Another potential effect of climate change is related to energy
transport from surface waters to the seafloor [261], [262].
Not exact matches
The major influences on ocean chemistry today are hydrothermal flow (hot
water that has circulated through the crust) and
surface weathering (the river
transport of material eroded
from land into the ocean).
«In that area, like on the eastern boundaries of other tropical oceans, nutrient - rich
waters from deeper
water layers are
transported to the
surface,» explains co-author Prof. Dr. Hermann Bange, also
from GEOMAR.
All of this is compounded by the fact that trees close their stomata (
surface pores that control gas exchange) when facing drought to prevent
water loss
from transpiration, but this can collapse the hydraulic
transport system.
He does so by, retreiving the fallen pinwheel
from the
Surface,
transport water from Faron to the Fire Sanctuary, and carry a large basin of Hot Pumpkin Soup to Levias.
Recreating the core tenets of the early arcade game, Aqua Kitty tasked players with protecting a pack of subaquatic, diver - suit clad felines
from a steady succession of foes who were hell - bent on
transporting the cats to the
water's
surface.
(In the global time average, diffusion of latent heat is in the same direction as sensible heat
transport, but latent heat will tend to flow
from higher to lower concentrations of
water vapor (or equilibrium vapor pressure at the liquid / solid
water surface), and regionally / locally, conditions can arise where the latent heat and sensible heat fluxes are oppositely directed.)
Finally, you mention
water vapour as a GHG... but
water vapour is the main cooling component in the atmosphere,
transporting heat
from the
surface to the radiative layer, so not really a true GHG.
Warm
surface water flows
from the tropical South Atlantic, through the Caribbean, and is then
transported, via the Gulf Stream and North Atlantic Drift, to the northernmost North Atlantic.
The wind stress on the
surface of the sea causes the
water level on a coast to rise if the net
transport of
water is towards land and to fall if it is away
from land.
As to the absorption of long - wave radiation
from the earth's
surface, while it may be true that carbon dioxide and
water together do absorb certain frequency ranges of that radiation, I don't think that that matters a whole lot because most of the heat
from the
surface is
transported to the top of the troposphere by conduction, convection and latent heat of vaporization of
water during the day.
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..
There is also a planetary boundary layer module that evaluates the turbulent
transport of heat and
water vapor
from the ground
surface into the atmosphere.
The extra boost
from the warmer
water is adding even more energy into this storm system, increasing the availability and
transport of moisture toward land and producing more efficient wind gusts to the
surface.
Mineral dust
from anthropogenic sources originates mainly
from agricultural practices (harvesting, ploughing, overgrazing), changes in
surface water (e.g., Caspian and Aral Sea, Owens Lake) and industrial practices (e.g., cement production,
transport)(Prospero et al., 2002).
Evaporation
from the
surface plays a key role, but the researchers also took into account how the evaporated
water is
transported into the atmosphere.
They combined simple energy balance considerations with a physical assumption for the way
water vapour is
transported, and separated the contributions of
surface heating
from solar radiation and
from increased greenhouse gases in the atmosphere to obtain the two sensitivities.
The amount of detrital petrological tracers
transported by icebergs and deposited in the ice - rafted debris belt (an Atlantic region between 40 - 50 ° N) greatly increases during episodes of southward and eastward advection of cold
surface waters and drift ice
from the Nordic and Labrador seas (Bond et al., 2001; figure 48 A).
And at the same time, krill also play a key role in slowing global warming, as they
transport carbon dioxide
from the
surface to the deep
water.
All that is needed is to add heat carried upwards past the denser atmosphere (and most CO2) by convection and the latent heat
from water changing state (the majority of heat
transport to the tropopause), the albedo effects of clouds, the inability of long wave «downwelling» (the blue balls) to warm
water that makes up 2 / 3rds of the Earth's
surface, and that due to huge differences in enthalpy dry air takes far less energy to warm than humid air so temperature is not a measure of atmospheric heat content.
The scientists estimated that the swarm consumed up to 74 percent of microscopic carbon - containing plants
from the
surface water per day, and their sinking fecal pellets
transported up to 4,000 tons of carbon a day to deep
water.
«The differences between sea
water temperature reported in the Log of Ship's Weather Observations and specially observed sea
surface temperature were studied for 6826 pairs of observations taken in the Pacific Ocean
from 3 Military Sea
Transport Service ships and 9 U.S. Navy Radar Picket ships during 92 different trips.
It's also important to point out, however, that although changes in evaporation, convection and latent heat
transport, humidity,
water vapor, clouds, and other quantities affect the
surface temperature response, they are excluded
from the Planck («no - feedback») response by definition.
Coastal upwelling occurs where Ekman
transport moves
surface waters away
from the coast;
surface waters are replaced by
water that wells up
from below.