Sentences with phrase «layer gets heated»

Your confusion arises simply because we are now discussing how the bulk of the ocean below the skin layer gets heated.

This warm air layer gets its heat reflected downwards during cloudy periods, especially during long night extensive cloudy periods, as a result, Arctic ocean ice doesn't thicken so much during darkness and leaves it up to summer sunlight (if there is some) to finish off what is left of it.

This warm air layer gets its heat reflected downwards during cloudy periods, especially during long night extensive cloudy periods, as a result, Arctic ocean ice doesn't thicken so much during darkness and leaves it up to summer sunlight (if there is some) to finish off what is left of it.

Not exact matches

Turn heat to high then shake the skillet to get vegetables into an even layer, and then then let sit and sear until browned.

I just couldn't seem to get the layered, subtle heat I wanted in this dish.

Increase the heat to high and add the beef in to the pot in a single layer and brown on all sides, turning with tongs (be careful not to crowd or overfill the pot as you will need to cook beef in batches to get a nice browning).

«The body is sensing a burn, and it's sacrificing the top layer of cells to say, «OK, they're going to die now to prevent letting the heat get farther into the body.»»

«The body is sensing a burn, and it's sacrificing the top layer of cells to say, «OK, they're going to die now to prevent letting the heat get farther into the body,»» Bosland said.

When the skillet is hot, but not smoking (if it starts to smoke, turn heat down a bit and wait 5 minutes before adding the pork) add the pork in a single layer (you may need to do this in 2 batches if your skillet is smaller) and allow it to cook for 2 - 3 minutes, so it can get a nice caramelization on it.

It heats up and cooks slightly further when broken in the steaming hot broth which gets an added layer of richness and creaminess.

Removing vernix from the skin gets rid of a natural insulating layer which can cause heat loss to be far more rapid.

Don't let your little one get too hot in the summer (overdressing can cause heat stress) or too cold in the winter (check out our vests and hoodies for that extra layer over your wrap).

Don't let your little one get too hot in the summer (overdressing can cause heat stress) or too cold in the winter (check out our vests and hoodies for that extra layer over your carrier).

Don't let your little one get too hot in the summer (overdressing can cause heat stress) or too cold in the winter (check out our vests and hoodies for that extra layer over your wrap or carrier).

We love that the aluminum core is between two layers of stainless steel so that you get optimal, even heating.

To take a specific example, the largest deviation (missing heat) was adequately explanained by increased heat exchange between 0 - 700 and 700 - 2000m ocean layers, so would it now be time to get the Arctic ice loss and the China - India brown cloud effect on Siberia and North Pacific correct?

Heat butter until it melts, let it cool and settle, then skim off the top layer of whey protein and pour off the butterfat, leaving the casein proteins on the bottom — you've got clarified butter.

For my second Design Darling blogger brunch, I knew I could get away with fewer layers since the outdoor patio at Bobo where I hosted the event is fully covered and heated (and was almost too warm with so many of us inside!).

Oh, and I also added the matching turtleneck sweater under the dress for added warmth and layering — the heat in our office isn't working right now and it gets COLD.

Vests are a great way to get the layered look without having a heat stroke in the summer.

I've been day dreaming about fall for a while now, I'm so ready for the heat to die down, add a few layers, and get back to the cozy basics!

What's great about them is they aren't a complete layer so you're not getting that extra bulk or heat that you'd get from an actual t - shirt underneath.

A long, layered cut allows your hair to air - dry brilliantly — no heat - styling needed, so you get great style and healthier locks.

This kind of weather calls for lots of light layers that can easily be shed when the heat gets to be too much.

I am not a huge summer girl because I hate the heat, don't LOVE laying out all day at the beach, and like layers (I know I live on the wrong coast), but... there is something for that magical time of year when it just starts to get hot and you can bust out your favorite jean shorts, have summer BBQs and get excited for the...

When the weather gets colder and we turn up the heat in our homes and add layers to our wardrobe, it's important to remember that our pets feel the effects of the dropping temperatures, as well.

We keep tabs on the latest in packing innovations (like machines that pack your suitcase for you), tips (like how to get your Thanksgiving dinner past airport security), and news (remember the time that man wore all his clothes at once to avoid a checked bag fee... and then passed out from the heat under all those layers?).

