-LSB-...] Go ice fishing and see which
temperature of water melts ice the fastest in this fun experiment from Science Sparks.
Not exact matches
You should be able to
melt the chocolate at a low
temperature if you use a double boiler (use a glass bowl over a pot
of steaming
water).
2 3/4 — 3 1/2 cups bread flour or all - purpose flour 1/4 cups sugar 1/2 teaspoon salt 1 tablespoon active dry yeast 5 tablespoons butter, softened 2/3 cup warm
water 1 egg, at room
temperature Cornmeal 1/4 cup
of butter,
melted
- * lukewarm
water shouldn't feel hot or cold, just roughly body
temperature - to make vegan: use 1/3 cup + 1 tbsp olive oil or
melted vegan margarine in place
of the butter in the filling.
2/3 cup raisins, optional 1 cup
water 2 cups old - fashioned oats (certified gluten - free, if needed) 2/3 cup chopped pecans (or walnuts), optional 2 teaspoons ground cinnamon 1 teaspoon ground ginger 1/2 teaspoon ground nutmeg 1 teaspoon baking powder 1/4 teaspoon fine sea salt 2 large eggs, room
temperature 2 teaspoons pure vanilla extract 1/3 cup pure maple syrup 1/4 cup (1/2 stick) unsalted butter,
melted 1 1/2 cups milk
of choice 1 1/2 cups grated carrots
Lemon glazed madeleines 3 large eggs, at room
temperature 2/3 cup (133g) granulated sugar 1/8 teaspoon salt 1 1/4 cups (175g) all purpose flour 1 teaspoon baking powder finely grated zest
of 1 lemon 9 tablespoons (126g) unsalted butter,
melted and cooled to room
temperature, plus additional
melted butter for preparing the molds Glaze: 1 cup (140g) icing sugar, sifted 2 tablespoons freshly - squeezed lemon juice 1 tablespoon
water Brush the indentations
of a madeleine mold with
melted butter.
When you want to use it, you may find it has hardened so you can either leave it at room
temperature for a while or you can place the glass jar inside a bowl
of boiling
water to
melt it quickly.
Hi petra, i live in indonesia, so pretty much room
temperature here is about 33 already, so its impossible to cool down the chocolate to 27 C, i tried to use cool
water and put in on the bottom
of melting chocloate (after i
melt it to 46C) then when it reach 27C i heat it to 33C, then i put it in my room and i use air conditioning
temperature of 25C, next day when i woke up it shows fat blooming.
i live in indonesia which is very hot and i check it with my
temperature that shows the condition
of room
temperature in here is about 32 celcius already, so when i try to cool down after i
melt the chocolate to to 46 C, its impossible to make it to 27 C, so i tried to use cool
water in a bowl and i put it on the bottom
of my chocolate that has been
melted until it reach 27C, and i heat it again to 31 C, then i put it in my room with air conditioning with
temperature of 25C, the next day when i woke up the fat bloom appear and the chocolate is not firm.
Makkonen says that one
of the key observations in VTT's research is that
of friction
melting the ice when the
temperature rises to form a
water film between the ice and the sliding material.
«Strong El Niño events cause large changes in Antarctic ice shelves: Oscillations
of water temperature in the tropical Pacific Ocean can induce rapid
melting of Antarctic ice shelves.»
But increasingly warmer summer
temperatures are
melting the ice
of the Bering Strait and Northwest Passage, opening a
water highway between the Pacific and the Atlantic.
The reason: until the end
of the
melting season the fate
of the ice is ultimately determined by the wind conditions and air and
water temperatures during the summer months.
These customary phase transitions manifest as an abrupt change in the state
of matter such as ice
melting to
water, or
water boiling to vapor, at some critical
temperature.
So when wind pulls warm
water up from down deep, the
temperature difference experienced at the interface
of the
water and ice can effectively submerse the glacier in a hot bath, with some areas experiencing more than a 10-fold increase in
melt rate.
The
melting occurs where the overlying ice is about 400 meters thicker, Siegert notes; the added pressure lowers the
melting temperature, just as the pressure
of an ice skater's blade creates a thin rind
of water underneath.
