Observational data on many key climatic variables is extremely limited, particularly for sluggish components of the system such
as deep ocean currents.
Not exact matches
These revealed a surprising link between stratospheric winds and
ocean currents as deep as 2 kilometers beneath the waves.
Thermohaline circulation, also known
as the
ocean's conveyor belt, refers to the
deep ocean density - driven
ocean basin
currents.
A March study shows that one large swath of the ice sheet sits on beds
as deep as 8,000 feet below sea level and is connected to warming
ocean currents.
The preliminary results, analyzed by paleoclimatologist Pierre Sepulchre of the Climate and Environment Laboratory, suggest that with any channel
deeper than 200 meters
currents behave
as though there's an entire
ocean there.
As changes happen in the polar regions, they are carried around the world by
ocean currents, both at the surface and in the
deep ocean.
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.
i.e. changes in precipitation, vegetation,
deep ocean currents, etc. are at any time
as likely to cool
as to heat.
As the abstract to K08 talks about
ocean currents and that was the impression I got from previous discussions of that paper I thought (2) was the main concern and specifically that the heat was going into the
deep ocean.
But
as cogently interpreted by the physicist and climate expert Dr. Joseph Romm of the liberal Center for American Progress, «Latif has NOT predicted a cooling trend — or a «decades - long
deep freeze» — but rather a short - time span where human - caused warming might be partly offset by
ocean cycles, staying at
current record levels, but then followed by «accelerated» warming where you catch up to the long - term human - caused trend.
Instead, they see a periodic slowdown in the vast turnover of oceanic
currents as locking in CO2 into the
deep oceans.
The clues found in sediments deposited during the late Holocene suggest that an
ocean current that circles the southern polar region, known
as Circumpolar
Deep Water, flowed underneath the Cosgrove Ice Shelf and melted it.
In the Atlantic
Ocean, the current known as the Atlantic Meridional Overturning Circulation (AMOC) ferries warm surface waters northward — where the heat is released into the atmosphere — and carries cold water south in the deeper ocean layers, according to the National Oceanic and Atmospheric Administra
Ocean, the
current known
as the Atlantic Meridional Overturning Circulation (AMOC) ferries warm surface waters northward — where the heat is released into the atmosphere — and carries cold water south in the
deeper ocean layers, according to the National Oceanic and Atmospheric Administra
ocean layers, according to the National Oceanic and Atmospheric Administration.
Third,
as first observed in the 1990s, the area is vulnerable to a regional
ocean current, ushered in by the shape of the sea floor and the proximity of the circumpolar
deep current.
«The top of the glacier is melting away
as a result of decades of steadily increasing air temperatures, while its underside is compromised by
currents carrying warmer
ocean water, and the glacier is now breaking away into bits and pieces and retreating into
deeper ground.»
However enough fresh cold water comes in on the polar
currents ensure that overall the
deep oceans stay
as cold
as (but no colder than) the poles.
This is not perfect because it is likely that climate effects such
as ocean currents and oscillations, changes in biology, ice extent and volume changes, cloud cover variations, etc... are causing a kind of climactic Brownian Motion, hiding the signal in what, lacking
deep understanding of these issues, we can only call noise.