Showing posts sorted by relevance for query spencer 1 or 2% cloud. Sort by date Show all posts
Showing posts sorted by relevance for query spencer 1 or 2% cloud. Sort by date Show all posts

Saturday, May 17, 2014

New paper shows cloud radiative effects are negative, not positive as assumed by climate models

A paper published yesterday in Climate Dynamics illustrates just a few of the large unresolved problems in modeling clouds, the largest source of climate modelling uncertainty. The authors attempted but were unable to reconcile cloud radiative effects with global precipitation and the atmospheric energy budget due to doubled CO2 concentration, unless the sign of cloud radiative effects is changed from positive [as falsely assumed by all IPCC models] to strongly negative. 

According to the paper, 
"because clouds are a large source of modelling uncertainty, we consider whether resolving errors in cloud simulation could reconcile modelled global mean precipitation trends of about 1–3 % K−1 with some estimates of observed trends of 7 % K−1 or more. This would require the radiative effect of clouds to change from one that increases atmospheric radiative absorption by about 0.5 Wm−2 K−1 to one that decreases it by −3.5 Wm−2 K−1 . Based on our results, this seems difficult to achieve within our current rationale for the tropics at least."
In other words, the net radiative effect of increased clouds from warming & increased evaporation of water vapor would be to decrease IR radiative absorption & increase IR radiative cooling of the atmosphere, an anti-greenhouse effect. Thus, IPCC climate models don't have either the magnitude or even the sign of radiative forcing from clouds correct, one of several reasons why the models greatly exaggerate warming and have been falsified at confidence levels of 95-98%+.

As Dr. Roy Spencer notes,
"The most obvious way for warming to be caused naturally is for small, natural fluctuations in the circulation patterns of the atmosphere and ocean to result in a 1% or 2% decrease in global cloud cover. Clouds are the Earth’s sunshade, and if cloud cover changes for any reason, you have global warming — or global cooling."
Climate Dynamics May 2014

The cloud radiative effect on the atmospheric energy budget and global mean precipitation

F. Hugo Lambert, Mark J. Webb, Masakazu Yoshimori, Tokuta Yokohata


Abstract
This study seeks to explain the effects of cloud on changes in atmospheric radiative absorption that largely balance changes in global mean precipitation under climate change. The partial radiative perturbations (PRPs) due to changes in cloud and due to the effects of the pre-existing climatological cloud distribution on non-cloud changes, known as “cloud masking”, are calculated when atmospheric CO2 concentration is doubled for the HadSM3 and MIROC models and for a large ensemble of parameter perturbed models based on HadSM3. Because the effect of cloud on changes in atmospheric shortwave absorption is almost negligible, longwave fluxes are analysed alone. We find that the net effects of cloud masking and cloud PRP on atmospheric absorption are both substantial. For the tropics, our results are reviewed in light of hypotheses put forward to explain cloud and radiative flux changes. We find that the major effects of clouds on radiation change are linked to known physical processes that are quite consistently simulated by models. Cloud top height changes are quite well described by the fixed anvil temperature hypothesis of Hartmann and Larson; cloud base heights change little, remaining near the same pressure. Changes in cloud geographical location and cloud amount are significant, but play a smaller role in driving radiative flux changes. Finally, because clouds are a large source of modelling uncertainty, we consider whether resolving errors in cloud simulation could reconcile modelled global mean precipitation trends of about 1–3 % K1 with some estimates of observed trends of 7 % K1 or more. This would require the radiative effect of clouds to change from one that increases atmospheric radiative absorption by about 0.5Wm2K1 to one that decreases it by 3.5Wm2K1 . Based on our results, this seems difficult to achieve within our current rationale for the tropics at least.


Sunday, August 3, 2014

New paper finds marine clouds cause a negative-feedback cooling effect on climate

A new paper published in Nature Geoscience finds global marine clouds exert a negative feedback cooling effect on Earth's surface temperatures. However, all current IPCC models adopt net positive feedbacks for water vapor and clouds, and this false assumption may account for a large portion of the exaggerated warming models project (in addition to the climate being less sensitive to CO2 than the IPCC assumes).

