Sentences with phrase «much ice means»

Since they can only hunt in water, too much ice means they head for human settlements.

Not exact matches

As for the cancer, 25 years and one month ago I ate a cherry ice cream cone at the same time your church prayed so that means my cone eating stopped the cancer as much as your prayer..

Or if it really means that much to you throw a scoop of vegan ice cream in there, it certainly can't hurt.

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They are lovely tasting treat, but much healthier than reaching for a bag of factory made chocolate cookies with icing in the middle — you know the ones I mean.

Because roasting the strawberries means you end up with a good bit of liquid (and because I didn't want to dilute the strawberry flavor too much) I decided not to add any additional water to mine, but to blend in a bunch of ice instead.

Which means I want to eat ice cream pretty much all the time (TheBetterhalf: How is this different from winter?).

I mean, I love ice cream, but there's only so much this tummy can take.

Kids would be getting the calcium we're so worried about (so much so that we serve artificially colored and flavored milk with as much sugar as a serving of ice cream) and presumably the higher calorie count would mean we don't need to serve the empty - calorie chocolate chip cake anymore.

«The fact that a large portion of the western flank of the Greenland ice sheet has become dark means that the melt is up to five times as much as if it was a brilliant snow surface.»

However, the discovery in 2015 of an oscillation in Enceladus's rotation known as a libration, which is linked to tidal effects, suggests that it has a global ocean and a much thinner ice shell than predicted, with a mean thickness of around 20 km.

Then at peak demand times, the ice or cold water is used to cool air for large office or industrial buildings, meaning they need much less power from the grid.

As global warming affects the earth and ocean, the retreat of the sea ice means there won't be as much cold, dense water, generated through a process known as oceanic convection, created to flow south and feed the Gulf Stream.

Many researchers think this is unrealistic and that the rate of ice loss will accelerate, which means that sea level could rise much faster than predicted.

Their findings indicated that twice as much soot was deposited on snow in winter compared with summer, meaning that the sunlight - absorbing soot likely caused greater melting of the Arctic ice cap during the winter.

The global mean temperature rise of less than 1 degree C in the past century does not seem like much, but it is associated with a winter temperature rise of 3 to 4 degrees C over most of the Arctic in the past 20 years, unprecedented loss of ice from all the tropical glaciers, a decrease of 15 to 20 % in late summer sea ice extent, rising sealevel, and a host of other measured signs of anomalous and rapid climate change.

It seems about 500 ppm CO2 could eventually mean an ice free planet, much lower than the circa 1000 ppm that ice sheet models seem to estimate.

There is so much ice there, just one glacier like the Totten glacier can raise global mean sea level by over one meter.

That means it's really high in salt and having one of these bagels has as much fat as having not one, but three scoops of Breyers Strawberry Ice Cream.

In your review of last year's Ice Age: Continental Drift, you said this about John Powell's style: «While it was easy to get invigorated by the sheer enthusiasm of it all back in 1998, having heard pretty much the same bag of tricks so many times over now means it's pretty hard to get the motivation to listen to any of them.»

The name John Curry won't mean much to anyone under 40, but in the 1970s he revolutionised ice - skating with a sublime infusion of artistry and balletic grace.

For three particular mismatches — sea ice loss rates being much too low in CMIP3, tropical MSU - TMT rising too fast in CMIP5, or the ensemble mean global mean temperatures diverging from HadCRUT4 — it is likely that there are multiple sources of these mismatches across all three categories described above.

Given that impacts don't scale linearly — that's true both because of the statistics of normal distributions, which imply that (damaging) extremes become much more frequent with small shifts in the mean, and because significant breakpoints such as melting points for sea ice, wet - bulb temperatures too high for human survival, and heat tolerance for the most significant human food crops are all «in play» — the model forecasts using reasonable emissions inputs ought to be more than enough for anyone using sensible risk analysis to know that we making very bad choices right now.

I am much less sure that the divergence between the PIOMAS ice volume and the CCSM4 ensemble mean (after shift) has anything to say about the whether CCSM4 is deficient or not.

It seems about 500 ppm CO2 could eventually mean an ice free planet, much lower than the circa 1000 ppm that ice sheet models seem to estimate.

In this regard, I would observe that at least one important AGW effect, rising sea level, does not depend on a specific regional outcome so much as on global mean T. (At least, I think this is so (because my understanding is that most of the rise comes from lower density of warmer water, not from melting ice sheets — though again, not 100 % sure on this point)-RRB-.

The base of the 3000 - m thick West Antarctic Ice Sheet (WAIS)-- unlike the much larger East Antarctic Ice Sheet — lies below sea level, and it has been recognized for a long time that this means it has the potential to change very rapidly.

