So for the whole history of time, we have three data points over 4 years
for ice depth on Mt. Blanc.
Not exact matches
Sub it in any recipe that calls
for melted butter to add
depth of flavor, or fold it into our
ice cream, along with some pecans.
Even when the thermometer plunged to 5 degrees in York City a few weeks ago, I walked to Cafe Grumpy, my local joint in Chelsea, and ordered an
iced redeye (
iced coffee with a shot of espresso; I like the espresso less
for its caffeine kick and more
for the nuttiness and
depth of flavor it imparts).
In surrendering top - line winger Jan Hlavac, solid defenseman Kim Johnsson and touted right wing prospect Pavel Brendl
for Lindros, Sather weakened his
depth on the
ice and at the trade table.
If you're looking
for the best
depth finder
for kayaks, canoes, or even
ice fishing, the Garmin Striker Fish Finder is it.
Besides its impressive
depth capabilities, the Striker 4 also has a flasher format option ideal
for ice fishing and vertical jigging.
Having NeMO outfitted with powerful synthetic aperture radar would enable it to spot
ice at
depth and help plan tapping that resource
for use by future Mars crews, he explains.
One such
ice core, known as the West Antarctic Ice Sheet Divide (WAIS Divide) core was drilled to a depth of more than two miles (3,405 meters), and much of it was analyzed in the DRI Ultra-Trace Laboratory for more than 30 different elements and chemical speci
ice core, known as the West Antarctic
Ice Sheet Divide (WAIS Divide) core was drilled to a depth of more than two miles (3,405 meters), and much of it was analyzed in the DRI Ultra-Trace Laboratory for more than 30 different elements and chemical speci
Ice Sheet Divide (WAIS Divide) core was drilled to a
depth of more than two miles (3,405 meters), and much of it was analyzed in the DRI Ultra-Trace Laboratory
for more than 30 different elements and chemical species.
The torpedo will travel under the
ice at a
depth of 15 metres
for a distance of about 10 kilometres.
It's an «excellent preliminary study,» that could help mission controllers zero in on landing sites
for future missions that feature, say, surface
ice of sufficient
depth, says astrobiologist Andrew Steele of the Carnegie Institution in Washington, D.C..
I propose to advance the search
for life on Mars by approaching the microbiology of ground
ice in the Antarctic Dry Valleys as an analogue to ground
ice on Mars, and by introducing a new mission concept
for the robotic exploration of Mars that would allow to drill to a
depth of several meters and search
for life in ground
ice.
Predicted age -
depth scales
for Siple Dome and Inland WAIS
ice cores in West Antarctica, Geophysical Research Letters, 23, 22, 3163 — 3166
Either way, the research hints at a basin
depth far larger than the 500 m (1,640 ft) minimum
ice depth needed
for the convection process to occur.
As a general matter, yes, but AIUI the increasing height (
depth) of the
ice face is the key factor
for accelerating retreat of these glaciers since it creates more surface area
for the warm water to work on.
master bedroom design
for small space sometimes it can seem counter intuitive but going dark can create
depth in a space a symmetrical look by the bed is just
icing on the cake masters bedroom design.
Skoda are also pushing more «Simply Clever» additions like an
ice scraper located in the fuel filler flap which now acts as a tyre tread
depth gauge too, USB ports
for the back seats and a double sided boot mat.
The ship is purpose built as an expedition vessel with a higher
ice - class, chart drawing tools, ship
depth sounding database, extractable forward sounding sonar, iceberg search lights, autonomous tracking system, oversized oil retention system
for self - sufficiency, and a full «expedition tools - deck» equivalent to a car - deck that holds 25 vehicles.
Look
for Azamara's first voyage to Peru with an overnight experience to Machu Picchu; Iceland with its fire - and -
ice attractions; and in -
depth exploring of smaller Greek isles.
Take,
for instance, an early example where Saltire is in full battle with a Roman champion; amidst the flat battlefield Saltire is kicked and suddenly finds himself on frozen - over water before the
ice gives way and Saltire plunges into the
depth.
Installation view, Walden, revisited, featuring Spencer Finch, Walden Pond (surface /
depth), 2013; David Brooks, Myopic Wall Composition (w / chainsaw - cut wood found in historic Walden Woods), 2014; Jane D. Marsching with Sarah Baumert, If Wind Now, 2011; Jane D. Marsching,
Ice Out at Walden, 2010; and Deb Todd Wheeler, Searching
for Imposters, 2014.
When the summit core was first drilled in 1976, the chemical composition of the
ice showed well - preserved annual layering throughout its
depth, accounting
for a time span of 1500 years.
At the summit,
for example, the mean annual T is about -30 C, and the temperature is quite constant to a
depth of 1500 m or more, due to advection of cold
ice downwards.
