In the SH,
changes in circulation related to an increase in the SAM from the 1960s to the present are associated with strong warming over the Antarctic Peninsula and, to a lesser extent, cooling over parts of continental Antarctica.
Not exact matches
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A study
relating to this — «Our study confirms many
changes seen
in upper Arctic Ocean
circulation in the 1990s were mostly decadal
in nature, rather than trends caused by global warming,» said Morison.
Secondly, if the potential cloud response is
related to
changes in circulation caused by the TSI or an ozone
related change, then it isn't an extra forcing at all — it is part of the feedback, and should already be incorporated
in models.
In a series of papers, we've shown that the warmer temperatures observed over the WAIS are the result of those same atmospheric circulation changes, which are not related to the SAM, but rather to the remote forcing from changes in the tropical Pacific: changes in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012
In a series of papers, we've shown that the warmer temperatures observed over the WAIS are the result of those same atmospheric
circulation changes, which are not
related to the SAM, but rather to the remote forcing from
changes in the tropical Pacific: changes in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012
in the tropical Pacific:
changes in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012
in the character of ENSO (Steig et al., 2012; Ding et al., 2011; 2012).
The
changes include
changes in the TOA energy dynamic
related to
changes in ocean and atmospheric
circulation —
changes in cloud.
In models at least, this kind of response would be most directly related to increases in stratification due to surface warming, as I understand it, and not directly to the kind of change in atmospheric circulation discussed in Dian's pape
In models at least, this kind of response would be most directly
related to increases
in stratification due to surface warming, as I understand it, and not directly to the kind of change in atmospheric circulation discussed in Dian's pape
in stratification due to surface warming, as I understand it, and not directly to the kind of
change in atmospheric circulation discussed in Dian's pape
in atmospheric
circulation discussed
in Dian's pape
in Dian's paper.
The strong warming
in the polar regions is
related to
changes in the thermohaline
circulation.
The issue with the Mauritsen and Stevens piece is that it tries to go well beyond a «what if» modeling experiment, and attempts to make contact with a lot of other issues
related to historical climate
change (the hiatus,
changes in the hydrologic cycle, observed tropical lapse rate «hotspot» stuff,
changes in the atmsopheric
circulation, etc) by means of what the «iris» should look like
in other climate signals.
Spatial variability of the rates of sea level rise is mostly due to non-uniform
changes in temperature and salinity and
related to
changes in the ocean
circulation.
Many believe
changes in wind
circulation related to global warming played a part.
By one measure (the EQSOI), the El Niño -
related changes in the atmospheric
circulation in 1997/98 and 2015/16 are tied; by another (the SOI), 1997/98 was stronger.
Since it spoke of
circulation changes and specifically referenced section 3.6.4, I too would have thought they were
in fact referring to NAO / NAM (maybe
related to NAM accounting for half the warming over Eurasia 1968 — 97?).
A new study, published
in Journal of Geophysical Research - Oceans, helps clarify how past and future coastal sea level
changes are
related to local winds and large - scale ocean
circulation.
I agree that the application of higher resolution model equipment does not help to reduce the uncertainty range of the sea level
in the Amsterdam harbours: assumptions about
changes in the heat storage, icecap melting and
changes in the gravity field dominate this uncertainty range (although some regiona features
related to oceanic
circulation and heat redistribution may be better resolved
in higher resolution models).
ENSO is ultimately driven by
change in sea surface pressure at high latitudes due to the coupled
circulation of the stratosphere and troposphere and the inter annual variations
in ENSO
relate to what we know as the Southern Annular Mode and the Northern Annular Mode.
The Quaternary glacial history of the Arctic Ocean is characterized by the repeated build - up and decay of circum - Arctic ice sheets on the continental shelves, the development and disintegration of ice shelves, and
related changes in ocean -
circulation patterns and sea ice cover50, 51,52,53,54,55.
What science is suggesting is that there are multi-decadal regimes that are
related to
changes in ocean and atmospheric
circulation in the broader Earth system.
Slow variations
in upper ocean heat content that have been observed
in the subpolar and marginal ice zone regions of the Atlantic since the mid-twentieth century are thought to be
related to
changes in the strength of the Atlantic Meridional Overturning
Circulation (AMOC).
One last point
related to my last post, is the extent / degree of magnitude of a more meridional atmospheric
circulation pattern (N.H. especially) could influence snow cover, cloud cover, and precipitation amounts which could set up stronger positive climatic feedbacks, which could then result
in an even more significant climatic
change going forward.
These millennial - scale teleconnections resulted from the bipolar seesaw behaviour of the Atlantic Ocean
related to
changes in the ocean
circulation.
Shows that the
changes in discharge extremes are
related to the regional pluriannual rainfall variability and the associated atmospheric
circulation as well as to tropical large - scale climatic indicators
The seasonal climate may
relate to
changes in the ocean
circulation pattern prior to 4.6 Ma that resulted
in an increased temperature and atmospheric pressure gradient between the east coast of North America and the Atlantic Ocean, but this climate phase seems to be only a temporary condition, as underlying and overlying sediment are both consistent with drier conditions.
Although we focus on a hypothesized CR - cloud connection, we note that it is difficult to separate
changes in the CR flux from accompanying variations
in solar irradiance and the solar wind, for which numerous causal links to climate have also been proposed, including: the influence of UV spectral irradiance on stratospheric heating and dynamic stratosphere - troposphere links (Haigh 1996); UV irradiance and radiative damage to phytoplankton influencing the release of volatile precursor compounds which form sulphate aerosols over ocean environments (Kniveton et al. 2003); an amplification of total solar irradiance (TSI) variations by the addition of energy
in cloud - free regions enhancing tropospheric
circulation features (Meehl et al. 2008; Roy & Haigh 2010); numerous solar -
related influences (including solar wind inputs) to the properties of the global electric circuit (GEC) and associated microphysical cloud
changes (Tinsley 2008).
Until we do, we can not make good predictions about future climate
change... Over the last several hundred thousand years, climate
change has come mainly
in discrete jumps that appear to be
related to
changes in the mode of thermohaline
circulation.»
Unlike Charney climate sensitivity, which is
related to the strength of feedbacks involving short timescale climate processes such as those involving clouds and water vapor, Earth System sensitivity also integrates feedbacks involving long timescale
changes in the cryosphere, terrestrial vegetation, and deep ocean
circulation.
Global - annual mean adjusted radiative forcing at the top of the atmosphere is,
in general, a reliable metric
relating the effects of various climate perturbations to global mean surface temperature
change as computed
in general
circulation models (GCMs).
Because
changes in tropical
circulation have been strongly
related to the recently observed planetary surface warming, this research is relevant to the issues of greenhouse warming.