Sentences with phrase «of ice export»

Gudmandsen provides a more detailed analysis of ice export from the Lincoln Sea north of the Canadian Arctic Archipelago into Baffin Bay, through Nares Strait between Greenland and Canada.

Not exact matches

Greenland's Department of Ice and Water, meanwhile, is looking to export its icebergs.

«We export a lot of blends to school nutritional programs, as well as blends for ice cream manufacture all over, including the Caribbean, South America, Asia and Africa,» says Matt Stelzer, vice president of operations.

Producing private label, branded and licensed products, Rolland produces about 65m litres of ice cream a year with roughly 25 % exported to -LSB-...]

@user5751924 — Russian exports (either via out - sourcing, or emigration, or malware, or cracking) of computer programming talent are on the scale of rocket launches, diamonds, and ice - breaking services — not on the scale of oil, steel, and natural gas.

Thinner ice also breaks up more easily, and the thinner the ice, the faster it seems to be exported from the Arctic to the Atlantic, says Rune Graversen of the Royal Netherlands Meteorological Institute.

During the past weeks, sea - ice thickness measurements were the main topic of the TIFAX (Thick Ice Feeding Arctic Export) campaign, which involved research aircraft using laser scanners and a towed electromagnetic proice thickness measurements were the main topic of the TIFAX (Thick Ice Feeding Arctic Export) campaign, which involved research aircraft using laser scanners and a towed electromagnetic proIce Feeding Arctic Export) campaign, which involved research aircraft using laser scanners and a towed electromagnetic probe.

Increased export of grounded ice after the collapse of northern Larsen Ice Shelf, Antarctic Peninsula, observed by Envisat ASAR, in Igarss: 2007 Ieee International Geoscience and Remote Sensing Symposium, Vols 1 - 12 — Sensing and Understanding Our Planice after the collapse of northern Larsen Ice Shelf, Antarctic Peninsula, observed by Envisat ASAR, in Igarss: 2007 Ieee International Geoscience and Remote Sensing Symposium, Vols 1 - 12 — Sensing and Understanding Our PlanIce Shelf, Antarctic Peninsula, observed by Envisat ASAR, in Igarss: 2007 Ieee International Geoscience and Remote Sensing Symposium, Vols 1 - 12 — Sensing and Understanding Our Planet.

The ice found its way into «the drinks of Maharajahs, of men and women in waterfront bars in midsummer in Martinique,» he says, over soft music that mixes in sounds referencing the industry and export geography.

In the past lobster was a big export and here in San Pedro a cargo plane full of ice would fly in to take the catch.

The works include reenactments of Vito Acconci's Seedbed (1972), in which the artist occupied the space under a false floor, masturbating and speaking through a microphone to visitors above; Valie Export's Action Pants: Genital Panic (1969) in which Export walked through a movie theater in crotchless pants, challenging the audience to turn from the images of women on the screen to a real female body; and Abramovic's own Lips of Thomas (1975), in which she ate a kilogram of honey and drank a liter of red wine before breaking her glass with her hand, incising a star in her stomach with a razor blade, whipping herself until she «no longer felt pain,» then lying down on an ice cross while a space heater suspended above her caused her to bleed even more profusely.

The» low frequency oscillation'that dominated the ice export through the Fram Strait as well as the extension of the sea - ice in the Greenland Sea and Davis Strait in the twentieth century may therefore be regarded as part of a pattern that has existed through at least four centuries.

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.

It seems that the near - zero replenishment of the MY ice cover after the summers of 2005 and 2007, an imbalance in the cycle of replenishment and ice export, has played a significant role in the loss of Arctic sea ice volume over the ICESat record.

Well, with the global oil exporting countries on track to consuming all the oil they produce by 2025 - 2030 the rest of the world will be back in the dark ages well before we get an ice - free Arctic.

The net trend in the past decennia is a cooling of the (deeper) Atlantic around South Greenland, which points to more cooler water / ice export from the Arctic.

In 2007 we had a persistent high sitting over the Canadian Arctic, which contributed significantly to the export of sea ice out of the Arctic.

Bottom line: the great ice loss of summer 2007 was substantially set up by the export of huge amounts of thick old ice many years earlier, as described here:

Second several papers by Rigor and others show that the loss of ice is due to changing wind patterns have caused greater ice export.

Nares Strait Recent ice advection patterns; warm water advances into the Arctic from the Atlantic; ice distribution patterns: all of these things show that conditions continue to be advantageous for export of ice through Fram Strait.

As soon as the ice in Nares Strait breaks up, a continuation of current trends will be advantageous for the export of substantial volumes of the remaining older ice through that channel, supplementing the export through Fram Strait.