According to the authors, 
"a 6% increase in the albedo of global marine stratiform clouds could offset the warming that would result from a doubling of atmospheric CO2 concentrations" i.e. just clouds over the oceans alone, not considering clouds over land.
and as previously noted by Dr. Roy Spencer,
"The most obvious way for warming to be caused naturally is for small, natural fluctuations in the circulation patterns of the atmosphere and ocean to result in a 1% or 2% decrease in global cloud cover. Clouds are the Earth’s sunshade, and if cloud cover changes for any reason, you have global warming — or global cooling."
According to the paper,  
"The estimated intrinsic [marine cloud] forcing is −0.49 ± 0.33 Wm−2, and for the extrinsic (cloud-cover effect) forcing, we estimate −0.46 ± 0.31 Wm−2" "We have also estimated the long-wave component of aerosol–cloud radiative forcing (Supplementary Information); the estimated long-wave TOA [Top Of Atmosphere] intrinsic and extrinsic forcings are −0.01 and 0.09 W m−2, respectively."
Adding the 4 forcings obtains a net shortwave and longwave marine cloud forcing of negative 0.87 Wm-2, higher than many climate sensitivity estimates for a doubling of CO2 levels. 


Global mean intrinsic aerosol-cloud radiative forcing by global marine clouds is estimated to be negative 0.49 Wm-2
Excerpt:

Using equations (1) and (2), we estimate the aerosol–cloud
 radiative   forcing   for   global   single-layer   marine   warm   clouds
 between   60◦ S   and   60◦ N.   The   estimated   intrinsic   forcing   is
 −0.49 ± 0.33 W m−2,   and   for   the   extrinsic   (cloud-cover effect)
 forcing, we estimate −0.46 ± 0.31 W m−2, a similar magnitude
 to the estimated intrinsic forcing (Supplementary Fig. 2). This
 corroborates the finding in ref. 21 that the combined Twomey
 and   LWP   effects   (that   is,   intrinsic   forcing)   are   comparable   in
 magnitude to the cloud-cover effect. It should be noted that the
 observed positive correlation between  cloud  cover and aerosol
 level may be subject to other processes or artefacts 22,23, including
 cloud contamination of satellite-retrieved AOD, co-variation of
 cloud fraction and relative humidity/wind speed, cloud processing
 of aerosols, and so on. Owing to uncertainties that cannot be
 quantified directly, the magnitude of the extrinsic forcing may
 be biased. We have also estimated the long-wave component of
 aerosol–cloud radiative forcing (Supplementary Information); the
 estimated long-wave Top Of Atmosphere intrinsic and extrinsic 
forcings are −0.01  and 0.09 W m−2, respectively.




Satellite-based estimate of global aerosol–cloud radiative forcing by marine warm clouds


Nature Geoscience
 
 
doi:10.1038/ngeo2214
Received
 
Accepted
 
Published online
 
Changes in aerosol concentrations affect cloud albedo and Earth’s radiative balance1. Aerosol radiative forcing from pre-industrial time to the present due to the effect of atmospheric aerosol levels on the micro- and macrophysics of clouds bears the largest uncertainty among external influences on climate change1. Of all cloud forms, low-level marine clouds exert the largest impact on the planet’s albedo2. For example, a 6% increase in the albedo of global marine stratiform clouds could offset the warming that would result from a doubling of atmospheric CO2 concentrations3. Marine warm cloud properties are thought to depend on aerosol levels and large-scale dynamic or thermodynamic states456. Here we present a comprehensive analysis of multiple measurements from the A-Train constellation of Earth-observing satellites, to quantify the radiative forcing exerted by aerosols interacting with marine clouds. Specifically, we analyse observations of co-located aerosols and clouds over the world’s oceans for the period August 2006–April 2011, comprising over 7.3 million CloudSat single-layer marine warm cloud pixels. We find that thermodynamic conditions—that is, tropospheric stability and humidity in the free troposphere—and the state of precipitation act together to govern the cloud liquid water responses to the presence of aerosols and the strength of aerosol–cloud radiative forcing.



