We used the ice thickness in December, ice movement from December to April, and ice concentration in June.
Not exact matches
Icing amounts are very general and will vary with consistency,
thickness applied and tips
used.
Tips and Notes to the crêpe maker: — I
use an
Ice cream scooper to portion the batter, this allow me to have equal
thickness every time.
Frozen bananas are the best with any smoothie because they add that
thickness without
using ice.
Clean Eating Green Smoothie Credit @dashingdish (check out her blog) 2 cups Fresh spinach 1/4 medium Banana 1/4 cup Strawberries, diced (about 3 - 4 berries) 1/2 cup Low fat cottage cheese 1 1/4 cup Vanilla or plain protein powder (I
use Designer Whey, which is 100 calories per scoop) 1 - 3 pkts Packets of stevia or sweetener of choice (or to taste) 5 - 10
Ice cubes (more or less depending on how thick you like it) 1/2 -1 cup Water (again, alter according to desired
thickness of shake) 1 You can not taste the cottage cheese at all, it makes for a creamy protein packed shake!
Use the
ice to adjust the
thickness to your preference.
In Grayslake, the Fire Protection District checks
ice thickness, and the Park District
uses a colored rating system to warn people about conditions.
Use frozen fruit or
ice to help increase smoothie
thickness.
Morris
uses the information she gathers on these trips to check the accuracy of data collected by a European satellite, Cryosat - 2, that tracks changes in the
thickness of polar
ice — information that tells scientists how quickly that
ice is thawing.
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.
The cores, some as long as 100 - feet, were transported to Dartmouth where the research team
used a light table to measure the
thickness and frequency of the
ice layers.
Scientists
used the data to explore Antarctic
ice thickness and the distribution of subglacial lakes.
Although CryoSat - 2 is designed to measure changes in the
ice sheet elevation, these can be translated into horizontal motion at the grounding line
using knowledge of the glacier and sea floor geometry and the Archimedes principle of buoyancy — which relates the
thickness of floating
ice to the height of its surface.
It will
use ice - penetrating radar to measure the
thickness of the moon's
ice shell, map its internal rifts and faults (clues to the tempo of its geologic activity) and locate pockets of water near the surface.
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.
Haas and his team, including Stephen Howell of Environment Canada, measured first - year and multiyear
ice thickness in the Canadian Arctic Archipelago
using an airplane equipped with an electromagnetic induction sounder or EM bird.
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.
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 pro
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 pro
Ice Feeding Arctic Export) campaign, which involved research aircraft
using laser scanners and a towed electromagnetic probe.
We calculate the WD gas age -
ice age difference (Delta age)
using a combination of firn densification modeling,
ice - flow modeling, and a data set of d15N - N2, a proxy for past firn column
thickness.
1994 A method for determining
ice -
thickness change at remote locations
using GPS.
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.
NASA and the USGS have
used MRO instruments to analyze the vertical structure and
thickness of buried
ice sheets, which preserve a detailed record of the Red Planet's past and could provide future human explorers with an easily - accessible water supply.
«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.»
The second is electromagnetic (EM) induction
ice thickness measurements gathered
using a helicopter by the Alfred Wegener Institute in April 2003.
It is argued that uncertainty, differences and errors in sea
ice model forcing sets complicate the
use of models to determine the exact causes of the recently reported decline in Arctic sea
ice thickness, but help in the determination of robust features if the models are tuned appropriately against observations.
Using comprehensive data sets of observations made between 1979 and 2001 of sea
ice thickness, draft, extent, and speeds, we find that it is possible to tune model parameters to give satisfactory agreement with observed data, thereby highlighting the skill of modern sea
ice models, though the parameter values chosen differ according to the model forcing
used.
There is no other reliable method to measure the
thickness of snow than to step on the
ice and
use poles like Marc did.
The steady state average
ice thickness at summer's end
used to be about 3 meters, and is now around half that.
There are two ways to categorize the amount of
ice: by measuring the extent (essentially the area of the ocean covered by
ice, though in detail it's a little more complicated) or
using volume, which includes the
thickness of the
ice.
Canadian
Ice Service, 4.7, Multiple Methods As with CIS contributions in June 2009, 2010, and 2011, the 2012 forecast was derived using a combination of three methods: 1) a qualitative heuristic method based on observed end - of - winter arctic ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT), Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Ice Service, 4.7, Multiple Methods As with CIS contributions in June 2009, 2010, and 2011, the 2012 forecast was derived
using a combination of three methods: 1) a qualitative heuristic method based on observed end - of - winter arctic
ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT), Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT), Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which
uses an optimal linear data filter to extrapolate NSIDC's September Arctic
Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea
ice predicto
ice predictors.
