The findings raise important questions about the relationship
between atmospheric change and soil ecosystems, says Michael Miller, a soil ecologist at Argonne National Laboratory near Chicago.
Not exact matches
This analysis is paired with highly quantitative accounts of the various links
between population growth; hunger and poverty; pollution and
atmospheric change; the extinction of species; and the effects of militarism.
There is also growing understanding of the links
between atmospheric problems such as local air pollution, acid rain, global climate
change and stratospheric ozone depletion.
Venus's climate, like Earth's, has varied over time - the result of newly appreciated connections
between geologic activity and
atmospheric change
«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.
And by carefully measuring and modeling the resulting
changes in
atmospheric composition, scientists could improve their estimate of how sensitive Earth's climate is to CO2, said lead author Joyce Penner, a professor of
atmospheric science at the University of Michigan whose work focuses on improving global climate models and their ability to model the interplay
between clouds and aerosol particles.
«It gives further evidence of the close links
between atmospheric CO2 and temperature, but also shows how heterogeneous this climate
change may be on land,» he adds.
Tiny
changes in
atmospheric pressure
between day and night can trigger landslides.
Observations of
atmospheric carbon dioxide made by aircraft at altitudes
between 3 and 6 kilometers (10,000 - 20,000 feet) show that seasonal carbon dioxide variations have substantially
changed during the last 50 years.
Kevin Trenberth, an
atmospheric scientist at the National Center for
Atmospheric Research in Colorado, gets asked the question so often about the connection
between big rain events and climate
change that he had this response via email: «Here we go again.»
«We came as close as one can to demonstrating a direct link
between climate
change and a large family of extreme recent weather events,» said Michael Mann, distinguished professor of
atmospheric science and director, Earth System Science Center, Penn State.
«Our finding that vegetation plays a key role future in terrestrial hydrologic response and water stress is of utmost importance to properly predict future dryness and water resources,» says Gentine, whose research focuses on the relationship
between hydrology and
atmospheric science, land / atmosphere interaction, and its impact on climate
change.
Washington, DC — Reservoirs of oxygen - rich iron
between the Earth's core and mantle could have played a major role in Earth's history, including the breakup of supercontinents, drastic
changes in Earth's
atmospheric makeup, and the creation of life, according to recent work from an international research team published in National Science Review.
Thus, it is plausible that
changes to
atmospheric ionization rates due to cosmic ray variability may affect the occurrence of electrical phenomena in the Venusian atmosphere (Nordheim et al. 2015) hence manifesting a relation
between space weather and meteorological phenomena.
Running
atmospheric computer models, British researchers found a connection
between climate
change and turbulence, and they predict that the average strength of turbulence will increase by 10 to 40 % by 2050.
Hi Andrew, Paper you may have, but couldn't find on «The phase relation
between atmospheric carbon dioxide and global temperature» CO2 lagging temp
change, which really turns the entire AGW argument on its head: http://www.sciencedirect.com/science/article/pii/S0921818112001658 Highlights: ►
Changes in global atmospheric CO2 are lagging 11 — 12 months behind changes in global sea surface temperature ► Changes in atmospheric CO2 are not tracking changes in human emi
Changes in global
atmospheric CO2 are lagging 11 — 12 months behind
changes in global sea surface temperature ► Changes in atmospheric CO2 are not tracking changes in human emi
changes in global sea surface temperature ►
Changes in atmospheric CO2 are not tracking changes in human emi
Changes in
atmospheric CO2 are not tracking
changes in human emi
changes in human emissions.
The El Niño - Southern Oscillation cycle refers to a fluctuation
between unusually warm (El Niño) and cold (La Niña) waters in the tropical Pacific, with associated
changes in
atmospheric circulation (the Southern Oscillation)(Figure 2 - 5).
-- The El Niño - Southern Oscillation cycle refers to a fluctuation
between unusually warm (El Niño) and cold (La Niña) waters in the tropical Pacific, with associated
changes in
atmospheric circulation (the Southern Oscillation)(Figure 2 - 5).
The main feedbacks
between climate and the ice sheet arise from
changes in ice elevation,
atmospheric and ocean circulation, and sea - ice distribution.
A number of other major restorations will have their World Premieres at the Festival: Carol Reed's
atmospheric Graham Greene adaptation of OUR MAN IN HAVANA (1959), set in Cuba at the start of the Cold War, makes timely viewing as US / Cuba relations thaw; Ken Russell's reworking of D.H. Lawrence scandalous classic WOMEN IN LOVE (1970) stars Oliver Reed, Alan Bates and Glenda Jackson and shows two couple's contrasting searches for love, and was restored by the BFI National Archive working alongside cinematographer Billy Williams; A MAN FOR ALL SEASONS (1966) is directed by Fred Zinnemann from a script by great British screenwriter, Robert Bolt from Bolt's play about Sir Thomas More, a perfect companion piece to Wolf Hall; Henry Fonda stars in the ripe - for - discovery WARLOCK (1959), a seething study of vengeance and repressed sexuality in a Utah mining outpost; and Bryan Forbes» THE RAGING MOON (1971) starring Malcolm McDowell and Nanette Newman in a tender story
between two young people in wheelchairs which was ahead of its time in its attempts to
change attitudes to disability.
They offer the viewer an opportunity to explore dichotomies
between past and present, expanse and its circumscription, stillness and the inexorable momentum of
atmospheric change.
The nearest I have come to thinking I'm seeing deep space in abstract painting (aside from no - account
atmospheric stuff) is in Anne's work from 3 years ago, where the difference
between the larger areas contrasted with other incredibly detailed areas, so that the focus of the work seemed to
change, to pull the viewer (well, me) in and out, like a kind of sucking in and pulling out, This is my punt, and I'm still unsure about it.
