Nieves said an example is the U.S. West Coast, where the phase of
a multi-decadal ocean climate pattern called the Pacific Decadal Oscillation has helped keep sea level rise lower during the past two decades.
Not exact matches
First, it probably needs to be made clearer that generally speaking radiative forcing and
climate sensitivity are useful constructs that apply to a subsystem of the
climate and are valid only for restricted timescales — the atmosphere and upper
ocean on
multi-decadal periods.
The Atlantic Multidecadal Oscillation (AMO), Pacific Decadal Oscillation (PDO), North Atlantic Oscillation (NAO), and El Niño - Southern Oscillation (ENSO) have all been found to significantly influence changes in surface air temperature and rainfall (
climate) on decadal and
multi-decadal scales, and these natural
ocean oscillations have been robustly connected to changes in solar activity.
«The
climate patterns responsible for the expected above - normal 2007 hurricane season continue to be the ongoing
multi-decadal signal (the set of oceanic and atmospheric conditions that have spawned increased Atlantic hurricane activity since 1995), warmer - than - normal sea surface temperatures in key areas of the Atlantic
Ocean and Caribbean Sea, and the El Nino / La Nina cycle»
Given those assumptions, looking at the forcing over a long - enough
multi-decadal period and seeing the temperature response gives an estimate of the transient
climate response (TCR) and, additionally if an estimate of the
ocean heat content change is incorporated (which is a measure of the unrealised radiative imbalance), the ECS can be estimated too.
Since the heat storage capacity of the
ocean is > 1000 times that of the atmosphere, having a solid handle on all these is crucial to accurately projecting even average mean
climate across
multi-decadal time.
This means that the heat content was «reset» to this earlier value, whereas the
multi-decadal global
climate model projects a more - or-less monotonic increase in
ocean heat content.
A detailed reanalysis is presented of a «Bayesian»
climate parameter study (Forest et al., 2006) that estimates
climate sensitivity (ECS) jointly with effective
ocean diffusivity and aerosol forcing, using optimal fingerprints to compare
multi-decadal observations with simulations by the MIT 2D
climate model at varying settings of the three
climate parameters.
The
multi-decadal climate shifts correspond precisely to changes in Pacific
Ocean circulation, and in global hydrological patterns.
There are lots of experts on small subsets of all the physics that go into
climate, radiative physics, clouds, aerosol,
oceans,
multi-decadal oscillations, solar, global ice, etc..
The near - linear rate of anthropogenic warming (predominantly from anthropogenic greenhouse gases) is shown in sources such as: «Deducing Multidecadal Anthropogenic Global Warming Trends Using Multiple Regression Analysis» «The global warming hiatus — a natural product of interactions of a secular warming trend and a
multi-decadal oscillation» «The Origin and Limits of the Near Proportionality between
Climate Warming and Cumulative CO2 Emissions» «Sensitivity of climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mixing
Climate Warming and Cumulative CO2 Emissions» «Sensitivity of
climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake» «Return periods of global climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mixing
climate to cumulative carbon emissions due to compensation of
ocean heat and carbon uptake» «Return periods of global
climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to ocean mixing
climate fluctuations and the pause» «Using data to attribute episodes of warming and cooling in instrumental records» «The proportionality of global warming to cumulative carbon emissions» «The sensitivity of the proportionality between temperature change and cumulative CO2 emissions to
ocean mixing»
Although not a focus of this study, the degree to which the
oceans themselves have recently warmed due to increased GHG, other anthropogenic, natural solar and volcanic forcings, or internal
multi-decadal climate variations is a matter of active investigation (Stott et al. 2006; Knutson et al. 2006; Pierce et al. 2006).
Given that, «
Climate simulations suggest that
multi-decadal periods of high and low variability in the phenomenon known as the El Niño - Southern Oscillation in the tropical Pacific
Ocean may be entirely unpredictable» DiNezio, 1014, we can not have confidence in any of our current ENSO forecasts
There are a number of inter-decadal and
multi-decadal cyclical patterns observable in the
climate system, particularly in
ocean surface temperatures.
They are dealing mostly with the atmosphere - the
climate models are even more compromised when trying to deal with the effect of the
oceans with their
multi-decadal and possibly multi-century patterns.
Sadly, the
climate science community has been on a
multi-decadal quest for proof of the «GHE» hypothesis, last I checked they are pointing towards the «deep
oceans» as the location of their prey.
Multi-decadal regime shift — chaotic — unpredictable — involving abrupt shifts in
ocean and atmospheric circulation — show the dynamical mechanism at the core of
climate on a global scale.
Scientists know of and study many different types of
climate variations, such as those on decadal and
multi-decadal timescales in the Pacific and North Atlantic
Oceans, each with its own unique characteristics.
Observe the stricking difference in the level of alarmism between the politicians and the quasi-humility of the
climate modellers describing the uncertainties in predicting the natural
multi-decadal phenomenon which are greatly influenced by
ocean circulation.