You make a big deal about «instantaneous», but even mixing in the upper 50 meters is not «instantaneous», so it really boils down to how fast heat gets mixed to deep layers.

Inside a greenhouse, hot air can rise only so far; so the cold layer of air on the bottom can get heated too.

On the global warming context, it's worth noting that while sea surface temperatures are hot, a more important factor for hurricane intensification (among many) is «tropical cyclone heat potential» (which includes the temperature of deeper layers of seawater that get churned up as a tropical storm passes).

The surface heat capacity C (j = 0) was set to the equivalent of a global layer of water 50 m deep (which would be a layer ~ 70 m thick over the oceans) plus 70 % of the atmosphere, the latent heat of vaporization corresponding to a 20 % increase in water vapor per 3 K warming (linearized for current conditions), and a little land surface; expressed as W * yr per m ^ 2 * K (a convenient unit), I got about 7.093.

Thus, some heat gets converted to kinetic energy, but that gets converted back to heat, either by viscosity or by thermally - indirect circulations that produce APE while pulling heat downward in the process (LHSO: Ferrel cell (driven by extratropical storm track activity), Planetary - scale overturning in the stratosphere and mesosphere (includes Brewer - Dobson circulation (I'm not sure if the whole thing is the Brewer - Dobson circulation or if only part of it is)-RRB-, some motions in the ocean; LVO: wind driven mixing of the boundary layer and of the upper ocean (though mixing itself tends to destroy the APE that the kinetic energy would create by forcing heat downward)-RRB-.

Add in that if it's the sun, the entire atmosphere will warm, since there's just simply more energy put in to the system, whereas if it is CO2 or other blanketing method, there's no extra energy put in, therefore the ground will warm and the upper air cool (since the upper air isn't getting the warming from the lower layers it used to get and the lower layers aren't losing the heat they used to).

If the surface layer of the ocean is not quickly exchanging energy with the troposphere, which it can do easily and quickly but retaining the energy, why is it not heating up far more rapidly, If you are saying it is getting rid of it to the deep oceans, how precisely is it doing this so quickly?

I just don't see how you get from W / M2 to temperature without dealing with the specific heat of the various layers of the atmosphere and oceans.

What do you get when you combine copious amounts of government grant money, layers of dishonesty, the heat of environmental activism, a few dollops of ambition, and a glaze of science in a political pressure cooker?

The amount of extra heat stored at the surface layer of the ocean wanting to get out is cubed.

If you're calculating that as AGWSF teaches you to calculate by the sleight of hand planckian graphic that the 300 mile wide visible layer atmosphere around the Sun defines its heat, then you get the fake fisics meme of 6,000 °C.

Nothing like a complex system with many thermodynamic boundary layers or different heat capacities if you get tired of crossword puzzles:)

The interior won't get hotter because it heats a new layer of steel on top of it.

The climate models have gotten more complex, for sure, with thousands of estimated parameters for warming potential, vorticity, circulation patterns, absorption of heat, pressure, energy, and momentum by various layers or atmosphere, land, ocean, and sea - ice.

This gets ride of hundred of words about about molecules interacting etc Then we get the isothermal case You did not comment on the fact that in the adiabatc case it needs a negligable amount of energy to raise a parcel of air from botton to top but if your silver wire delivers heat from the bottom layer to the top layer the outside work must be done to restore DALR.

TURBULANT FLOW; (wind in surges, eddies, chaotic flow, spkiy erratic velocity) Layer of hot air canopy gets MIXED and heat in the boudary escapes to the sky.

Do you see how a house also gets heating below its insulating layer by a fireplace?

Do you understand how when heat gets inside an insulating layer it can be trapped by said insulator?

Why, because that boundary layer of air created by those little tiny hairs, get disturbed, gets mixed and heat exchange happens.

If I use a time step which is too long then too much heat gets transferred from the layers below the surface to the 5 mm surface layer in the one time step, the model starts oscillating — and finally «loses the plot».

If more DLR from more CO2 enters the skin layer, less heat from absorbed SWR will need to flow upwards, and the ocean will get warmer.

It will get warmer as heat transfers from the hot surface to the colder layers below.

Put a heat lamp on a dimmer to minimize visible radiation over a pot of water and see if the layer just below the surface of the pot gets cooler.