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Topic: Getz Ice Shelf

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	Bathroom Shelf (Site not responding. Last check: 2007-10-10)
		This ice shelf was called a bay by the Australasian Antarctic Expedition, 1911-14, under Douglas Mawson, who named it for Joseph Cook, Prime Minister of the Commonwealth of Australia in 1914.
		Sunda Shelf - Geologically, the Sunda Shelf is an extension of the continental shelf of Southeast Asia, covered during interglacials by the South China Sea, which isolates as islands Borneo, Sumatra Java and smaller islands.
		Getz Ice Shelf - Getz Ice Shelf is an Antarctic ice shelf, over 480 km (300 mi) long and from 32 to 96 km (20 to 60 mi) wide, bordering the Hobbs and Bakutis Coasts of Marie Byrd Land between McDonald Heights and Martin Peninsula.
	www.gj-ceramics.com /bathroomshelf.html (771 words)

	Getz Ice Shelf - Wikipedia, the free encyclopedia
		Several large islands are partially or wholly embedded in the ice shelf.
		The ice shelf westward of Siple Island was discovered by the USAS in December 1940.
		Named by the USAS (1939-41) for George F. Getz of Chicago, Illinois, who helped furnish the seaplane for the expedition.
	en.wikipedia.org /wiki/Getz_Ice_Shelf (198 words)

	Spartanburg SC \| GoUpstate.com \| Spartanburg Herald-Journal
		Nearly all of Antarctica is covered by an ice sheet that is, on average, 2.5 kilometres thick.
		Because ice flows, albeit slowly, the ice within the ice sheet is younger than the age of the sheet itself.
		The George VI Ice Shelf, which may be on the brink of instability [2], has probably existed for approximately 8000 years, after melting 1500 years earlier [3].
	www.goupstate.com /apps/pbcs.dll/section?category=NEWS&template=wiki&text=climate_of_Antarctica (1177 words)

	SCAR » Report 13
		The overall theme of the meeting was, primarily, the coordination of ice radar sounding surveys of the grounding zone of the entire Antarctic Ice Sheet, and secondarily, the coordination of surface mass balance measurements and surface ice velocities.
		Establishing velocities of glaciers, ice streams, ice sheets, and ice shelves is essential to calculate the discharge of the mass balance equation.
		Velocities on the shelf near the DeVicq Glacier increase westward to near 0.5 km yr -1 and reach 0.6 km yr -1 at the glacier.
	www.scar.org /publications/reports/13/taskgroup3.html (7466 words)

	Microwave Shelf (Site not responding. Last check: 2007-10-10)
		Continental shelf - The continental shelf is the extended perimeter of each continent, which is covered during interglacial periods such as the current epoch by relatively shallow seas (known as shelf seas) and gulfs.
		Shackleton Ice Shelf - Shackleton Ice Shelf () is an extensive ice shelf fronting the coast of Antarctica for about 384 km (95E to l05E), projecting seaward about 145 km in the western portion and 64 km in the east.
		The existence of this ice shelf was first made known by the USEE under...
	pans.vvvvvv3.com /microwaveshelf.html (1064 words)

	Feb 1 - In the Amundsen Sea (Site not responding. Last check: 2007-10-10)
		The thinning is greatest in the parts of the ice sheet and glaciers that extend into and float on the sea, known as “ice shelves” and “glacier tongues”.
		Specifically, the cause has been proposed to be melting of the base of the floating ice as a result of upwelling of relatively warm water from the deep ocean onto the continental shelf.
		Yellow areas are ice (ice sheet, glaciers, icebergs and sea ice), fl areas are open water and white areas are high cloud.
	www.antarctica.ac.uk /Living_and_Working/Diaries/RRS_James_Clark_Ross/antarctic2005_2006/17/index.html (2134 words)

	highlightcavesandkarst (Site not responding. Last check: 2007-10-10)
		Although glaciology includes research on snow and ice of all kinds, most glaciological research is done on the large ice sheets of Antarctica and Greenland.
		The icebreaker cruised past Ross Ice Shelf in March, days before the biggest known iceberg of the century was released.
		Ice input above and output across the 2,000-meter ice elevation contour line allowed ice thickening and thinning rates to be calculated for all sectors around the ice sheet.
	www.agiweb.org /geotimes/july01/highlightglaciology.html (619 words)

