Sentences with phrase «more ice volume»

That is lower land temperatures are followed by more ice volume several months later.

Not exact matches

For a thicker shake, you can toss in more ice cubes; you'll add volume without the calories.

Ice cream prices have risen by more than a quarter over the past five years and sales volumes have declined, but most Europeans still consider ice cream an affordable treat, according to new research from MintIce cream prices have risen by more than a quarter over the past five years and sales volumes have declined, but most Europeans still consider ice cream an affordable treat, according to new research from Mintice cream an affordable treat, according to new research from Mintel.

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The fifth and sixth planets, both in the habitable zone, are more than half water — a volume so large that the water pressure alone could force much of it into a form of ice, Unterborn says.

The thickness of the ice, and its overall volume, may be a more important measure of what is happening in the Arctic over the long term, even though it is not as simple to measure, said Overland.

The volume of ice divergence has doubled since 2000 due to a more mobile ice cover as multiyear ice has declined, which can explain the drastic ice reduction in the Arctic Ocean in recent years.

With a volume of more than 700,000 cubic miles and an average thickness of 4,000 feet, the West Antarctic Ice Sheet (WAIS) holds enough water to raise sea levels by 15 to 20 feet — and it is already sweating off 130 billion tons of ice per yeIce Sheet (WAIS) holds enough water to raise sea levels by 15 to 20 feet — and it is already sweating off 130 billion tons of ice per yeice per year.

A 2013 computer simulation of this process found increased aerosols alone did result in more lightning due to ice crystal collisions, although at very large aerosol volumes the effect was muted.

What is alarming is that the volume of water and the extent and rapidity of its movement is suprisingly much greater than previously believed, and that a possible, perhaps likely, effect of this on ice sheet dynamics is to make the ice sheets less stable and more likely to respond more quickly to global warming than previously expected.

Greenland's ice sheet melted nearly 19 billion tons more than the previous high mark, and the volume of Arctic sea ice at summer's end was half what it was just four years ago, according to new NASA satellite data obtained by the Associated Press (AP).

«Conversely, there is more and better evidence across Iceland that when the ice sheet underwent major reduction at the end of the last glacial period, there was a large increase in both the frequency and volume of basalt erupted — with some estimates being 30 times higher than the present day.

These significant depths suggest that Ceres» subsurface is no more than 40 percent ice by volume, and the rest may be a mixture of rock and low - density materials such as salts or chemical compounds called clathrates.

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.

The volume of sea ice left at the end of the summer melt season seems to vary more from year to year than had perhaps been previously appreciated; after declining for several years, sea ice volume shot up after the unusually cool summer of 2013, the data revealed.

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- a lot of focus was put on sound effects in order to immerse players in the world of Hyrule - the development team worked with Sound Racer, a studio specialized in sound effects - this studio also worked on Xenoblade Chronicles X - they recorded more than 10 000 different sounds for the game - the team used a school bag to simulate the sound of rubbing leather - for the sound of «normal» footsteps, they mixed various kinds of sands - for the sounds of equipment, they had to search for various materials and find ways to use them - they used an actual block of ice to recreate the sound of footsteps on ice - with the ice block, it always ended up melting, or getting cracks when the staff had to walk on it - Link's footsteps were made by a woman - depending on Link's actions and the equipment he's using / wearing, the recorded sounds were separated out individually - the volume is changed as needed to make a particular sound stand out - check out sound effect samples here

By these circles getting smaller, you see overall that the ice volume is shrinking, but you also see the seasonal differences with September values decreasing more than the winter values.»

Considering ice volumes over the last decade, CCSM4 AR4 is predicting a decline of some 200 cu km pa while PIOMAS models suggest something more like 600 cu km pa.

In contrast, the much more expansive ice volume maxima (equivalently, sea level minima) during a glacial maximum is more defined.

It must be pointed out that the ice has been thinning more appreciatively in west Greenland of late and that ice sheet melting can only contribute a moderate amount of freshwater volume each year.

So whilst the ice is more mobile because it's thinner, the fact that it's thinner means less volume is transported, the two factors balancing to give no increase in volume transport.

I wish you would say that in the beginning, because Ice takes up more volume than water.

Since the volume of ice at risk under BAU is within a factor of two of the volume of ice at risk during a deglaciation under orbital forcing, while the forcing is much more rapidly applied under BAU, looking at sea level rise rates in the paleo - record might actually be considered a search for lower limits on what to expect if reticence did not run so strongly in our approach.