Friday, May 9, 2014

New paper finds clouds have a net negative-feedback cooling effect

A paper published today in Climate Dynamics finds that clouds have a large net negative feedback cooling effect on the Earth and atmosphere. However, all current IPCC models adopt net positive feedbacks for water vapor and clouds, and this false assumption may account for a large portion of the exaggerated warming models project:


According to the authors, "A large degree of uncertainty in global climate models (GCMs) can be attributed to the representation of clouds and how they interact with incoming solar and outgoing longwave radiation." The paper finds "The averaged SW [shortwave from the Sun], LW [longwave IR from the Earth], and net CRFs [total cloud fractions] from CERES EBAF are −50.1, 27.6, and −22.5 Wm−2, respectively, indicating a net cooling effect of clouds on the TOA [top of the atmosphere] radiation budget."

By way of comparison, the net cooling effect from clouds of -22.5 W/m2 at the top of the atmosphere is about 6 times greater than the assumed radiative forcing from a doubling of CO2 levels of 3.7 W/m2.

As 
Dr. Roy Spencer notes,
"The most obvious way for warming to be caused naturally is for small, natural fluctuations in the circulation patterns of the atmosphere and ocean to result in a 1% or 2% decrease in global cloud cover. Clouds are the Earth’s sunshade, and if cloud cover changes for any reason, you have global warming — or global cooling."
Indeed, the authors of this paper find that " CF [total cloud fraction] is a primary modulator of warming (or cooling) in the atmosphere" and that the net effect of more clouds produces a net negative-feedback cooling effect. 

Evaluation of CMIP5 simulated clouds and TOA radiation budgets using NASA satellite observations

Erica K. Dolinar et al 

A large degree of uncertainty in global climate models (GCMs) can be attributed to the representation of clouds and how they interact with incoming solar and outgoing longwave radiation. In this study, the simulated total cloud fraction (CF), cloud water path (CWP), top of the atmosphere (TOA) radiation budgets and cloud radiative forcings (CRFs) from 28 CMIP5 AMIP models are evaluated and compared with multiple satellite observations from CERES, MODIS, ISCCP, CloudSat, and CALIPSO. The multimodel ensemble mean CF (57.6 %) is, on average, underestimated by nearly 8 % (between 65°N/S) when compared to CERES–MODIS (CM) and ISCCP results while an even larger negative bias (17.1 %) exists compared to the CloudSat/CALIPSO results. CWP bias is similar in comparison to the CF results, with a negative bias of 16.1 gm−2 compared to CM. The model simulated and CERES EBAF observed TOA reflected SW and OLR fluxes on average differ by 1.8 and −0.9 Wm−2, respectively. The averaged SW [shortwave], LW [longwave], and net CRFs [total cloud fractions] from CERES EBAF are −50.1, 27.6, and −22.5 Wm−2, respectively, indicating a net cooling effect of clouds on the TOA [top of the atmosphere] radiation budget. The differences in SW and LW CRFs between observations and the multimodel ensemble means are only −1.3 and −1.6 Wm−2, respectively, resulting in a larger net cooling effect of 2.9 Wm−2 in the model simulations. A further investigation of cloud properties and CRFs reveals that the GCM biases in atmospheric upwelling (15°S–15°N) regimes are much less than in their downwelling (15°–45°N/S) counterparts over the oceans. Sensitivity studies have shown that the magnitude of SW cloud radiative cooling increases significantly with increasing CF at similar rates (~−1.25 Wm−2 %−1) in both regimes. The LW cloud radiative warming increases with increasing CF but is regime dependent, suggested by the different slopes over the upwelling and downwelling regimes (0.81 and 0.22 Wm−2 %−1, respectively). Through a comprehensive error analysis, we found that CF [total cloud fraction] is a primary modulator of warming (or cooling) in the atmosphere. The comparisons and statistical results from this study may provide helpful insight for improving GCM simulations of clouds and TOA radiation budgets in future versions of CMIP.

Related:


Wednesday, August 28, 2013

New paper finds a significant increase of solar energy at Earth's surface from 1979-2011

A paper published today in Atmospheric Chemistry and Physics finds a significant increase of solar energy reaching the Earth's surface over the period from 1979-2011. According to the authors, the observed global brightening "corresponds to an increase of 2.7 W m−2 of solar energy reaching the Earth's surface and an increase of 1.4% or 2.3 W m−2 absorbed by the surface, which is partially offset by increased longwave cooling [from 'greenhouse' gases] to space." By way of comparison, the alleged increase of radiative forcing from CO2 during the same time period is 0.8* W m-2, 70% less than the effect of global brightening. As noted by Dr. Roy Spencer, a 1-2% change in solar energy received at Earth's surface can alone account for global warming - or global cooling.

