Find the flavor that satisfies your sweet tooth at Freds Water Ice, a lovely ice cream shop in the Philadelphia region of Philadelphia. Children are more than welcome to dine at this ice cream shop, where theres something for everyone on the menu. Wanna soak up the sun? Come grab a bite at Freds Water Ice and sit out on their gorgeous patio.Save your formal dress for another occasion ? a nice top is the perfect fit for Freds Water Ices business casual code. For those in a hurry, the ice cream shop lets you take your grub to go.You can leave your car curbside with nearby street parking. Freds Water Ice offers parking for all diners, including those who travel by bike.Treat yourself to an affordable meal at Freds Water Ice and save some cash for another day. Dont leave the dollar bills at home ? youll need cash at Freds Water Ice. When you need something to cool you off, pay Freds Water Ice a visit and treat yourself to some tasty ice cream.

References. Arbuckle, W.S., 1986. Ice Cream (4th ed). New York: Van Nostrand Reinhold.. Belitz, H.D., Grosch, W., & Schieberle, P., 2009. Food Chemistry (4th ed). Berlin: Springer.. Ben-Yoseph E, Hartel RW. 1998. Computer simulation of ice recrystallization in ice cream during storage. J Food Eng 38(3):309-29.. Cook, K. L. K., & Hartel, R. W. 2010. Mechanisms of Ice Crystallisation in Ice Cream Production. Comprehensive Reviews in Food Science and Food Safety. 9 (2).. Damodaran, S., (1996) Functional properties. In: Nakai, S., Modler, H.W. (Eds.), Food Proteins - Properties and Characterization. VCH Publisher, New York, pp. 167-234.. Donhowe, D. P., Hartel R. W., and Bradley R.L., 1991. Determination of ice crystal size distributions in frozen desserts. J. Dairy Sci. 74.. Donhowe, D. P. (1993) Ice Recrystallization in Ice Cream and Ice Milk. PhD thesis, University of Wisconsm-Madison.. Donhowe, D. P., and R. W. Hartel. 1996. Recrystallization of ice in ice cream during controlled accelerated ...

Ice-nucleating particles (INPs), which are precursors for ice formation in clouds, can alter the microphysical and optical properties of clouds, thereby impacting the cloud lifetimes and hydrological cycles. However, the mechanisms with which these INPs nucleate ice when exposed to different atmospheric conditions are still unclear for some particles. Recently, some INPs with pores or permanent surface defects of regular or irregular geometries have been reported to initiate ice formation at cirrus temperatures via the liquid phase in a two-step process, involving the condensation and freezing of supercooled water inside these pores. This mechanism has therefore been labelled pore condensation and freezing (PCF). The PCF mechanism allows formation and stabilization of ice germs in the particle without the formation of macroscopic ice. Coal fly ash (CFA) aerosol particles are known to nucleate ice in the immersion freezing mode and may play a significant role in cloud formation. In our current ...

Antifreeze proteins (AFPs) enhance the survival of organisms inhabiting cold environments by affecting the formation and/or structure of ice. We report the crystal structure of the first multi-domain AFP that has been characterized. The two ice binding domains are structurally similar. Each consists of an irregular β-helix with a triangular cross-section and a long α-helix that runs parallel on one side of the β-helix. Both domains are stabilized by hydrophobic interactions. A flat plane on the same face of each domains β-helix was identified as the ice binding site. Mutating any of the smaller residues on the ice binding site to bulkier ones decreased the antifreeze activity. The bulky side chain of Leu174 in domain A sterically hinders the binding of water molecules to the protein backbone, partially explaining why antifreeze activity by domain A is inferior to that of domain B. Our data provide a molecular basis for understanding differences in antifreeze activity between the two domains of this

Antifreeze proteins (AFPs) are a unique class of proteins that bind to growing ice crystal surfaces and arrest further ice growth. AFPs have gained a large interest for their use in antifreeze formulations for water-based materials, such as foods, waterborne paints, and organ transplants. Instead of commonly used colligative antifreezes such as salts and alcohols, the advantage of using AFPs as an additive is that they do not alter the physicochemical properties of the water-based material. Here, we report the first comprehensive evaluation of thermal hysteresis (TH) and ice recrystallization inhibition (IRI) activity of all major classes of AFPs using cryoscopy, sonocrystallization, and recrystallization assays. The results show that TH activities determined by cryoscopy and sonocrystallization differ markedly, and that TH and IRI activities are not correlated. The absence of a distinct correlation in antifreeze activity points to a mechanistic difference in ice growth inhibition by the ...

Everybody knows that sliding on ice or snow, is much easier than sliding on most other surfaces. But why is the ice surface slippery? This question has engaged scientists for more than a century and continues to be subject of debate. Researchers from AMOLF, the University of Amsterdam and the Max Planck Institute for Polymer Research (MPI-P) in Mainz, have now shown that the slipperiness of ice is a consequence of the ease with which the topmost water molecules can roll over the ice surface.. Winter sports such as skiing, speed skating, figure skating, and curling require the slippery surfaces of ice and snow. While the fact that the ice surface is slippery is widely acknowledged, it is far from being completely understood. In 1886 John Joly, an Irish physicist, offered the first scientific explanation for low friction on ice; when an object - i.e. an ice skate - touches the ice surface the local contact pressure is so high that the ice melts thereby creating a liquid water layer that lubricates ...

Understanding the causes of recent catastrophic ice shelf disintegrations is a crucial step towards improving coupled models of the Antarctic Ice Sheet and predicting its future state and contribution to sea-level rise. An overlooked climate-related causal factor is regional sea ice loss. Here we show that for the disintegration events observed (the collapse of the Larsen A and B and Wilkins ice shelves), the increased seasonal absence of a protective sea ice buffer enabled increased flexure of vulnerable outer ice shelf margins by ocean swells that probably weakened them to the point of calving. This outer-margin calving triggered wider-scale disintegration of ice shelves compromised by multiple factors in preceding years, with key prerequisites being extensive flooding and outer-margin fracturing. Wave-induced flexure is particularly effective in outermost ice shelf regions thinned by bottom crevassing. Our analysis of satellite and ocean-wave data and modelling of combined ice shelf, sea ice and wave

TY - JOUR. T1 - Inhibition of Gas Hydrate Nucleation and Growth: Efficacy of an Antifreeze Protein from the Longhorn BeetleRhagium mordax. AU - Perfeldt, Christine Malmos. AU - Chua, Pei Cheng. AU - Daraboina, Nagu. AU - Friis, Dennis. AU - Kristiansen, Erlend. AU - Ramløv, Hans. AU - Woodley, John. AU - Kelland, Malcolm A.. AU - von Solms, Nicolas. PY - 2014. Y1 - 2014. N2 - Antifreeze proteins (AFPs) are characterized by their ability to protect organisms from subfreezing temperatures by preventing tiny ice crystals in solution from growing as the solution is cooled below its freezing temperature. This inhibition of ice growth is called antifreeze activity, and in particular, certain insect AFPs show very high antifreeze activity. Recent studies have shown AFPs to be promising candidates as green and environmentally benign inhibitors for gas hydrate formation. Here we show that an insect antifreeze protein from the longhorn beetle, Rhagium mordax (RmAFP1), the most potent protein yet found ...

The researchers were tipped off to this mechanism by the massive amount of meltwater they observed on the ice sheets surface during their summer field campaigns, and they wondered if it was affecting the ice sheet. During the last several decades, atmospheric warming above the Greenland Ice Sheet has caused an expanding area of the surface to melt during the summer, creating pools of water that gush down cracks in the ice. The meltwater eventually funnels to the interior and bed of the ice sheet.. As the meltwater drains through the ice, it carries with it heat from the sun.. The sun melts ice into water at the surface, and that water then flows into the ice sheet carrying a tremendous amount of latent energy, said William Colgan, a coauthor and CIRES adjunct research associate. The latent energy then heats the ice.. The new model shows that this speeds up ice flow in two major ways: One, the retained meltwater warms the bed of the ice sheet and preconditions it to accommodate a basal water ...

