Bottom water temperature is usually close to or above zero.
It concluded what fishermen who know this cold - loving fish would have predicted: As
the bottom water temperature increased, the probability of catching a cod decreased.
Cold
bottom water temperatures of 0,5 °C was observed during the warm interstadials, which is fairly similar to what we have today.
• The methanetrack.org website has shown significant increases in atmospheric methane concentrations over Antarctica this austral winter (which I believe are due to increases in methane emissions from the Southern Ocean seafloor due to increases in the temperature of
bottom water temperatures), and if this trend continues, then the Southern Hemisphere could be a significant source of additional atmospheric methane (this century).
Shakhova et al (2013) argue that
bottom water temperatures are increasing more than had been recognized, in particular in near - coastal (shallow) waters.
The observations from the Laptev Sea in 2007 indicate that
the bottom water temperatures on the mid-shelf increased by more than 3 C compared to the long - term mean as a consequence of the unusually high summertime surface water temperatures.
Since the Arctic has and will be warmed considerably, Arctic
bottom water temperatures and their future evolution projected by a climate model were analyzed.
The record confirms that convection similar to modern took place in the Nordic seas during interstadials with cold
bottom water temperatures (BWTs) close to modern temperatures.
Measurements of stable isotopes of planktonic and benthic foram and diatom shells have been taken from hundreds of deep - sea cores around the world to map past surface and
bottom water temperatures.
She found that annual
bottom water temperatures have increased over the last 14 years, correlating with a release of about 17 teragrammes of methane a year, accentuated by storms.
Not exact matches
If
water did not decrease in density as the
temperature approached freezing, the
water in ponds and rivers would freeze from the
bottom up instead of from the top down and lots of fish and other forms of life would perish in the winter.
Bring to a boil before reducing to simmer over a low
temperature, then leave uncovered for 2 - 3 hours until thick — making sure to stir and add more
water if it starts to stick to the
bottom of the pan.
I cooked them up to 260 degrees, the very
bottom of the «hard ball» stage, as that was the
temperature at which the goo firmed up nicely when dropped in
water.
for the miso caramel: adapted from food52 ingredients: 25 g sugar 10 g
water 20 g heavy cream, room
temperature or slightly warmer 1 teaspoon shiro miso directions: Put the sugar and
water in a heavy
bottomed saucepan and bring to a boil.
Butter cake from Modern Classics Book 2: Cookies, Biscuits & Slices, Small Cakes, Cakes, Desserts, Hot Puddings, Pies & Tarts (Morrow Cookbooks) Cake: 1/2 cup + 1 tablespoon (127g) unsalted butter, very well softened 1 teaspoon vanilla extract 1 cup + 1 1/2 tablespoons (218g) caster sugar 3 eggs 1 1/2 cups + 1 1/2 tablespoons (225g) all purpose flour, sifted 1/2 teaspoon baking powder, sifted 1/4 teaspoon baking soda, sifted pinch of salt 1/2 cup (120 ml) whole milk, room
temperature Icing: 1 cup (140g) icing sugar, sifted 1 - 2 tablespoons lemon juice or
water Preheat the oven to 160 °C; butter a 20 cm (8in) round cake pan, line the
bottom with baking paper and butter the paper as well.
Heat a large pot of salted
water over high until tiny bubbles appear on the
bottom (
water temperature should be about 180 °F).
To remove the popsicles, either let them sit out for 5 - 10 minutes until soft enough to pull out, or submerge the
bottom of the popsicle mold (up to the edge of the top) in room -
temperature water for 10 - 15 seconds, then gently pull to release.
Sensors located at the top and
bottom of the tank read
water pressure,
temperature, and level, and safety switches shut the system down if the
water level gets too high or too low, respectively.
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.
In Chicago, the Park District will use a new high - tech system that uses computer software to give real - time predictions of bacteria counts based on such factors as
water temperature, modeling of the lake
bottom and wave action monitored by buoys.
The depth finder transducer comes with a built - in
water temperature sensor and can track from the
bottom up at speeds as fast as 75 mph.
It has some mapping capabilities as well as showing you the depth,
water temperature, and
bottom structure, as well as the size and depths of different fish.
It senses
water depth,
temperature,
bottom contour, and the sizes of different fish, all shown in icons on the LCD display, which can be backlit for night fishing.