*5.35*ln(391.63/336.78)
Atmos. Chem. Phys., 13, 8505-8524, 2013
www.atmos-chem-phys.net/13/8505/2013/
doi:10.5194/acp-13-8505-2013

A net decrease in the Earth's cloud, aerosol, and surface 340 nm reflectivity during the past 33 yr (1979–2011)
J. Herman1,2, M. T. DeLand2,3, L.-K. Huang2,3, G. Labow2,3, D. Larko2,3, S. A. Lloyd2,5, J. Mao2,4, W. Qin2,3, and C. Weaver2,4
1Joint Center for Earth Systems Technology (JCET) Center, University of Maryland, Baltimore County, Catonsville, MD 21228, USA
2NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
3Science Systems and Applications (SSAI), Inc., Lanham, MD 20706, USA
4Earth System Science Interdisciplinary Center (ESSIC), University of Maryland, College Park, MD 20740, USA
5Wyle Science, Technology and Engineering, Houston, TX 77058, USA

Abstract. Measured upwelling radiances from Nimbus-7 SBUV (Solar Backscatter Ultraviolet) and seven NOAA SBUV/2 instruments have been used to calculate the 340 nm Lambertian equivalent reflectivity (LER) of the Earth from 1979 to 2011 after applying a common calibration. The 340 nm LER is highly correlated with cloud and aerosol cover because of the low surface reflectivity of the land and oceans (typically 2 to 6 RU, reflectivity units, where 1 RU = 0.01 = 1.0%) relative to the much higher reflectivity of clouds plus nonabsorbing aerosols (typically 10 to 90 RU). Because of the nearly constant seasonal and long-term 340 nm surface reflectivity in areas without snow and ice, the 340 nm LER can be used to estimate changes in cloud plus aerosol amount associated with seasonal and interannual variability and decadal climate change. The annual motion of the Intertropical Convergence Zone (ITCZ), episodic El Niño Southern Oscillation (ENSO), and latitude-dependent seasonal cycles are apparent in the LER time series. LER trend estimates from 5° zonal average and from 2° × 5° , latitude × longitude, time series show that there has been a global net decrease in 340 nm cloud plus aerosol reflectivity. The decrease in cos2(latitude) weighted average LER from 60° S to 60° N is 0.79 ± 0.03 RU over 33 yr, corresponding to a 3.6 ± 0.2% decrease in LER. Applying a 3.6% cloud reflectivity perturbation to the shortwave energy balance partitioning given by Trenberth et al. (2009) corresponds to an increase of 2.7 W m−2 of solar energy reaching the Earth's surface and an increase of 1.4% or 2.3 W m−2 absorbed by the surface, which is partially offset by increased longwave cooling [from 'greenhouse gases'] to space. Most of the decreases in LER occur over land, with the largest decreases occurring over the US (−0.97 RU decade−1), Brazil (−0.9 RU decade−1), and central Europe (−1.35 RU decade−1). There are reflectivity increases near the west coast of Peru and Chile (0.8 ± 0.1 RU decade−1), over parts of India, China, and Indochina, and almost no change over Australia. The largest Pacific Ocean change is −2 ± 0.1 RU decade−1over the central equatorial region associated with ENSO. There has been little observed change in LER over central Greenland, but there has been a significant decrease over a portion of the west coast of Greenland. Similar significant decreases in LER are observed over a portion of the coast of Antarctica for longitudes −160° to −60° and 80° to 150°.

Monday, December 10, 2012

New paper finds more evidence of the 'poor performance' of climate models

A new paper published in the Journal of Climate finds there has been "little to no improvement" in simulating clouds by state-of-the-art climate models. The authors note the "poor performance of current global climate models in simulating realistic [clouds]," and that the models show "quite large biases...as well as a remarkable degree of variation" with the differences between models remaining "large." 