Analyzing satellite and in - situ ocean data, the researchers said a large amount of pack ice and fresh water was exported into the northwest Labrador Sea in the summer of 2007.

While a negative AO leads to warmer temperatures over the Arctic, it also tends to reduce the flow of sea ice out of the Arctic by affecting the winds that can export the ice to warmer waters, where it melts.

The absence of anomalous features evident in 2007 in SLP and stratospheric and surface winds in spring in 2011 indicates that accelerated decline associated with the former will not be an artifact of dynamical phenomena, although a thinner and more mobile ice cover may lower the wind forcing threshold required for increased ice export.

The June outlook reflects the fact that winds during the last two weeks have reversed the flow of the buoys and sea ice in the Beaufort Gyre and Transpolar Drift Stream, slowing export and sequestering sea ice in the Arctic.

Surface weather patterns are central in driving export, deformation, and compaction of ice, transporting heat and moisture, and are linked to cloud cover.

In Fram Strait, Rigor et al. predicts reduced export of sea ice from the Arctic Ocean.

Low heights in the Atlantic side suggest colder temperatures and less sea ice export, while north of Siberia winds are now offshore, which may reverse the persistence of sea ice in that region.

The thinner wintertime ice combined with strengthened southerlies in spring promotes an earlier break - up of the ice pack in the Eurasian coastal region, resulting in significant sea ice export.

At the workshop and from recent publications, there is near consensus that the 2007 sea ice minimum was due to the combination of almost two decades of preconditioning (thinning and increased ice export) plus a rare supportive weather pattern in summer 2007.

Surface weather patterns are central in driving export, deformation, and compaction of ice, and transporting heat and moisture, and are linked to cloud cover.

Long - term changes in atmospheric circulation have resulted in an increased amount of perennial sea ice being exported through Fram Strait rather than being recirculated (e.g., Beaufort Gyre); this was what set up the 2007 record September minimum.

ii) ice - 605 cover associated sea - level - pressure changes that reorganize winds and thereby direction of freshwater and sea ice export between the Arctic Basin and marginal seas;

Another side effect of the high pressure has been increased export of sea ice from the Central Arctic, as illustrated by this animation from «Wipneus» on the Arctic Sea Ice Forice from the Central Arctic, as illustrated by this animation from «Wipneus» on the Arctic Sea Ice ForIce Forum:

In terms of wind conditions, weak, southerly mean winds over the Fram Strait would presumably have reduced ice export out of the Arctic.

To summarise the arguments presented so far concerning ice - loss in the arctic basin, at least four mechanisms must be recognised: (i) a momentum - induced slowing of winter ice formation, (ii) upward heat - flux from anomalously warm Atlantic water through the surface low ‐ salinity layer below the ice, (iii) wind patterns that cause the export of anomalous amounts of drift ice through the Fram Straits and disperse pack - ice in the western basin and (iv) the anomalous flux of warm Bering Sea water into the eastern Arctic of the mid 1990s.

In the Beaufort and Chukchi seas, ice distribution mimicks the Beaufort Gyre circulation pattern with advection of ice from the high Canadian Arctic into the Beaufort Sea and export of ice northward in the Chukchi Sea.

However, due to strong divergence and export, first ‐ year ice (FYI) was much thinner than in 2015, giving rise to expectations of earlier FYI melt and disappearance in 2016 than in 2015.

Behavior of the sea ice over the past winter and the spring and the large positive temperature anomalies in the Arctic (as high as 20 degrees C over large regions in the past winter) suggest that an extent near that of the 2012 minimum may occur again if there is large export of sea ice out to the Atlantic Ocean via the Fram Strait.

But accelerating the export of ice in winter depletes the Arctic Ocean of older thicker ice, leaving the extent of the thinner ice pack more sensitive to summer melt.

The roughly factor of two increase in speed shown is partly due to decreases in ice thickness and strength, but it is safe to predict that if cyclonic storm events like this one ending 2015 continue penetrating the eastern Arctic Ocean, they will increase ice export and reduce summer 2016 ice extent.

The subsequent increase in multiyear sea ice culminated during the past 2500 years and is linked to an increase in ice export from the western Arctic and higher variability of ice - drift routes.

Thin ice makes it more difficult to rely on conventional wisdom, although this year has proven that a lack of melting momentum during May and June followed by weather conditions during July and August that do not favour melt / export / compaction can still prevent a record, even if volume was at a record low for much of the year.

Considering no special atmospheric pattern for enhanced ice melt or ice export out of Fram Strait results in an estimate of 5.4 million square kilometers.