In association with El Niño, the heat redistribution in the ocean creates a major reorganization
of atmospheric convection, severely disrupting global weather patterns from Australia to India and from South Africa to Brazil.
This is incorrect because about half of the additional delta eK is a result
of atmospheric convection that causes friction within the system and in contact with the earth's surfaces.
«The authors write that «the El Niño - Southern Oscillation (ENSO) is a naturally occurring fluctuation,» whereby «on a timescale of two to seven years, the eastern equatorial Pacific climate varies between anomalously cold (La Niña) and warm (El Niño) conditions,» and that «these swings in temperature are accompanied by changes in the structure of the subsurface ocean, variability in the strength of the equatorial easterly trade winds, shifts in the position
of atmospheric convection, and global teleconnection patterns associated with these changes that lead to variations in rainfall and weather patterns in many parts of the world,» which end up affecting «ecosystems, agriculture, freshwater supplies, hurricanes and other severe weather events worldwide.»»
Furthermore, the majority of the Earth's precipitation falls in the tropics and is a direct result
of atmospheric convection; it is therefore a key area for improving ESMs representation of the earth system.
Not exact matches
A key giveaway that aerosols were behind the effect was that the lightning was most pronounced at times
of the year when powerful
atmospheric convection currents form that can carry the aerosol particles high into the sky (Geophysical Research Letters, doi.org/cc7b).
The evaluation
of the data show a clear correlation between the sea surface temperatures in the Irminger Sea in summer, the amount
of surface freshwater in this region and the
atmospheric conditions and onset
of convection in the following winter.
«For various periods over the last 60 years, we have been able to combine important processes:
atmospheric variability, such as the North Atlantic Oscillation, water and air temperatures, the occurrence
of fresh surface water, and the duration
of convection,» explains Dr. Marilena Oltmanns from GEOMAR, lead author
of the study.
A Columbia Engineering team led by Pierre Gentine, professor
of earth and environmental engineering, and Adam Sobel, professor
of applied physics and applied mathematics and
of earth and environmental sciences, has developed a new approach, opposite to climate models, to correct climate model inaccuracies using a high - resolution
atmospheric model that more precisely resolves clouds and
convection (precipitation) and parameterizes the feedback between
convection and
atmospheric circulation.
In the future, Romps plans to look at the distribution
of lightning - strike increases around the U.S. and also explore what lightning data can tell climatologists about
atmospheric convection.
These
convection changes can in turn drive the formation
of an
atmospheric ridge in the North Pacific, resulting in significant drying over California.
For the past few years, Houze has filled a valued role as a collaborator with PNNL staff scientists, advancing the science
of clouds and sharing his legacy
of transformative research influencing how meteorologists and climatologists think about
atmospheric convection.
Changes in Hadley circulation affects
convection and thus
atmospheric moisture content and cloud cover which may in turn affect net solar heating as well as the transfer
of heat from Earth to space.
Normally, this connection is due to the aforementioned
atmospheric convection and rainfall, but during the summer and fall
of 2014, when those warm waters should have produced rainfall and pushed El Niño along, the atmosphere remained relatively dry.
Wang, W., and M. Schlesinger, 1999: The dependence on
convection parameterization
of the tropical intraseasonal oscillation simulated by the UIUC 11 - layer
atmospheric GCM.
And energy out mostly by radiation, however, as much as 20 %
of escaping energy is simply highly energized
atmospheric molecules; which furthers vertical
convection all the way out to the inside
of Earth's magnetic bottle, and the Van Allen radiation belt.
Sensitivity
of atmospheric water vapor content to the parameters
of this new representation
of convection is also being evaluated through use
of the so - called adjoint
of the scheme.»
http://www.cpc.ncep.noaa.gov/products/outreach/glossary.shtml Low
atmospheric pressure tends to occur over warm water (and high over cold water), partly because
of deep
convection over the warm water.
Whether the activity
of TCs (TC - scale dynamics and cumulus
convection together) is determined by the global climatic condition (SST,
atmospheric composition and general circulation).
Large scale dust storms change the
atmospheric opacity and
convection; as always when comparing mean temperatures, the altitude at which the measurement is made matters, but to the extent it is sensible to speak
of a mean temperature for Mars, the evidence is for significant cooling from the 1970's, when Viking made measurements, compared to current temperatures.
The point isn't a «perpetual increase in
atmospheric pressure» — that's a misnomer — if you consider the MASS
of the atmosphere that is continuously «pumped» from cold air to hot air to cold air again, high up in the atmosphere — that creates «potential energy» from the kinetic energy
of the
convection — adiabatic expansion
of the atmosphere is the result — the adiabatic compression occurs on the return trip
of the previously warmed (from radiative energy) air as it completes the «cycle» as it comes back down!
Incidentally, the experiments
of Tyndall and Fourier were done in closed containers to block
convection and therefore do not represent open
atmospheric conditions whatsoever.
That, combined with the change in location
of the
convection, cause drastic changes in global
atmospheric circulation patterns.
Of course, this doesn't mean that much, since the «closed» system will not be open to the vacuum of space, and is not subject to other atmospheric processes like convection and to cloud and precipitation feedbacks, all of which render the experiment fairly meaningles
Of course, this doesn't mean that much, since the «closed» system will not be open to the vacuum
of space, and is not subject to other atmospheric processes like convection and to cloud and precipitation feedbacks, all of which render the experiment fairly meaningles
of space, and is not subject to other
atmospheric processes like
convection and to cloud and precipitation feedbacks, all
of which render the experiment fairly meaningles
of which render the experiment fairly meaningless.
