Not exact matches
The Earth's axis fluctuates between having a tilt of 22 degrees and 24 degrees and when the tilt is 24 degrees, there is a larger difference between
summer and winter and this has an influence on the violent shifts in climate between
ice ages and interglacial
periods.
«Under the 4 - degree Celsius scenario, we would have a high probability of a three - month
ice free
period in the
summer months by 2050.
In some parts of the Arctic, sea
ice loss is causing polar bears to spend longer
periods on shore each
summer.
The
summer minimum Arctic sea
ice extent has decreased by 40 percent during the same time
period.
Though technically considered a temperate species, the whales are spending more time in Arctic waters each
summer because there is more plankton and a longer
period without sea
ice.
It confirmed that the mean albedo, or surface reflectivity, of the Arctic
ice zone in late
summer declined over an almost three - decade
period, between 1982 and 2009.
«Reduced sea
ice cover over a longer
period of time over the
summer could mean improved foraging for belugas,» said Hauser, who is also a researcher at the University of Alaska Fairbanks.
«The combined sea
ice data suggest that the seasonal Arctic sea
ice cover was strongly reduced during most of the early Holocene and there appear to have been
periods of
ice free
summers in the central Arctic Ocean.
The new paper uses alkenones from the Svalbard islands and is among the first studies that present Arctic
summer temperature change over the
period from the end of the last
Ice Age some 12000 years ago.
This warm air layer gets its heat reflected downwards during cloudy
periods, especially during long night extensive cloudy
periods, as a result, Arctic ocean
ice doesn't thicken so much during darkness and leaves it up to
summer sunlight (if there is some) to finish off what is left of it.
Researchers have attributed glacial decline to increasing temperatures, which have reduced the
period of glacial accumulation and extended the
period of
summer ice melting (ablation).
At the time of the image, the Martian south pole was experiencing a
summer period but during the winter the
ice mass would reach far into the surrounding smoother terrain.
Because of this,
ice deposits in the polar regions are likely to be diminished in the
summer period, while the build - up of
ice in Tombaugh Regio may have endured for millions of years.
Recent
summers on the vast, white expanse of the Greenland
ice sheet have featured some spectacular
ice melt, including an alarming
period in 2012 when nearly the whole surface showed signs of melt.
This warm air layer gets its heat reflected downwards during cloudy
periods, especially during long night extensive cloudy
periods, as a result, Arctic ocean
ice doesn't thicken so much during darkness and leaves it up to
summer sunlight (if there is some) to finish off what is left of it.
One thing I note in the 1900 - present graph is that the
summer ice levels start dropping in the 1950's during the cool
period of recent global warming.
Does it mean the first time the
summer sea
ice goes beneath this threshold or does it imply a probability of encountering low -
ice conditions over a
period of time?
Rising temperatures cause the sea
ice to melt earlier in the year, driving the bears to shore before they have built sufficient fat reserves to survive the
period of scarce food in the late
summer and early fall.
The work pointing to
periods of recovery on the way to a largely
ice - free
summer later in the century is still valid....
This afternoon, I asked Marika Holland, a climate and
ice modeler at the National Center for Atmospheric Research, to consider recent
ice trends in light of her work with Jennifer E. Kay and Alexandra Jahn on a paper finding likely
periods of
ice recovery on the way to an
ice - free Arctic in
summer.
Loso, M.G. (2008)
Summer Temperatures during the Medieval Warm
Period and Little
Ice Age Inferred from Varved Proglacial Lake Sediments in Southern Alaska, Journal of Paleolimnology 41, 117 - 128, DOI: 10.1007 / s10933 -008-9264-9.
The sea
ice at the end of this
summer's
period of melting is predicted to match or beat the all - time record low of 2007 and one research group at the University of Bremen in Germany has already announced that the
ice this year has already set a record.
Scientists at the National Snow and
Ice Data Center, in Boulder, Colorado measured the sea ice at the end of the 2012 summer period of melting and the measurements do not bode well for the extraordinary wildlife, ecology and cultures of the regi
Ice Data Center, in Boulder, Colorado measured the sea
ice at the end of the 2012 summer period of melting and the measurements do not bode well for the extraordinary wildlife, ecology and cultures of the regi
ice at the end of the 2012
summer period of melting and the measurements do not bode well for the extraordinary wildlife, ecology and cultures of the region.
Glacial
periods give way to interglacials on some occasions when the Northern Hemisphere's
summer solar insolation (the amount of solar radiation received by Earth's surface) increases alongside corresponding decreases in
ice volume and increases in temperature and atmospheric carbon dioxide (CO2).
1400 — 1549 the pre-culmination
period of the Little
Ice Age 1550 — 1849, the culmination
period which contains the «years without a
summer» 1850 — 1967, the post-culmination
period in which a definite retreat of glaciers and substantial atmospheric warming occurred.