Ah, but thats the thing, isnt it? It was just Ice Girl and Ice Friend at 6 a.m. ice the morning I brought the Ice Halo and my camera (BTW, cool time-lapse photos, hey?). Ice Girl is 15 and shes deeply aware of how small movements and deviations from the standard high school teen wardrobe can affect her social status for the day. I couldnt get her to wear the Ice Halo at any session but her Wednesday 6 a.m. session where she and Ice Friend share the ice with no one else. I asked the girls about the product. They both liked it; although Ice Girl tugged and pulled at it way more than Ice Friend did. However, when I asked the girls if they would wear it at a practice with other skaters and they both just smiled awkwardly and said no.. Thats the problem, isnt it? This is a great product, but I know Ice Girl would never wear it. Shes not the trail-blazing type. Shes not the kind of kid who looks at the scientific evidence and says, Yep, Ill wear that. Ice Friend said that she probably wouldnt wear it, ...

You may be seeing ice fisherman on parts of Pawtuckaway Lake, but there is still a lot of open water, and that could spell danger for anyone venturing out. Please never go on the ice alone, and always check the thickness before you step on it. Remember, ice thickness can vary from location to location, so always keep checking! The graphic above has rough minimum measurements you should consult before doing so. However, the U.S. Army Cold Regions Research & Engineering Laboratory in Hanover, NH, offers a rule of thumb on ice thickness: There should be a minimum of six inches of hard ice before individual foot travel, and eight to ten inches of hard ice for snow machine or All-Terrain Vehicle travel. Temperatures this season have varied wildly, with snow, rain, thawing and freezing weather creating dangerous conditions on the ice. Ice can be thick, but not strong, because of varying weather conditions. Weak ice is formed when warming trends break down ice, then the slushy surface re-freezes. The New

In situ measurements of water vapor and temperature from recent aircraft campaigns have provided evidence that the upper troposphere is frequently supersaturated with respect to ice. The peak relative humidities with respect to ice (RHI) occasionally approached water saturation at temperatures ranging from -40°C to -70°C in each of the campaigns. The occurrence frequency of ice supersaturation ranged from about 20% to 45%. Even on flight segments when no ice crystals were detected, ice supersaturation was measured about 5-20% of the time. A numerical cloud model is used to simulate the formation of optically thin, low ice number density cirrus clouds in these supersaturated regions. The potential for scavenging of ice nuclei (IN) by these clouds is evaluated. The simulations suggest that if less than about 5 x 10¯³ to 2 x 10¯² cm¯³ ice nuclei are present when these supersaturations are generated, then the cirrus formed should be subvisible. These low ice number density clouds scavenge ...

Quartzofeldspathic ultramylonites from the Alpine Fault Zone, one of the worlds major, active plate boundary-scale fault zones have quartz crystallographic preferred orientations (CPO) and abundant low-angle (,10° misorientation) boundaries, typical microstructures for dislocation creep-dominated deformation. Geometrically necessary dislocation density estimates indicate mean dislocation densities of ~109 cm-2. A significant proportion (~30%) of grain boundaries (,10° misorientation) are decorated by faceted pores, commonly with uniformly-oriented pyramidal shapes. Only grain boundaries with ,10° misorientation angles in polymineralic aggregates are decorated by pores. Mean grain boundary pore densities are ~5 × 108 cm-2. Grain boundary pores are dissolution pits generated during syn-deformational transient grain boundary permeability, nucleating on dislocation traces at dilatant grain boundary interfaces. They have not been removed by subsequent grain boundary closure or annealing. Pore ...

If the current trend continues or gets worse, Antarctica could become the largest contributor to sea level rises in the world. It could start to lose more ice than Greenland within a few years, said Jianli Chen, of the University of Texas at Austin.. Chens team used data from the Nasa mission to see how Earths gravitational pull varied month to month between April 2002 and January 2009. Measurements taken over the south pole reflect changes in the mass of the Antarctic ice sheets.. The survey confirmed the West Antarctic ice sheet is melting rapidly with the loss of about 132-billion tonnes of ice a year, but revealed unexpected melting in the larger East Antarctic ice sheet.. The scientists used a computer model to take account of ongoing movements in the Earths surface caused by the retreat of glaciers at the end of the last ice age. Uncertainties in the model gave the scientists only a broad estimate of ice loss in the East Antarctic ice sheet of between five-billion and 109-billion ...

Explaining the vibrations. In the new study, Godin and his co-author, Nikolay Zabotin, used two theoretical models of the Ross Ice Shelf to show vibrations within the ice could create the atmospheric waves.. One model approximates the ice shelf as a smooth rectangular slab of ice, while the other approximates the ice as a layered fluid. The authors incorporated known properties of the ice sheet such as elasticity, density, and thickness into each model to calculate the time it would take vibrations in the ice to complete one cycle.. They found both models predict that the ice shelf produces vibrations within a 3- to 10-hour period, which matches the duration of vibrations seen in the atmosphere. These ice shelf vibrations would likely also produce atmospheric waves with a vertical wavelength of 20 to 30 kilometers (12 to 18 miles), another feature of the observed waves.. Even in this simplified description [of the ice], it readily explains the most prominent features of the observations, Godin ...

Ice core research: Researchers from the section Physics of Ice, Climate and Earth (PICE) at the Niels Bohr Institute, University of Copenhagen, have succeeded in making a method to enlighten an otherwise dark period in climate history. Working with the ice core ReCap, drilled close to the coast in East Greenland, postdoc Marius Simonsen wondered why the dust particles from the interglacial period - the warmer period of time between the ice ages - were several times bigger than the dust particles from the ice age. His research led to the invention of a method able to map the advancement of the glaciers in cold periods and the melting in warmer periods. This data is important for the climate models we use to predict sea level rise. The result is now published in Nature Communications.. The larger particles of dust dont travel far - they come from East Greenland. Based on the hypothesis that the bigger dust particles in the ice couldnt have come from afar, the then PhD student, Marius Simonsen, ...

Dry ice is a frozen form of a gas called carbon dioxide. You may be familiar with dry ice as the frosty pellets that ice-cream vendors use to keep their ice cream frozen for hours at a time.. Dry ice is called dry because it doesnt melt into a liquid, like ice that is made from water.. Dry ice changes directly back to a gas as it thaws, and disappears into the air. Dry ice is a great deal colder than ordinary ice. This means you have to be careful with it.. Holding it in your bare hands for more than a few moments can cause frostbite, which is very dangerous.. When frozen carbon dioxide is exposed to the air, it evaporates slowly as a gas without going through the melting stage in the way that ice made from water does.. The fact that dry ice has a freezing point much lower than that of water makes it useful as a refrigerant, particularly for the storage of things that need to be kept very cold.. When powdered dry ice is added to such liquids as acetone (used in the manufacture of chloroform) ...

At 4.41 million square kilometers or 1.79 million square miles, 2015 was the fourth-smallest summer sea ice minimum extent in recorded history. This is 1.87 million square kilometers below the 1981 to 2010 average extent. This chart shows the disturbing trend over the last thirty years. The sea ice extent at the end of the melt season is on a decline. And not only is the ice extent getting smaller, but the ice is also thinning at an alarming rate. In fact, some computer models project we are on track to see an ice-free summer within 20 years. Thats 40 to 50 years earlier than previously forecast. One source of heat to the arctic is through warmer ocean currents via the Pacific and Atlantic pathways. This lateral heat underplates the sea ice, and so the ice melts from below as well as from above.. The more the ice melts, the more ocean surface is exposed that can absorb heat from the sun. This warms the water and the region even further, melting even more ice. This scenario has direct ...

In contrast to secular scientists, creation researchers think there was just one Ice Age that was caused by the Genesis Flood.1 Intense volcanism and rapid seafloor spreading during the Flood would have greatly warmed the worlds oceans. This would have resulted in a tremendous amount of evaporation. The increased atmospheric moisture produced intense snowfall on mountaintops and at high latitudes. Summer cooling caused by residual post-Flood volcanism prevented snow and ice from melting, allowing thick ice sheets to grow rapidly after the Flood.. Recent ICR research has highlighted a devastating problem with the main argument for the secular Ice Age theory, found fossil evidence in support of the Flood Ice Age model, and revealed clues that secular age models are assigning too much time to the deep Antarctic ice cores.2-4 ICR has also just published my book explaining the Flood Ice Age model and how it relates to the global warming debate.5. In many ways, the Flood Ice Age model is vastly ...

