Here we quantify the processes that controlled variations in methane emissions between 1984 and 2003 using an inversion model
of atmospheric transport and chemistry.
Badgley J. E., S. Jeong, X. Cui, S. Newman, J. Zhang, C. Priest, M. Campos - Pineda, A. E. Andrews, L. Bianco, M. Lloyd, N. Lareau, C. Clements and M. L. Fischer (February 2017): Assessment
of an atmospheric transport model for annual inverse estimates of California greenhouse gas emissions.
Atmospheric scientists measure the amount of CH4 gas in the atmosphere and use these data, along with models
of atmospheric transport, to estimate the amount of CH4 released at Earth's surface.
Since what goes north must eventually go south (after taking into account the very small amounts
of atmospheric transport and the amount of flow through the Bering Strait), all of the other changes will balance.
Atmospheric scientists measure the amount of CH4 gas in the atmosphere and use these data, along with models
of atmospheric transport, to estimate the amount of CH4 released at Earth's surface.
«We used a UK Met Office computer model
of atmospheric transport to look back in time, at where the air samples we collected had travelled from.»
And because the comb measurements can be averaged over the entire path length rather than relying on a few spot measurements, the comb method is better matched to the scale
of atmospheric transport models.
Not exact matches
Black carbon is the soot - like byproduct
of wildfires and fossil fuel consumption, able to be carried long distances via
atmospheric transport.
The complex interactions
of atmospheric turbulence and heat
transport affect global climate.
«Using a numerical climate model we found that sulfate reductions over Europe between 1980 and 2005 could explain a significant fraction
of the amplified warming in the Arctic region during that period due to changes in long - range
transport,
atmospheric winds and ocean currents.
The researchers found that large - scale features
of atmospheric circulation — in particular, the strength and position
of the Aleutian Low, a semi-permanent, subpolar area
of low pressure located in the Gulf
of Alaska near the Aleutian Islands — largely determined the timing
of snowmelt during spring in Alaska, by either facilitating or inhibiting the
transport of warm, moist air into the region.
Because air temperature significantly alters
atmospheric dynamics, which in turn affects moisture
transport, scientists speculate that this increase
of high altitude moisture may be tied to global warming.
To investigate the layers and composition
of clouds and tiny airborne particles like dust, smoke and other
atmospheric aerosols,, scientists at NASA's Goddard Space Flight Center in Greenbelt, Maryland have developed an instrument called the Cloud - Aerosol
Transport System, or CATS.
Using 19 climate models, a team
of researchers led by Professor Minghua Zhang
of the School
of Marine and
Atmospheric Sciences at Stony Brook University, discovered persistent dry and warm biases
of simulated climate over the region
of the Southern Great Plain in the central U.S. that was caused by poor modeling
of atmospheric convective systems — the vertical
transport of heat and moisture in the atmosphere.
«This emphasizes the importance
of large - scale energy
transport and
atmospheric circulation changes in restoring Earth's global temperature equilibrium after a natural, unforced warming event,» Li said.
The temperature gradient creates
atmospheric circulation, which
transports heat from areas
of equatorial excess to the cold polar regions.
Astrid Schnetzer, associate professor
of marine, earth and
atmospheric sciences at NC State, wanted to know how domoic acid gets
transported to depth via marine snow after a toxic algal bloom and how long it may persist.
Collision
of climate variants One, called the negative phase
of the Indian Ocean Dipole, is an
atmospheric circulation in the tropical Indian Ocean that
transports water from west to east.
The research team believe this is probably due to a weakening
of the
atmospheric circulation which
transports freshwater from the dry to wet regions
of the globe.
This diagram shows types, and size distribution in micrometres,
of atmospheric particulate matter This animation shows aerosol optical thickness
of emitted and
transported key tropospheric aerosols from 17 August 2006 to 10 April 2007, from a 10 km resolution GEOS - 5 «nature run» using the GOCART model.
Transport and lifetime
of atmospheric particles simulated by a quasi-global process model indicates how these particles impact the regional US western states
Why It Matters: On average,
atmospheric rivers hit the western United States only a few times each winter, but they
transport significant amounts
of moisture that converges in the mountains producing heavy precipitation.
The
transport processes are also very variable from winter to winter and the amount
of ozone pumped into the Arctic is also correlated with temperature (this is not a causal relationship — the correlation exists, because variability in temperatures and in ozone
transport are both driven by the same
atmospheric processes).
A NOAA website on
atmospheric rivers contains this fascinating statistic that illustrates just how much moisture can be
transported by winds in the mid-to-upper atmosphere: «A strong
atmospheric river
transports an amount
of water vapor roughly equivalent to 7.5 - 15 times the average flow
of liquid water at the mouth
of the Mississippi River.»
Here we apply a «state
of the art»
atmospheric chemistry
transport model to show that large emissions
of CH4 would likely have an unexpectedly large impact on the chemical compositioof the atmosphere and on radiative forcing (RF).
