The other theme was the discussion of the spectral irradiance changes — specifically by how much the UV
changes over a solar cycle are larger in magnitude than the changes in the total irradiance.
Our understanding 48 of the «ion - aerosol clear air» mechanism as a whole relies on a few model investigations that simulate GCR 49
changes over a solar cycle (Kazil et al., 2012; Pierce and Adams, 2009a; Snow - Kropla et al., 2011) or during 50 strong Forbush decreases (Bondo et al., 2010; Snow - Kropla et al., 2011).
The main origin: solar UV maxima and minima are far more pronounced (10 %) than the overall solar energy (1 %)
changes over a solar cycle.
The total energy
change over a solar cycle is quite small, which has led many to argue that solar variability has little impact on climate.
Not exact matches
They then infer a higher temperature sensitivity to
changes in radiance
over this
cycle and conclude that maybe 0.1 K temperature increase would be possible due to the variation in
solar radiance, or about 30 % (if you push it) of the total temperature anomaly
over this period.
For example, 2005 is near
solar minimum in the 11 year
cycle, and radiance now is about 1 - 2 W / m ^ 2 less than a few years ago, which means Pluto and Mars are getting LESS
solar radiance on the time scale of the atmosphere and polar cap
changes, EVEN IF the radiance averaged
over the whole
cycle was higher.
«What is generally required [for proving
solar forcing of climate
change] is a consistent signal
over a number of
cycles (either the 11 year sunspot
cycle or more long term variations), similar effects if the timeseries are split, and sufficient true degrees of freedom that the connection is significant and that it explains a non-negligible fraction of the variance.»
In my opinion, climate behaves in a far from linear way, with loads of factors to take into account, so in most cases it would be very difficult to find climate records react consistently (
over several
solar cycles / decades / centuries) in the same way to say a
solar change (see the Hoyt & Schatten 1998 book).
The
solar - cloud connection is quite real (after two satellite measured sun
cycles), but can't explain the rather fast and huge
changes in radiation balance
over the previous period.
This would cause a
change of 4.75 degrees K for the 100 % reference
change in GCR
over the 11 year
solar cycle (and a non physical decrease of more than 100 % in cloud cover — are negative high clouds cooling and negative low clouds warming?
This is the case even if there is a
change in the mean radiance
over decades (between
solar cycles) because the year - to - year variation within a
cycle is larger than the variation between
cycles, and we measured
solar radiance in 1999 - 2005.
I noticed that the
change in cloud cover from the minimum to maximum of the
solar cycle was 2 percent, much less than the 10 %
change in CO2,
over the period of their study.
I could go through a dozen... examples: the skill associated with
solar cycles,
changing the ozone in the stratosphere; the skill associated with orbital
changes over 6,000 years.
The
change in insolation due to orbital
changes are significant, of the order of 50 W / m2, or 50 times larger than the
change of TSI
over the
solar cycle.
But as there is little
change in the configuration of the continents
over the past million years, we may assume that the same
changes in terrestrial /
solar cycles will have a similar effect on temperature.
But it doesn't make all that much difference to global warming anyway, because the total peak - to - trough
change in insolation
over a complete
solar cycle is only about 1 % anyway.
At the top of atmosphere the the inward radiative flux is about 1360 W / m - 2 in the latest estimate — but
changes a little bit
over an 11 year
solar cycle.
According to their modeling studies, the difference in the amount of incoming
solar radiation, in this case, primarily in the ultraviolet (UV) wavelengths, during the minima and maxima of the 11 - yr
solar cycle are large enough to produce a characteristic
change in the winter circulation pattern of the atmosphere
over North America... When the NAO is in its negative phase, more cold air can seep south from the Arctic and impact the lower latitudes of Europe and the eastern U.S., which helps spin up winter storm systems.
«The results also show that ionisation of the atmosphere by cosmic rays accounts for nearly one - third of all particles formed, although small
changes in cosmic rays
over the
solar cycle do not affect aerosols enough to influence today's polluted climate significantly.»
The
change in total
solar irradiance
over recent 11 - year sunspot
cycles amounts to < 0.1 %, but greater
changes at ultraviolet wavelengths may have substantial impacts on stratospheric ozone concentrations, thereby altering both stratospheric and tropospheric circulation patterns... This model prediction is supported by paleoclimatic proxy reconstructions
over the past millennium.
As time and the
solar / climactic
cycles march on, natural
changes ahead might end up putting a - not insignificant dent - in the harvested energy (measured in kwh / yr) of a larger 20MW PV system
over a quarter century.
The authors found that consistent with previous research,
changes in
solar and volcanic activity, land cover, and incoming
solar radiation due to the Earth's orbital
cycles were the main contributors to the cooling between the MWP and LIA (the years 900 — 1600), and probably also caused the cooling
over the full 2,000 - year period.
7.4.5.3 Synthesis Although there is some evidence that ionization from cosmic rays may enhance aerosol nucleation in the free troposphere, there is medium evidence and high agreement that the cosmic ray - ionization mechanism is too weak to influence global concentrations of CCN or their
change over the last century or during a
solar cycle in any climatically significant way.
