The project, called the Arctic Ice Dynamics Joint Experiment, was the first major study of how sea - ice moves and changes due to
ocean and atmosphere influences.
The induction of kinetic energy from the land surface materialing interacting with available incident photons is a primary source of kinetic energy, via conduction and convection, to
the oceans and atmosphere influencing both.
Not exact matches
Science questions the answers, e.g. hurricanes are caused by warm moist
ocean air being drawn up into the cooler
atmosphere and creating a wind pattern though we are still open to consider other factors that may have
influence on this cycle.
A study led by scientists at the GEOMAR Helmholtz Centre for
Ocean Research Kiel shows that the ocean currents influence the heat exchange between ocean and atmosphere and thus can explain climate variability on decadal time sc
Ocean Research Kiel shows that the
ocean currents influence the heat exchange between ocean and atmosphere and thus can explain climate variability on decadal time sc
ocean currents
influence the heat exchange between
ocean and atmosphere and thus can explain climate variability on decadal time sc
ocean and atmosphere and thus can explain climate variability on decadal time scales.
«I never considered that weather events tens of kilometers high in the
atmosphere significantly
influence the decadal - to century - scale circulation kilometers deep into the
ocean,» says climatologist Judah Cohen of Atmospheric
and Environmental Research in Lexington, Massachusetts, who did not take part in this study.
The models must track how carbon dioxide
and other greenhouse gases cycle through the whole system — how the gases interact with plant life,
oceans, the
atmosphere —
and how this
influences overall global temperatures.
That region, he says, is susceptible to even small amounts of warming
and cooling from the
atmosphere —
and how cold the water gets
influences how much or how little it sinks, thereby driving or delaying, respectively, the
ocean conveyer belt.
The next step was see how those factors were
influenced by ENSO; while El Niños
and La Niñas are defined by how much warmer or colder than normal tropical Pacific
ocean waters are, they trigger a cascade of reactions in the
atmosphere that can alter weather patterns around the globe.
«The tropical Pacific
ocean -
atmosphere system has been called a sleeping dragon because of how it can
influence climate elsewhere,» said lead author Aradhna Tripati, a UCLA assistant professor in the departments of Earth, planetary
and space sciences,
and atmospheric
and oceanic sciences.
When these worms began to mix up the
ocean floor's sediments (a process known as bioturbation), their activity came to significantly
influence the
ocean's phosphorus cycle
and as a result, the amount of oxygen in Earth's
atmosphere.
Covering nearly 5.5 million square miles, the frozen mass exerts an enormous
influence on the global climate, reflecting sunlight back into space
and cooling Earth's
atmosphere and oceans.
For half a century, the Florida State University Geophysical Fluid Dynamics Institute (GFDI) has been a global leader in the study of fluid flow
and motion — the ways that the circulation of liquids
and gases
influence our
oceans,
atmosphere and groundwater.
Together with shipboard
and satellite data, the global network of measuring sites provides further understanding of the
ocean -
atmosphere system
and its
influence on global climate
and biological productivity.
These changes might
influence interactions between the
ocean and the
atmosphere such as the air - sea gas exchange
and the emission of sea - spray aerosols that can scatter solar radiation or contribute to the formation of clouds.
ENSO events, for example, can warm or cool
ocean surface temperatures through exchange of heat between the surface
and the reservoir stored beneath the oceanic mixed layer,
and by changing the distribution
and extent of cloud cover (which
influences the radiative balance in the lower
atmosphere).
The latter is almost linearly related to changes in ice sheet volume; the former, however, is
influenced by a range of factors, including
atmosphere /
ocean dynamics
and changes in Earth's gravitational field, rotation,
and crustal
and the mantle deformation associated with the redistribution of mass between land ice
and the
ocean.
The
atmosphere is simply electrifying as suspense builds throughout the live shows,
and the
ocean breeze reminds visitors that they are in a very spiritual island;
influenced by centuries of beliefs in the mystical
and divine.
