Here's the reason that I found for cooling in some areas, thermohaline circulation disruption (such
as the gulf stream).»
Of course, if the aforementioned scenario isn't enough, you can also reference the effects of slowing thermohaline circulation (such
as the gulf stream) and acidification, which Coby already mentioned.
For me, that means I'd like to see it broken down, which Coby has done well so far, by (these are just examples i'd like to see): Factors and evidence supporting or effectively debunking a) ocean acidity, which in itself has produced a number of alarming effects including less saline density in turn causing a slowing of thermohaline circulation (such
as the gulf stream) b) photosynthesis - carbon sinks vs. sources or any direction that you'd like to take using what science knows CO2 to have an effect on.
Not exact matches
Of course, I dread the icy
gulfs we'll cross
as we descend along the
stream we'll ford at journey's end.
First,
as pointed out by Masters, there was a big loop in the jet
stream over the continent, funnelling warm air northwards from the
Gulf of Mexico.
Diffenbaugh Josue Viv: Do you see the
gulf stream waters staying warmer than usual
as a factor of stronger tropical systems affecting the northern east coast?
Recent monitoring does suggest a significant weakening but debate continues over whether the
gulf stream may «switch off»
as a result of the increased flows of fresh water from northern latitude rainfall and melting of the Greenland icecap.
Incessant mountain rain, snow and melting glaciers in a comparatively small region of land that hugs the southern Alaska coast and empties fresh water into the
Gulf of Alaska would create the sixth largest coastal river in the world if it emerged
as a single
stream, a recent study shows.
What unites them is a shared view of Africa, less
as a place than
as a concept, a cultural force — one that runs through the world the way a
gulf stream runs through an ocean, part of the whole, but with its own tides and temperatures.
And the same it seems all over the polar region, must wait for official November data, but if the Arctic becomes permanently warmer this suggests that a
gulf stream failure may be catastrophic not
as much for Europe but much worser for the South Atlantic.
I think these are simply features of global climate that are embedded and
as predictable
as other large features like hurricane patterns, the
gulf stream, the jet
stream, sea ice extent and mass, global glacial conditions, sea level etc..
The link between the NAO and the
Gulf Stream seems to be confirmed,
as there is a cooling trend visible of the sea surface temperatures in the
stream over the past years.
• Moist
Gulf of Mexico air failed to
stream northward in late spring
as cyclone and frontal activity were shunted unusually northward.
Also large amount of ocean heat travels poleward [such
as with
gulf stream heating Europe].
LIA wasn't GLOBAL cooling; but colder in Europe, north America — because Arctic ocean had less ice cover - > was releasing more heat / was accumulating - > radiating + spreading more coldness — currents were taking that extra coldness to Mexican
gulf — then to the Mediterranean — because Sahara was increasing creation of dry heat and evaporating extra water in the Mediterranean — to top up the deficit —
gulf stream was faster / that was melting more ice on arctic also
as chain reaction — Because Mediterranean doesn't have enough tributaries, to compensate for the evaporation deficit.
Either this is a truism (the sun must be heating the ocean surface first) or it is meant to take into account the complex circulations that occur in the ocean, like the
Gulf Stream's involvement in a vertical rise of waters from deep ocean layers in one region and sinking of the cooled surface waters
as the
stream reaches its northern limit.
2] here is why US was WET, WET, WET: before Gibraltar straights and the English Chanel opened — there was no «
Gulf - stream» Now, as soon as the surface water in the Mexican gulf warms up — GOES east,, as on a convayer - belt — no time to produce enough moisture in the
Gulf -
stream» Now,
as soon
as the surface water in the Mexican
gulf warms up — GOES east,, as on a convayer - belt — no time to produce enough moisture in the
gulf warms up — GOES east,,
as on a convayer - belt — no time to produce enough moisture in the air.
[Though it seems to me it's obvious that south pole is actually cooling and transporting greater amounts, but just taking
Gulf stream as starting point.
Just
as a jet
stream in the atmosphere separates zones of higher and lower air pressure, the fast - moving
Gulf Stream separates areas of differing MSL
as it runs up the Atlantic coast.
(If you did not intend to have the opening suggest that little or nothing has changed on this
gulf stream risk issue, please take this
as constructive criticism of * your * reporting; — RRB - and consider at least a small non-sensational statement next time that several pieces of evidence suggest that risks vis a vis the
gulf stream may be higher than the «tiny» risk level previously thought) HB