Canadian
Ice Service, 4.7 (+ / - 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method based on observed end - of - winter Arctic ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Ice Service, 4.7 (+ / - 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method based on observed end - of - winter Arctic
ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that
uses an optimal linear data filter to extrapolate the September sea
ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea
ice predicto
ice predictors.
According to the second study, which measured changes in the
thickness and height of
ice using radar and laser altimetry instruments flown as part of NASA's Operation IceBridge campaign, the glacier lost between 984 and 1,607 feet in
thickness from 2002 to 2009.
And the sonar systems on Los Angelos class fast attack submarines, like the one I went under the
ice on, that could measure
ice thickness, were of the active variety, projecting sound and listening to the echos, and were rarely, if ever
used up there.
Corrigendum to «
Using records from submarine, aircraft and satellites to evaluate climate model simulations of Arctic sea
ice thickness» published in The Cryosphere, 8, 1839 - 1854, 2014.
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.
Although CryoSat - 2 is designed to measure changes in the
ice sheet elevation, these can be translated into horizontal motion at the grounding line
using knowledge of the glacier and sea floor geometry and the Archimedes principle of buoyancy — which relates the
thickness of floating
ice to the height of its surface.
Improvements in seasonal forecasting practice arising from recent research include accurate initialization of snow and frozen soil, accounting for observational uncertainty in forecast verification, and sea -
ice thickness initialization
using statistical predictors available in real time.
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).
These were modified from the CFS v2.0 initial conditions by thinning the
ice pack by 60 cm — the
thickness which we
used as a cutoff in making our 2010 SIO estimates.
«
Ice thickness is then calculated
using a combination of the freeboard measurements and estimates of snow depth and density derived from a climatology [Warren et al., 1999]»
Researchers
used data from IceBridge's
ice - penetrating radar — the Multichannel Coherent Radar Depth Sounder, or MCoRDS, which is operated by the Center for Remote Sensing of Ice Sheets at the University of Kansas, Lawrence, Kan. — to determine ice thickness and sub-glacial terrain, and images from satellite sources such as Landsat and Terra to calculate veloci
ice - penetrating radar — the Multichannel Coherent Radar Depth Sounder, or MCoRDS, which is operated by the Center for Remote Sensing of
Ice Sheets at the University of Kansas, Lawrence, Kan. — to determine ice thickness and sub-glacial terrain, and images from satellite sources such as Landsat and Terra to calculate veloci
Ice Sheets at the University of Kansas, Lawrence, Kan. — to determine
ice thickness and sub-glacial terrain, and images from satellite sources such as Landsat and Terra to calculate veloci
ice thickness and sub-glacial terrain, and images from satellite sources such as Landsat and Terra to calculate velocity.
And for years nuclear submarines (Russian, American and British) have been measuring
ice thickness from the bottom,
using their sonar.
That gives you a profile of
ice thickness, and it is straightforward in principle to
use it to calculate the
ice volume — though in practice it remains an awful lot of numbers to crunch.
The new
ice thickness estimates will also be
used to improve on - going seasonal predictions of sea
ice extent.
The ensemble consists of seven members each of which
uses a unique set of NCEP / NCAR atmospheric forcing fields from recent years, representing recent climate, such that ensemble member 1
uses 2005 NCEP / NCAR forcing, member 2
uses 2006 forcing..., and member 7
uses 2011 forcing... In addition, the recently available IceBridge and helicopter - based electromagnetic (HEM)
ice thickness quicklook data are assimilated into the initial 12 - category sea
ice thickness distribution fields in order to improve the initial conditions for the predictions.
To make
use of that potential we would need good estimates of sea
ice thickness, such as might be obtained from ICESat or CryoSat (i.e., complete spatial coverage).
Canadian
Ice Service, 4.7 (± 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method based on observed end - of - winter Arctic ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Ice Service, 4.7 (± 0.2), Heuristic / Statistical (same as June) The 2015 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method based on observed end - of - winter Arctic
ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that uses an optimal linear data filter to extrapolate the September sea ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
ice thickness extents, as well as winter Surface Air Temperature, Sea Level Pressure and vector wind anomaly patterns and trends; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that
uses an optimal linear data filter to extrapolate the September sea
ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
ice extent timeseries into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea
ice predicto
ice predictors.
Ice - ocean model simulations, on the other hand, have requirements with respect to data density and quality, e.g., for observed ice thickness fields used in initialization of model runs, that are currently not being met by existing data sources (with the exception of, e.g., satellite - observed ice concentration field
Ice - ocean model simulations, on the other hand, have requirements with respect to data density and quality, e.g., for observed
ice thickness fields used in initialization of model runs, that are currently not being met by existing data sources (with the exception of, e.g., satellite - observed ice concentration field
ice thickness fields
used in initialization of model runs, that are currently not being met by existing data sources (with the exception of, e.g., satellite - observed
ice concentration field
ice concentration fields).
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.