Sentences with phrase «for ice streaming»

The grounding line is where the ice stream become afloat, so if a subglacial lake breaches to the ocean, unless it is deep for the ice stream to become floating, it will not alter the grounding line in and of itself.

Not exact matches

To know him you must gird as for war and wade the rivers when they are bitter cold — in sleet - filled gloom, or in freezing blue weather when the leafless alders gleam in pale sunlight along the streams, and ice forms in the guides of your rod.

For hundreds of years, the Kaskawulsh Glacier formed a wall that segregates snow and ice meltwater into two streams: the Slims River, which joins with other streams and crosses Alaska before draining into the Bering Sea, and the Kaskawulsh

The following day, carrying a heavy pack of sampling equipment over mud and ice, she stumbled a few times during a hike to a stream for measurements.

Aeolian deposition is responsible for sorting and transporting lithogenic matter (primarily sand - and clay - sized particles), containing microbial cells from the surrounding desert environments (soils, ephemeral streams, glaciers, etc.) onto the ice covers that range in thickness from 3 to 20 meters.

These flow rates are unprecedented: they appear to be the fastest ever recorded for any glacier or ice stream in Greenland or Antarctica, the researchers say.

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.

Virtually ice - free summers in the arctic sea could well arrive by 2030, with troubling implications for accelerated albedo feedback and possibly disruptive changes in the jet stream.

A subglacial aquifer bed model and water pressure dependent basal sliding relationship for a West Antarctic ice stream.

An additional new feature is the increasingly visible fast dynamic response of ice shelves, for example, the dramatic breakup of the Larsen B Ice Shelf in 2002, and the acceleration of tributary glaciers and ice streams, with possible consequences for the adjacent part of the ice sheeice shelves, for example, the dramatic breakup of the Larsen B Ice Shelf in 2002, and the acceleration of tributary glaciers and ice streams, with possible consequences for the adjacent part of the ice sheeIce Shelf in 2002, and the acceleration of tributary glaciers and ice streams, with possible consequences for the adjacent part of the ice sheeice streams, with possible consequences for the adjacent part of the ice sheeice sheets.

This ice stream is unlikely to collapse in our lifetime — but the same can not be said for future generations.

Cryotherapy also known as cold therapy, dates all the way back to the early BC's, from Napoleon's Soldiers and Horses utilising freezing cold streams in 1812 for recovery, to the first ever ice bath in the US being used in 1895.

And we re streaming all the us job it s cake versus ice cream for.

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How long I slept I do not know, and never shall know; but I awoke suddenly, and with a start, for it seemed as if a stream of ice - cold water was pouring over my face.

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Walking up the muddy wet dirt paths, crossing over the streams of the waterfalls, slippery rocks and fallen treat, the trek took a good 1.5 hours before finally reaching the main fall - a majestic 45 m drop, landing in a shallow pool of ice cold water, perfect for cooling off after the sweaty walk.

It's a journey even Indiana Jones would have to brace himself for: an hour - long rainforest hike, a swim across an ice - cold stream into the narrow mouth of a cave, and then a slippery descent into the dark, cavernous depths where bats, spiders, and ancient scorpion - like amblypygi lurk in the nooks.

I didn't realise I'd broken it, and it was beautiful weather, and I pitched my tent and stuck my leg into an ice - cold stream for about two days.

The jet stream pattern — particularly the strongly negative NAO [North Atlantic Oscillation] and associated blocking — that has been in place for the last 2 weeks and is projected to be with us into next week is exactly the sort of highly amplified (i.e., wavy) pattern that I'd expect to see more of in response to ice loss and enhanced Arctic warming.

The PIG is not dominated by its ice shelf, hence the potential for rapid ice stream response.

This illustrates two things, that PIG flow regime has not changed much for quite awhile and two that all the action from topography and changing basal conditions is happening lower in the ice stream.

For the LIM experiment, we enlisted James Fastook to incorporate the marine instability mechanism published by Robert Thomas in 1977 to make grounded ice margins retreat when ice downdrawn by ice streams became thin enough to become afloat along the WAIS marine margins.

