Not exact matches
By mapping current
conditions with the help of Inuit hunters as well as by compiling maps of the
past based on oral histories and the memories of elders, the researchers hope to capture the Inuit's special understanding of
sea ice.
«Southern Ocean: Reconstructing environmental
conditions over the
past 30,000 years:
Sea -
ice zone has a major influence on the ecosystem.»
Our study underlines that these
conditions have led to a large loss of
ice and significant rises in global
sea level in the
past.
The advantage of such partially - coupled models is that they can be driven by
past atmospheric
conditions and the simulations match well the observed
sea ice variability, which is strongly forced by the atmosphere.
The main source of my Arctic comfort level — besides what I learned while camped with scientists on the North Pole
sea ice — is the growing body of work on
past variations * in
sea ice conditions in the Arctic.
Arbetter et al. (National
Ice Center); 4.4; Statistical The system determines the relationships between sea ice and atmospheric conditions over the past ten years to determine the likelihood of ice being present this ye
Ice Center); 4.4; Statistical The system determines the relationships between
sea ice and atmospheric conditions over the past ten years to determine the likelihood of ice being present this ye
ice and atmospheric
conditions over the
past ten years to determine the likelihood of
ice being present this ye
ice being present this year.
This is substantially lower than the earlier estimates, reflecting both lower than average
sea ice extent used as initial
conditions this summer and a persistent downward trend in
sea ice extent over the
past decade (and longer).
Similar
sea ice trends and weather
conditions were present during the spring seasons preceding
past ice shelf retreats (e.g., 2001 to 2002).
If climate models are able to reproduce
past warm climatic
conditions (such as those of the LIG), including the extent of Arctic
sea ice cover, we will have additional confidence in their representation of Arctic processes and their projections for the future20, 21,22,23.
By combination of this
sea ice proxy IP25 with (biomarker) proxies for open - water phytoplankton productivity such as brassicasterol, dinosterol or a specific tri-unsaturated HBI (HBI - III) 37,38,39,40,41, a more precise (semi-quantitative) reconstruction of present and
past Arctic Ocean
sea ice conditions from marine sediments are now available (Supplementary Fig. 1; see Metho 6ds for some more details).
Proxy data such as those generated from
ice core samples, measurements of tree rings intervals, bore samples taken from sediments from the ocean and
sea floor, and measurement of gases from bubbles trapped in
ice are some examples of preserved physical characteristics of the
past used by scientists to reconstruct prevailing climatic
conditions in the
past.
Now we have poor hunting
conditions in the Bering Strait touted as evidence that «walrus migration patterns have changed» with the implication that this is because ``... the
past eight years have had the eight lowest amounts of summer
sea ice on record» due to man - made global warming.
Research from the
past 10 years has shown that climate change leads to longer seasons without
sea ice, Stirling's team wrote, «resulting in polar bears coming ashore to fast [go without food] for several months in progressively poorer
condition.»