Not exact matches
Almost exactly a year ago, a 251 - square -
kilometer sheet
of ice broke
from the Petermann Glacier in Greenland and started slowly drifting into the open ocean.
Although a British team was unsuccessful in its quest to penetrate Lake Ellsworth, a group
of Russian scientists successfully retrieved samples
from Lake Vostok, thousands
of kilometers away on the Eastern Antarctic
Ice Sheet.
Its 500 - meter by 120 - meter array
of 677 detectors in glass globes dangle like love beads
from electrical cables 1.5
kilometers down into South Pole
ice.
Scientists have drilled into one
of the most isolated depths in all
of the world's oceans: a hidden shore
of Antarctica that sits under 740 meters
of ice, hundreds
of kilometers in
from the sea edge
of a major Antarctic
ice shelf.
Scientists find translucent fish in a wedge
of water hidden under 740 meters
of ice, 850
kilometers from sunlight
Icebergs that have calved off the edge
of the glacier are visible floating out to sea — but so are cracks hundreds
of kilometers inland
from Jakobshavn, on what would otherwise be a flat expanse
of ice.
This isolated cavity
of seawater, down at the grounding zone, sits deep beneath the back corner
of the
ice shelf — 850
kilometers back
from where the edge
of the
ice meets the open sea.
And down the coast
from Goose Cove, a Port Hope Simpson crab fisherman captured some footage
of a smaller, almost five -
kilometer - long chunk
of the
ice island floating in open waters.
From 1994 to 2003, the overall loss
of ice shelf volume across the continent was negligible: about 25 cubic
kilometers per year (plus or minus 64).
Several Russian news outlets are reporting that Russian scientists have successfully drilled to Antarctica's Lake Vostok, a massive liquid lake cut off
from daylight for 14 million years and buried beneath 2 miles (3.7
kilometers)
of ice.
Whereas Pluto's putative ocean could in principle support life, it is probably locked beneath perhaps 200
kilometers of ice and very far
from Earth, making it a much less appealing target for astrobiological studies than other, closer subsurface oceans known to exist in the solar system, such as those within the icy moons circling Jupiter and Saturn.
The Dark Zone
of Greenland
ice sheet is a large continuous region on the western flank
of the
ice sheet; it is some 400
kilometers wide stretching about 100 kilometres up
from the margin
of the
ice.
The new images, at resolutions
of about 80 meters per pixel, show a striking shoreline, where smooth plains
of nitrogen
ice from Pluto's «heart» rub up against water
ice mountains several
kilometers high.
With light sensors sunk
kilometers deep into the
ice sheet, IceCube's detector is so huge that it could pick up traces
of a million neutrinos
from a Milky Way supernova.
The Lance sailed east and around 80
kilometers from the small island
of Hopen moored next to a large expanse
of pack
ice on May 2.
The minimum amount
of ice cover each summer had fluctuated above and below six million square
kilometers from 1979 through 2000.
Enkelmann appreciates the challenge
of collecting samples here because this range has the highest peaks
of any coastal mountain range and is only 20
kilometers from the Pacific Ocean, but she points out that it is a tough area to study because
of the big
ice sheets.
An international team including researchers
from the Laboratoire de Planétologie Géodynamique de Nantes (CNRS / Université de Nantes / Université d'Angers), Charles University in Prague, and the Royal Observatory
of Belgium [1] recently proposed a new model that reconciles different data sets and shows that the
ice shell at Enceladus's south pole may be only a few
kilometers thick.
Gas giants are probably born further out, beyond some 400 million
kilometers, where
ice crystals can develop and accumulate into planetary cores that are massive enough to attract large amounts
of gas
from the disk.
Satellites
from NASA and other agencies have been tracking sea
ice changes since 1979, and the data show that Arctic sea
ice has been shrinking at an average rate
of about 20,500 square miles (53,100 square
kilometers) per year over the 1979 - 2015 period.
