Of course, other reasons could exist
for glacier retreat (e.g. Kilimanjaro's glacier retreat is apparently due not to increased temperatures but rather to decreased participation — and perhaps human clearing of trees has a role in that!)
He says: «However, as far as the mid-19th century is concerned, forcings due to GHG concentrations are insignificant so we are only left with natural forcings (or causes) as an explanation
for glacier retreat.»
However, as far as the mid-19th century is concerned, forcings due to GHG concentrations are insignificant so we are only left with natural forcings (or causes) as an explanation
for glacier retreat.
He says: «However, as far as the mid-19th century is concerned, forcings due to GHG concentrations are insignificant so we are only left with natural forcings (or causes) as an explanation
for glacier retreat.»
Not exact matches
«There's no question that as
glaciers retreat, more ground will become available
for exploration and more discoveries could be made in that part of the world,» said Fronk.
At Pine Island Glacier,
for instance — one of West Antarctica's largest
glaciers, and previously one of its fastest
retreating spots — the research suggests that the grounding line has recently stabilized.
But the need
for pigment to provide this extra protection waned as modern human populations migrated northward over the past 60,000 years or so, while the need to absorb UVB light became greater, particularly
for those humans who migrated to the far North behind
retreating glaciers less than 10,000 years ago.
But the need
for pigment to provide this extra protection waned as modern human populations migrated northward over the past 60,000 years or so, Elias said, while the need to absorb UVB light became greater, particularly
for those humans who migrated to the far North behind
retreating glaciers less than 10,000 years ago.
Recent research has fingered the ocean as a trigger
for tidewater
glacier retreats.
The cave system had been sealed
for hundreds of thousands of years, but an opening called the Aach spring made it accessible when Alpine
glaciers retreated northward around 16,000 to 20,000 years ago.
Geologists had predicted the plunge
for weeks, citing the
retreat of an underlying
glacier that had held the rock in place.
By 1900, increased emissions of soot could have triggered the loss of more than 15 m of ice from a
glacier's surface; by 1930, the loss could have totaled 30 m or more — magnitudes and timing that can easily account
for the Alpine glacial
retreat, the scientists contend.
«It means that these animals were here before the
glaciers covered central Iowa, and that they returned
for a short time after the
glaciers retreated as well,» Hill said.
And, worryingly, the research suggests that as these
glaciers melt and
retreat backward, the shape of the seabed will continue to expose many of them to warm ocean water
for hundreds of miles as the ice moves inland.
A downward slope,
for instance, might cause the
glacier to
retreat more quickly, while ridges or other topographical features might help to slow or halt the backward motion.
For comparison, one of the fastest moving
glaciers, the Jakobshavn ice stream in southwest Greenland, has
retreated 35 kilometers (21.7 miles) over the last 150 years.
For a pair of recent studies, UCI and NASA JPL scientists examined three neighboring
glaciers in West Antarctica that are melting and
retreating at different rates.
«These
glaciers will keep
retreating for decades and even centuries to come and we can't stop it,» said lead study author Eric Rignot, a glaciologist at the University of California, Irvine, and NASA's Jet Propulsion Laboratory in Pasadena, Calif. «A large sector of the West Antarctic Ice Sheet has passed the point of no return.»
From satellite observations such as radar interferometry, Rignot and his colleagues conclude a common cause underlies the
retreat of West Antarctica's largest
glaciers, including Pine Island Glacier, known
for cleaving massive icebergs, and its neighbor, Thwaites Glacier.
A new study has found
for the first time that ocean warming is the primary cause of
retreat of
glaciers on the western Antarctic Peninsula.
I seem also to remember a comment by Bindschadler stating that while GIS
glaciers could
retreat inland from warming oceans, there could be no similar escape
for Antatctica.
Analysis of the data reveals that 87 % of
glaciers have
retreated (click on the image
for a more detailed figure) and that the change from advance to
retreat has occurred progressively with latitude.
Although scientists have known
for decades that Qori Kalis and the other Quelccaya
glaciers are melting, new observations indicate that the rate of
retreat is increasing, Professor Thompson said.
«This widespread
retreat of mountain
glaciers may be our clearest evidence of global warming as they integrate many climate variables,» Professor Thompson told the American Association
for the Advancement of Science conference in San Francisco.
