Not exact matches
A steam plume rises
from Bogoslof volcano as hot lava
heats the
seawater during an eruption in August 2017.
Charlie's research told him that during El Niño weather cycles, the surface
seawaters in the Great Barrier Reef lagoon, already
heated to unusually high levels by greenhouse gas — induced warming, were being pulsed
from a mass of ocean water known as the Western Pacific Warm Pool onto the reef's delicate living corals.
Hydrothermal vents, where
heated, mineral - laden
seawater spews
from cracks in the ocean crust, are home to various diverse organisms.
The models reveal a «hydrothermal siphon» driven by
heat loss
from deep in the Earth and the flow of cold
seawater down into the crust and of warmed water up out of the crust.
The
seawater is
heated by the magma; the hot water rises again, leaches metals and other elements
from the ground and is released as a black colored solution.
The
heat apparently derives
from a chemical reaction between mantle rock and
seawater.
By Year 1.1 billion, deep - sea hematite - bearing rock found in the Marble Bar chert formation of northwestern Australia indicates that iron - rich water gushed
from volcanically
heated seafloor vents were able to mix with cooler oxygen - rich
seawater (Ohmoto et al, Nature Geoscience, March 15, 2009; PSU press release, and in EurkaAlert; and Sid Perkins, ScienceNews, April 11, 2009).
In this
seawater spa hotel in Biarritz you feel as if you are on a cruise ship, gazing over the Bay of Biscay
from vast windows, private terraces and a
heated pool on the deck.
The study also revealed that the ice melting that was caused by the storm was the result of
heat coming
from the stirring of
seawater layers below the ice.
The open cycle consists of the following steps: (i) flash evaporation of a fraction of the warm
seawater by reduction of pressure below the saturation value corresponding to its temperature (ii) expansion of the vapor through a turbine to generate power; (iii)
heat transfer to the cold
seawater thermal sink resulting in condensation of the working fluid; and (iv) compression of the non-condensable gases (air released
from the
seawater streams at the low operating pressure) to pressures required to discharge them
from the system.
And that
heat transfer
from as yet unfrozen
seawater may generate the higher arctic pressures that drive cold air masses southward.