But measurements
from the Gravity Recovery and Climate Experiment (GRACE) satellites, which weigh
ice by measuring its gravitational tug
from space, suggest that West Antarctica as a whole is losing
ice — together with the Antarctic Peninsula, about 150 cubic
kilometers per year as
of 2005.
This 500 -
kilometer - wide
ice ball shoots out large geysers
of ice crystals, which apparently originate
from underground lakes near the satellite's south pole.
Hawkings and his collaborators spent three months in 2012 and 2013 gathering water samples and measuring the flow
of water
from the 600 - square -
kilometer (230 - square - mile) Leverett Glacier and the smaller, 36 - square -
kilometer (14 - square - mile) Kiattuut Sermiat Glacier in Greenland as part
of a Natural Environment Research Council - funded project to understand how much phosphorus, in various forms, was escaping
from the
ice sheet over time and draining into the sea.
Ice - clad moon
of Jupiter blasts jets hundreds
of kilometers into the sky, possibly
from subsurface ocean
Surprise find The team's actual mission was to survey ocean currents near the Ross
Ice Shelf, a slab of ice extending more than 600 miles (970 kilometers) northward from the grounding zone of the West Antarctic Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
Ice Shelf, a slab
of ice extending more than 600 miles (970 kilometers) northward from the grounding zone of the West Antarctic Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
ice extending more than 600 miles (970
kilometers) northward
from the grounding zone
of the West Antarctic
Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
Ice Sheet into the Ross Sea, to model the behavior
of a drill string, a length
of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment samples.
A year and half ago, physicists working with the massive IceCube particle detector — a 3D array
of 5160 light sensors buried
kilometers deep in
ice at the South Pole — spotted ghostly subatomic particles called neutrinos
from beyond our galaxy.
Geysers
of vapor — a couple
of hundred
kilometers tall and possibly erupting at supersonic speeds — occasionally spew
from the south polar regions
of Europa, one
of Jupiter's
ice - covered moons, a new study suggests.
The collaboration's report on the first cosmic neutrino records
from the IceCube Neutrino Observatory, collected
from instruments embedded in one cubic
kilometer of ice at the South Pole, was published Nov. 22 in the journal Science.
A study evaluating the origins
of shrubs and herbs on a group
of islands in the Arctic Circle finds that seeds arrived
from hundreds
of kilometers away to restore plant communities lost during the last
ice age — all in a matter
of a few thousand years.
Warmth
from the Earth has melted about 2000 cubic
kilometers of water, making Lake Vostok by far the largest
of more than 70 known lakes within the Antarctic
ice.
Images
from NASA's Galileo probe a few years ago, coupled with previous observations, suggest that Europa's
ice - covered surface may conceal a global, liquid ocean tens
of kilometers deep.
The giant
ice island is 46 square miles (120 square
kilometers), and separated
from the terminus
of the Petermann Glacier, one
of Greenland's largest.
Below the ocean may be a few hundred miles (or
kilometers)
of a heavier form
of ice that may exist under higher pressures on above a rocky core roughly 1,800 to 2,100 miles (3,000 to 3,400 km (more
from Cassini news release; Lorenz et al, Science, March 21, 2008; Richard A. Kerr, ScienceNOW Daily News, March 20, 2008; David Shiga, New Scientist, March 20, 2008; and Charles Q. Choi and Andrea Thompson, Space.com/MSNBC, March 20, 2008).
Nat» l Public Radio in the US is reporting the
ice shelf story at the moment, though it happened a while back: «The Ayles Ice Shelf — 66 square kilometers (41 square miles) of it — broke clear 16 months ago from the coast of Ellesmere Island....&raq
ice shelf story at the moment, though it happened a while back: «The Ayles
Ice Shelf — 66 square kilometers (41 square miles) of it — broke clear 16 months ago from the coast of Ellesmere Island....&raq
Ice Shelf — 66 square
kilometers (41 square miles)
of it — broke clear 16 months ago
from the coast
of Ellesmere Island....»