	Dr Jezek's Modified Script
		Because the ice sheet is deforming, because it is deforming over a complex bed, and because it's being channeled between mountain-passes in many places, the surface of the ice sheet becomes disrupted and results in long flow patterns being superimposed on the ice sheet surface.
		Snow is dumped on the surface of the ice sheet and for the ice sheet to remain in equilibrium some amount of that snow has to eventually be melted off or calved off into the sea.
		This is the Wordie Ice Shelf on the western flank of the Antarctic Peninsula.
	ku-prism.org /video/Ken/Kenscript.html (5970 words)

	TEA: Reynolds- -- 2.28.2000
		I went up in the ice tower, with the "seal people." We were looking for penguins, seals and whales to count for their population study.
		Ice picks up these things as it slides along bedrock, and when it breaks off as an iceberg, it takes them with it.
		While we were sailing along the edge of the Ross Ice Shelf a week or so back, we all took turns using a radar scope to get the range, or distance between the ship and the ice shelf.
	tea.armadaproject.org /reynolds/2.28.2000.html (1613 words)

	Glacial Geomorphic Features on the Antarctic Continental Shelf and Correlation to Substrate: Implications for Behavior ... (Site not responding. Last check: 2007-10-10)
		A coast-parallel trough extends along the inner shelf, whereas the outer shelf is occupied by troughs oriented offshore.
		Based on the extent of the trough and glacial grooves, it is apparent that the ice sheet extended to the shelf break.
		Where crystalline bedrock is the substrate, ice tended to follow the structural grain of the bedrock and carved deep troughs.
	igloo.gsfc.nasa.gov /wais/pastmeetings/abstracts00/Wellner.htm (731 words)

	American Whiskey: A Visit to Bardstown and the Oscar Getz Whiskey Museum
		She told us about the history of Oscar Getz’s collection itself, how the museum came to be where it is now (it used to be his own private collection, which he took on tour to various cities around the country), and what they would like to do to increase and improve it in the future.
		We never did ask Mary what her actual position with the museum is, but she certainly treated it as though it and everything in it were her own personal possessions.
		The Getz family purchased the old Tom Moore Distillery in Bardstown in 1944, changing its name to The Barton Distillery (possibly because the Old Barton label already existed historically, although there are no examples to confirm this).
	www.ellenjaye.com /getz.htm (1833 words)

	Relating rock-floored ice streams to calving ice shelves (Site not responding. Last check: 2007-10-10)
		A massive calving event from the Ross Ice Shelf occurred during the cruise, and sections of Getz Ice Shelf observed in satellite imagery showed advanced stages of disintegration that may soon culminate in massive calving events, notably where De Vicq Glacier has punched through the ice shelf, shattering the ice shelf and itself.
		All of these troughs on the continental shelf are fore-deepened by glacial erosion, which has exposed rugged bedrock floors on the inner portion of the troughs.
		That ice shelf is supplied by ice streams from East Antarctica that are floored on rugged bedrock, according to interpretations of Radarsat imagery.
	igloo.gsfc.nasa.gov /wais/pastmeetings/abstracts00/Hughes.htm (457 words)

	Woods Hole Field Center Publications, Abstracts In Press (Site not responding. Last check: 2007-10-10)
		The length of the northern coastline is 1,197 km, of which 38 per cent is ice wall.
		The coastline is dominated by large ice shelves that are, from west to east, the Sulzberger Ice Shelf (15,261 km
		The overall trend is noteworthy, because it is a possible indication of changing environmental conditions that may be related to reported thinning of the Getz Ice Shelf and the presence of warm bottom water along much of the Marie Byrd Land coast.
	woodshole.er.usgs.gov /bibliographies/inpress/3364.html (429 words)

	TEA: Reynolds- -- 2.25.2000
		At 7 AM we nosed into an immense ice floe, several miles across, and I got a chance to go out with "the ice people," that is Dr. Shusun Li and his group.
		We were lowered down to the ice floe surface the same way we boarded the ship, using the forward deck crane and a netted ring to stand on.
		While I was sleeping we'd gotten out of the pack ice and into a large area of open water near the Getz Ice Shelf.
	tea.armadaproject.org /reynolds/2.25.2000.html (1229 words)