Scientists agree that a doubling of
atmospheric CO2 levels could result in temperature increases of
between 1.5 and 4.5 °C, caused by rapid
changes such as snow and ice melt, and the behaviour of clouds and water vapour.
The link
between global temperature and rate of sea level
change provides a brilliant opportunity for cross-validation of these two parameters over the last several millenia (one might add - in the relationship
between atmospheric [CO2] and Earth temperature in the period before any significant human impact on [CO2]-RRB-.
The lag
between decreases in sea ice extent during late summer and
changes in the mid-latitude
atmospheric circulation during other seasons (when the recent loss of sea ice is much smaller) needs to be reconciled with theory.
A measure of the difference in sea level pressure
between the western (e.g., Darwin, Australia) and central / eastern (e.g., Tahiti) equatorial Pacific, representative of the east - west
changes in
atmospheric circulation associated with the El Nino / Southern Oscillation phenomenon.
But wouldn't a closer model be the first order ODE, where the difference
between absorbed solar power and lost black body power has to equal the
change in temperature with respect to time multiplied by the terrestrial and
atmospheric combined heat capacity:
Now, if there's a single take - away from this summary, it would be that the science on the relationship
between fossil fuel combustion, rising
atmospheric carbon dioxide, and global warming and climate
change was really settled by 1979.
The lag
between decreases in sea ice extent during late summer and
changes in the mid-latitude
atmospheric circulation during other seasons (like autumn and winter, when the recent loss of sea ice is much smaller) have been demonstrated empirically, but have not been captured by existing dynamical models.
The significant difference
between the observed decrease of the CO2 sink estimated by the inversion (0.03 PgC / y per decade) and the expected increase due solely to rising
atmospheric CO2 -LRB--0.05 PgC / y per decade) indicates that there has been a relative weakening of the Southern Ocean CO2 sink (0.08 PgC / y per decade) due to
changes in other
atmospheric forcing (winds, surface air temperature, and water fluxes).
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).
Claquin et al's model - derived findings show a
change in tropical
atmospheric forcing of «-- 2.2 to — 3.2 W m — 2»
between PI and LGM earth, due to the increased albedo of
atmospheric dust.
The approximately 20 - year lag (
between atmospheric CO2 concentration
change and reaching equilibrium temperature) is an emerging property (just like sensitivity) of the global climate system in the GCM models used in the paper I linked to above, if I understood it correctly.
What would affect
atmospheric CO2 directly is the
changes in the total amount of stored C in vegetation and soil, which is
changed by imbalances
between C - fixation and respiration / decomposition / oxidation.
The concentration in the last 400 million years has probably
changed between 15 and 30 percent,
changing total
atmospheric pressure I assume.
[UPDATE 3/6, 1 p.m.:] Isaac Held, a climate modeler at the Geophysical Fluid Dynamics Laboratory in Princeton, N.J., responded today with some caution about seeking relationships
between the ocean and
atmospheric changes around the tropics, and also drawing conclusions about their relationship to global warming.
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.
So the observed
change in CO2 and temperature since 1850 tell us that doubling
atmospheric CO2 should cause an increase in global temperature of somewhere
between 0.7 °C and 1.4 °C
Determining the mechanisms and feedbacks involved in climate
change at the end of the last ice age therefore requires an understanding of the relationship
between the southern margin ice retreat and connected meltwater events to
atmospheric and sea surface temperatures, ice - rafting Heinrich events, sea level rise, and
atmospheric greenhouse gas concentrations.
We have not not quantified accurately the factors that cause these large natural
changes in
atmospheric CO2, nor the interactions
between them, nor the interactions
between natural and humanmade
changes.
Everything else that might try to alter that base level simply results in
atmospheric circulation
changes (atmosphere includes oceans for this purpose) that adjust the rate of conversion
between kinetic and potential energy so as to keep the base level of system energy content stable.
This empirical science published by NASA is undeniable, and most alarmist scientists accept, although grudgingly - the relationship
between changes in
atmospheric CO2 levels and
changes in temperature are, at best, significantly lame weak.
The Kirtland Turner & Ridgwell method has found an empirical relationship
between the average ocean carbon isotope excursion, the
atmospheric CO2 level, and the duration of the carbon input that generated the climate
change.
I do, however, recognize the point of your suggestion that year to year fluctuations in the rate of CO2
change can involve flux
changes between atmospheric and terrestrial or oceanic sources that add to or subtract from the human contribution.
We show the one - to - one relationship
between changes in
atmospheric properties and time - dependent
changes in temperature and its distribution on earth.
Understanding the climate impact of natural
atmospheric particles An international team of scientists, led by the University of Leeds, has quantified the relationship
between natural sources of particles in the atmosphere and climate
change.
Consistent with reanalysis data (Fig. 4) and theoretical considerations (36, 39), continental rainfall is assumed to be proportional to the mean specific humidity within the
atmospheric column The effect of an offset
between these quantities does not
change the model behavior qualitatively (see SI Appendix).
Add to that the period
between 2000 - 2014 with little or no
change in global estimated temperatures, despite a large increase in
atmospheric C02.
«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.»
Future emails will include: the difference
between contrails / vapour trails and Stratospheric Aerosol Injection observations on covert
atmospheric spraying (their tactics have
changed in the last few weeks — this has been noticed globally) who is controlling the spraying — who are «they» much of the northern hemisphere is burning — California, Canada, Siberia (2,000 mile smoke clouds), Sweden etc..