The net loss in volume and hence sea level contribution
of the Greenland
Ice Sheet (GIS) has doubled in recent years
from 90 to 220 cubic
kilometers / year has been noted recently (Rignot and Kanagaratnam, 2007).
In our paper, based on data
from Jason Box
from the Geologic Survey
of Denmark and Greenland, we estimated that the Greenland
ice sheet has already come out
of equilibrium since the beginning
of the 20th century and has since added about 13,000 cubic
kilometers of meltwater to the ocean.
With green features in its construction and even greener intentions, it's a great addition to the tourism circuit in the very popular southern area
of the country.Located at 5
kilometers from El Calafate and surrounded by The Glaciers National Park, Glaciarium attempts to add some extra meaning to the amazing natural beauty that surrounds it: the park in which it's located is around 4,500 sq
kilometers and comprises 47 glaciers, the largest
ice cap outside Antarctica and Greenland.
You see, I found a MODIS satellite image
from July 6th 2011 and I don't see any «
kilometers of sea
ice» that you would have to smash through to get to Longyearbyen.
Nearly the entire
ice cover
of Greenland,
from its thin, low - lying coastal edges to its 2 - mile - thick (3.2 -
kilometer) center, experienced some degree
of melting at its surface, according to measurements
from three independent satellites analyzed by NASA and university scientists.
From whale bones, 42 Arctic driftwood, 26 and patterns
of Arctic shoreline erosion, 25 we also know that during the Holocene, Arctic summer sea
ice retreated 1000
kilometers further north than seen today.
From what scientists have learned, this ice sheet is far from static: It has «streams» of fast - moving ice running toward the sea at a rate of several kilometers a y
From what scientists have learned, this
ice sheet is far
from static: It has «streams» of fast - moving ice running toward the sea at a rate of several kilometers a y
from static: It has «streams»
of fast - moving
ice running toward the sea at a rate
of several
kilometers a year.
This is a decrease
from the average rate
of ice loss for June 2010
of -85,210 square
kilometers per day, and is slower than climatology (average
of -84,050 square
kilometers per day for 1979 - 2000).
Rigor et al. (Polar Science Center, University
of Washington); 5.4 Million Square
Kilometers; Heuristic This estimate is based on the prior winter Arctic Oscillation (AO) conditions, and the spatial distribution
of the sea
ice of different ages as estimated
from a Drift - age Model (DM), which combines buoy drift and retrievals
of sea
ice drift
from satellites (Rigor and Wallace, 2004, updated).
A regression - based forecast for September
ice extent around Svalbard (an area extending
from 72 — 85N and 0 — 40E), which uses May sea surface temperatures, the March index
of the Arctic Oscillation, and April
ice conditions as predictors, yielded a mean
ice extent in September 2010
of 255,788 square
kilometers around Svalbard.
From July 1 - July 20, the rate
of ice loss averaged -79,810 square
kilometers per day.
Dozens
of autonomous buoys deployed on the sea
ice as far as 20
kilometers away
from the vessel measured the growth and melting
of sea
ice to give indications
of ocean heat flux on a larger scale.
BBC News reports that data
from Europe's Cryosat spacecraft shows that Arctic sea
ice coverage was nearly 9,000 cubic
kilometers (2,100 cubic miles) by the end
of this year's melting season, up
from about 6,000 cubic
kilometers (1,400 cubic miles) during the same time last year.
From October 1 to 15,
ice extent increased only 378,000 square
kilometers (146,000 square miles), less than a third
of the 1981 to 2010 average gain for that period.
Sea
ice extent for September 2007 was 4.3 million square
kilometers — a reduction
of more than 40 %
from the 1980s and a rapid decline to more than 20 % below the previous record minimum.
As
of 13 August, «Sea
ice extent is currently tracking at 5.4 million square
kilometers (2.1 million square miles), with daily extents running at 940,000 square
kilometers (361,000 square miles) below previous daily record lows, a significant decline
from past years.»