	Australian Antarctic Division - 12 February (ANAN No. 92)
		Severe ice conditions the next day led to the ship becoming beset, but it was able to proceed westwards along the coast after a 12-hour delay, and eventually reached Cape Colbeck, at the eastern approach to the Ross Sea, on 17 January after a difficult passage through ice.
		Ice conditions worsened as the passage continued westwards into the Ross Sea due to the continued presence of several very large icebergs in that region (ANAN-64/03, 16 January 2002), and a severe blizzard was also encountered.
		At the same time, that ice also prevented another tour ship, New Zealand company Heritage Expeditions' vessel' 'Akademic Shokalskiy', from travelling further south into the Ross Sea, a situation that led to the cancellation of a planned climbing and skiing expedition to Mount Erebus (ANAN-91/05, 29 January 2003).
	www.aad.gov.au /default.asp?casid=5895 (1023 words)

	Climate of Antarctica - Wikipedia, the free encyclopedia
		1936-1989: Wordie Ice Shelf significantly reduced in size.
		1995: The Larsen A ice shelf disintegrated in January of 1995.
		of the Larsen B ice shelf disintegrated in February of 2001.
	en.wikipedia.org /wiki/Climate_of_Antarctica (1392 words)

	Feb 9 - Our Next Week in the Amundsen Sea (Site not responding. Last check: 2007-10-10)
		After finishing work in the Getz area, the ship headed further east to the Dotson Ice Shelf, the next ice shelf in the direction of Pine Island on the coast bordering the Amundsen Sea.
		A schedule of work similar to that of the Getz Ice Shelf was under taken here, but this was as far to the east in the region as was possible for the ship to go due to the dangerous ice conditions described last week.
		The ice edge, having been blown down by the fresh Northerly winds of the pas few days, was much further south than where we much further south than where we had entered the pack just a couple of weeks previously.
	www.antarctica.ac.uk /Living_and_Working/Diaries/RRS_James_Clark_Ross/antarctic2005_2006/18a/index.html (1652 words)

	coverstory
		A forty percent reduction in the thickness of Arctic sea ice means around 16 feet of ice melted in the past 20 years, and Schneider says scientists are saying the loss of the Earth’s great ice sheets could signal a fast-approaching crisis point.
		Polar ice twice the size of Texas has melted in the last 27 years, and if current trends continue, there could be no ice in the Arctic during the summer by the end of the century.
		Melting glaciers and ice sheets will add volume to the oceans, but Schneider says this effect is miniscule compared to the rise of sea and ocean levels due to the heat expansion of a warmer ocean.
	www.livingstonweekly.com /coverstory.html (10028 words)

	Adventure Associates \| Antarctica \| Semi-Circumnavigation of Antarctica (Site not responding. Last check: 2007-10-10)
		We plan helicopter flights beyond the fast ice to a seldom-visited region of Antarctica: the spectacular Dry Valleys, where virtually no precipitation has fallen for millions of years and the sole vegetation is lichen that grows inside rocks.
		We follow Scott’s Discovery expedition into Terra Nova Bay, located between Cape Washington and the Drygalski Ice Tongue – the glacial extension that was dramatically shortened by a collision with the massive iceberg B-15A in April 2005.
		Dense pack ice often challenges vessels near Cape Hallett, where scientists from the US and New Zealand established a base for the International Geophysical Year (1957–58).
	www.adventureassociates.com /antarctica/ross/semicircum/itinerary.html (961 words)

	Antarctic Glacier Velocity
		Yet, to understand the ice sheet dynamics fully, we must carefully document all of the coastal changes associated with advance and retreat of ice shelves, outlet glaciers, and ice streams.
		A critical parameter of ice sheets is their velocity field, which, together with ice thickness, allows the determination of discharge rates.
		Tongues on coastlines where ice shelves are narrow or absent tend to be short, perhaps due to vigorous ocean-current and wind regimes.
	geochange.er.usgs.gov /data/antarctica/glacier-velocity/Core/meta/report.html (2171 words)

	Frigidaire Refrigerator Shelf (Site not responding. Last check: 2007-10-10)
		Calder explains clearly frigidaire refrigerator shelf and logically how frigidaire refrigerator shelf and why refrigeration components work, how to keep them working efficiently frigidaire refrigerator shelf and economically, frigidaire refrigerator shelf and what to look for when something goes wrong.
		With Calder's maintenance frigidaire refrigerator shelf and troubleshooting tips, you'll be able to keep it running for years to come frigidaire refrigerator shelf and keep those ice cubes tinkling in that frosted glass.
		Abbot Ice Shelf - The Abbot Ice Shelf () is an ice shelf 400 km (250 mi) long and 64 km (40 mi) wide, bordering Eights Coast from Cape Waite to Phrogner Point.
	ge54.georgeandbills.com /frigidairerefrigeratorshelf.html (1298 words)

