The updated prediction of
ice thickness from the PIOMAS model, submitted by Zhang, continues to show an ice - free Northwest Passage (Figure 2a).
Figure 3: Average
ice thickness from 21st March — 17th April 2017, as estimated by the radar sensor aboard CryoSat - 2.
Sea
ice thickness from the ESA CryoSat - 2 altimeter, provided by NSIDC and Nathan Kurtz at the NASA Goddard Space Flight Center.
Our method uses estimates of
ice thickness from a coupled ice - ocean model as predictors for a statistical forecast of the minimum ice extent in September.
And for years nuclear submarines (Russian, American and British) have been measuring
ice thickness from the bottom, using their sonar.
• Calibrate the retrospective simulations of
ice thickness from our numerical model against the aggregate of all the observation systems by removing the mean difference between the model and the observations to create a Calibrated Model Ice Thickness Record.
While sea ice thickness observations are sparse, here we utilize the ocean and sea ice model, PIOMAS (Zhang and Rothrock, 2003), to visualize mean sea
ice thickness from 1979 to 2018.
Wadhams (University of Cambridge); 4.1; Heuristic Based on recent EM measurements of first year ice thickness merged into probability density functions of
ice thickness from recent submarine voyage and subtracting an assumed summer melt of up to 2 m.
The DM model has been validated using independent estimates of ice type from QuikSCAT (e.g., Nghiem et al. 2007) and in situ observations of
ice thickness from submarines, electromagnetic sensors, etc. (e.g., Haas et al. 2008; Rigor 2005).
Over the sea ice field the observations include: sea ice freeboard height and hence sea
ice thickness from radar altimetry; sea ice surface temperature and sea ice drift from respectively infrared radiometer and imaging spectrometer under cloud free conditions.
Scientists from the University of Erlangen - Nuremberg Institute of Geography and from the Laboratoire de Glaciologie et Gophysique de l'Environnement in Grenoble, France, used radar data from satellites such as ESA's Envisat and observations of
ice thickness from airborne surveys in a complex model to demonstrate, for the first time, how the buttressing role of the ice shelves is being compromised as the shelves decline.
Inferring Histories of Accumulation, Ice Flow, and
Ice Thickness from Internal Layers in Ice Sheets.
ICESat - 2 will add to our understanding of Arctic sea ice by measuring sea
ice thickness from space, providing scientists more complete information about the volume of sea ice in the Arctic and Southern oceans.
Not exact matches
The study uses data
from two NASA missions — Operation IceBridge, which measures
ice thickness and gravity
from aircraft, and Oceans Melting Greenland, or OMG, which uses sonar and gravity instruments to map the shape and depth of the seafloor close to the
ice front.
Millan, a UCI graduate student researcher in Earth system science, and his colleagues analyzed 20 major outlet glaciers in southeast Greenland using high - resolution airborne gravity measurements and
ice thickness data
from NASA's Operation IceBridge mission; bathymetry information
from NASA's Oceans Melting Greenland project; and results
from the BedMachine version 3 computer model, developed at UCI.
•
From 1976 to 1999 the average
thickness of
ice in the Arctic Ocean had dropped 43 percent.
«We needed measurements
from an airplane to measure the
thickness of the
ice.
the south - bound expedition had cleared that vast plain of floating
ice which flows down
from the great mountains of the interior and covers the southern part of Ross Sea throughout an area above 20,000 square miles with an
ice sheet approximately 800 feet in
thickness, and had begun to climb the heights which form the mountainous embayment at the head of Ross Sea.
«The
ice shelf generally breaks at points that are between a half and full
thickness of the
ice sheet
from the edge,» summarises Christmann.
After compiling 10 floe - scale maps of the
ice from the Weddell, Bellingshausen, and the Wilkes Land regions of the continent, the researchers found that the sea
ice thickness tended to be highly variable, with many ridges and valleys, they report online today in Nature Geoscience.
Initial interpretations of data
from Cassini flybys of Enceladus estimated that the
thickness of its
ice shell ranged
from 30 to 40 km at the south pole to 60 km at the equator.
Researchers
from Norway and China have collaborated on developing an autonomous buoy with instruments that can more precisely measure the optical properties of Arctic sea
ice while also taking measurements of
ice thickness and temperature.
Ambient geothermal heat emanating up
from the seafloor melts the underside of the
ice sheet at a rate of several penny
thicknesses per year.
The lakes are fed by geothermal heat that seeps up
from the Earth's interior, melting away the bottom of the
ice sheet at a rate of several dime -
thicknesses per year and liberating water
from the
ice.
For their work Maksym and co-investigators Guy Williams
from the University of Hobart, Tasmania and Jeremy Wilkinson of the British Antarctic Survey in Cambridge, UK, used a robot known as an autonomous underwater vehicle (AUV) to cruise under
ice in three regions near the coast and measure the
thickness directly over a much larger area.
Hu's experiments, for example, show everything
from the
thickness of
ice as it flows over a wing, the heat transfer of individual water droplets as they freeze, the irregular speed of freezing droplets on a wing or blade and the finger - like patterns of
ice formation.
