Sentences with phrase «cool bottom water»

Periodically, parts of the south coast experience local, wind - driven upwelling of cool bottom water, while the fast flow of the current itself drives upwelling of deep waters, where the shelf widens to form the Agulhas Bank [11].

Close to shore, warm surface layers overlie cool bottom waters during summer [10], but this marked stratification is broken down by winter storms.

Not exact matches

Also, our apartment is cool so I put the dough in my bottom oven with a pan of hot water on the bottom to creat the warmth.

Tools recommended: - Large canning pot with a rack - funnel made for canning - ladle, preferably stainless steel - cooling rack - large heavy - bottom stainless steel pot for cooking the jam - jar lifter (made specifically for lifting jars out of hot water)- magnetic lid lifter for getting those lids out of the boiling water

You can put pan bottom in a bowl of cool water to quickly cool the syrup.

Our trick for rising was to put the bowl of dough into a large foam cooler that had a pan of warm water on the bottom and covered the cooler to keep the moist warmth in.

Directions: Bring a large pot of water to a boil / Cut a small X on the bottom of each tomato and blanch in the boiling water for 30 seconds / Remove from pot, let cool, then peel away the skin and chop coarsely / In a large soup pot, heat the olive oil and add the onions and garlic.

To loosen the popsicles from the molds, run the bottom of the molds under cool or lukewarm water for a few minutes.

I cooled in the fridge and its is hard as a rock on top and water on the bottom.

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.

The bottom is an insulated cooler, capable of holding 12 juice boxes, coconut water or beer.

Much as what unfolded during the crisis in Japan, the computer modeling suggested that fuel in one of the two reactors on the Peach Bottom site would begin to melt as soon as nine hours after a loss of cooling water flow.

Common examples include the fact that liquid water expands on cooling below 4 C, which is responsible for lakes freezing from the top rather than the bottom.

Peach Bottom's Mark I containment would then fail roughly 20 hours after the earthquake if there was no restoration of cooling water.

Surface waters become warm enough (in spring) or cool enough (in autumn) to reach 4 ° Celsius, the temperature at which these waters become dense and sink toward the lake's bottom, mixing the waters.

Cool, dense water tends to stay near the bottom and warmer buoyant water near the top.

Convection on the other hand is the movement of heated bodies themselves, like boiling water in a pot where the water at the bottom gets heated and rises to the top while the cool water from the top descends, moving closer to the flame.

Although bottom waters might be a refuge for cool - water fish species, hypoxia can force fish to seek less suitable habitats.

As it streams to the surface and mixes with the cold bottom water (at a temperature of 2 degrees C), the vent water quickly cools and dumps its load of minerals.

Set the bottom of the pot in a ice - water bath to cool, stirring frequently so that the mixture remains smooth.

That being said, if you're an extremely experienced swimmer and / or have a good swim buddy to swim with, there are some really cool things you can do without necessarily having to just swim laps back and forth in a pool while staring at the black line at the bottom of the water.

Be summer cool and splashy: If you are going to the beach or walking in the rains, it can be irksome for the bottom portion of your trousers or jeans dragging in the water puddles.

Kenny is in front of a really cool hole on the bottom right that was surrounded by water, amazing!

To cool a dog with water, you have to do it from the bottom — on their paws, chest and stomach.

Reef One / Casco's BABY biOrb is an exciting new addition to the biOrb smart aquarium family.Requiring just 4 gallons of water, it is the «baby» aquarium of the family.Ideal for novice fish keepers or those with limited space, the BABY biOrb utilizes the same powerful filtration and similar lighting to its larger siblings.The acrylic aquarium comes with stylish tops and bottoms in five different colors including cool pink and blue.www.biorbusa.com

The white sandy bottom and exceptionally crystal clear cool water with an incredible assortment of fish and vegetation make this place very unique.

Have your lunch at Metcalf Bottoms picnic area before setting out on one of the hiking trails that are easily accessible from the picnic area or try trout fishing in one of the numerous cool water streams and rivers.

The heat sink is the cold bottom water which the heat engine can pump up to cool the ocean surface and the overlying atmosphere.

This loss of heat to the atmosphere makes the water cooler and denser, causing it to sink to the bottom of the ocean.

The anomolous expansion of liquid water with cooling at temperatures less than 4 °C, means that the bottom of a frozen garden pond can remain relatively warm, if it is deep enough.