The increase could be due to a combination
of stronger winds spreading out the sea ice and fresh
water from
melting ice on land diluting seawater so it freezes at higher
temperatures.
Dr. Jerison studies systems governed by simple rules that nonetheless exhibit complex behaviors, such as phase transitions — for instance, when a slight
temperature increase causes ice to
melt into liquid
water; and threshold phenomena — for instance, when a small extra deposit
of soil causes a stable slope to topple over into a landslide.
«The DIC lakes are situated within bedrock troughs in mountainous terrain, exist at
temperatures well below the pressure -
melting point, do not receive surface meltwater input, and likely consist
of hypersaline
water derived from dissolution
of a surrounding salt - bearing geological formation,» the researchers reported.
The research published in Nature Communications found that in the past, when ocean
temperatures around Antarctica became more layered - with a warm layer
of water below a cold surface layer - ice sheets and glaciers
melted much faster than when the cool and warm layers mixed more easily.
Sea level rise has two primary components: the expansion in volume
of seawater with increased
temperature and the addition
of water in ocean basins from the
melting of land - locked ice, including Antarctica and Greenland.
Thousands
of studies conducted by researchers around the world have documented changes in surface, atmospheric, and oceanic
temperatures;
melting glaciers; diminishing snow cover; shrinking sea ice; rising sea levels; ocean acidification; and increasing atmospheric
water vapor.
And then, if the ocean surface
water was «diluted» with isotopic light
melt water, would this not be reflected with a similar drop in the Greenland ice cores, just by a changing isotope signature
of the source, instead
of a
temperature drop?
The intensifying effects
of warming
temperatures on
water shortages have been detected in remote northern New Mexico, where
melting snowfall feeds one
of the Southwest's most important rivers.
The underlying logic is sound: as sea ice
melts, it exposes darker ocean
water, which absorbs more
of the sun's heat, causing the
water temperatures to increase.
The Arctic is warming more than twice as fast as the rest
of the planet, because as ice
melts at the top
of the world, there is less
of it to reflect sunlight back into space, so more
of it is absorbed by ocean
waters; more absorbed sunlight means even warmer
temperatures, which means more ice
melt a circular process known as Arctic amplification.
Glacier speed also depends on bottom drag (which is a function
of temperature and lubrication by
melt water) and also stresses within the ice sheet / shelf as well.
Rising ocean
waters and air
temperatures are essentially putting ice in a vise grip
of warming and speeding up
melt.
Scientists previously believed that
temperature and sunlight drive the growth
of phytoplankton but using satellite data, the researchers
of the study showed that the amount
of water that leaves the
melting glaciers in the Antarctic is the biggest contributor to the abundance
of phytoplankton in the coastal polynyas.
«On the phase diagram
of water with density functional theory potentials: The
melting temperature of ice Ih with the Perdew - Burke - Ernzerhof and Becke - Lee - Yang - Parr functionals.»
Days are getting hotter, nights are getting cooler, and rising
temperatures are causing the essential source
of the region's
water — high mountain glaciers — to
melt away.
The second major source
of lead is the
water from the home
water heater, which because
of the high
temperatures,
melts some minerals, including lead.
«Environmental scientists have been saying for some time that the global economy is being slowly undermined by environmental trends
of human origin, including shrinking forests, expanding deserts, falling
water tables, eroding soils, collapsing fisheries, rising
temperatures,
melting ice, rising seas, and increasingly destructive storms,» 6.
Rising Seas: Warmer ocean
water temperatures, the pumping
of ground
water, and
melting of the polar ice sheets have added
water to the oceans, contributing to sea level rise.
Before today's basic refrigerator could ever be born though, scientists had to tease apart the meaning
of temperature, find a standard way to measure it, discover what it takes for
water to freeze, and how ice
melts.
Scientists agree that a doubling
of atmospheric CO2 levels could result in
temperature increases
of between 1.5 and 4.5 °C, caused by rapid changes such as snow and ice
melt, and the behaviour
of clouds and
water vapour.
