With one AWARE location near the coast and another in the interior, project scientists aim to compare
how atmospheric systems passing through West Antarctica affect both locations, and how those changes translate to wider global shifts.
The debate is not how gases behave in isolation in laboratory conditions but rather
how the atmospheric system behaves as a whole with all its complexity and nuances, and it is because of this that many are skeptical as to whether in reality there is any significant «greenhouse» effect.
Not exact matches
Lozier (p. 1507) discusses
how recent studies have challenged our view of large - scale ocean circulation as a simple conveyor belt, by revealing a more complex and nuanced
system that reflects the effects of ocean eddies and surface
atmospheric winds on the structure and variability of the ocean's overturning.
«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.
To test his idea, Salzmann used a computer model of the Earth
system to find out
how the climate would react to a doubling of the
atmospheric carbon - dioxide concentration.
The models aimed to simulate
how the planet's climate
system would react to rising CO2 levels, relying on a combination of mathematics, physics, and
atmospheric science.
Find out
how researchers are using data from the U.S. Department of Energy's
Atmospheric Radiation Measurement (ARM) Climate Research Facility — the world's most comprehensive outdoor laboratory and data archive for research related to
atmospheric processes that affect Earth's climate — to improve earth
system models.
This symposium brings together experts across disciplines to better understand
how planets like Earth, Venus and Mars have changed over time — from their
atmospheric composition, geology, chemical composition and interactions with the Sun — to help understand what it takes to support life and whether it could exist beyond our solar
system.
However, if the loss of Arctic Sea ice has significantly changed global
atmospheric circulation patterns, then we are dealing with a different
system that has only been in existence since 2007, and we do not know
how often to expect crop failures.
Mike's work, like that of previous award winners, is diverse, and includes pioneering and highly cited work in time series analysis (an elegant use of Thomson's multitaper spectral analysis approach to detect spatiotemporal oscillations in the climate record and methods for smoothing temporal data), decadal climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70 year oscillation in the climate
system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST changes, a finding recently reaffirmed by a study published in Nature), in showing
how changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in
atmospheric chemistry (an analysis of beryllium - 7 measurements).
The equilibrium climate sensitivity (ECS) is a convenient yardstick to measure
how sensitively the climate
system responds to perturbations in the
atmospheric concentration of greenhouse gases such as CO2.
For some, a few hundred ppm of
atmospheric CO2 may seem like small potatoes —
how could that possible affect the temperature of the very massive climate
system?
That allows us to extrapolate theories as to
how it MIGHT change the
atmospheric system as a whole.
I will now analyse
how the
system could work and show that composition changes not involving changes in mass only affect
atmospheric volume and circulation patterns and not surface temperature.
BBD - With all due respect, the study does nothing to explain
how the scientific community has failed to come to grips with the fact that there is now pretty good evidence that we do not understand
how the climate
system works well enough to accurately determine the impact of additional
atmospheric CO2.
there is now pretty good evidence that we do not understand
how the climate
system works well enough to accurately determine the impact of additional
atmospheric CO2.
Further, trying to reduce the complexity of the
atmospheric system to a verbal discussion is rather like learning
how to ride a bicycle from a book.
Do you agree that a nation that refuses to reduce its ghg emission to its fair share of safe global ghg emissions on the basis of cost to it is implicitly taking a position on
how high
atmospheric concentrations of ghgs should be allowed to rise and that the higher atmosphere ghg concentrations rise the more people and the ecological
systems on which life depends will be harmed?.
Do you agree that a nation that refuses to reduce its ghg emission to its fair share of safe global ghg emissions on the basis of cost to it is implicitly taking a position on
how high
atmospheric concentrations of ghgs should be allowed to rise and that the higher atmosphere ghg concentrations rise the more people and the ecological
systems will be harmed?.
What's new here is the application of a detailed version of one of the world's premier climate
system models, the CCSM, to understand
how rising levels of
atmospheric carbon dioxide affected conditions in the world's oceans and land surfaces enough to trigger a massive extinction hundreds of millions of years ago.»
And then in January of this year there was another publication, that came up with a perhaps better convincing route to explain
how indeed Arctic depressions can lead to anticyclonal weather
systems later on than
atmospheric wave patterns: snow cover.
On top of this, large questions remain over
how cirrus cloud thinning could affect other aspects of the climate
system, such as
atmospheric circulation, the paper concludes:
PNNL researchers are expanding knowledge of fundamental
atmospheric processes, developing state - of - the - art modeling capabilities, and improving understanding of
how human and natural
systems interact.
Counters: «Once the model finishes producing the data representing
how radiative forcing has changed over time, we can then go back and analyze that data to see
how the climate
system in terms of temperature and other factors will change based on empirical relationships between
atmospheric factors and changes in temperature.»
Once the model finishes producing the data representing
how radiative forcing has changed over time, we can then go back and analyze that data to see
how the climate
system in terms of temperature and other factors will change based on empirical relationships between
atmospheric factors and changes in temperature.
which reveal
how the climate
system is responding to rapid human - made changes of
atmospheric composition, especially
atmospheric carbon dioxide (CO2).
Reporting in Geophysical Research Letters, researchers looked at
how the impacts caused by different strengths of geoengineering differed from region to region, using a comprehensive climate model developed by the UK Met Office, which replicates all the important aspects of the climate
system, including the
atmospheric, ocean and land processes, and their interactions.
Related Volcanoes, Tree Rings, and Climate Models: This is
how science works Fossil Focus: Using Plant Fossils to Understand Past Climates and Environments
Atmospheric oxygen over Phanerozoic time Coupled carbon isotopic and sedimentological records from the Permian
system of eastern Australia reveal the response of
atmospheric carbon dioxide to glacial growth and decay during the late Palaeozoic Ice Age
Using
atmospheric general - circulation models, as well as coupled ocean - atmosphere models, he investigates the interactions between large - scale climate
systems such as ocean and wind currents to understand natural variability and
how climate responds to human - made forcings.
Currently, many observing
systems capture elements of
how climate is changing, such as direct measurements of
atmospheric and ocean temperature.
It's not clear to me
how you intend your statement about «tinkering with dynamic
systems» — but if you mean a 30 % augmentation of the
atmospheric concentration of CO2, I'd say that qualifies, all right.
In a new study published in the Journal of Climate, the Community Earth
System Model Large Ensemble (CESM - LENS) of simulations is used to explore
how various characteristics of the mid-latitude
atmospheric circulation (zonal flow, synoptic blockings, jet stream meanders) evolve along the course of the 21st century under the RCP8.5 scenario of anthropogenic emissions.
But it's a marker for the high level of
atmospheric energy the
system is now pumping out and
how potentially damaging it could ultimately become.