Terran: An examination of a map of glacier velocity for either the Pine Island presented in this post or of the ice streams feeding the Ross Ice Shelf indicate that most of the ice sheet region is not a fast flow regiice streams feeding the Ross Ice Shelf indicate that most of the ice sheet region is not a fast flow regiIce Shelf indicate that most of the ice sheet region is not a fast flow regiice sheet region is not a fast flow region.

The mechanism for their rapid movement is being intensively studied because of the possibility that rapid ice - stream flow may cause the ice sheet to disintegrate, resulting in a disastrous rise in world - wide sea level.

The discovery is significant in relation to the mechanism for rapid movement of the ice streams, which are huge, fast - flowing ice currents within the slow - moving ice sheet that covers most of Antarctica.

I think there is evidence that AGW has caused the decline in arctic sea ice, which may be responsible for the changes seen in the paths of the jet stream, which may be responsible for the blocking high over Greenland which was responsible for Sandy's left turn.

You say that there is evidence that AGW has caused the decline in arctic sea ice, which may be responsible for the changes seen in the paths of the jet stream, which may be responsible for the blocking high over Greenland which was responsible for Sandy's left turn.

[13] According to Arctic researcher Jennifer Francis, «The Arctic warmth is the result of a combination of record - low sea - ice extent for this time of year, probably very thin ice, and plenty of warm / moist air from lower latitudes being driven northward by a very wavy jet stream.»

Although it is documented that the ice stream in Greenland has been melting for some time, scientists now believe that this has been happening for many years.

There have been many primarily anthropogenic changes in the past, but the major jet stream changes caused by the retreat of the North American Ice Shield seems to be much more determinative for Holocene changes in Saharan rainfall.

«Mid-latitude economies such as those in Europe and the United States could be threatened, for example, by a suggested link between sea - ice retreat and the strength and position of the jet stream, bringing extreme winter and spring weather,» the paper states.

LIA wasn't GLOBAL cooling; but colder in Europe, north America — because Arctic ocean had less ice cover - > was releasing more heat / was accumulating - > radiating + spreading more coldness — currents were taking that extra coldness to Mexican gulf — then to the Mediterranean — because Sahara was increasing creation of dry heat and evaporating extra water in the Mediterranean — to top up the deficit — gulf stream was faster / that was melting more ice on arctic also as chain reaction — Because Mediterranean doesn't have enough tributaries, to compensate for the evaporation deficit.

All of these characteristics (except for the ocean temperature) have been used in SAR and TAR IPCC (Houghton et al. 1996; 2001) reports for model - data inter-comparison: we considered as tolerable the following intervals for the annual means of the following climate characteristics which encompass corresponding empirical estimates: global SAT 13.1 — 14.1 °C (Jones et al. 1999); area of sea ice in the Northern Hemisphere 6 — 14 mil km2 and in the Southern Hemisphere 6 — 18 mil km2 (Cavalieri et al. 2003); total precipitation rate 2.45 — 3.05 mm / day (Legates 1995); maximum Atlantic northward heat transport 0.5 — 1.5 PW (Ganachaud and Wunsch 2003); maximum of North Atlantic meridional overturning stream function 15 — 25 Sv (Talley et al. 2003), volume averaged ocean temperature 3 — 5 °C (Levitus 1982).

The model is not quite state - of - the - art, in that it does not solve the full Stokes equation but a simpler form of the dynamical system that is appropriate for ice shelves and ice streams.

Factors that come into play for regional weather (and indeed global weather) are Earth's seasons, ocean patterns, upper winds, Arctic sea ice, and the shifting shape of the jet stream (see below).

While climate change does not affect Earth's tilt, it does have potential implications for many of the other factors that influence winter weather in the US, including Arctic sea ice, the polar jet stream, the polar vortex, and El Niño.

One is that the evidence for change in the expected direction if climate change was having an effect — that is, changes in physical (ice sheets, stream flow, coastal erosion etc.) and biological systems (timing of breeding events, shifting species ranges, population declines etc.)-- is overwhelming.

A constant stream of DOBs are wandering over for Magnum ice - creams and chips to sustain them on their journey.