Arctic sea ice has been shrinking more rapidly, falling to its lowest volume and second lowest area on record during the 2011 summer melt season.

Another possibility might be a slowing of deep circulation (not sure how much there is, mind), in which case the opposite occurs, and the surface waters heat up even faster, leading to yet more rapid surface melt, smaller winter ice volumes and so on.

Volume, in contrast, is crucial in determining the vulnerability of Arctic sea ice to rapid future reductions (since thin ice is much more prone to react strongly to a single warm summer, making single very - low sea - ice summers more likely), and the thickness of the ice determines the exchange of heat between ocean and atmosphere.

This suggests that summer ice volume is more sensitive to AW than summer ice extent»

The buttresses of ice frozen around Antarctica's edges, hundreds of meters thick in many cases, are also in the sea, but they can act like doorstops and — once moved out of the way — can allow huge volumes of ice on the continent (in theory) to move toward the sea more easily.

A fingerprinting study of the ocean data, compared to GHG / aerosols, ice volumes, solar variance and volcanic influences may give some more insight...

So, I was curious about your recent paper and whether there was any discussion of changes in the THC poleward of the GIS shelf vs the data from the RAPID program line located at 26.5 N. With the decline in minimum extent and volume of sea - ice, one might expect to see more THC sinking into the Arctic Ocean, with consequences for both climate and weather.

If you're not refuting the volume analysis, then I can't see how you can say focusing on ice volume is «a bit funky» — it's clearly a more important measure of the system's ability to recover, which is the central point of this post.

The main issue is that sea ice is fresher than sea water (has less salt), and since salty water is more dense (1028 kg / m3) than fresher water (1004 kg / m3 for 5 psu), the volume of sea water displaced by the ice is slightly less than the volume of the ice if it melted.

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.

That this year's record low is happening three weeks earlier than previous lows means that the 2012 ice extent and volume will continue to decrease even more until sea ice begins to regrow again in early fall.

Moreover, beneath the surface, ice volume is dropping even more precipitously.

As to sea level rise due to displacement of mantle, because rock is denser than ice, more water must be drawn from the sea to displace the mantle than the volume of the mantle displaced.

Glacial periods during the 100,000 - year cycles have been characterised by a very slow build - up of ice which took thousands of years, the result of ice volume responding to orbital change far more slowly than the ocean temperatures reacted.

The resulting picture shows that ice volume has changed much more dramatically than ocean temperatures in response to changes in orbital geometry.

BC Building Code box ice, on right, lost about 40 per cent more volume during Ice Box Challenge than the Passive House box iice, on right, lost about 40 per cent more volume during Ice Box Challenge than the Passive House box iIce Box Challenge than the Passive House box iceice.

Still more striking, and significant, has been a severe decline in the average thickness of the ice pack, and thus of its volume (graph).

Ice volume data paints a picture even more dire: the Arctic has actually lost not one third but two thirds of September sea iIce volume data paints a picture even more dire: the Arctic has actually lost not one third but two thirds of September sea iceice.

In that case it is important to have a more precise statement, so I went back to check the reference Journal of Marine Systems Volume 48, Issues 1 - 4, July 2004, Pages 133 - 157 Sea ice from the Kara Sea region reaches Fram Strait from 2 to 4 years (min 2 years) on average, and while sea ice from the Laptev Sea takes roughly 4 — 6 years (min 3 years) to reach Fram Strait»... from the East Siberian, Chukchi and Beaufort seas within 6 — 10 years.

I find it interesting to see that the HOC is increasing the strongest around antartica in the deep while the see ice area (not volume) shows slight increase and surface temperature is more or less constant.

The number of cryospheric elements now routinely monitored from space is growing, and current satellites are now addressing one of the more challenging elements, variability of ice volume.

It snows more until the ice volume is enough to cause the ice to spread out and make it colder.

It can be more reliably estimated than ice volume and ice mass.

More on that in due course, but first let's take a look at the PIOMAS volume graph at the end of November, courtesy of the wondrous Wipneus on the Arctic Sea Ice Forum:

For example Arctic Sea Ice volume and extent has not dramatically declined this year as compared to the last few more recent years.

Given the estimated trend and the volume estimate for October — November of 2007 at less than 9,000 km3, one can project that at this rate it would take only 9 more years or until 2016 + / -3 years to reach a nearly ice - free Arctic Ocean in summer.