Two model studies show an explicit dependence of
ocean heat transport on resolution, ranging between 4 ° and 0.1 ° (Fanning and Weaver, 1997a; Bryan and Smith, 1998).
Webb, R.S., D.H. Rind, S.J. Lehman, R.J. Healy, and D. Sigman, 1997: Influence of
ocean heat transport on the climate of the Last Glacial Maximum.
The YD shows strongly up in GRIP but is much less pronounced in the Antarctic cores because interrupting the AMOC turns poleward
ocean heat transport on and off causing abrupt NH climate change.
Not exact matches
«We found that
heat transported by
oceans would have a major impact
on the temperature distribution across a planet, and would potentially allow a greater area of a planet to be habitable.
«The Importance of Planetary Rotation Period for
Ocean Heat Transport» is published in the journal Astrobiology
on Monday, July 21, 2014.
Because
ocean currents play a major role in
transporting the planet's
heat and carbon, the ECCO simulations are being used to understand the
ocean's influence
on global climate and the melting of ice in polar regions.
These systems play a major role in
transporting heat and carbon, and are therefore indispensable to understanding the
ocean's influence
on climate.
A continual cycle of
heat and moisture is pulled from the tropical
ocean and
transported around the globe
on belts of atmospheric energy.
During a postdoctoral fellowship at MIT, Cambridge USA, his research interest focused
on the interaction between
ocean eddies and deep convection regions and their respective
heat and density
transports.
At the same time, increasing depth and duration of drought, along with warmer temperatures enabling the spread of pine beetles has increased the flammability of this forest region — http://www.nature.com/nclimate/journal/v1/n9/full/nclimate1293.html http://www.vancouversun.com/fires+through+tinder+pine+beetle+killed+forests/10047293/story.html Can climate models give different TCR and ECS with different timing / extent of when or how much boreal forest burns, and how the soot generated alters the date of an ice free Arctic
Ocean or the rate of Greenland ice melt and its influence
on long term dynamics of the AMOC
transport of
heat?
Based
on transient climate model simulations of glacial - interglacial transitions (rather than «snapshots» of different modeled climate states), Ganopolski and Roche (2009) proposed that in addition to CO2, changes in
ocean heat transport provide a critical link between northern and southern hemispheres, able to explain the apparent lag of CO2 behind Antarctic temperature.
3) Can you confirm that the temperature and net flux data for GISS - E2 - R, available via the CMIP5 portals and KNMI Climate Explorer are based
on a model corrected to fix the
ocean heat transport problem which you identified in the Russel
ocean model in your 2014 paper?
There is a tremendous amount of
ocean heat transport from both the Pacific and the Atlantic going
on in the Arctic.
These processes affect the
transport of water,
heat, salinity, nutrients and carbon in the
ocean, impacting
on the climate system by modifying it's ability to absorb human - emitted carbon dioxide and excess
heat resulting from increased carbon dioxide concentrations.
The conventional view
on the connection between the AMOC and Arctic sea ice is that a weakening of the AMOC should reduce
ocean poleward
heat transport and, hence, expand sea ice.
I happen to think
ocean heat transport is the primary factor so would consider just a slow down in melt rate an error
on the melting side of the argument.
AGW climate scientists seem to ignore that while the earth's surface may be warming, our atmosphere above 10,000 ft. above MSL is a refrigerator that can take water vapor scavenged from the vast
oceans on earth (which are also a formidable
heat sink), lift it to cold zones in the atmosphere by convective physical processes, chill it (removing vast amounts of
heat from the atmosphere) or freeze it, (removing even more vast amounts of
heat from the atmosphere) drop it
on land and
oceans as rain, sleet or snow, moisturizing and cooling the soil, cooling the
oceans and building polar ice caps and even more importantly, increasing the albedo of the earth, with a critical negative feedback determining how much of the sun's energy is reflected back into space, changing the moment of inertia of the earth by removing water mass from equatorial latitudes and
transporting this water vapor mass to the poles, reducing the earth's spin axis moment of inertia and speeding up its spin rate, etc..
Warm currents
transport heat from lower latitudes poleward and tend to occur
on the western sides of
oceans.
While the circulation of the Atlantic
Ocean has a complex three - dimensional spatial structure, the zonally integrated flow in the basin, referred to as the Atlantic Meridional Overturning Circulation (AMOC), is largely responsible for the net northward oceanic
heat transport on climate - relevant timescales.
A commentator
on the ClimateAudit thread has asked Gavin Schmidt, in a comment submitted to RealClimate, whether temperature and net flux data for GISS - E2 - R available via the CMIP5 portals and KNMI Climate Explorer are based
on a model corrected to fix the
ocean heat transport problem.
On account of its ability to absorb and
transport enormous amounts of
heat, the
ocean also plays an outsized role in climate change and is an important factor in the explaining the asymmetric response of the north and south poles to the changing climate.
These oscillations are superimposed
on a long term trend of increasing poleward
ocean heat transport.
We think, based
on basic physics and computer model simulations, that this can induce
ocean currents that
transport heat laterally and thereby affect climate.
This implies stronger
transport of
heat to the deep
ocean and polar
oceans than is going
on today, and suggests the observations are tracking in that direction.
The global oceanic conveyer belt, is a unifying concept that connects the
ocean's surface and thermohaline (deep mass) circulation regimes,
transporting heat and salt
on a planetary scale.
actually the average temperature depends strongly
on meridional circulation that
transports a lot of
heat towards the high latitudes — especially with
oceans that are, to say the least, not very well described and understood.
3) Can you confirm that the temperature and net flux data for GISS - E2 - R, available via the CMIP5 portals and KNMI Climate Explorer are based
on a model corrected to fix the
ocean heat transport problem which you identified in the Russell
ocean model in your 2014 paper?
These experiments provide new insight into mechanisms of past climate changes
on Earth, which have been driven in part by tectonic changes in
ocean basins and consequent changes in
ocean circulation and
heat transport.
Effects of tropical cyclones
on ocean heat transport in a high resolution coupled general circulation model.
Atlantic meridional
ocean heat transport at 26N: impact
on subtropical
ocean heat content variability
Air - sea interaction, wave dynamics and wave breaking, effect of near - surface turbulence
on heat, gas, and momentum
transport, infrared remote sensing, upper -
ocean processes, coastal and estuarine processes.
Fasullo and Trenberth (2008b) went
on to evaluate the temporal and spatial characteristics of meridional atmospheric energy
transports for
ocean, land, and global domains, while Trenberth and Fasullo (2008) delved into the
ocean heat budget in considerable detail and provided an observationally based estimate of the mean and annual cycle of
ocean energy divergence and a comprehensive assessment of uncertainty.