Not exact matches
These
significant depths suggest that Ceres» subsurface is no more than 40 percent
ice by
volume, and the rest may be a mixture
of rock and low - density materials such as salts or chemical compounds called clathrates.
To establish this uncertainty in the
ice -
volume record (Schweiger et al. 2011), we spent a
significant effort drawing on most types
of available observations
of ice thickness thanks to a convenient compilation
of ice thickness data (Lindsay, 2010).
It seems that the near - zero replenishment
of the MY
ice cover after the summers
of 2005 and 2007, an imbalance in the cycle
of replenishment and
ice export, has played a
significant role in the loss
of Arctic sea
ice volume over the ICESat record.
Significant volumes of freshwater were released in the North Atlantic and Arctic at the beginning
of the Holocene by the decay
of the residual continental
ice (Nesje et al., 2004).
Still more striking, and
significant, has been a severe decline in the average thickness
of the
ice pack, and thus
of its
volume (graph).
Using a large
volume of 126 proxy temperature records from the Northern Hemisphere, they found (1) a clearly discernible Medieval Warm Period (MWP)(950-1150) and Little
Ice Age (LIA)(1450 - 1850), (2) «likely unprecedented» modern temperatures (relative to the last 1,000 years), as well as a (3) «
significant» link between the high temperatures
of the MWP and recent times and the high solar activity that characterized both periods (the Medieval Maximum and the Modern Grand Maximum).
Some parts
of the Antarctic
ice sheet are also losing
significant volume (very high confidence).
This research highlights the importance
of accounting for large amounts
of ground
ice that can make up a
significant portion
of total permafrost
volume in some areas.