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The floating ice shelves surrounding the Antarctic Ice Sheet restrain the grounded ice-sheet flow. Thinning of an ice shelf reduces this effect, leading to an increase in ice discharge to the ocean. Using eighteen years of continuous satellite radar altimeter observations we have computed decadal-scale changes in ice-shelf thickness around the Antarctic continent. Overall, average ice-shelf volume change accelerated from negligible loss at 25 ± 64 km3 per year for 1994-2003 to rapid loss of 310 ± 74 km3 per year for 2003-2012. West Antarctic losses increased by 70% in the last decade, and earlier volume gain by East Antarctic ice shelves ceased. In the Amundsen and Bellingshausen regions, some ice shelves have lost up to 18% of their thickness in less than two decades. ...

The sea ice that floats on the Arctic Ocean is covered with snow all winter. The snow-covered ice is bright white so it absorbs very little of the solar energy that gets to it. And during the Arctic winter, very little solar energy gets to it anyway. The Sun stays low on the horizon, days are short, and above the Arctic Circle there is at least one day of winter when the Sun does not make an appearance at all. Summer is warmer than winter but it becomes even warmer as the ice changes and melts. How does this happen? As summer approaches, the Sun climbs higher in the sky each day and the weather gets a little warmer. Warmer temperatures melt the snow, exposing the bare sea ice. Pools of melt water form on the ice and cracks called leads break the ice into pieces like a puzzle. The exposed ice is darker in color than the snow. The pools and cracks are also darker. And where the ice has melted, dark ocean water is exposed. Because all these changes make the surface darker, the albedo is lower, more ...

My understanding is that your ice melt index is an approximation for ice melting at the surface of the sheet but is not a good approximation for total ice loss. Its about as good (slightly more, but not massively) as sea ice extent is an approximation for total ice loss/gain. The difference being 15% coverage is counted as highly as 100% when it comes to extent, so the more broken up the ice (which is more likely in the summer and more likely still for thin ice) the worse extent is an analogue for ice volume.. [Response: Huh? Lets not confuse things! Sea ice is floating ice 1-4 m thick. The melt were talking about here is melt on the land ice - the hundreds-of-m-thick glacier ice (the Antarctic ice sheet), and the floating ice shelves (also hundreds of m thick, and NOT the same thing as sea ice. The point is that melt on the surface of the ice sheet is almost all refrozen, so the ice melt index has little or nothing to do with mass loss. These are totally separate things (except when lots of ...

Psychrophilic organisms produce AFPs in order to prevent ice growth during freezing. Some studies have demonstrated that these proteins are extremely effective in the inhibition of recrystallization of ice even at very low concentrations [49]. However, their working mechanism is not well understood. Moreover, their properties offer the opportunity to exploit AFPs for biotechnological applications, especially in food industry. In frozen food products, freezing provides a multitude of small ice crystals, but it is also important to prevent the formations of large ice crystals [50]. AFPs from Antarctic bacteria GU1.7.1, GU3.1.1 and AFP5.1 were able to reduce the damage associated to ice, probably through the reduction of the size of large ice crystals in buffer solution. This phenomenon was evidenced when zucchini and cucumbers tissues were treated with a commercial and bacterial AFPs, where small pore were (red asterisk Figs. 1, 2) formed on plant cell walls of treated tissues in comparison to the ...

For example, 1 to 2 cups Dutch chocolate ice cream and 12 oz. Ask most wine professionals, and theyll tell you, Pairing wine with ice cream is one of those impossible pairings. Go with beer or have a sip of whiskey, instead. But what if you are presented with a situation where wine is your only option, or what if you simply love wine and ice cream together? Ice cold. Hold the dispenser button to drop your ice cream and try to match to the model. This is, perhaps, the best way for a bottle of stout, a scoop of ice cream and a splash of heavy cream to go on a date with ones taste buds [source: Christensen]. So eating chilies in the summer is not recommended as the added heat will lead to pitta disturbances like rashes, cold sores, acne, and heartburn. Use chocolate ice cream with your soda. A shot is exactly what Whirly Birds unique ice cream gets, in the form of a wand that shoots negative-320-degree liquid nitrogen into a bowl of ice cream base, flavors and mix-ins. This was so yummy! ...

The portion of the West Antarctic ice sheet that flows into the Ross Sea is thinning in some places and thickening in others. These changes are not caused by any current climatic change, but by the combination of a delayed response to the end of the last global glacial cycle and an internal instability. The near-future impact of the ice sheet on global sea level is largely due to processes internal to the movement of the ice sheet, and not so much to the threat of a possible greenhouse warming. Thus the near-term future of the ice sheet is already determined. However, too little of the ice sheet has been surveyed to predict its overall future behavior. ...

Large areas of the Arctic Ocean are covered with sea ice, the extent, thickness, concentration and properties of which change seasonally, interannually and on longer time scales. The Arctic Ocean is often difficult to access, making satellite remote sensing the only means to obtain information about the sea ice on a pan-Arctic scale. In order to improve the processing and interpretation of satellite data and imagery, in-situ calibration and validation are necessary. In spring 2011, measurements on first year sea ice north of Svalbard were performed during two scientific cruises with the ships KV Svalbard and RV Lance as a part of the CryoVEx 2011 project. During these cruises, detailed measurements of snow and ice thickness, freeboard, and snow density were performed on ice stations and from a helicopter. The data collected contributes to the calibration and validation of the SIRAL sensor data from the CryoSat-2 radar altimeter satellite, which measures the freeboard of sea ice for ...

2008-06-09 · Ice machine/CPM: Insurance cover, cost, worth it? time to try and get things sorted before the surgery and this time they have recommended a game ready ice machine. 2012-07-12 · Welcome to the Game Ready Shoulder Wrap Application Video. This video demonstrates how to apply the Game Ready Shoulder Wrap. Contact Game Ready for. Game Ready Ice Machine User Manual Complete how-to videos, user guides, and customer support services assure proper treatment and For … Discharge Process and Instructions. For safety and regulatory reasons, Game ready ice therapy machine or ice cube. CPM (continuous passive motion). Hello /rACL. I am four days post op and am renting the game ready machine. It has done wonders, but has just now sprung a leak and the dressing is... Discharge Process and Instructions. For safety and regulatory reasons, Game ready ice therapy machine or ice cube. CPM (continuous passive motion). ...

Le Mars has grown up alongside a family-run dairy operation which has become one of the largest ice cream manufacturers in the U.S. In 1994, Le Mars was officially recognized by the Iowa legislature as The Ice Cream Capital of the World thanks to the fact that more ice cream is made by Wells Enterprises, Inc. in a single location than in any other city in the world. This claim to fame has punctuated the communitys tourism industry as fans of ice cream and the Blue Bunny® brand descend upon the community for events such as the annual Ice Cream Days festival and to visit the Ice Cream Parlor, located in the heart of the downtowns vibrant business district. In fact, on June 12, Wells Enterprises cut the ribbon on its re-imagined and rebranded Wells Visitor Center and Ice Cream Parlor with an expanded ice cream menu and interactive experience. Learn more by visiting www.ilovewells.com.. Family ownership and the sweet spot of success. Wells Enterprises, Inc., founded by Fred H. Wells Jr. in Le ...

An analytical approximation for the steady state dynamic recrystallized grain size is combined with a simple nucleation criterion to assess the propensity for dynamic recrystallization. In line with observation, the criterion predicts dynamic recrystallization in 99.9995% pure Al but not in material 99.5% pure. It also agrees with the observation that zone refined ferrite can display dynamic recrystallization at high temperatures and low strain rates but not at lower hot working temperatures. The criterion is applied here to common wrought magnesium alloys to argue that conventional dynamic recrystallization is expected under normal hot working conditions ...

