Sentences with phrase «meaning warm surface waters»

With an El Niño now under way — meaning warm surface waters in the Pacific are releasing heat into the atmosphere — and predicted to intensify, it looks as if the global average surface temperature could jump by around 0.1 °C in just one year.

Not exact matches

A new El Niño cycle — warmer surface waters — began last summer, which may mean that stratospheric water levels could change again.
Because water expands as it warms, that heat also meant that sea surface heights were record high, measuring about 2.75 inches higher than at the beginning of the satellite altimeter record in 1993.
In general, the regions of expanding warming upwelling water in the Indian Ocean, North Pacific, or wherever they are, must create slight bulges in the surface, and the regions of shrinking, cooling, sinking water in the Arctic must create slight depressions in the sea surface (again, I mean in a very low pass sense — obviously storms, tides, etc, create all kinds of short - terms signals obscuring this).
The water vapor cooled the Earth, the snow cooled the atmosphere with resulting increase in surface albedo which does reflect radiative heat, meaning the Earth gets less warm, not colder because of it.
Other experts point out one of the biggest natural factors behind the plateau is the fact that in 2008 the temperature cycle in the Pacific flipped from «warm mode», in which it had been locked for the previous 40 years, to «cold mode», meaning surface water temperatures fell.
The warmer the ocean becomes, the less water rises from deeper down, meaning fewer resources will be brought to the surface water where phytoplankton live.
New Dutch research has shown for instance the overturning has been relatively weak in recent years [which means cold water has accumulated close to the surface instead of sinking to deeper waters, one of two reasons why there has been a lull in upper ocean warming].
Francisco (09:12:57): Go ahead and explain how additional heat in the atmosphere moves from the atmosphere to the ocean surface, and from there to the deep oceans, ** without first producing any warming in the atmosphere or on the ocean surface water ** Just because you don't know how it can happen, does not mean that it is not happening, just that you don't understand how.
Many readers seem to think the «+» means positive as in «warm surface water» and that, conversely, the «--» means negative as in «cold surface water».
In 1997 and 1998 there was a strong El Nino event in the equatorial Pacific, meaning that the surface water there was unusually warm.
The hurricane churned up water 100 or even 200 meters below the surface, said Trenberth, but this water was still warmmeaning that the storm could keep growing and strengthening.
Presumably you mean a patch of water on the ocean cooled by a value D degs.C would reduce the surface temperature by more than an equal and opposite patch of water warmed by D Degs.C would warm it *.
With 2), there's still something I don't get... and this applies just as much to your answer as to any answers you would get from climate science, since clouds are clouds (i.e droplets of water), and water vapour is a gas, so their back - radiation explanation doesn't even apply in the case of clouds (not saying it physically could apply anywhere but hopefully you get what I mean)... what I don't get is, you liken them to a blanket, but a blanket is next to you, clouds are separated from the surface by quite a bit of atmosphere — so why is it warmer the next morning at the surface when the clouds are there?
This would make the surface ocean less salty, which (along with the warming) makes the surface waters less dense, and less likely to sink, meaning that the AMOC would weaken or maybe collapse completely.
Yet an increase in the surface area of crevasses can accelerate the flow because it means more of the ice's interior is exposed to warming by surface melt water.
It means that the global sea surface temperatures used by Endersbee in his calculations have been controlled by warming of the sea surface waters outside the tropical sea surface i.e. mainly the warming of the sea surface waters of higher latitudes where the sea surface CO2 sinks are.
Because the temperature gradient in a planet's troposphere is the state of thermodynamic equilibrium which the Second Law of Thermodynamics says will evolve, the planet's supported surface temperature is autonomously warmer than its mean radiating temperature, so warm in fact on Earth that we need radiating gases (mostly water vapour) to reduce the gradient and thus cool the surface from a mean of about 300K to about 288K, this being confirmed by empirical evidence (as in the study in my book) which confirms with statistical significance that water vapour cools rather than warms, all these facts thus debunking the greenhouse conjecture.
«''» Earth that we need radiating gases (mostly water vapour) to reduce the gradient and thus cool the surface from a mean of about 300K to about 288K, this being confirmed by empirical evidence (as in the study in my book) which confirms with statistical significance that water vapor cools rather than warms, all these facts thus debunking the greenhouse conjecture.
Note: LOTI provides a more realistic representation of the global mean trends than dTs below; it slightly underestimates warming or cooling trends, since the much larger heat capacity of water compared to air causes a slower and diminished reaction to changes; dTs on the other hand overestimates trends, since it disregards most of the dampening effects of the oceans that cover about two thirds of the Earth's surface.
What they forget to mention is that this warming is not by radiative means but simply by the latent heat in water vapour stolen from what would have been a warmer surface.
The «note» you refer to goes: «Note: LOTI provides a more realistic representation of the global mean trends than dTs below; it slightly underestimates warming or cooling trends, since the much larger heat capacity of water compared to air causes a slower and diminished reaction to changes; dTs on the other hand overestimates trends, since it disregards most of the dampening effects of the oceans that cover about two thirds of the earth's surface
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