A continual cycle
of heat and moisture is pulled from the tropical ocean and
transported around the globe on belts
of atmospheric energy.
Already an international sensation, Boris Akunin's latest page - turner
transports the reader back to the glamorous, dangerous past in a richly
atmospheric tale
of suspense on the high seas.
Others include poisoning
of water supplies, high levels
of atmospheric ash, crop damage, and disruption to
transport.
Following the excellent number
of votes from you all and the wonderful Awards event in 2015, at the fabulously
atmospheric Dinosaur Gallery in the Natural History Museum, we weredelighted to host the 2016 Awards at the London
Transport Museum on 22 June 2016.
The modern age
of steam trains, iron bridges and extended public
transport networks was perfectly captured by Monet's series
of atmospheric paintings.
The eight computer generated photo - paintings located in the lower level
of the gallery are a reflection
of the invisible energy surrounding nature and inspired by drawings Mori made in front
of the ocean back in her native Japan.The photo - paintings emitted a cosmic and
atmospheric aura that made me feel as if I was
transported into a distant serene galaxy.
For instance, there is no evidence that, with the current configuration,
atmospheric heat
transports have vastly different modes
of behaviour — and so they are unlikely to suddenly flip into a new state.
It is still popular nomenclature in physical oceanography and
atmospheric dynamics to refer to the bodily
transport of energy by a fluid as «heat
transport.»
At the very least he needs to provide a pointer to «the calculations
of the sensitivity
of the mean climate to a doubling
of CO2 concentration» that he has found are ignoring changes in non-radiative
atmospheric heat
transport.
One is to acknowledge that calculation
of radiation
transport through a partially opaque atmosphere is one
of those problems that seems easy until you try to write down the equations, and then you find it's a monster — the great mathematical physicist S. Chandrasekhar spent years working on it and wrote a book full
of equations on stellar atmospheres that I think hardly anyone in
atmospheric physics even tries to read.
The (apparent) slower rate
of projected model warming for a higher absolute temperature may be related to other factors like cloud amount and geographical distribution at higher absolute humidity, or increases in convective
transport (due to more
atmospheric instability) at higher absolute humidity.
The
transport processes are also very variable from winter to winter and the amount
of ozone pumped into the Arctic is also correlated with temperature (this is not a causal relationship — the correlation exists, because variability in temperatures and in ozone
transport are both driven by the same
atmospheric processes).
RE # 11 The role
of hurricanes in the poleward heat
transport immediately leads to the question, how is the poleward heat
transport divided between
atmospheric and oceanic routes?
I hadn't heard about the heat
transport via the atmosphere, but it didn't surprise me — that is what the jet streams are all about — a wind caused by an
atmospheric temperature differential, given a little bit
of a spin.
Alaska Arctic Tundra CH4 Flux Study — Impacts
of AGW / CC Published 8 - Jan 2018 Estimating regional - scale methane flux and budgets using CARVE aircraft measurements over Alaska Conclusions Analysis
of CH4 column enhancements supplemented by simulated
atmospheric transport allowed us to estimate the monthly - mean CH4 fluxes from our study domain (50 — 75 N, 130 — 170 W).
As the ocean circulation takes up the role
of transporting heat poleward the
atmospheric circulation spins down.
This is due to the fact that changes in
atmospheric transport and deposition in the case
of 10Be or changes in the carbon cycle in the case
of 14C can influence the measured concentrations.
Redistribution
of heat (such as vertical
transport between the surface and the deeper ocean) could cause some surface and
atmospheric temperature change that causes some global average warming or cooling.
The correct way to ensure conservation
of energy is at the grid cell level, i.e. you make sure that there's no creation or destruction
of energy within each
atmospheric cell and in
transport processes among cells.
In GCMs, the global mean evaporation changes closely balance the precipitation change, but not locally because
of changes in the
atmospheric transport of water vapour.
Its findings suggest that changing storm patterns and the ensuing droughts are due to a southern shift in the Hadley cell, the large - scale pattern
of atmospheric circulation that
transports heat from the tropics to the subtropics.
If it were not for convective energy
transport, the terrestrial greenhouse effect would be 66K for the current
atmospheric composition instead
of the current climate 33K, which takes convective energy
transport into account.
An
atmospheric general circulation model coupled to a simple mixed layer ocean was forced with altered implied ocean heat
transports during a period
of increasing trace gases.
This product primarily exploits high - quality measurements
of air samples collected at tens
of sites around the world by various laboratories (119 sites for CO2, 30 sites for CH4 and 127 sites for N2O), in combination with a numerical model
of atmospheric tracer
transport (Chevallier et al. 2010, Bergamaschi et al. 2013, Thompson et al. 2014).
This mass
of warm water, nicknamed «the Blob,» was the result
of a persistent
atmospheric high - pressure ridge in the Northeastern Pacific that decreased cooling and
transport of surface water.