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This is designed for an old-fashioned ice cream maker that yields 1 gallon; be sure to scale recipe down if you have a countertop model. Kayla, thank you! Do you not have the cook the egg mixture? Start by creaming (or mixing) the eggs* and the sugar together. Nostalgia Products. Your metal canister should have a fill line. It was easy and my taste test before sticking it in the freezer to firm up tells me it is very yummy. This post may contain affiliate links which means we receive a small commission at no cost to you when you make a purchase. HOMEMADE STRAWBERRY ICE CREAM with no eggs! I have been searching for an easy, delicious and fail-safe ice cream recipe. My God, best ice cream ever. Strawberry Ice Cream. Tag us on Instagram @mellockcuff and hashtag #aomrecipes so we can see! It was delicious, very creamy, not grainy like some homemade ice creams. Privacy Policies, Altered ingredient amounts. This strawberry ice cream recipe is made using an old-fashioned ice cream maker, not the crank ...

Second, the ice cream produced has ice residue.To make the ice cream taste smooth and reduce the generation of ice scum, it is necessary to explain from the aspects of the ice cream machine.1. The rat

Neal Gottlieb is founder of Three Twins Ice Cream Neal Gottlieb, Founder, Three Twins Ice Cream Neal Gottlieb launched Three Twins Ice Cream seven years ago. [...] instead of spending $110,000 on getting an MBA from a fancy university, he decided to carpe diem and invested his $70,000 lifes savings and a $25,000 loan from his parents in starting his own Bay Area creamery. [...] he sort of liked ice cream - Im actually more of a savory guy, he admits. [...] organic ice cream seemed like a sure bet, especially given how much crap is out there. For months he was the companys sole employee, making the ice cream in the morning, operating the store all day, and cleaning up at night. To boost business, Gottlieb followed the old adage of spending money to make money. [...] anyone who has been to his Napa scoop shop knows that the ice cream entrepreneur never takes himself too seriously. What other expensive ice cream packages do you offer? Once we climb the mountain, we will chip away at the

This was an interesting melt season, said Walt Meier, a sea ice researcher at NSIDC. At the beginning of August we were at record low ice levels for that time of the year, so a new minimum record low could have been in the offering.. But unlike 2012, the year with the lowest ice extent on record, which experienced a powerful August cyclone that smashed the ice cover and accelerated its decline, the 2019 melt season didnt see any extreme weather events. Although it was a warm summer in the Arctic, with average temperatures 7 to 9 degrees Fahrenheit (4 to 5 degrees Celsius) above what is normal for the central Arctic, events such as this years severe Arctic wildfire season or European heat wave ended up not having much impact on the sea ice melt.. By the time the Siberian fires kicked into high gear in late July, the Sun was already getting low in the Arctic, so the effect of the soot from the fires darkening the sea ice surface wasnt that large, Meier said. As for the European heat wave, ...

George VI Ice Shelf is the largest ice shelf on the western side of the Antarctic Peninsula and its northern margin marks the southern most latitudinal limit of recent ice shelf retreat. As part of a project to reconstruct the long-term (Holocene) history of George VI Ice Shelf we studied two epishelf lakes impounded by the ice shelf at Ablation Point, on the east coast of Alexander Island. These lakes, Moutonnée and Ablation, are stratified water bodies with a lower marine layer and an upper freshwater layer. To determine if their sediment records could be used to detect past changes in the presence or absence of the ice shelf it was necessary to describe their present-day limnology and sedimentology. We measured water column chemistry and sampled the water column and sediments of the lakes along vertical and horizontal transects. We analysed these samples for diatoms, stable isotopes (δ18O, δ2H, δ13CDIC, δ13Corg), geochemistry (TOC, TN, C/N ratios) and physical sedimentology (grain-size). ...

Glacial ice currently occupies roughly 11% of Earths surface and contains approximately 70% of the planets freshwater. Once thought to be inhospitable due to the physiochemical challenges presented by freezing temperatures, the basal zones of glaciers and ice sheets have recently been identified as a potential habitat for psychrophilic microorganisms with the ability to mediate biogeochemical cycles on a global scale. Basal ice is found in the deepest layers of a glacier and has distinct chemical and physical characteristics as a result of its proximity to the glacier bed. Basal ice is generally the warmest ice found in a glacier and often contains entrained debris and sediment from the underlying subglacial substrate which may provide nutrients and redox couples for microorganisms immured in the basal ice matrix. ATP/ADP concentrations and ratios, enrichment culturing, 16S rRNA surveys, and cell counts were combined with nutrient, major ion, and gas chemistry analyses to evaluate the microbial

Arctic Climatology Project. 2000. Environmental Working Group joint U.S.-Russian sea ice atlas. Edited by F. Tanis and V. Smolyanitsky. Ann Arbor, MI: Environmental Research Institute of Michigan in association with the National Snow and Ice Data Center. CD-ROM. http://nsidc.org/data/g01962.html. Cavalieri, D. J., C. L. Parkinson, P. Gloersen, and H. J. Zwally. 1996, updated yearly. Sea Ice Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave Data, Version 1. [Indicate subset used]. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. doi: http://dx.doi.org/10.5067/8GQ8LZQVL0VL.. Fetterer, F., and V. Troisi. 1997. AARI 10-Day Arctic Ocean EASE-Grid Sea Ice Observations. Boulder, CO, USA: National Snow and Ice Data Center. Digital media. http://nsidc.org/data/nsidc-0050.html. Gloerson, P., D. Cavalieri, W.J. Campbell, and J. Zwally. 1990. Nimbus-7 SMMR polar radiances and Arctic and Antarctic sea ice concentrations. Boulder, CO: ...

Continental margin drill core and seismic data indicate that between 3.0 and 2.5 Ma, high-latitude climate cooling drove both the West and East Antarctic Ice Sheets towards their present expanded cold polar state. Ice margins developed permanent marine termini with ice shelves. Direct physical sedimentary records of Antarctic Ice Sheet variability (e.g. ice-rafted debris, proximal glacimarine cycles) and more distal ocean records of sea-ice distribution (e.g. diatom palaeoecology), thermohaline circulation (e.g. sortable silt), ocean temperatures (e.g. δ18O), frontal dynamics and surface circulation (e.g. palaeoecological assemblages and sea-surface temperature (SST) reconstructions) all show a strong covariance with the 41 kyr cycle in Earths obliquity between 3 and 1 Ma. Glacial periods are characterised by northward expansion of seasonal sea ice, SSTs up to 6°C colder than now, equatorward migration of frontal zones by 5-10° latitude, intensification of zonal westerly winds, invigorated ...

We had lunch in a neighbouring hotel as part of the Irish trade delegation, and then, in the afternoon - ice cream! We went to Ouca, a shop with fairly wild flavours from a western perspective - a seasonal pumpkin, black sesame ice cream, salty soy ice cream lotus blossom ice cream, red bean (azuki) ice cream, etc. The flavours were fun, but I think it was an Italian pre-fabricated base, if Im not wrong. An interesting concoction that they served had agar-agar cubes with ice cream and red beans, topped with a sugar sauce. ...

When I was a teenager I decided I liked ice cream sandwiches - chocolate cookie with vanilla ice cream. And my early teen years were when my best friend and I ran the Peach Stand on the highway for her grandfathers peach farm. We always had tons of peaches in the summer and peach ice cream was a treat we really enjoyed. Later, when I was married and moved to Texas, I discovered Bluebell Fresh Peach Ice Cream. That was a great facsimile of what we had made at home in earlier years. Luckily, my grandmother had given me a Waring Ice Cream Parlour machine one year for my birthday. It was electric and used table salt, but it was still messy. However, it was much easier than hand-cranking or having to find ice cream salt ...

That old ice cream machine eventually gave out, but my dad continues to insists on making ice cream with a hand crank. He was able to find one for purchase a few years back. Today all of my kids know Poppas ice cream making rules, and they all pitch in willing to help. It really is a delicious family tradition!. I, on the other hand, enjoy my electric ice cream making machine. It does the same job as my dads but I get to plug it in and walk away. 30 minutes later - we get to enjoy fresh ice cream.. We have one child that is dealing with EOE and cannot eat dairy, egg, soy, plus other food items. Traditional ice cream is off the table for Dom. He has discovered coconut milk based ice cream and really enjoys having this for a treat. I decided to try making it here at home - it is soooooo easy! And the kids exclaim, they LOVE it!. ...

