Not exact matches
The thickness
of the
ice, and its overall
volume, may be a more
important measure
of what is happening in the Arctic over the long term, even though it is not as simple to measure, said Overland.
Abstract: Mid - to late - Holocene sea - level records from low - latitude regions serve as an
important baseline
of natural variability in sea level and global
ice volume prior to the Anthropocene.
While extent is a traditional measure
of sea
ice,
volume is also
important.
And it's also
important to remember that, while sea
ice is increasing in Antarctica, glaciers and
ice shelves are all melting rapidly, producing large
volumes of fresh water.
However, atmospheric CO2 content plays an
important internal feedback role.Orbital - scale variability in CO2 concentrations over the last several hundred thousand years covaries (Figure 5.3) with variability in proxy records including reconstructions
of global
ice volume (Lisiecki and Raymo, 2005), climatic conditions in central Asia (Prokopenko et al., 2006), tropical (Herbert et al., 2010) and Southern Ocean SST (Pahnke et al., 2003; Lang and Wolff, 2011), Antarctic temperature (Parrenin et al., 2013), deep - ocean temperature (Elder eld et al., 2010), biogeochemical conditions in the Northet al., 2008).
Volume gives us an idea on how much freshwater is stored in Arctic sea
ice — an
important element in the global - Arctic hydrological cycle, i.e., the cycle
of distillation due to freezing, and subsequent export, and melt.
Clearly, the sea
ice volume data plot is the single most
important topic
of discussion, yet in the article it is shown in Figure 1 with a poor vertical scale and amongst linear trend lines which mislead and make the curve appear to be linear and reach the zero point far out in the future.
The
ice loss amounts to a freshwater
volume which should have made an
important contribution to the observed decrease in salinity in the northern Atlantic — probably including the «great salinity anomaly»
of the 1970s, famous amongst oceanographers.
If you're not refuting the
volume analysis, then I can't see how you can say focusing on
ice volume is «a bit funky» — it's clearly a more
important measure
of the system's ability to recover, which is the central point
of this post.
While it's
important to know the
volume of an
ice sheet - or how much space it takes up - it can change without affecting the amount
of ice that is present.
In that case it is
important to have a more precise statement, so I went back to check the reference Journal
of Marine Systems
Volume 48, Issues 1 - 4, July 2004, Pages 133 - 157 Sea
ice from the Kara Sea region reaches Fram Strait from 2 to 4 years (min 2 years) on average, and while sea
ice from the Laptev Sea takes roughly 4 — 6 years (min 3 years) to reach Fram Strait»... from the East Siberian, Chukchi and Beaufort seas within 6 — 10 years.
The long - term trend is what matters, and the most
important of all metric in sea
ice is
volume.
There is, however, a subtle but
important qualification: if Artic
ice should melt, the sea level will not change because the
volume of water created by melting
ice is equal to the
volume of water that
ice displaces when floating.
Stroeve said that sea
ice volume, which incorporates measurements
of ice extent as well as thickness, is a more
important metric than sea
ice extent alone.
Trends in sea
ice thickness /
volume are another
important indicator
of Arctic climate change.