Human
influence has been detected in warming of the
atmosphere and the
ocean, in changes in the global water cycle, in reductions in snow
and ice, in global mean sea level rise,
and in changes in some climate extremes.
ENSO events, for example, can warm or cool
ocean surface temperatures through exchange of heat between the surface
and the reservoir stored beneath the oceanic mixed layer,
and by changing the distribution
and extent of cloud cover (which
influences the radiative balance in the lower
atmosphere).
At the Paris meeting, nearly 2,000 participants, from countries on all continents
and at all levels of development, flowed through dozens of sessions examining an array of policies
and actions at all scales that could limit our
influence on the
atmosphere and oceans and limit risks that changes in the climate will derail human progress.
And since the 1970 ′ s on average there's about a 4 % increase in water vapor over the Atlantic Ocean and when that gets caught into a storm, it invigorates the storm so the storm itself changes, and that can easily double the influence of that water vapor and so you can get up to an 8 % increase, straight from the amount of water vapor that's sort of hanging around in the atmosphe
And since the 1970 ′ s on average there's about a 4 % increase in water vapor over the Atlantic
Ocean and when that gets caught into a storm, it invigorates the storm so the storm itself changes, and that can easily double the influence of that water vapor and so you can get up to an 8 % increase, straight from the amount of water vapor that's sort of hanging around in the atmosphe
and when that gets caught into a storm, it invigorates the storm so the storm itself changes,
and that can easily double the influence of that water vapor and so you can get up to an 8 % increase, straight from the amount of water vapor that's sort of hanging around in the atmosphe
and that can easily double the
influence of that water vapor
and so you can get up to an 8 % increase, straight from the amount of water vapor that's sort of hanging around in the atmosphe
and so you can get up to an 8 % increase, straight from the amount of water vapor that's sort of hanging around in the
atmosphere.
We know that the number of tropical cyclones is
influenced by several factors: the seasonal cycle, the geography,
ocean temperatures
and the wind structure in the
atmosphere.
Since Mars has no
oceans and a thin
atmosphere, the thermal inertia is low,
and Martian climate is easily perturbed by external
influences, including solar variations.
So with this reasoning, I have convinced myself that the initial conditions
and short term variability of the
ocean /
atmosphere may well be very important in
influencing the ultimate longer term trajectory of the climate system.
These must have an important effect on latent
and sensible heat fluxes from the
ocean to the
atmosphere,
and ultimately
influence the TOA radiative imbalance
and the
ocean heat storage.
Roger Revelle, one of the pioneering researchers in the study of the human
influence on the
atmosphere, carbon cycle
and climate, gave a prescient lecture on carbon dioxide, climate
and the
oceans in 1980 that was recorded by the Lawrence Livermore National Laboratory
and now surfaces via the Web site Climate Science TV.
Human
influence has been detected in warming of the
atmosphere and the
ocean, in changes in the global water cycle, in reductions in snow
and ice, in global mean sea level rise,
and in changes in some climate extremes (see Figure SPM.6
and Table SPM.1).
(3) Subordinate to solar activity alone, atmospheric water vapor / cloud formation
and movement is the largest known variable that
influences temperature changes in the
atmosphere of the earth,
and the earth's
oceans.
While the individual flows are relative huge, the fact that
oceans and vegetation are each opposite makes that the
influence in the
atmosphere is resticted: 16 ppmv in Barrow, 8 ppmv at MLO, 2 ppmv at the south pole.
Dan Barrie, program manager at NOAA, called the research «compelling»
and said: «[It] provides a powerful illustration of how the remote eastern tropical Pacific guides the behaviour of the global
ocean -
atmosphere system, in this case exhibiting a discernible
influence on the recent hiatus in global warming.»
The interaction of
ocean and atmosphere is a complicated one, with a number of factors at work that
influence the growth of sea ice.