Since the deeper waters are very isolated from the surface and several degrees cooler than the surface waters, this means that the 3 oC heating of the surface can not be caused by the (cooler) bottom waters.

(Dekens 2007), corresponding to the cooling by Antarctic Bottom waters and its effect on subsurface waters.

The liquid condensed at the bottom evaporates creating local cooling and rises; the way ocean water and all water does from the surface as an enormous pool of evaporative phase change refrigerant for the surface (and the atmospheric bath of nitrogen / oxygen).

Contributions of Warm Saline Deep Water (WSDW) diminished, and the influential Antarctic Intermediate Water (AAIW) was increasingly cooled by much colder Antarctic Bottom Water.

The sinking of cold brine either penetrated to the abyss forming near freezing bottom water, or slowly cooled the subsurface waters as the brine was turbulently mixed with its surroundings.

During cooling periods, when ice sheets are expanding, ocean bottom water accumulates heavy oxygen isotopes (oxygen 18).

Not that Fred Staples will be back, but from the EPA Endangerment Response to Comments document: «For example, as a disproof of the greenhouse effect, the paper by Gerlich and Tscheuschner presents the example of a pot of water, noting that the bottom of the pot will be cooler if it is filled with water than if it is empty.

How can a body of water cooling at the top be warming at the bottom when the putative warming source is the AGW effect which is top - down?

Cold water at the poles dissolves atmospheric oxygen, cools even more, and sinks to the bottom, slowly moving to the equator, carrying the dissolved oxygen.

Latent heat plays a part in the troposphere — the bottom 6 to 10 km of the atmosphere — as warm, moist air rises it cools, water vapour condenses and heat is released.

The 1500 BTU / day heat loss would cool 50 gallons of water by (1500 BTU / day) / -LRB-(50 gal)(8.3 lb / gal)(1 BTU / lb - F)-RRB- = 4 F a day from heat loss through the bottom and sides.

The evaporative, conductive and radiative processes combined then set up a thermal gradient causing an upward flow of energy from water to air from where that 1 mm layer touches the ocean bulk below, up across the cooler layer then to the Knudsen layer by reversing the normal (warm at the top and cool at the bottom) temperature gradient which exists from that 1 mm layer down to the ocean bottom.

Weyl (1968), speculating that the «temporary stagnation» of the bottom water would end because of warming by the interior heat of the Earth; the role of glacial meltwater suppressing North Atlantic Deep Water production was also pioneered by Worthington (1968); a neat explanation of the entire circulation in terms of water evaporating from the North Atlantic more than from the cooler North Pacific was indicated by Warren (1water would end because of warming by the interior heat of the Earth; the role of glacial meltwater suppressing North Atlantic Deep Water production was also pioneered by Worthington (1968); a neat explanation of the entire circulation in terms of water evaporating from the North Atlantic more than from the cooler North Pacific was indicated by Warren (1Water production was also pioneered by Worthington (1968); a neat explanation of the entire circulation in terms of water evaporating from the North Atlantic more than from the cooler North Pacific was indicated by Warren (1water evaporating from the North Atlantic more than from the cooler North Pacific was indicated by Warren (1983).

The water runs down the radiator (cooling on the way), and is collected by the grey gutter along the bottom, which takes it back to the

Now the sun would be expected to set up an undisturbed gradient from cold at the bottom to warm at the top but it does not because upward radiation from the surface plus energy drawn upwards by evaporation at the surface creates a layer 1 mm deep near the surface (the subskin) which is 0.3 C cooler than the water below it.

We know where it starts — in the Arctic Ocean where warm water brought there by currents cools, sinks, and flows south along the bottom until it reaches West Antarctic.

In vertical profiles of water from the Gulf of Maine (above), cool, dense water is on the bottom and warmer, less dense water floats on top.

A warm band of relatively constant temperature (18 - 22 °C) and salinity (36.0 - 36.2 psu) is observed near the bottom year - round just inshore of the shelf break, bounded by seasonally variable waters on the inshore side, and by fluctuating waters subject to cool - water upwelling events and warm Gulf Stream intrusions on the offshore side.

Our climate model exposes amplifying feedbacks in the Southern Ocean that slow Antarctic bottom water formation and increase ocean temperature near ice shelf grounding lines, while cooling the surface ocean and increasing sea ice cover and water column stability.