While bristling over the personal nature of Greenberg's attack, he insists that he is far
from dogmatic on the issue of
ice thickness.
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.
Ice originating
from the Arctic Ocean showed a mean
thickness of more than three metres on average.
Rising polar temperatures caused the average
thickness of winter Arctic sea
ice to decrease
from about 12 feet to 6 feet between 1978 and 2008, and thinner
ice melts more readily.
Using all available geologic, tectonic and geothermal heat flux data for Greenland — along with geothermal heat flux data
from around the globe — the team deployed a machine learning approach that predicts geothermal heat flux values under the
ice sheet throughout Greenland based on 22 geologic variables such as bedrock topography, crustal
thickness, magnetic anomalies, rock types and proximity to features like trenches, ridges, young rifts, volcanoes and hot spots.
The researchers combined data gathered
from the buoys between 2002 and 2015 with satellite estimates of
ice thickness in this region to better understand changes affecting the Arctic Ocean in recent years.
On Titan, the largest features may be made by changes in the
thickness of its
ice shell due to tidal forces
from Saturn.
Khan and his colleagues combined GNET data with
ice thickness measurements taken by four different satellites: the Airborne Topographic Mapper (ATM), the Ice, Cloud and Land Elevation Satellite (ICESat), and the Land, Vegetation and Ice Sensor (LVIS) from NASA; and the Environmental Satellite (ENVISAT) from the European Space Agen
ice thickness measurements taken by four different satellites: the Airborne Topographic Mapper (ATM), the
Ice, Cloud and Land Elevation Satellite (ICESat), and the Land, Vegetation and Ice Sensor (LVIS) from NASA; and the Environmental Satellite (ENVISAT) from the European Space Agen
Ice, Cloud and Land Elevation Satellite (ICESat), and the Land, Vegetation and
Ice Sensor (LVIS) from NASA; and the Environmental Satellite (ENVISAT) from the European Space Agen
Ice Sensor (LVIS)
from NASA; and the Environmental Satellite (ENVISAT)
from the European Space Agency.
From an altitude of just over 700 km, CryoSat will precisely monitor changes in the
thickness of sea
ice and variations in the
thickness of the
ice sheets on land.
As significant uncertainties about the
thickness of the surface
ice still exist, some planetary scientists have identified two possible mechanisms for how possible volcanic heat can escape to the surface
from Europa's rocky mantle and be carried upward by buoyant oceanic currents.
The following site states German researchers
from the Alfred - Wegener - Institute for Polar and Marine Research found that mean
ice thickness in September 2007 is 1 metre, down by half
from 2001.
One example offered in their paper is typical: On Oct 3, 2015, an NSF / NCAR research aircraft took off
from southern Chile and flew south to measure the
thickness of the Antarctic
ice shelf.
Level 2 data represent geolocated geophysical properties (e.g
ice thickness), derived
from Level 1B measurements (e.g. radar echo delay).
Antarctic
ice shelf
thickness changes calculated
from ICEsat data.
First, we expect the
ice thickness distribution in April 30
from redistribution (divergence / convergence) of sea
ice during December and April, based on the daily
ice velocity data.
Finnish Meteorological Institute has been doing estimates of two essential sea
ice parameters — namely, sea
ice concentration (SIC) and sea
ice thickness (SIT)-- for the Bohai Sea using a combination of a thermodynamic sea
ice model and Earth observation (EO) data
from synthetic aperture radar (SAR) and microwave radiometer.
The
thickness of the remaining, multi-year
ice, along with its geographic location, will make it more difficult to melt than the
ice that was spread across the Arctic, and exposed to Pacific and Atlantic ocean currents, along with runoff
from fresh water rivers.
At FMI algorithms and procedures have been developed for producing daily thin
ice thickness (< 0.5 m) charts for the Arctic in wintertime based on
ice surface temperature which is retrieved
from the thermal infrared data of the MODIS spectrometer.
«He has pioneered the use of AUVs (autonomous underwater vehicles) to measure under -
ice topography and has worked with the Royal Navy since the 1970s in carrying out
ice thickness measurement work
from Navy submarines on Arctic deployments.»
So what we need is detailed topo maps of the bed and
thickness of the GIS, and to work out a map of the «net buoyancy», or some such (i.e. total
ice area density subtracted
from the area density of a hypothetical column of water resting on the bed and extending up to sea level).
Progress towards establishing
ice thickness records
from satellite (ICESat, Envisat, and CryoSat - 2) will change this over time, but these sources won't yield a record before these measurements began and satellite retrievals of
ice thickness have their own issues.
... the confusion came most likely
from a confusion in definitions of what is the permanent
ice sheet, and what are glaciers, with the «glaciers» being either dropped
from the Atlas entirely or colored brown (instead of white)... there is simply no measure — neither
thickness nor areal extent — by which Greenland can be said to have lost 15 % of its
ice.
They have several
ice thickness measurements varying
from just 6 points (1990) to more than dozen.
Miller, P. A., S. W. Laxon, and D. L. Feltham (2007), Consistent and contrasting decadal Arctic sea
ice thickness predictions
from a highly optimized sea
ice model, J. Geophys.