«Our finding that convective features change drastically at resolutions
of 2 kilometers or more opens up new avenues for research into the interactions between
convection and global
atmospheric circulation that would have been invisible at coarser resolutions.»
Deep moist
atmospheric convection controls the development
of major weather systems like hurricanes, drives the global transport
of energy within the climate system and strongly influences the uncertainty
of projected climate change.
By Amber Bentley (Aged 11) In just 16 pages, this wonderful book covers the structure
of the atmosphere, solar radiation, the water cycle, clouds, fronts,
convection, air pressure, air masses, the global
atmospheric circulation, making weather observations, forecasting, synoptic charts, hurricanes, regional climate, palaeoclimates and anthropogenic climate change.
Further analysis reveals that overlying surface evaporation and
atmospheric convection are modulated as a result
of these forced changes to the temperature
of the upper coastal Atlantic Ocean.
The primary purpose
of this web site is to make people more aware
of the enormous energy production potential
of atmospheric upward heat
convection.
The intertropical convergence zone is distinguished by a wide band
of cumulus and cumulonimbus clouds that are created by dynamic
atmospheric lifting due to convergence and
convection.
14), addresses the mechanisms
of atmospheric heat transfer not only via radiation but also by
convection, which is not mentioned once in the IPCC's scientific reports (Ref.
A comparison
of the radiative equilibrium temperatures with the observed temperatures has indicated the extent to which the other
atmospheric processes, such as
convection, large - scale circulation, and condensation processes, influence the thermal energy balance
of the system.
The strength
of the vertical movement is controlled by the same factors that control
atmospheric convection elsewhere.
I'd have to see some sort
of computational model based on good
atmospheric convection physics that pops up with the good old DALR to the same old top
of troposphere even if there is no actual loss
of heat up there.
Bernie (05:54:00): «The strength
of the vertical movement is controlled by the same factors that control
atmospheric convection elsewhere.
I'll mention just one (
of many) negative feedbacks in the
atmospheric thermodynamic system —
convection.
(Lapse rate based primarily on
atmospheric density) Yes,
of couse
convection, evaporation, and relative conduction spreads would continuesly conduct said atmosphere.
The real GHE is the reduction
of surface emissivity, also possibly coupled
convection as
atmospheric GHG thermal - emission Poynting Vectors annihilate the UP PVs in that wavelength interval.
But in a given model you can often find ways
of altering the model's climate sensitivity through the sub-grid
convection and cloud schemes that affect cloud feedback, but you have to tread carefully because the cloud simulation exerts a powerful control on the
atmospheric circulation, top -
of - atmosphere (TOA) and surface radiative flux patterns, the tropical precipitation distribution, etc..
Thirty years later, the relevance
of this study has been realized in the development
of stochastic approaches to represent cumulus
convection and its upscale energy transports, and in the emerging efforts to resolve these multi-scale processes in
atmospheric simulations at the cloud system - resolving scale (approx. 1 km).
The role
of convection and the subsequent condensation out
of water vapour into clouds and then rainfall is currently incapable
of quantification as a means
of slowing or offsetting any
atmospheric greenhouse effect but it certainly does those things.
In the future, Romps plans to look at the distribution
of lightning - strike increases around the U.S. and also explore what lightning data can tell climatologists about
atmospheric convection.
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
atmospheric vortex engine exploits the natural energy content
of the vortex produced during upward heat
convection in the atmosphere.
However, the availability
of non-radiative means for vertical transport
of energy, including small - scale
convection and large - scale
atmospheric motions, must be accounted for, as is done in our
atmospheric general circulation model.
The physics that must be included to investigate the moist greenhouse is principally: (i) accurate radiation incorporating the spectral variation
of gaseous absorption in both the solar radiation and thermal emission spectral regions, (ii)
atmospheric dynamics and
convection with no specifications favouring artificial
atmospheric boundaries, such as between a troposphere and stratosphere, (iii) realistic water vapour physics, including its effect on
atmospheric mass and surface pressure, and (iv) cloud properties that respond realistically to climate change.
Process - based studies have focused on understanding the role
of the land surface on climate, with research looking into the regional impact
of historical or hypothetical (future scenario) land - use change on climate, as well as understanding diurnal - scale relationships between surface fluxes
of heat and moisture and subsequent
atmospheric processes such as
convection and the generation
of precipitation.
How can one arrive at a level
of certainty exceeding 90 % about any aspect
of the Earth's climate whilst attributing a value
of zero to all the main (and obvious) factors namely the sun, the oceans, evaporation and condensation, clouds and
atmospheric convection.
The IPCC summary is deeply flawed as a scientific document and as I have explained in other recent articles it appears impossible for increased levels
of atmospheric CO2 at the puny levels caused by mankind to affect the characteristics
of the atmosphere enough to significantly enhance the greenhouse effect and even if it could do so then any such effect would be quickly neutralised by the primary solar / oceanic driver and the oceans acting in conjunction with evaporation, condensation and
atmospheric convection (which includes clouds and rain).
To my way
of thinking «
atmospheric heat can only be trapped, or slowed down, by a reduction in
convection.
Answer obvious, and pertains only to anvils in frigid baths (or similar concepts), but it is completely irrelevant to the discussion at hand: it has NO relationship to
atmospheric physics, due to «other factors,» such as
convection and evaporation / condensation
of water.