As Dr. Roy Spencer points out in his book
"The most obvious way for warming to be caused naturally is for small, natural fluctuations in the circulation patterns of the atmosphere and ocean to result in a 1% or 2% decrease in global cloud cover. Clouds are the Earth’s sunshade, and if cloud cover changes for any reason, you have global warming — or global cooling."

This new paper is one of many that demonstrate current climate models do not even approach the level of accuracy [within 1 - 2%] or 'consensus' required to properly model global cloud cover, and therefore cannot be used as 'proof' of anthropogenic global warming, nor relied upon for future projections.

Prior posts on clouds and the abject failure of climate models


Simulating clouds with global climate models: A comparison of CMIP5 results with CMIP3 and satellite data

Axel Lauer1,* and Kevin Hamilton1,2
1 International Pacific Research Center, University of Hawaii at Manoa, Honolulu, Hawaii
2 Department of Meteorology, University of Hawaii at Manoa, Honolulu, Hawaii

Abstract
Clouds are a key component of the climate system affecting radiative balances as well as the hydrological cycle. Previous studies from the Coupled Model Intercomparison Project Phase 3 (CMIP3) showed quite large biases in the simulated cloud climatology affecting all GCMs [global climate models] as well as a remarkable degree of variation among the models, which represented the state-of-the-art circa 2005. Here we measure the progress that has been made in recent years by comparing mean cloud properties, interannual variability, and the climatological seasonal cycle from the CMIP5 models with satellite observations and with results from comparable CMIP3 experiments. We focus on three climate-relevant cloud parameters: cloud amount, liquid water path, and cloud radiative forcing. We show that intermodel differences are still large in the CMIP5 simulations. We find some small improvements of particular cloud properties in some regions in the CMIP5 ensemble over CMIP3. In CMIP5 there is an improved agreement of the modeled interannual variability of liquid water path as well as of the modeled longwave cloud forcing over mid and high latitude oceans with observations. However, the differences in the simulated cloud climatology from CMIP3 and CMIP5 are generally small and there is very little to no improvement apparent in the tropical and subtropical regions in CMIP5.

Comparisons of the results from the coupled CMIP5 models with their atmosphere-only versions run with observed SSTs show remarkably similar biases in the simulated cloud climatologies. This suggests the treatments of subgrid-scale cloud and boundary layer processes are directly implicated in the poor performance of current GCMs [global climate models or general circulation models] in simulating realistic cloud fields.

Friday, October 26, 2012

Seven recent papers that disprove man-made global warming

Re-posted from the Australian Climate Skeptics Party website:

Has Man-made global warming been disproved? A Review of Recent Papers.
Anthony Cox and Jo Nova
Introduction
Climate Change was described in 2007 by the soon to be, briefly, Australian prime Minister, Kevin Rudd, as the “greatest moral, economic and environmental challenge of our generation.” By Climate Change Rudd meant anthropogenic global warming, or global warming as it was originally described by Al Gore.
Government attempts to ‘solve’ global warming are framed by hyperbole and urgent policies. These policies involve the expenditure of vast amounts of money1,2 and are justified because we are told “The science is settled”3.
Science is never settled. Richard Feynman said [The Meaning of it All, 1999]:
The exception proves that the rule is wrong. That is the principle of science. If there is an exception to any rule, and if it can be proved by observation, that rule is wrong.
The dominant argument for global warming contradicts Feynman’s “principle of science”. This dominant argument is that a majority of scientists, a consensus, support it4. But as Feynman notes consensus is a false proof of a scientific theory because only one contradictory bit of empirical evidence is sufficient to refute that theory.
In fact not one but seven recent peer-reviewed papers have revealed what would seem to be fatal flaws in global warming. Global warming says there has been an increase in the global average temperature since the mid-20th century and its projected continuation. According to the Intergovernmental Panel on Climate Change [IPCC] “most of the observed increase in globally averaged temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations.” [AR4, Working Group 1, page 10].
For purposes of this essay then global warming is the increase in global average temperature primarily caused by human emissions of greenhouse gases, primarily carbon dioxide [CO2].
The seven papers discussed use different methods to critique global warming but are all based on empirical data and are in rough agreement that any increase in global average temperature due to a doubling of CO2 is more likely to be about half a degree than the 3.26 degrees determined by the IPCC [AR4, Box 10.2]. The extent of the change in global average temperature to a doubling in COis known as the climate sensitivity [see Figure 8].
A forcing is a factor external to or introduced to the climate system which affects, for a period, the radiative balance at the Tropopause, the boundary between the Troposphere and the Stratosphere. The IPCC recognises 2 main types of forcings; greenhouse gases, the most dominant one being CO2, and solar radiation. A feedback is a change in another quantity in the climate system as a response to a change in a forcing. The IPCC assumes that an increase in forcing from an increase in anthropogenic CO2 causes a feedback by an increase in water vapour [AR4, FAQ 1.3]. This process is measured by the change in global average temperature. However, as some scientists note, the distinction between a forcing and a feedback is not clear:
However, disadvantageously, including non-instantaneous processes clearly blurs the distinction between forcing and feedback as there is no longer a clear timescale to separate the two; further including these processes in the forcing incorporates more uncertain aspects of a climate models response [Forster et al., 2007].5
The following papers clarify this uncertainty between forcings and feedbacks and show that the global warming science is not clear about the distinction or effects. The papers show the IPCC assumptions about the role of CO2 and water vapor, particularly in the form of clouds, are incorrect and that the IPCC conclusions about climate sensitivity are both exaggerated and wrong. In doing so, these papers also vindicate Feynman’s maxim.