Are you looking for a colorful summertime punch to inject some deliciousness to a party or lazy day around the house? Look no further than a party drink using Ruggles Ice Creams new Unicorn flavor ice cream! Our new Unicorn flavor ice cream features a mix of smooth and creamy Raspberry Sour and Cotton Candy ice creams blended with purple glittery frosting and purple sprinkles. By adding our Unicorn ice cream with one (or two) other ingredients you can complete the perfect punch. We think the best way to complete this punch is with any flavor of the soda. Fill a punch bowl or container with the soda and then scoop in as many frozen scoops of Unicorn Ice Cream as your taste buds desire! A possible option to take… Read More ...

Offering ten times better resolution than any other satellite images, GlobIce provides incredibly accurate information about sea ice dynamics in the Arctic. With missions like ESAs CryoSat producing increasingly detailed measurements of the thickness and extent of polar ice, the high-resolution maps produced by GlobIce could also help interpret the data.. GlobIce can also be used to interpret other critical data, such as the ice thickness measurements now being provided by CryoSat, said Dr Laxon.. Although the GlobIce project primarily focused on developing operational products for the Arctic region, it has recently been prototyped to generate products over the Antarctic. Sample products of the Antarctic are now available for August and September 2010.. Owing to the different characteristics of south polar sea ice, which makes it difficult to monitor from many low-resolution sensors, there is very little sea ice dynamics data available. GlobIce could be used to fill this gap in the ...

Acknowledgments: We thank the NASA Operation IceBridge project team and the National Snow and Ice Data Center and acknowledge the use of MCoRDS airborne radar data from the Center for Remote Sensing of Ice Sheets (CReSIS) generated with support from the University of Kansas NSF grant ANT-0424589 and NASA Operation IceBridge grant NNX16AH54G. We thank the Polar Geospatial Center who provided the DEM under NSF Office of Polar Programs awards 1043681, 1559691, and 1542736. We thank F. Habbal, G. Ng, S. Palmer, and T. Richter for support during fieldwork; S. Grasby for providing us with an estimate for the geothermal heat flux; S. Kempf for assistance with radar data processing; and T. Benham for providing bedrock elevations from the spring 2000 radar data set. We also thank N. Wolfenbarger, N. Ross, an anonymous reviewer, and the editors M. Kelly and P. Bierman for providing feedback on the manuscript. This is University of Texas Institute for Geophysics (UTIG) contribution 3255. Funding: This ...

From 7 to 9 February 2014 Saku Suurhall arena for the first time will be presenting the world famous ice show for the whole family DISNEY ON ICE. Bright program Fantasy World takes the viewer into the world of fairy four based on favorite Disney cartoon company. The audience brought the characters from such films as Cars, The Little Mermaid, Fairies and Toy Story. On the ice, of course, there will be Mickey and Minnie Mouse. Ice show Fantasy World will be shown in Tallinn only four times.. Presentation of Fantasy World from Disney on Ice - exciting and full of surprises ice journey that will take children and their parents in the world of racing from the Cars cartoon will peek into the bedroom of Andy to meet there with the characters Toy Story 3 , went to the depths of the underwater world, along with the Little mermaid Ariel, and from there to the Valley of the fairies - a visit to Tinker Bell.. According to Eva Palm, the main promoter of the company Live Nation Baltics, ...

1] Wintertime satellite-derived ice surface velocities, from 2001 through 2007, suggest an increase in ice velocity in the wet snow zone of Southwest Greenland. We present a thermomechanical model to evaluate the influence of surface meltwater runoff on englacial temperatures, via cryo-hydrologic warming (CHW), as a possible mechanism to explain this velocity increase at Sermeq Avannarleq. The model incorporates CHW through a previously published dual-column parameterization. We compare model simulations with (i) CHW active over the entire ice thickness (base case CHW), (ii) CHW active only in the surface 80 m of the ice sheet (surface CHW), and (iii) no CHW to represent a traditional thermomechanical model. The horizontal extent of CHW is prescribed based on equilibrium line altitude position and thus incorporates the upstream expansion of the ablation zone over the past decade. The base case CHW simulations reproduce the observed increase in inland ice velocity between 2001 and 2007 ...

Andersen, S., R. Tonboe, L. Kaleschke, G. Heygster, and L. T. Pedersen. 2007. Intercomparison of Passive Microwave Sea Ice Concentration Retrievals over the High-Concentration Arctic Sea Ice. J. Geophys. Res., 112, C08004, doi:10.1029/2006JC003543.. Belchansky, G. I., and D. C. Douglas. 2002. Seasonal Comparisons of Sea Ice Concentration Estimates Derived from SSM/I, OKEAN, and RADARSAT Data. Rem. Sens. Environ., 81: 67-81.. Carsey, F. D. (Ed.). 1992. Microwave Remote Sensing of Sea Ice. American Geophysical Union, 462 pp.. Cavalieri, D., C. Parkinson, N. DiGirolamo, A. Ivanov (2011). Intersensor calibration between F13 SSM/I and F17 SSMIS for global sea ice data records. IEEE Geosci. Remote Sens. Lett., 9(2), 233-236, doi:10.1109/LGRS.2011.2166754.. Cavalieri, D., C. Parkinson, P. Gloersen, J. Comiso, and H. J. Zwally (1999). Deriving Long-term Time Series of Sea Ice Cover from Satellite Passive-microwave Multisensor Data Sets. J. of Geophys. Res., 104(C7):15,803-15,814.. Cavalieri, D. J., C. ...

8tracks radio. Online, everywhere. - stream 181 yuri on ice playlists tagged with yuri!!! on ice from your desktop or mobile device.

Antifreeze proteins (AFPs) aid the survival of cold-adapted organisms by inhibiting the growth of ice crystals in the organism. The binding of AFPs to ice separates the melting point from the freezing point of the ice crystal (thermal hysteresis, TH). Although AFPs were discovered more than 40 years ago, the mechan

Our walking and running movement patterns require friction between shoes and ground. The surface of ice is characterised by low friction in several naturally occurring conditions, and compromises our typical locomotion pattern. Ice skates take advantage of this slippery nature of ice; the first ice skates were made more than 4000 years ago, and afforded the development of a very efficient form of human locomotion. This review presents an overview of the physics of ice surface friction, and discusses the most relevant factors that can influence ice skates dynamic friction coefficient. It also presents the main stages in the development of ice skating, describes the associated implications for exercise physiology, and shows the extent to which ice skating performance improved through history. This article illustrates how technical and materials development, together with empirical understanding of muscle biomechanics and energetics, led to one of the fastest forms of human powered locomotion.

Greenland ice cores provide excellent evidence of past abrupt climate changes. However, there is no universally accepted theory of how and why these Dansgaard-Oeschger (DO) events occur. Several mechanisms have been proposed to explain DO events, including sea ice, ice shelf buildup, ice sheets, atmospheric circulation, and meltwater changes. DO event temperature reconstructions depend on the stable water isotope (δ18O) and nitrogen isotope measurements from Greenland ice cores: interpretation of these measurements holds the key to understanding the nature of DO events. Here, we demonstrate the primary importance of sea ice as a control on Greenland ice core δ18O: 95% of the variability in δ18O in southern Greenland is explained by DO event sea ice changes. Our suite of DO events, simulated using a general circulation model, accurately captures the amplitude of δ18O enrichment during the abrupt DO event onsets. Simulated geographical variability is broadly consistent with available ice core ...

Until now, few groups reported the antifreeze activity of cyclic glycopeptides;however, the tedious synthetic procedure is not amenable to study the intensive structure activity relationship. A series of N-linked cyclic glycopeptoids and glycopeptide have been prepared to evaluate antifreeze activity as a function of peptide backbone cyclization and methyl stereochemical effect on the rigid Thr position. This study has combined the cyclization protocol with solid phase peptide synthesis and obtained significant quantities of homogeneous cyclic glycopeptide and glycopeptoids. Analysis of antifreeze activity revealed that our cyclic peptide demonstrated RI activity while cyclic glycopeptoids showed no RI activity. These results suggest that the subtle changes in conformation and Thr orientation dramatically influence RI activity of N-linked glycopeptoidsnd glycopeptide have been prepared to evaluate antifreeze activity as a function of peptide backbone cyclization and methyl stereochemical effect ...