It can display the
water temperature and depth and uses icons for the approximate depth and location of fish, while also showing the
bottom contour and weeds.
The Deeper App for iOS and Android interprets the data from the dual sonar frequencies to show colorful, detailed bathymetric maps as well as depth,
bottom contour, and
water temperature.
The HawkEye FT1P is a step up from our budget pick because it has a more detailed
bottom structure display as well as being able to sense the
water temperature.
The drawback with this budget model is its lack of
water temperature sensing, limited
bottom composition display and its inability to display the sizes of the different fish it senses.
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.
Rising
temperatures in the
bottom water layers could be the reason for the oxygen decline.
Known as the Antarctic
Bottom Waters (AABW), these deep, cold
waters play a critical role in regulating circulation,
temperature, and availability of oxygen and nutrients throughout the world's oceans.
al, (June, 2005): [During the Paleocene - Eocene thermal maximum (PETM), sea surface
temperature (SST) rose by 5 Deg C in the tropics and as much as 9 Deg C at high latitudes, whereas
bottom -
waters temperatures increased 4 to 5 C.
Bottom -
water temperature and current velocities have also fluctuated in relation to decadal — millennial scale climatic changes during the last de-glaciation and Holocene (Bianchi and McCave, 1999; Marchitto and deMenocal, 2003; Farmer et al., 2011; Cronin et al., 2012).
Bleaching can be caused by a host of human - induced and natural factors such as (top) intense sunlight combined with elevated
water temperature; (middle) diseases caused by bacteria, fungi, and viruses; and (
bottom) coastal pollution that reduces
water quality and increases susceptibility to bleaching.
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.
Water coming from the vents had a temperature of 17 degrees C compared to 2 degrees C for the surrounding bottom w
Water coming from the vents had a
temperature of 17 degrees C compared to 2 degrees C for the surrounding
bottom waterwater.
The combination of the
water's
temperature and salinity determines whether it rises to the surface, sinks to the
bottom, or stays at some intermediate depth.
The oxygen isotopic composition and
temperature of Southern Ocean
bottom waters during the last glacial maximum.
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.
The bone - crushing pressures and eyebrow - singing
temperatures maintain this
water in a plasma state, creating a dense, deadly ocean at the
bottom of its atmosphere.
HOW: Put a bowl under the spigot found at the
bottom of the hot
water tank, known as the T&P valve (
temperature and pressure), and open and close it a few times.
That
temperature, by the way, is when
water begins to accumulate bubbles on the
bottom of the kettle.
Most of the areas are all sand
bottom and
water temperatures hover around 75 - 85 degrees from May through November, hence no wetsuits are required.
The resort offers spacious beach strip, 1 km long and 20 m - 80 m wide, a calm sea with sandy
bottom that gradually becomes deeper, a natural park with rare tree species and curative mineral
waters springs with
temperature of 45 ° С, low mineral content, hyperthermal, hydrocarbonic, with traces of calcium, sodium, magnesium, sulphides, chlorides.
- the suit is battery - powered - the battery lets the suit stay inflated for 45 minutes to an hour - if the suit deflates with the user in it, it can become a very dangerous situation, as the user might suffocate - users bring a bottle of
water or a small fan with them inside the suit due to extremely hot
temperatures - the latest model of the suit allows the person wearing it to hear what people outside are saying - there's a small strip of clear PVC surrounding the
bottom of the Pikachu's feet - this allows the operator to see where they're walking - the operator is also able to see clearly through the suit's eyes - there's a mechanism which allows the operator to control the movement of the ears - the recommended height for an operator is 155 cm - the suit is 20 kg and the operator has to bear some of its weight on their shoulders through a harness
It was cased, plugged at the
bottom and the casing was filled with
water to facilitate
temperature measurements.
The structure of the ocean circulation basically anchors this region to something like pre-industrial
temperatures, at least until deep
bottom water originating in the North Atlantic also warms.
The resulting weaker density stratification allowed more vertical mixing of the
water column during storms in late September and early October, leading to the observed warming of the near -
bottom layer in the still ice - free Laptev Sea... Warmer
water temperatures near the seabed may also impact the stability of the shelf's submarine permafrost.»
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.
That seems a way more satisfactory approach than the crude estimate in Hansen et al (2013) that I've been using, which relies on an interpretive leap from a deep
water temperature proxy (oxygen isotope ratios from the microscopic shells of
bottom - dwelling marine critters).