GFDL's research encompasses the predictability
and sensitivity of global
and regional climate; the structure, variability, dynamics
and interaction of the
atmosphere and the
ocean;
and he ways that the
atmosphere and oceans influence,
and are
influenced by various trace constituents.
Plants
and plankton
influence the composition of the
atmosphere, play a part in the water cycle,
and regulate
ocean chemistry.
The evolution of El Niño - Southern Oscillation (ENSO) variability can be characterized by various
ocean -
atmosphere feedbacks, for example, the
influence of ENSO related sea surface temperature (SST) variability on the low - level wind
and surface heat fluxes in the equatorial tropical Pacific, which in turn affects the evolution of the SST.
New research by Misra
and Mishra in the Journal of Geophysical Research:
Atmospheres shows that differences in the
ocean bathymetry (or topography) of two novel numerical climate model integrations can
influence the
ocean currents
and their impact on regional climate.
Obviously, any portion of the
atmosphere /
ocean is
influenced by its neighbors,
and them by theirs, etc..
Henry's Law still holds, as the amount of free CO2 in the water follows the increase in the
atmosphere, but free CO2 is less than 1 % of the total amount of carbon in the
oceans surface layer, the bulk are bicarbonates
and carbonates, which don't follow Henry's Law, but
influence the amount of free CO2.
In times when the
oceans are warming, there could be several factors that
influence this, each with varying contributions based on natural
and / or anthropogenic variability: 1) Greater solar output 2) Less aerosols in the
atmosphere 3) Less cloudiness (especially of a certain type) 4) Increased greenhouse gases
These two mechanisms are so strongly dependent on the temperature difference between the
ocean surface ant the
atmosphere that the net
influence on the skin temperature
and on the net heat transfer between the
ocean and the
atmosphere is negligible.
Regardless of near term outcomes — it is odds on for a cooler sun
and more upwelling in the Pacific
Ocean this century — providing a cooling
influence on the
oceans and atmosphere and the inevitable regional variability in rainfall.
Ice significantly reduces the heat flux between
ocean and atmosphere; through its high albedo it has a strong
influence on the radiation budget of the entire Arctic.
That suggests that cooling may start with changes in the
ocean circulation,
influencing the northern sea surface
and atmosphere, said co-author Jerry McManus, a professor at Lamont - Doherty Earth Observatory.
And because the Arctic is the fastest - warming region on Earth, and because atmosphere and ocean influence each other, the steady loss of sea ice each year has forced a change in wind patter
And because the Arctic is the fastest - warming region on Earth,
and because atmosphere and ocean influence each other, the steady loss of sea ice each year has forced a change in wind patter
and because
atmosphere and ocean influence each other, the steady loss of sea ice each year has forced a change in wind patter
and ocean influence each other, the steady loss of sea ice each year has forced a change in wind patterns.
[click, Image 2] Climate predictions are focused on longer - term
influences of the sun,
oceans, land,
and ice on the
atmosphere.
The fractal properties of the ice cover
and its extreme variability strongly
influence the
atmosphere -
ocean interactions
and the dynamics of the Arctic marine ecosystems.
Detecting trends in Atlantic
and eastern North Pacific hurricane activity is challenged by a lack of consistent historical data
and limited understanding of all of the complex interactions between the
atmosphere and ocean that
influence hurricanes.4, 5,6
Solar UV
influences on
ocean /
atmosphere coupling — as Lockwood
and others have suggested recently — seems a more likely mechanism in climatologically important tropical marine zones.
Since the
ocean temperature affects the air above the water
and movements of air in the
atmosphere contribute to our weather, El Niño can
influence weather patterns.
As the term implies, global warming is the gradual increase in the average temperature of the
atmosphere and ocean due to human
influences.
These areas of open water
influence: (1) the land by allowing more
ocean waves
and more coastal erosion, (2) Greenland outlet glaciers by exposing the glacier fronts to warmer
ocean waters,
and (3) the
atmosphere by providing a source of heat
and moisture during autumn.