1      Lindzen and Choi –The Earth has a safety release valve

Figure 1 6
From Wielicki, B.A., T. Wong, et al, 2002: Evidence for large decadal variability in the tropical mean radiative energy budget. Science, 295, 841-844.
If global warming is going to happen it will be due to feedbacks. If the feedbacks are positive it means that as the world warms, atmospheric conditions would have to change to keep evenmore of the sun’s energy inside our system. But Richard Lindzen and Yong-Sang Choi show that as the world warms Earth’s dynamic system changes to let more of the infra red or long-wave energy out to space [LW from Figure 1]. It’s like a safety release valve. This means that the system has negative feedbacks (like almost all known natural systems). The changesdampen the effects of extra CO2. If there is no net amplifying positive feedback there is no catastrophe. Because Lindzen & Choi are looking at long-wave radiation leaving the planet [outgoing long-wave radiation], this is a way of assessing all forms of feedbacks at once. We can’t tell which part of the system is responsible: clouds, humidity, ice-cover or vegetation, but we know the net effect of all of them together is that when the world warms, more energy escapes from the planet.
Their research was first posted in 20097 and updated in 20108 as a response to earlier criticisms. In the 2009 paper Lindzen & Choi measured changes in the outgoing long-wave radiation leaving from the top of the atmosphere during periods that the world warmed. Their findings were a direct contradiction to global warming because they showed that increased CO2did not block outgoing long-wave radiation. With no blockage the level of available energy in the climate system also did not increase. With no increase of available energy there was no energy to cause positive feedbacks and increase temperature.
Kevin Trenberth, a leading climate modeler, criticized the first paper. Those criticisms concerned the extent of satellite data used by Lindzen & Choi, their concentration on the tropics and various statistical methodologies. All of these complaints were addressed by the subsequent paper. They still found that outgoing long-wave radiation increased as the world warmed, which was different to what all the models predicted.