However, heat store in the Atlantic Layer (temperature maxima at ~ 300 m) and in waters of Pacific origin (maxima at ~ 50 m
depth in the western Arctic) are prime candidates
for releasing heat to the underside of the Arctic
ice.
Significant contribution of insolation to Eemian melting of the Greenland
ice sheet
for an in -
depth discussion about these differences.
The team, which Marc led and provided the logistical support
for, deployed from Resolute to Nord Greenland before setting up a rustic field camp on the sea
ice for six days, during which time we mechanically drilled the
ice to measure thickness, measuring snow
depth in a grid pattern along the flight lines as well as dragging instruments along the surface that produced the same measurements
for comparison to the airborne data.
So the north polar sea
ice has been steadily thinning in
depth and shrinking in area
for more than 30 years.
Measuring the distance apart and speed of 2 satellites in space orbiting the earth to the width of a human hair with no margin
for error [damn those drift recalculations], and taking into account unknown factors with respect to the true values
for water
depth, water weight at different salt concentrations,
ice depth magma flows, volcanic activity etc [ie making a lot of guesses], plus taking human motivation on board [like CO2 increase must melt
ice surely] can give you an accurate measurement of the volume
ice in Antarctica.
Can anyone point me to literature about how we know that everything in the
ice core keeps the same relative
depth, or if it is known not to, how measurements are adjusted to acount
for differential drift?
Studies show that taking the full ocean
depth,
ice melt, and other factors into account, Earth is estimated to have gained 0.40 ± 0.09 W m − 2 since 1960 and 0.72 W m − 2 since 1992 [Cheng et al., 2017]-- 18 % higher than
for the top 2,000 - meter OHC alone.
Furthermore we recommend that effort should be put into developing an inter-annually varying snow
depth and density over sea
ice product
for the
ice - covered oceans.
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.
The Antarctic
ice sheet reached the coastline
for the first time at ca. 33.6 Ma and became a driver of Antarctic circulation, which in turn affected global climate, causing increased latitudinal thermal gradients and a «spinning up» of the oceans that resulted in: (1) increased thermohaline circulation and erosional pulses of Northern Component Water and Antarctic Bottom Water; (2) increased deep - basin ventilation, which caused a decrease in oceanic residence time, a decrease in deep - ocean acidity, and a deepening of the calcite compensation
depth (CCD); and (3) increased diatom diversity due to intensified upwelling.
A post-season report will provide an in -
depth analysis of factors driving sea
ice this summer as well as explore the scientific methods
for predicting seasonal conditions.
Onshore measurements had to be used as a proxy
for on -
ice snow
depth, since there are no data
for snow
depth over sea
ice on Hudson Bay.
Large regions of the seabed around the Greenland and Antarctic
ice sheets are undersampled
for water
depth, including most regions under
ice shelves.
See also the Sea Surface Temperature Anomalies,
Ice and Snow Cover, 1 year animation, from Environment Canada,
for snow
depth records over the last 365 days that include Hudson Bay.
There are important implications of this poor record of snow
depth observations over sea
ice for predicting future conditions.
Bosse (Citizen Scientist / Public), 4.1 (± 0.43), Statistical (Same as June) Just as in the two years before I calculate the value
for the September - minimum of the arctic sea
ice extent of the year n (NSIDC monthly mean
for September) from the Ocean Heat Content (0... 700m
depth) northward 65 ° N during JJAS of the year n - 1.
A post-season report provides an in -
depth analysis of factors driving sea
ice extent this summer as well as explore the scientific methods
for predicting seasonal
ice extent.
Over that time, the globally averaged temperature difference between the
depth of an
ice age and a warm interglacial period was 4 to 6 °C — comparable to that predicted
for the coming century due to anthropogenic global warming under the fossil - fuel - intensive, business - as - usual scenario.
-- Migration of CO2 through the
ice core: in «hot» -LRB--23 degr.C)
ice cores: a broadening of the resolution with 10 % to 100 % at
depth, that means that the resolution is 22 years to 40 years instead of 20 years
for the Siple Dome
ice core.
At 72 meter
depth (
for the Law Dome
ice cores) the CO2 level in average still is only 7 years older than the air at the surface.
A post-season report will provide an in -
depth analysis of factors driving sea
ice extent this summer as well as explore the scientific methods
for predicting seasonal
ice extent.
To make it clear: nobody ever has «but» the
ice core data and atmospheric data together, without counting the layers
for ice (which is the age at closing
depth) and the CO2 level changes in firn (which give a nice trend from atmospheric to closing
depth).
For the Law Dome
ice cores, that is at 72 m
depth, where the
ice is closing, but still has open bubbles.