For many decades after that it will be a matter of «making hay when the sunshines» in the Arctic
summers and the
ice free
period of those
summers will grow longer and longer..
The trend in concentrated sea
ice extent in the Arctic
summer is not uniform across the study
period but mostly a phenomenon of the latter half from 1998 - 2014.
The antarctic
summer ice minimum extend dropped about 50 % during this
period, suggesting warm ocean waters.
These preliminary results showed that, if current melt rates continue, the Arctic could see
ice free
periods during
summer starting in less than 10 years.
The arctic
summer ice minimum extent also dropped, about 20 to 25 %, during this
period when air temperatures were falling.
There were
periods when more
ice melted during
summer, and
periods when less melted.
A survey of trends in dispersed and concentrated sea
ice extent in the Arctic in the northern
summer and northern winter and in the Antarctic in the southern
summer and southern winter for the
period 1979 - 2015 shows a negative trend in dispersed and concentrated sea
ice extent in the Arctic in the northern
summer amid rising surface temperature in the northern hemisphere.
Annual net balance on eight North Cascades glaciers during the 1984 - 1994
period has been determined by measurement, of total mass loss from firn and
ice melt and, of residual snow depth at the end of the
summer season.
«The combined sea
ice data suggest that the seasonal Arctic sea
ice cover was strongly reduced during most of the early Holocene and there appear to have been
periods of
ice free
summers in the central Arctic Ocean.»
«A paper recently published in the journal Weather finds that global
summer average sunshine [solar short - wave radiation that reaches Earth's surface] dimmed during the
period 1958 - 1983 [prompting an
ice age scare], but markedly increased from 1985 - 2010.»
With the current increasing rate of climate changes, the North Pole may become
ice free for extended
periods every
summer.
Atmospheric - circulation patterns in June — July were generally favorable for preservation of sea
ice, at least compared to the same
period in
summer 2007.
Climate models suggest
periods of stability (with variations around a stationary
summer mean extent) with intermittent years of rapid reductions in
ice extent as the Arctic warms (see Serreze, Mark C. 2011.
The ends of
Ice Ages appear to correspond to
periods of the 25k year precession cycle when the sun is closer in the northern
summer, which tends to remove the glaciers over time.
Some previous models project an
ice - free
summer period in the Arctic Ocean by 2040 (Holland et al., 2006), and even as early as the late 2030s using a criterion of 80 % sea
ice area loss (e.g., Zhang, 2010).
Chukchi Sea and Southern Davis Strait bears, for example, are doing very well — contrary to all predictions — despite marked declines in
summer sea
ice because they have ample food during their critical spring feeding
period when sea
ice is abundant.»
«There were indeed some warm
period in those decades, but the sea
ice came no where close to the
summer lows we're seeing now.»
The Maunder Minimum occurred during the depths of the Little
Ice Age, a
period of feeble
summers and bitingly cold winters, war, pestilence and famine.
Specifically, the estimate is calculated by multiplying the average (for the
period 1985 - 2007) amount of
ice that does not survive the
summer (between the March maximum and the September minimum) by this year's March extent.
Such events would likely be driven by extended
periods of rainfall over the
ice during
summer heating events.
Today, a huge rift has nearly bisected a large frontal section of the Larsen C
Ice shelf — an ice system many times the size of its now deceased companions Larsen A and Larsen B. And during December — a period when Antarctica was warming into Austral Summer — this massive crack grew by 18 kilomete
Ice shelf — an
ice system many times the size of its now deceased companions Larsen A and Larsen B. And during December — a period when Antarctica was warming into Austral Summer — this massive crack grew by 18 kilomete
ice system many times the size of its now deceased companions Larsen A and Larsen B. And during December — a
period when Antarctica was warming into Austral
Summer — this massive crack grew by 18 kilometers.
As sea
ice declines, it becomes thinner, with less
ice build - up over multiple years, and therefore more vulnerable to further melting.15 Models that best match historical trends project northern waters that are virtually
ice - free by late
summer by the 2030s.25, 26,12 Within the general downward trend in sea
ice, there will be time
periods with both rapid
ice loss and temporary recovery, 27 making it challenging to predict short - term changes in
ice conditions.
The
summer of 2012 witnessed
periods of extremely rapid sea
ice melt.
Conclusions Early
ice breakup in
summer and / or late freeze - up in fall can not exclusively be blamed when polar bears struggle to get through the
ice - free
period.
Zhakarov's model is conceptually simple: during
periods of high precipitation when winter
ice forms readily,
summer ice cover increases, the atmosphere cools, the arctic front together with its associated rain belt shifts south so that freshwater input to the Arctic Ocean decreases, and winter
ice cover is thicker, has a deeper draft, and so survives better in
summer.