Zoarces americanus (4ny6, 1ame, 1b7i, 1b7k, 1ekl, 1gzi, 1hg7, 1jab, 1kde, 1kdf, 1msi, 1msj, 2ame, 2jia, 2msi, 2msj, 2spg, 3ame, 3qf6, 4msi, 5cr7, 5msi, 6ame, 6msi, 7msi, 8ame, 8msi, 9ame, 9msi ...

Antifreeze protein from an Antarctic fish [ PDB file ] [ PubMed link ] Many animals that live in extremely cold climates produce proteins that act to prevent the formation of ice crystals in the bodily fluids of the organism. Antarctic fish produce a range of such proteins, as the water temperatures can drop below 0 degrees Celsius. We have determined the structure of the type I antifreeze protein (SS3) from the blood of the shorthorn sculpin at both 5 degrees and -5 degrees. The structure largely comprises a long alpha-helix that displays conserved Thr residues (red) along a single surface. These residues are important for preventing the growth of ice crystals, although the mechanism of action is not currently understood. An additional short helix exists at the N-terminus of the protein, although the conformational relationship between the two helices is not well defined. This is the first solution structure of a wild-type type I antifreeze protein ...

The Greenland Ice Sheet is losing mass at accelerated rates in the 21st century, making it the largest single contributor to rising sea levels. Faster flow of outlet glaciers has substantially contributed to this loss, with the cause of speedup, and potential for future change, uncertain. Here we combine more than three decades of remotely sensed observational products of outlet glacier velocity, elevation, and front position changes over the full ice sheet. We compare decadal variability in discharge and calving front position and find that increased glacier discharge was due almost entirely to the retreat of glacier fronts, rather than inland ice sheet processes, with a remarkably consistent speedup of 4-5% per km of retreat across the ice sheet. We show that widespread retreat between 2000 and 2005 resulted in a step-increase in discharge and a switch to a new dynamic state of sustained mass loss that would persist even under a decline in surface melt. Glacier retreat is the main process behind

The reason I recommend using dry ice is that it is inexpensive and very easy to find. It is easy to handle (although its extremely cold temperature can cause skin damage after prolonged exposure) and it makes amazing ice cream. Many of the grocery stores in my area stock it and you will probably use less than a couple of dollars worth of dry ice for each batch of ice cream. You may have heard of using liquid nitrogen to freeze ice cream on TV or even on some other blogs. What most of these shows dont mention is that, while liquid nitrogen itself is inexpensive, the specially designed containers required to transport it can be incredibly expensive. It simply isnt a practical thing for home chefs to use unless they have a friend with easy access to liquid nitrogen and the means to transport and store it safely.. The dry ice technique can be made using any flavor of ice cream. Follow the recipe of your choosing and, instead of pouring the mixture into an ice cream maker, break out your dry ice! ...

Fire & Ice at ChillRx does more than just help our clients look and feel amazing!! It actually improves immunity, reduces pain & inflammation, detoxifies and helps with weight loss!!. Fire & Ice at ChillRx is a carefully choreographed sequence of infrared sauna and whole body cryotherapy. Infrared sauna must precede the whole body cryotherapy….and here is why!. The Fire element for Chill Fire & Ice is a 35 to 50 minute full-spectrum infrared sauna session. The Chill infrared sauna produces near-, mid- and far-infrared light-imparting the maximum number of benefits for our clients!! Infrared saunas differ from traditional saunas…. Our infrared sauna directly heats body tissue-so the ambient temperature inside the sauna is not stiflingly hot! Traditional saunas first heat the ambient environment and then indirectly raises body temperature. Many people who do not like traditional saunas prefer an infrared sauna experience because they do not feel stifled by high ambient temperature.. Infrared ...

Little is known about the diversity of microorganisms and range of habitable environments that exist beneath the Greenland Ice Sheet. This project will characterize geochemical and microbial (bacterial and viral) properties of basal ice from a 2537 m deep ice core in North Eastern Greenland (NEEM). The ice core project is led by the Center of Ice and Climate at the Niels Bohr Institute, Denmark with funding support from NSF and 12 other partner nations. The 2.3 m basal ice sequence contains 12 discrete debris-rich ice layers, with intervening clean (debris-poor ice). The debris-rich layers reflect interaction with the ice-sheet bed, and the incorporation of basal debris. The research has three primary objectives: 1) Characterize the cell density and phylogenetic diversity of the microbial community, 2) Determine likely biogeochemical weathering processes occurring in the subglacial environment, and 3) Model the interaction between these measured parameters. This work will integrate with results ...

Colostrum is the first milk produced by a female mammal. It is high in protein, carbohydrate and antibodies. People are constantly looking for healthier food options including immune enhancing foods. Ice cream is a popular dairy dessert and the influence of colostrum on ice cream characteristics is not known. The objective was to study the impact of various amounts of colostrum on the key attributes of ice cream. Ice creams were manufactured with 0, 1.5, 3.0 and 4.5 g colostrum per pint (473 mL) of ice cream. Ice cream manufacture was replicated three times. Colostrum incorporation increased aerobic counts, apparent viscosity, but decreased meltdown resulting in slower melting of the ice creams and had no influence on flavor. In an attempt to make healthier ice creams, colostrum incorporation can be recommended in ice cream manufacture.

Additionally, the weight of the Greenland ice has depressed the interior of the continent and disrupted any drainage that existed prior to being covered in ice. If the ice should be completely melted, a significant fraction of the water wont make it to the oceans until isostatic rebound removes the bowl. The bottom line is that theoretical calculations converting the ice volume of Greenland to an increase in ocean level overstates the immediate effect.. I would also like to draw your attention to this graph. https://www.climate.gov/news-features/event-tracker/new-record-temperature-southwest-greenland. It shows the alltime record summer temp for Summit station in inland Greenland. Notice that it barely got above 0C. Since summers are only 2 months long here how in the hell is Greenland supposed to melt any appreciable amount even if global temps went up 4C. The summit is 2 miles high and the mean thickness of the ice in all of Greenland is 2135 metres or 7000 ft. Since this total of ice is ...

Biological organisms play a surprisingly large role in how rain and snow forms, a new study shows.. Research, published today in the journal Science, says more of these bacteria and other microorganisms seed ice formation in the atmosphere than anyone realised.. The finding could help researchers improve climate forecasts and better understand the relationship between the biosphere and climate, the authors conclude. The discovery could also one day be used to bring rain to dry areas, says lead author Brent Christner, an assistant professor from Louisiana State University.. Scientists have long known that the ice crystals in clouds that become rain or snow need to cling to some kind of particle, called ice nucleators, to form in temperatures above minus 40°C.. But they did not realise, until now, that the most active particles involved in this process are biological ones, Christner says.. Every snow and ice sample weve looked at, we found biological ice nucleators, he says. Heres a ...

Drizzle with the chocolate syrup and give a quick stir. Welcome to Go Go Go Gourmet! Maranda learns how to make an ice cream soda at Plainwell Ice Cream Co. Black & White Chocolate soda with vanilla ice cream. here is all you need: chocolate ice cream. Stir to blend thoroughly. My motto? 2-3 scoops of chocolate ice cream; 1-2 Tablespoons Chocolate syrup; 2 Tablespoons milk; ½ can of soda water (roughly 4oz.) Want a cookbook of our best dessert recipes? I love finding treasures in Goodwill! Add seltzer-served with another scoop on … Stir to blend thoroughly. Theres an ice cream stand down the street from my childhood home that made the best ice cream ever (I suppose theres a chance that it could be just my childhood memories - kind of like how I remember Spaghettios being amazing, but having eaten them as an adult, I realize theyre not nearly as good as I remember.) Unflavored … Chocolate ice cream soda. Start with chocolate syrup to make the perfect ice cream soda. Join our mailing list ...