But does that mean the public should doubt recent science concluding that the remarkable sea - ice retreat of 2007, which turned about half of the Arctic Ocean into an open blue sea, is unique in at least a century, and probably much longer?

That means that the ice is at an altitude of over ten thousand feet where the temperature is much cooler than a mere six or so feet as in the north.

«Because of its reflectivity, Arctic sea ice is a critical cooling component of the earth's climate system; its loss will mean a much hotter world,» added Mr. Pomerance.

Since its inception 8 years ago, the NCAR / CU sea ice pool has easily rivaled much more sophisticated efforts based on statistical methods and physical models to predict the September monthly mean Arctic sea ice extent (e.g. see appendix of Stroeve et al. 2014 in GRL doi: 10.1002 / 2014GL059388; Witness the Arctic article by Hamilton et al. 2014 http://www.arcus.org/witness-the-arctic/2014/2/article/21066).

That may not sound like much, but the temperature difference between today's world and the last ice age was about 5C, so seemingly small changes in temperature can mean big differences for the Earth.

For most of the 2000s, satellite data shows the glaciers lost about as much ice as they gained, meaning they stayed roughly stable.

The effects of ice melt on ocean circulation were not included in the latest assessment by the United Nations» Intergovernmental Panel on Climate Change (IPCC), meaning Hansen's predictions would occur much earlier and be less gradual than envisioned in the consensus reports of the IPCC.

This means that it does not matter to polar bears how much area the Arctic Basin ice covers in September — for their needs, 1.0 mkm2 would be plenty.

The fact that a great deal of the melt in Arctic sea ice is affected by the accumulating heat in the oceans and the fact that energy is advected to the Arctic via the oceans in much larger amounts than via the atmosphere and the extreme loss we've seen in Arctic sea ice volume as a result means nothing to the «skeptics».

''... the world today is on the verge of a level of global warming for which the equilibrium surface air temperature response on the ice sheets will exceed the global mean temperature increase by much more than a factor of two.»

You wrote - «The fact that a great deal of the melt in Arctic sea ice is affected by the accumulating heat in the oceans and the fact that energy is advected to the Arctic via the oceans in much larger amounts than via the atmosphere and the extreme loss we've seen in Arctic sea ice volume as a result means nothing to the «skeptics».»

This means ice thickness and volume won't drop as much (that's a guess, I haven't modeled it).

We meant human - caused climate change as that's the pernicious kind (it's too bad we can't ask our ancestors how much they liked the very natural ice age).

«If the area becomes warmer that means that the ice doesn't have as much time to grow.

Your mistake means you're pretty much illiterate on the subject of ice ages.

Melting polar ice, rising sea levels, floods, droughts and hurricanes are all in there — even though these are largely contradicted not just by the actual evidence, but even by the much more cautious contents of the vast technical reports they were meant to be «synthesising».

In past decades, winter meant thick, years - old pack ice would extend over much of the Arctic Ocean.

Dr Cook says: «We considered that a lake was dangerous if there were settlements or infrastructure down - valley from the lake, and if the slopes and glaciers around the lake were very steep, meaning that they could shed ice or snow or rock into the lake, which would cause it to overtop and generate a flood — a bit like jumping into a swimming pool, but on a much bigger scale.

The wide range of studies conducted with the ISCCP datasets and the changing environment for accessing datasets over the Internet suggested the need for the Web site to provide: 1) a larger variety of information about the project and its data products for a much wider variety of users [e.g., people who may not use a particular ISCCP data product but could use some ancillary information (such as the map grid definition, topography, snow and ice cover)-RSB-; 2) more information about the main data products in several different forms (e.g., illustrations of the cloud analysis method) and more flexible access to the full documentation; 3) access to more data summaries and diagnostic statistics to illustrate research possibilities for students, for classroom use by educators, or for users with «simple» climatology questions (e.g., annual and seasonal means); and 4) direct access to the complete data products (e.g., the whole monthly mean cloud dataset is now available online).

Losing land ice means sea levels will rise, and if we lose a lot of ice in Greenland and Antarctica — which we are very much on track for doing — sea levels could rise several meters.

But the Greenland ice sheet temperature record shows a similar trend over the glacial - interglacial transition, be it with much larger swings, as that mainly reflects the North Atlantic seawater temperature: http://www.climatedata.info/Proxy/Proxy/icecores.html That means that the CO2 - temperature ratio is probably less than 15 ppmv / °C.

And in modern times, the Bering Sea maintains a layer of sea ice from about November to May every year, meaning that today's SSTs are sub-zero for much of the year in this region.

Physically, Hansen's findings mean that Earth's ice is melting and its seas are rising much faster than expected.