And given that at least some
retreating glaciers reveal earlier habitations beneath (in Scandinavia
for example), this is a highly legitimate question.
It has always seemed to me that the
retreat of mountain
glaciers around the world is one of the most compelling pieces of evidence
for global warming.
Those who legitimately question the case
for man - made global warming (AGW) do not question whether
glacier retreat is evidence of global warming.
Scientists recognized that climate change is rapidly altering the landscape in Antarctica, particularly when it comes to
glacier retreat and ice shelf collapse, so they made a pact
for how they would approach research as huge chunks of ice broke off.
The first one I looked at is an «own goal»
for the contrarians, as it involves Phil Jones bemoaning the discrepancy between
glacier retreat in high altitudes, and comparative lack of warming in the UAH troposphere record.
As a general matter, yes, but AIUI the increasing height (depth) of the ice face is the key factor
for accelerating
retreat of these
glaciers since it creates more surface area
for the warm water to work on.
The climatic conditions that cause an advance or a
retreat may be different
for glaciers located in different climate regimes (see Chapter 4).
The rapid shrinkage of
glaciers around the Antarctic Peninsula, coupled with the potential
for ice - shelf collapse and grounding line
retreat, raises concerns
for the future of the West Antarctic Ice Sheet, and this is an area of urgent current research [3].
For example, scientists know that once giant
glaciers begin to
retreat, in some parts of the world simple geography dictates nothing can stop them from melting into the sea.
Soil and rocks on the Earth's surface reveal the advance and
retreat of
glaciers over the land surface, and fossilized pollen traces out rough boundaries of where the climate conditions were right
for different species of plants and trees to live.
French Prime Minister Manuel Valls visited the Mer de Glace (the Sea of Ice) Friday on Mont Blanc, where the
retreating glacier has been documented
for more than a century, through water colors painted before the invention of the still camera, black - and - white photos depicting a then - modern steam locomotive chuffing alongside the ice and today's high - definition satellite photos.
The real shocker
for me was seeing just how far these
glaciers are
retreating each year.
Retreat to the protected lands of Prince William Sound's calm waters and pristine
glaciers, and Katmai National Park to witness the iconic grizzlies fishing
for salmon, or explore the premiere marine life in the aquatics of Kenai Fjords National Park and the Inside Passage.
Similar conclusions can be made
for more
glaciers world - wide, where the 1940 - 1945 period shows the largest
retreat.
Evidence of melting
glaciers and of Spanish wine - makers having to relocate their vineyards because it is getting too warm in their current location seem to be harder
for the science haters to refute (though I always seem to get the «but not all
glaciers are in
retreat» counter-argument).
Yet the SUV is now the scapegoat
for retreating glaciers.»
Most of the field studies cited in support of the dominance of precipitation effects
for East African
glacier retreat only support the role of precipitation in the initial stages of the
retreat, up to the early 1900's.
I seem also to remember a comment by Bindschadler stating that while GIS
glaciers could
retreat inland from warming oceans, there could be no similar escape
for Antatctica.
Data from the tropical and subtropical Andes suggest that changes in precipitation and cloud cover in the latter portion of the 20th century are minor, and that changes in these quantities are unlikely candidates
for explaining Andes
glacier retreat.
If tropical
glaciers continue to
retreat despite an increase in precipitation, that will constitute a powerful case
for the role of air temperature.
Re # 40: -LSB-... As
for the 1940s, I'm not familiar with the details of GNP, but in Washington State where I live,
glaciers did
retreat substantially until about the 1940s, before advancing again until the late 1970s.
The
retreat of many mountain
glaciers in Asia is a serious issue with respect to water resources
for tens of millions of people (many people, indeed).
[Response: But
glacier retreat is much further along than in the 1930s (see here
for instance)-- and that's the key
for sea level rise.
But look at, say, Wisconsin, with many meters of loess blown there as the
glaciers retreated, then populated as plants took over the area,
for ten thousand years.
In general, tidal
glaciers are cyclical, advancing over 1,000 years or so and then rapidly
retreating for one or two centuries.
We are talking about a
retreat that is unstoppable because we think we have enough evidence to say that these
glaciers will keep
retreating for decades and even centuries to come....