I scream…you scream…we ALL will be screaming for this ice cream! Thats right, a cookies n cream ice cream that is gluten free and dairy free. A dream come true for me. Cookies n cream ice cream was always my favorite flavor of ice cream as a kid. I love the abundance of chunks of chocolate sandwich cookies that get soft from the vanilla ice cream. Yum to the max!. I made this special treat to celebrate back-to-school last week. Every celebration is better with ice cream. My kids thought I was the coolest mom on the block when I served it to them in a gluten free ice cream cone. This ice cream is dangerous, like for real. It is so, so, so creamy and tastes just like the original. Ive found my new favorite. Cookies n cream ice cream…get in my belly ...

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Using data from a NASA radar that flew aboard Indias Chandrayaan-1 spacecraft, scientists have detected ice deposits near the moons north pole. NASAs Mini-SAR instrument, a lightweight, synthetic aperture radar, found more than 40 small craters with water ice. The craters range in size from 1 to 9 miles (2 to15 km) in diameter. Although the total amount of ice depends on its thickness in each crater, its estimated there could be at least 1.3 million pounds (600 million metric tons) of water ice. The emerging picture from the multiple measurements and resulting data of the instruments on lunar missions indicates that water creation, migration, deposition and retention are occurring on the moon, said Paul Spudis, principal investigator of the Mini-SAR experiment at the Lunar and Planetary Institute in Houston. The new discoveries show the moon is an even more interesting and attractive scientific, exploration and operational destination than people had previously thought. During the past ...

The cryosphere is a key component of the Earth system. The distribution of regional snow/ice cover is affected mainly by factors such as wind, topography, snowfall, and temperature. As global warming continues, extreme weather and climate events frequently occur, including snow/ice disasters. There are several types of snow/ice disasters on different spatial scales, such as snow and ice avalanche, drifting and blowing snow, snowstorm, flood, building collapse, traffic hazards, snow and ice accretion, etc., which cause great damages to human lives and the social economy. Thus, studies on the physical processes and formation mechanism of snow/ice disasters, prediction and early warning systems, as well as control engineering are of great significance to preventing snow/ice disasters from damaging the society.This research topic focuses on 1) blowing/snowing processes influenced by the coupling effect of multiple factors, such as topography, turbulence, solar radiation, temperature, humidity and

Cleveland, OH - January 18, 2012 - Pierres Premium Ice Creams signature rich and creamy taste is now available - lactose free! Pierres is adding two flavors of Lactose Free Premium Ice Cream - Vanilla and Chocolate - to its famous assortment of delicious and innovative ice creams and frozen treats…satisfying even those who typically avoid ice cream due to an intolerance to lactose. Lactose intolerance is caused by a bodys inability to break down the natural sugars or lactose naturally contained in dairy products. Pierres Lactose Free Premium Ice Cream is made with the freshest, finest ingredients along with a lactase enzyme, which breaks down the lactose in the ice cream. Pierres Lactose Free Premium Ice Cream, available at most stores where Pierres products are sold, is packaged in specially designed red Pierres Premium Ice Cream containers. The containers feature the words Lactose Free printed in a pattern along the lid rim along with a bright yellow Lactose Free logo located just ...

Boba ice cream bars are a frozen food, mainly eaten as a dessert or snack. It is an ice cream bar with boba bits throughout. The ice cream is usually made from dairy products, such as milk and cream, and can be flavored with other ingredients, such as green tea, thai tea, etc. The boba (or tapioca pearls) is made out of tapioca starch, becoming gelatinous when cooked. It is a combination of both creaminess from the ice cream and chewiness from the boba. The bars should be kept frozen and defrosted a little before eating. Boba ice cream bars consist of ice cream and boba. A mixture of whole milk, heavy whipping cream, sugar, vanilla, and any additional flavors are mixed in a bowl until the mixture is homogeneous. Once homogeneous, the mixture is poured into an ice cream maker. Our boba consists of tapioca starch, sweet rice flour (mochiko), brown sugar, and water. The dough is rolled into tiny spheres. The spheres are cooked in boiling water. When done, it is cooled in an ice bath so that they ...

As a place that is known for its calorie-filled coffee concoctions, I wasnt surprised that Starbucks has their own line of calorie-filled coffee ice cream concoctions, although these pints of ice cream cant be bought in one of the dozens of Starbucks locations within a 10 miles radius of you. The new Starbucks Ice Cream line replaces the old Starbucks Ice Cream line made by Dreyers and features milk and cream thats free from recombinant bovine growth hormones (rBGH). It comes in four different flavors and I chose the plain ol coffee flavor because I wasnt feeling very adventurous at the time of purchase to try any of the other flavors - caramel macchiato, mocha frappuccino and java chip frappuccino - all of which are apparently brought to us by the letter O.. The Starbucks Coffee Ice Cream is made up of coffee and espresso ice creams. If you look closely at it you can see the swirls the two ice creams make and if you listen very carefully to the ice cream you might be able to hear the ...

Scientists using simulation found that the Eurasian ice sheet, which is 20 thousand years ago covered all the Northern part of Eurasia, disappeared in less than 500 years. This glacier is the size comparable to the modern West Antarctic ice shield, so the experts will be able to adjust their forecasts about the melting of the ice of Antarctica and raising the level of the World ocean: these events can happen in the next hundred years. The results of a study published in the journal Nature Geoscience.. 20 thousand years ago the entire Northern part of Eurasia covered by the Eurasian ice sheet, three times surpassing the size of the modern ice sheet of Greenland. Later, 13,5-14,7 thousand years ago, there was a period of a rapid rise in ocean levels due to melting glaciers, which represent Meltwater Pulse 1A (themeltwater pulse 1A, MWP1a). The Global sea level at that time rose to 40-60 mm per year and eventually rose to tens of meters. Meltwater flowed into the ocean from glaciers, but what ...

Sea ice increases in Antarctica do not make up for the accelerated Arctic sea ice loss of the last decades, a new NASA study finds. As a whole, the planet has been shedding sea ice at an average annual rate of 13,500 square miles (35,000 square kilometers) since 1979, the equivalent of losing an area of sea ice larger than the state of Maryland every year.

This grant will investigate the potential of carbon-14 in ice cores as an absolute dating tool, as a tracer of the past cosmic ray flux and as a recorder of the past fossil fraction of the global methane budget. Cosmic ray particles produce carbon-14 from oxygen-16 directly within near-surface glacial ice and firn. This in-situ produced carbon-14 quickly reacts to form 14C-containing carbon dioxide, carbon monoxide, and methane in the ice matrix. Some or all of the resulting 14C-bearing gases may be lost from the firn to the atmosphere. This research will provide a thorough characterization of in-situ cosmogenic 14C in glacial firn and shallow ice in the Summit region of Greenland. It will examine the retention of cosmogenic 14C in ice grains at all depth levels in the firn column, the partitioning of 14C between carbon dioxide, carbon monoxide, and methane, as well as the production rates and accumulation of cosmogenic 14C in shallow ice below firn close-off. A thorough understanding of ...

A Consolidated PBY-5A Catalina plane, serial 7278, was damaged beyond repair in an accident at Greenland ice cap, Greenland. All seven crew members survived.

With an icy exterior covering a global ocean, Europa has long been a target of interest in the search for life beyond Earth. Europa exists in a dynamic environment, subject to intense irradiation and impact as well as immense tides from Jupiter. These processes deliver important thermal and chemical energy that could be critical to supporting a putative biosphere. In the past few decades the debate about habitability of Europa has been focused strongly on the thickness of the ice shell. However, an arguably more critical question is: how does the ice shell recycle? New analysis of Europas enigmatic chaos terrains, indicates that chaos features form in the presence of a great deal of liquid water, and that large liquid water bodies exist within 3km of Europas surface comparable in volume to the Great Lakes. The detection of shallow subsurface lakes implies that the ice shell is recycling rapidly and that Europa may be currently active. In this presentation, we will explore environments on ...

Jul 5, 2020 - Explore Raydean Reeses board Blackberry Ice Cream on Pinterest. See more ideas about blackberry ice cream, ice cream, ice cream recipes.