	Storage Shelf Plan (Site not responding. Last check: 2007-10-10)
		Wrigley Gulf - Wrigley Gulf () is an embayment about 115 miles wide along the coastline of Antarctica, lying seaward of the Getz Ice Shelf.
		Nearly a right angle in plan, its limits are described by Grant Island, Dean Island, and Siple Island, which are partially or wholly embedded in the ice shelf.
		Dalton Iceberg Tongue extends north from the east part of the shelf.
	crate.vvvvvv3.com /storageshelfplan.html (688 words)

	The Antarctic Sun
		Ancillary investigations include veterinary exams of the seals (including drawing blood and tissue samples for health and genetic assessments), fishing trawls to examine seal prey, and physical oceanography and sea-ice studies to characterize the seals' environment and preferred locations.
		We then turned northward to make several passes through the remaining pack ice from the continental shelf all the way to its northern limits, at around 65-68 degrees south latitude.
		Thus far, our peak winds have been in the range of 50 mph and the air temperature has remained near freezing, which is to be expected given the maritime climate at sea.
	antarcticsun.usap.gov /oldissues99-2000/2000_0123/nbp.html (902 words)

	Circumnavigation of Antarctica aboard expedition vessels
		Further to the west, substantial numbers of Emperor Penguins are believed to breed in the area of the Lazarev Ice Shelf which we hope to explore for the first time.
		We hope to be able to approach the Phantom Coast and Getz Ice Shelf, a virtually unexplored and exciting sector of the continent.
		Sailing along the immense Ross Ice Shelf which is equivalent to the size of France, we hope to land by helicopter on top of the 100-foot high ice barrier.
	www.condorjourneys-adventures.com /antarctica_cruise5.asp (3496 words)

	Our Stations (Site not responding. Last check: 2007-10-10)
		We need to measure the thickness of the ice, the height of sea-level and the concentration of greenhouse gases in the atmosphere.
		the purpose of the station is to study the ice shelf and volcanic activity.
		It is situated on the Ross ice shelf at 160degrees West Longitude which would allow supplies in and out.
	www.cap.nsw.edu.au /ccccollie/our_stations.htm (3262 words)

	Operation Highjump: The Great Antarctic Expedition
		On January 21, young sailor Vance Woodall, from the USS YANCEY, was working on the ice in the unloading area when a tractor nearby picked up a load of snow roller sleds to move in to the barrier cache area.
		Suddenly, on either January 30 or February 1 (the record is unclear), PBM pilot Lieutenant Commander David E. Bunger lifted from the bay and headed south for the continent some hundred miles distant.
		The plane suddenly entered an "ice blink", streams of sunshine trapped beneath the clouds, bouncing off the snow "in a million directions, as if each ice fragment were a tiny mirror".
	www.south-pole.com /p0000152.htm (6646 words)

	Australian Antarctic Division - 12 February (ANAN No. 92)
		The veteran researcher had published extensively on polar matters and 1,930-m Mount Llano in the Prince Olav Mountains near the southern fringe of the Ross Ice Shelf was named after him.
		'Ice Kites' expedition member Brian Cunningham apologised to his supporters in an e-mail on 4 February for his claim last month that the "general hostility" of Antarctica's environment has been "demonised by a succession of polar trekkers" (ANAN-91/09, 29 January 2003).
		Cunningham and his 'Ice Kites' companion Jamie Young only spent a little over a week on the continent during their aborted expedition (ANAN-90/03, 17 January 2003).
	www.aad.gov.au /default.asp?casid=5649 (4799 words)

	[No title] (Site not responding. Last check: 2007-10-10)
		Remainder of area analyzed using DMSP SSM/I ice concentrations from 30 May 2000.
		Summary: 30% OLS infrared, 70% SSM/I. Amundsen Sea (150W-90W): Portions of sea in the vicinity of the Getz Ice Shelf visible on OLS 152.1534Z, 152.1244Z, 152.0919Z, 151.1620Z, 151.1548Z, 151.1257Z and 151.0931Z.
		Summary: 40% OLS infrared, 60% SSM/I. Weddell Sea (30W-30E): Due to a lack of imagery, the sea was analyzed using DMSP SSM/I ice concentrations from 30 May 2000.
	www.natice.noaa.gov /PUB/antarctica/metadata/2000/ameta000529.txt (282 words)

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