The physical processes by which energy might be added into the glacier material include: (A) convection between the glacier surfaces and local surrounding atmosphere and
water, (B) direct radiation onto the exposed surfaces
of the material, (C) addition
of material that is at a
temperature higher than the
melting temperature onto the top
of the glacier (rain, say), (D) Sublimation
of the ice directly into the atmosphere, and (E) conduction into the material from the contact areas between the glacier and surrounding solid material.
[1] CO2 absorbs IR, is the main GHG, human emissions are increasing its concentration in the atmosphere, raising
temperatures globally; the second GHG,
water vapor, exists in equilibrium with
water / ice, would precipitate out if not for the CO2, so acts as a feedback; since the oceans cover so much
of the planet,
water is a large positive feedback;
melting snow and ice as the atmosphere warms decreases albedo, another positive feedback, biased toward the poles, which gives larger polar warming than the global average; decreasing the
temperature gradient from the equator to the poles is reducing the driving forces for the jetstream; the jetstream's meanders are increasing in amplitude and slowing, just like the lower Missippi River where its driving gradient decreases; the larger slower meanders increase the amplitude and duration
of blocking highs, increasing drought and extreme
temperatures — and 30,000 + Europeans and 5,000 plus Russians die, and the US corn crop, Russian wheat crop, and Aussie wildland fire protection fails — or extreme rainfall floods the US, France, Pakistan, Thailand (driving up prices for disk drives — hows that for unexpected adverse impacts from AGW?)
I suspect that what was happening was that there was mass loss, but there was also thermal expansion
of the ice, as
melt water drained down through the ice and froze, depositing its heat
of fusion and raising the
temperature.
A climate statement would be that the average
temperature of the boiling
water is 100ºC at normal pressure» What if your pot has a lid that has certain weight and might
melt down over the time?
A climate statement would be that the average
temperature of the boiling
water is 100ºC at normal pressure» What if your pot has a lid that has certain weight and might
melt down over the time?
Like a glass
of water with ice cubes, any extra energy tends to go into
melting rather than
temperature changes.
And then, if the ocean surface
water was «diluted» with isotopic light
melt water, would this not be reflected with a similar drop in the Greenland ice cores, just by a changing isotope signature
of the source, instead
of a
temperature drop?
The model showed that there should be a seasonal cycle in the behavior
of the shallow -
water hydrates just below the seafloor, with some additional hydrates forming while the
water temperature is cooler and then
melting when the
water is warmer.
While anomalies are the darling
of staticians, where the base line environmental
temperatures cross the freezing point /
melt point
of water, the anomalies from those
temperature data sets are just the average
of nonsense.
«As a coastal city located on the tip
of a peninsula, San Francisco is vulnerable to sea level rise, and human activities releasing greenhouse gases into the atmosphere cause increases in worldwide average
temperature, which contribute to
melting of glaciers and thermal expansion
of ocean
water — resulting in rising sea levels,» the ordinance reads.
When the ocean absorbs CO2 from the air, not only does that CO2 increase the
temperature of the
water, and cause more ice
melt, but it also causes ocean acidification.
Also at New York Times (though what to make
of «scientists said the ice sheet was not
melting because
of warmer air
temperatures, but rather because
of the relatively warm
water, which is naturally occurring, from the ocean depths»...?)
4 Contribution to SLR
Melting land base ice Thermal expansion
of water due to increase in the
temperature.
Snowfall varies across the region, comprising less than 10 %
of total precipitation in the south, to more than half in the north, with as much as two inches
of water available in the snowpack at the beginning
of spring
melt in the northern reaches
of the river basins.81 When this amount
of snowmelt is combined with heavy rainfall, the resulting flooding can be widespread and catastrophic (see «Cedar Rapids: A Tale
of Vulnerability and Response»).82 Historical observations indicate declines in the frequency
of high magnitude snowfall years over much
of the Midwest, 83 but an increase in lake effect snowfall.61 These divergent trends and their inverse relationships with air
temperatures make overall projections
of regional impacts
of the associated snowmelt extremely difficult.