Ice discharge is controlled by three major factors: ice thickness, glacier valley shape and ice velocity. Researchers used data from IceBridges 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 velocity. The team used several years of observations to ensure accuracy. Glacier discharge may vary considerably between years, said Ellyn Enderlin, glaciologist at the University of Maine, Orono, Maine and the studys lead author. Annual changes in speed and thickness must be taken into account. ...

To investigate the sequence of events between climate changes at low latitudes and in Greenland, we provide here the first 17O-excess record from a Greenland ice core during Dansgaard-Oeschger events 7 to 13, encompassing H4 and H5. Combined with other ice core proxy records, our new 17O-excess data set demonstrates that stadials are generally characterised by low 17O-excess levels compared to interstadials. This can be interpreted as synchronous change of high-latitude temperature and lower-latitude hydrological cycle (relative humidity at the oceanic source of evaporation or change in the water mass trajectory/recharge) and/or an influence of local temperature on 17O-excess through kinetic effect at snow formation. As an exception from this general pattern, stadial 9 consists of three phases, characterised first by Greenland cooling during 550 ± 60 years (as shown by markers of Greenland temperature δ18O and δ15N), followed by a specific lower-latitude fingerprint as identified from several ...

Current knowledge on Arctic sea ice extent and thickness variability is reviewed, and we examine whether measurements to date provide evidence for the impact of climate change. The total Arctic ice extent has shown a small but significant reduction of (2.1 ± 0.9)% during the period 1978-87, after apparently increasing from a lower level in the early 1970s. However, open water within the pack ice limit has also diminished, so that the reduction of sea ice area is only (1.8 ± 1.2)%. This stability conceals large interannual variations and trends in individual regions of the Arctic Ocean and sub-Arctic seas, which are out of phase with one another and so have little net impact on the overall hemispheric ice extent. The maximum annual global extent (occurring during the Antarctic winter) shows a more significant decrease of 5% during 1972-87. Ice thickness distribution has been measured by submarine sonar profiling, moored upward sonars, airborne laser prohlometry, airborne electromagnetic ...

Concepts of solid and fluid mechanics, integrated with materials and thermal sciences, provide a valuable framework for addressing large-scale phenomena of flow, fracture, and hydrology on our planets major ice sheets. This presentation surveys their application to the following: (a) Large iceberg calving as the enigmatic source of the long-period glacial earthquakes identified along the margins of the Greenland Ice Sheet, (b) Rapid glacial underflooding events as natural hydraulic fractures, like in a well-characterized spontaneous supra-glacial lake drainage on Greenland, and (c) Partial internal melting from shear heating as a control on flow resistance at the margins of the rapidly flowing (, 100 m/yr) ice streams on the Western Antarctic Ice Sheet, and perhaps as a process selecting their marginal locations. The studies have been done at Harvard in collaboration with Victor C. Tsai (now at Caltech), Thibaut Perol, John D. Platt, Jenny Suckale (now at Stanford), Colin R. Meyer, and Matheus ...

The last glacial period exhibited abrupt Dansgaard-Oeschger climatic oscillations, evidence of which is preserved in a variety of Northern Hemisphere palaeodimate archives. Ice cores show that Antarctica cooled during the warm phases of the Greenland Dansgaard-Oeschger cycle and vice versa, suggesting an interhemispheric redistribution of heat through a mechanism called the bipolar seesaw(4-6). Variations in the Atlantic meridional overturning circulation (AMOC) strength are thought to have been important, but much uncertainty remains regarding the dynamics and trigger of these abrupt events. Key information is contained in the relative phasing of hemispheric climate variations, yet the large, poorly constrained difference between gas age and ice age and the relatively low resolution of methane records from Antarctic ice cores have so far precluded methane-based synchronization at the required sub-centennial precision. Here we use a recently drilled high-accumulation Antarctic ice core ...

The S-layer of Caulobacter is a two-dimensional paracrystalline array on the cell surface composed of a single protein, RsaA. We have established conditions for preparation of stable, soluble protein and then efficient in vitro recrystallization of the purified protein. Efficient recrystallization and long range order could not be obtained with pure protein only, though it was apparent that calcium was required for crystallization. Recrystallization was obtained when lipid vesicles were provided, but only when the vesicles contained the specific species of Caulobacter smooth lipopolysaccharide (SLPS) that previous studies implicated as a requirement for attaching the S-layer to the cell surface. The specific type of phospholipids did not appear critical; phospholipids rather different from those present in Caulobacter membranes or archaebacterial tetraether lipids worked equally well. The source of LPS was critical; rough and smooth variants of Salmonella typhimurium LPS as well as the rough ...

1KDF: Refined solution structure of type III antifreeze protein: hydrophobic groups may be involved in the energetics of the protein-ice interaction.

1KDF: Refined solution structure of type III antifreeze protein: hydrophobic groups may be involved in the energetics of the protein-ice interaction.

Looking for a fun treat for your class while discussing Space? Try our Astronaut Ice cream sandwich! This freeze dried ice cream sandwich doesnt need refrigeration and is individually wrapped, so its easy to share! For the best space ice cream, buy our Astronaut ice cream sandwiches at Educational Innovations.

The reason your scoopable LN2 cooled ice cream melts fast is mostly because un-aerated ice cream needs to be warmer to be scoopable. It is basically at or close to the melting temperature when you are scooping it.. Normally produced Ice cream is usually highly aerated making it softer than expected and easily scoopable at a lower temperature. The aeration also reduces the thermal conductivity of the ice cream which slows down the melting process a bit more.. You can whip some air into the ice cream mix beforehand to make it behave closer to commercially produced ice cream, though it will change the texture in the process. Adding less milk and more cream will also let you whip more air into it.. ...

This summer is going to be wintry at the Westside Shopping and Leisure Centre in Bern - with a Glice® artificial ice rink offering free skating fun from June 3 to June 29! Stop by to see what our ecological ice is all about! Find out more about the opening hours and program highlights here.. @westsidebern. Glice® artificial ice rinks leverage the superb glide factor of a unique molecular technology: https://www.glicerink.com/synthetic-ice-rink-technology/. Get in touch with our team in your region to get started on your own artificial ice rink project: https://www.glicerink.com/synthetic-ice-rink-contact-buy-rent/. #westsidebern #glice #bern #glice_switzerland #shopping_center #artificial_ice_rink #ice_skating ...

Looking for online definition of slender ice plant in the Medical Dictionary? slender ice plant explanation free. What is slender ice plant? Meaning of slender ice plant medical term. What does slender ice plant mean?

Blue Ice Cypress is a rare cultivar of Arizona Cypress. (Like Carolina Sapphire, it must be propagated from cuttings and cannot be grown from seed.). The key word here is BLUE! Probably the most startling blue color of any southern conifer. Blue Ice Cypress can be used as a privacy screen, Christmas Tree, or as a DRAMATIC focal point in the landscape. Blue Ice Cypress makes a beautiful blue backdrop for contrasting shrubs and flowers.. Hardy in zones 7 - 9. Blue Ice Cypress is more columnar than other Cypress, prefers hot dry conditions, likes moisture but wants well drained soil, and prefers full sun.. Once established, Blue Ice Cypress grows 2 1/2′ - 3′ per year and reaches 30′ tall or better and 8′ - 10′ wide. Space Blue Ice Cypress as close as 5 feet apart for a quick screen.. ----. ...

When we think of ice cream we dont typically think of gluten. Ice cream should be made from Milk, Cream, Sugar and Flavorings, it should be gluten free. Read on to find out what else may be lurking in that bowl or gluten free cone.. A dear friend of mine stopped by the other day to visit after my surgery. She brought a few groceries; some fresh fruit, vegetables, and ice cream. She thought it would be nice for my son to have a treat. I thanked my friend profusely while my husband put the groceries away. The brand of ice cream my friend brought was Turkey Hill, and that evening, after reading the label I realized that the ice cream would need to be discarded. The Allergen Statement on the container simply stated CONTAINS MILK. My son is not allergic to milk, so why was I planning on discarding the ice cream? A closer inspection of the ingredients showed hidden allergens. When you or your loved one suffers from food allergies or sensitivities label reading skills are not only important, they ...