Take
solar vs. GHGs: 1.5 W / m2
solar change (TOA)
over a
solar cycle has a large effect in the stratosphere: During a
solar cycle, the largest
change is in the short waves: 10 % more during high
solar activity: that affects ozone building, the temperature in the stratosphere and increases the polewards flow in the stratosphere.
As Don Easterbrook and others note, hardly a significant length in temperatures that can
cycle over hundreds and even thousands of years, caused by either
solar input
changes or circulations within the oceans.
They concluded that with a bit of help from
changes in
solar output and natural climatic
cycles such as the El Nino Southern Oscillation (ENSO), the growth in the volume of aerosols being pumped up power station chimneys was probably enough to block the warming effect of rising greenhouse gas emissions
over the period 1998 - 2008.
They are mainly derived from the Shaviv reference (provided in the link above) that concludes that the
solar signal is amplified as indicated by the magnitude of
changes in ocean heat content (and other less direct measures)
over the course of the 11 year
solar cycle.
Long - term trends and
changes (longer than
solar cycle) can partly be caused by long - term
changes of trend drivers of
solar / space weather origin like geomagnetic activity, which in terms of the aa - index was increasing
over almost the whole 20th century (e.g., Mursula & Martini 2006), even though now it is low.
«
Over the 11 - year
solar cycle, small
changes in the total
solar irradiance (TSI) give rise to small variations in the global energy budget.
This is achieved through the study of three independent records, the net heat flux into the oceans
over 5 decades, the sea - level
change rate based on tide gauge records
over the 20th century, and the sea - surface temperature variations... We find that the total radiative forcing associated with
solar cycles variations is about 5 to 7 times larger than just those associated with the TSI variations, thus implying the necessary existence of an amplification mechanism, although without pointing to which one.
Whether there be radiative gases, biosphere
changes, volcanic events, ocean
cycles,
solar cycles, albedo variations or asteroid strikes the same mechanism restores balance
over time.
I think they show that both
cycles are underlain by a longer, larger
cycle giving a background rising trend
over the period for which the
solar changes from 1600 to date would be a primary candidate.
Changes in the meridional circulation
over longer periods can explain some of the more dramatic variations of the ampltude of the
solar cycle [see e.g. http://arxiv.org/abs/1101.4342].
Modelling studies from both Pierce & Adams (2009) and Kazil et al. (2012) concluded that global cloud condensation nuclei (CCN) would not be sensitive to
changes in the ion - induced nucleation rate
over a
solar cycle.
The Intergovernmental Panel on Climate
Change estimates a median of 48 gram CO2 - equivalent / kWh for building
solar panels,
over the complete life
cycle.
Changes in the CR flux during large FD events are of the same order of magnitude as changes experienced over the decadal solar cycle, but occur over a period of several days (Čalogović et al.
Changes in the CR flux during large FD events are of the same order of magnitude as
changes experienced over the decadal solar cycle, but occur over a period of several days (Čalogović et al.
changes experienced
over the decadal
solar cycle, but occur
over a period of several days (Čalogović et al. 2010).
Over a
solar cycle, the amount of output
changes by about + / - 0.5 W / m2, or less than 0.1 %.
Based on these results, we conclude that (1) the sensitivity
changes of the PMO6V radiometers within VIRGO during the first two years have very likely not been correctly evaluated; and that (2) the TSI variations
over cycle 23 and the
change in the TSI levels between the minima in 1996 and 2008 are consistent with the
solar surface magnetism mechanism.
Similar conclusions were reached by Agee et al. (2012), who examined ISCCP data
over the recent
solar minimum (between
solar cycles 23 and 24), during which time high levels of CR were recorded, and yet no corresponding cloud
changes were observed to suggest a connection to
solar activity.
Climate model simulations indicate that
changes in
solar radiation a few times larger than those confirmed in the eleven - year
cycle, and persisting
over multi-decadal time scales, would directly affect the surface temperature.
The report which contains statements like this: «Although there is some evidence that ionization from cosmic rays may enhance aerosol nucleation in the free troposphere, there is medium evidence and high agreement that the cosmic ray - ionization mechanism is too weak to influence global concentrations of CCN or their
change over the last century or during a
solar cycle in any climatically significant way.
The forcing from
changes in total
solar irradiance alone does not seem to account for these observations, implying the existence of this unknown amplifying mechanism.The cosmic ray - ionization mechanism is too weak to influence global concentrations of CCN or their
change over the last century or during a
solar cycle in any climatically significant way.
«there is medium evidence and high agreement that the cosmic ray - ionization mechanism is too weak to influence global concentrations of CCN or their
change over the last century or during a
solar cycle in any climatically significant way.
I came to think of
solar radiation as being the ultimate (and only) external forcing of the climate system, which, except for the orbital seasonal
changes and the 11 - year sunspot
cycle, has been essentially constant
over the past several decades of precision
solar irradiance monitoring.
SSTs however have been influenced by other forcings, such as greenhouse gases,
over the last few decades, and these transient
changes will obviously affect the
solar cycle influence.