) West Antarctic
ice sheet [94] to likely rapid non-linear response
extending up to multi-meter sea
level rise [97]--[98].
Includes every feature in the Preferred package plus features for more advanced pilots or longer flights including
extended forecasts; 6
levels of graphical turbulence and
Icing NOWcast.
So what we need is detailed topo maps of the bed and thickness of the GIS, and to work out a map of the «net buoyancy», or some such (i.e. total
ice area density subtracted from the area density of a hypothetical column of water resting on the bed and
extending up to sea
level).
«Neogene extension and basin deepening in the West Antarctic rift inferred from comparisons with the East African rift and other analogs WE LeMasurier — Geology, 2008 intl-geology.geoscienceworld.org Abstract The West Antarctic rift system differs from other volcanically active rift systems in two unusual respects: (1) the rift floor lies 1000 — 2000 m lower in elevation than others, and (2) four interior
ice - filled troughs
extend between 1500 m and 2555 m below sea
level.
If you mean sea
levels hundreds of feet above current
levels, or
ice caps that once
extended to the tropics, then sure.
Ice shelf - A floating slab of ice of considerable thickness extending from the coast (usually of great horizontal extent with a level or gently sloping surface), often filling embayments in the coastline of the ice shee
Ice shelf - A floating slab of
ice of considerable thickness extending from the coast (usually of great horizontal extent with a level or gently sloping surface), often filling embayments in the coastline of the ice shee
ice of considerable thickness
extending from the coast (usually of great horizontal extent with a
level or gently sloping surface), often filling embayments in the coastline of the
ice shee
ice sheets.
I recently gave a talk about the powerful relationships among various co - factors including seasonal sunlight, seasonal temperature change, sea
level, and even tectonic activity that
extends back to the bipolar Quaternary
ice - ages and interglacial warm periods of last 2.6 million years.
(See: NYT: Missing Its Spots: «Sun may be on verge of falling into an
extended slumber» — could cause «
extended chilly period» — «Cosmic ray
levels correlate well with climate
extending back thousands of years» — July 21, 2009 & Also see: «Sun Sleeps»: Danish Scientist declares «global warming has stopped and a cooling is beginning... enjoy global warming while it lasts» — Sun is «heading towards «a grand minimum» as we saw in Little
Ice Age» — Sept. 11, 2009)
This ocean will be incredibly important for sea
level rise, because the easiest way to destabilise the Antarctic
Ice Sheet is to warm up the ocean and melt the ice shelves (the edges of the ice sheet which extend over the ocean) from bel
Ice Sheet is to warm up the ocean and melt the
ice shelves (the edges of the ice sheet which extend over the ocean) from bel
ice shelves (the edges of the
ice sheet which extend over the ocean) from bel
ice sheet which
extend over the ocean) from below.
The potential for unstable
ice sheet disintegration is controversial, with opinion varying from likely stability of even the (marine) West Antarctic
ice sheet [94] to likely rapid non-linear response
extending up to multi-meter sea
level rise [97]--[98].
We're leaving Europe's shoreline now, though it would have
extended farther west back in the icy periods when the sea
level was a lot lower because
ice sheets locked up so much water.
The last time the polar regions were significantly warmer than present for an
extended period (about 125,000 years ago with Co2 at 287ppm), reductions in polar
ice volume led to 4 to 6 meters of sea
level rise.