Sentences with phrase «through fram»

However, the Beaufort Sea High has re-established during August, combined with a strong low over Eurasia, leading to enhanced transport of ice through Fram Strait and acceleration in the rate of ice loss, particularly in the Chukchi Sea (Figure 4).

Flushing through Fram Strait occurs almost constantly, no matter how thick the ice is, or what Oscillation dominates, its a natural phenomena of great consistency.

The Arctic Ocean's Transpolar Drift exits the Arctic Basin by its only deep - water channel through Fram Strait just east of Greenland.

Differences between surface winds and SLP, and vortex splitting and sea ice extent composites exhibit conditions that are unfavorable to export through Fram Strait in May, 2009; southwesterly versus southeasterly winds in the Beaufort Sea region may also limit free ice drift conditions and inhibit the acceleration evident in years exhibiting record lows in sea ice extent.

The Transpolar Drift Stream now sweeps across most of the Arctic Ocean, carrying most of the older, thicker sea ice out of the Arctic Ocean through Fram Strait (lower right).

The outgoing flow through Fram Strait carries with it large volumes of fresh water as fragmented pack ice, a flow that is strongly episodic at decadal scale and is associated with the series of so called Great Salinity Anomalies observed within the circulation of the subarctic gyre and in the Nordic seas that were discussed in the previous chapter.

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.

The NAO went into a strongly + ve mode from 1989 to 1995, having a role in expulsion of Arctic multi-year ice through the Fram Strait.

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.

The ice export through Fram Strait has shown no significant trend during the past 30 years (Kwok, Spreen et al., and others).

There is very little ice in the East Greenland Sea, a region fed by the outflow of ice through Fram Strait from the Arctic Ocean.

When it comes to ice that is lost through transport (through the fram straight for example), probably.

Does the ice get blown out through the Fram strait or not?

«Regression maps of SIM during the wintertime (January — March) AO index show 1) an increase in ice advection away from the coast of the East Siberian and Laptev Seas, which should have the effect of producing more new thin ice in the coastal flaw leads; 2) a decrease in ice advection from the western Arctic into the eastern Arctic; and 3) a slight increase in ice advection out of the Arctic through Fram Strait.

Arctic Oscillation has tended towards a state with lower than average ice export through Fram Strait, but that may be moderating.

We can observe the gyre in the Beaufort Sea, offshore of the Canadian and Alaskan coasts as well as the ice flux leaving the Arctic Ocean through the Fram Straight, between Greenland and the Svalbard archipelago.

Inflow from the North Atlantic Current enters through the Fram Strait, cooling and sinking to form the deepest layer of the halocline, where it circles the Arctic Basin counter-clockwise.

In addition, there is a sea level pressure (SLP) ridge over Greenland that drives strong northerly winds through the Fram Strait, facilitating ice export.

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.

The Transpolar Drift and Beaufort Gyre formerly brought new ice into the main pack and exported old ice - mainly on the Atlantic side through Fram Strait.

They consist of heavily fragmented ice much of which is being advected through the Fram Strait.

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.

The positive phase also tends to increase the transport of thick, multiyear ice out of the Arctic through the Fram Strait.

With no anchoring of the old ice and the on - going push through Fram Straight the whole future of the Arctic over the next few months looks like it will be determined by how the wind blows.

It had a role due to increased ice fluxes through the Fram Strait in the early 1990s, when the AO / NAO was very positive.

There's an ocean net heat flux of 3.8 T Watt through the Fram Strait (between Iceland and Greenland) with 2.3 T Watt through the Bering Strait, both into the Arctic.

On the losses over the last two springs, has that mostly been through physical transport through the Fram Straight?

It's worth bearing in mind that despite the increase in area export, volume export through Fram shows no trend, e.g. Spreen et al: http://soa.arcus.org/abstracts/fram-strait-sea-ice-volume-export-estimated-between-2003-and-2008-satellite-data This is because the ice being exported has thinned even as area export has increased.

Thus the anomaly map is consistent with cold water from the Arctic flowing through the Fram Strait down into the blob.

Those atmospheric patterns shifted to cyclonic in the early - to mid-1960s driving the accumulated freshwater and sea ice through Fram Strait — the main source of the Great Salinity Anomaly in the late 1960s.

In addition to an overall retreat, IIRC one change since then has been that the first - year ice has broken through the Fram Strait, which seems significant since that hasn't been observed to happen before.

There is no trend in net mass of ice transported through the Fram Strait.

While Rampal et al may not explain the difference so much because of the observed difference between recent volume and area transport through Fram.

http://www.ifm.zmaw.de/research/remote-sensing-assimilation/sea-ice/sea-ice-volume-flux/ Although due to increase of speed of transport through Fram, area flux has increased in recent years (Smedsrud et al, 2008).

(My particular area of interest is the North Atlantic from the Irminger Sea north through the Fram Strait but mostly the northern part.)

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.

# 19 Gareth John Evans, Out of interest, the Arctic Oscillation / North Atlantic Oscillation (which are intrinsically linked) seem to have a key role in both the Arctic ice loss (outflushing through the Fram Strait)-- Rigor / Wallace) and the Mediterranean drying e.g. Figen Mekik's post at RC http://www.realclimate.org/index.php/archives/2007/10/sweatin-the-mediterranean-heat/

# 19 Gareth John Evans, Out of interest, the Arctic Oscillation / North Atlantic Oscillation (which are intrinsically linked) seem to have a key role in both the Arctic ice loss (outflushing through the Fram Strait)-- Rigor / Wallace) and the Mediterranean drying e.g. Figen Mekik's post at RC http://www.realclimate.org/index.php/archives/2007/10/sweatin-the-mediterranean-heat/

The only deep exit from the Arctic is through Fram Strait, which divides Greenland and Norway's Svalbard islands.

Examining the CyroSat - 2 sea ice thickness map for this spring, Stefan Hendricks further explained: «The Transpolar Drift Stream, a well - known current in the Arctic Ocean, will be carrying the majority of the thick, perennial ice currently located off the northern coasts of Greenland and Canada through the Fram Strait to the North Atlantic.

Not exact matches

Now that he's got a strong footing in running three locations of the business in northwest Indiana, Baur is working to help custom picture framers compete in a changing market through a full - service firm he recently launched — KB Consulting.

Now living in Toronto, Snow has created a reputation as a «framer of vision» who, through his inventive and provocative work, has amazed and astounded audiences for more than fifty years.

A late lunch, a quick detour to drop something at the framers, and then a solitary walk through the backstreets to Hollybush Gardens.

The preferred ridging through» 07 - ’12 leading to strong Fram ice loss and GIS melt?

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