2      Spencer and Braswell – Cloud feedback is net negative

In a 2007 paper Roy Spencer and Danny Braswell undertook empirical measurements of cloud radiative forcings which are a net result of blockage by clouds of solar radiation coming in to the atmosphere [cooling] and blockage by clouds of long-wave radiation leaving the atmosphere [warming]; they concluded that
“the net radiative effect of clouds…is to cool the ocean atmosphere system during its tropospheric warm phase and warm it during its cool phase.” 9
That is, clouds moderate or dampen temperature movement in either direction.
Spencer & Braswell’s papers in 200810 and 201011 took a different approach to Lindzen & Choi. Spencer & Braswell looked more closely at the nature of feedbacks and forcings and the difficulty of putting a value on feedbacks. The IPCC models assume that clouds change inresponse to temperature, so they are a “feedback” [AR4, WG1, 8.6.3.2]. But as Spencer & Braswell show in their 2008 and 2010 papers clouds can be a forcing factor as well. This means that if something other than temperature affects cloud cover (like changes in ocean currents or air circulation) the change in clouds would then force the temperature to change.
The latest IPCC report acknowledges that the models don’t simulate clouds well and that’s where the main uncertainties lie. If clouds are not just a forcing in their own right, and provide negative feedback [by shading the earth] that would seriously undermine the premise of global warming. This point is illustrated by two other recent papers.
The first is a report by The Climate Process Team on Low Latitude Cloud Feedbacks on Climate Sensitivity [CPT] 12. CPT found “strongly negative net cloud feedback” in a warming world. Utilizing the climate models from NCAR, GFDL and NASA, CPT found this negative feedback concentrated in the Tropics.
Similarly Allan 201113 based his study on cloud “radiative effect” in the Tropics and concluded a “net cooling of the climate system” from clouds because solar blocking, cooling, was greater than long-wave blocking, warming. However unlike CPT, Allan did not regard this cooling as a feedback since the cloud cooling was not a response to temperature.
Spencer & Braswell provide proof that it’s very difficult to find definitive feedback signals in a dynamic system that is never at equilibrium. The only feedback they can calculate in their 2008 and 2010 papers is negative and means a climate sensitivity of about 0.6 °C for a doubling of CO2, though it’s only applicable over short time-frames. They show the near impossibility of establishing climate sensitivity over long time frames. But if climate sensitivity to CO2 is as low as they find, and dwarfed by potential cloud forcing, it would mean no postponed effect from CO2. We have had all the effect there is and there will be no stored heat lying dormant to cause future climate change. This would explain Trenberth’s concern, expressed in the CRU e-mails that the pro-global warming scientists “can’t account for the lack of warming at the moment and it is a travesty that we can’t”.
Spencer & Braswell’s 201114 paper confirms the difficulty in distinguishing cloud feedback and forcing. They also find the global warming models have substantially overestimated the climate sensitivity due to their lack of understanding of this distinction. One of the reasons that the models have failed to distinguish the effect of clouds on temperature is the difference in time it takes for the radiative effects of temperature and clouds to occur in the system; temperature effects are immediate while those of clouds take some months as Figure 2 [Figure 3 from Spencer & Braswell 2011] shows.
Figure 2
Spencer & Braswell 2011 has received considerable vitriol from the global warming science. This is unwarranted because this science concedes it has a lack of understanding of clouds. Spencer & Braswell have offered an explanation of clouds strongly correlated with and consistent with observations. The criticism of them would seem, therefore, to be based on preserving the global warming theory rather than answering Trenberth’s concern.

3      R.S. Knox and D.H. Douglass – The missing heat is not in the ocean.

The dominant explanation for where Trenberth’s missing warming or heat is that it is in the ocean. This missing heat is the difference between the climate effects, particularly change in global average temperature, which global warming predicted we would have and the much lower change in global average temperature we have had. In 2009 modeling von Shuckmann et al15 seemed to have found this missing heat at depths of 2000 metres in the ocean. One immediate problem for von Shuckmann et al is found in the NOAA graph in Figure 3. This graph is based on data for ocean heat content to depths of 700 metres which show no warming from 2003:
Figure 3: [http://www.nodc.noaa.gov/OC5/3M_HEAT_CONTENT/index.html]

The problem this shows for von Shuckmann et al [and other papers which also use modeling to ‘find’ deep-ocean warming16] is; how could the ocean depths be warming when the ocean top was cooling?
A second problem was raised in 2 papers by the team of Ablain17 and Cazenave18; they showed that not only was the rate of sea level rise decreasing but the steric part of the sea level rise, which is based on ocean heat content, was also decreasing from 2006.
The third contradiction to von Shuckmann et al and the missing heat is in Knox and Douglass’s paper19. Knox & Douglass are both imminent atmospheric physicists and have already written a number of papers dealing with ocean based climatic events and the connection between the ocean radiative rate of change [Fohc] and the radiative rate of change at the top of the atmosphere [Ftoa].
In their latest paper Knox & Douglass showed that not only was ocean heat content declining but that the Fohc was negative, which meant more radiative energy was leaving the ocean than being stored:
Figure 4 From Knox & Douglass page 1. Fohc left scale.
Figure 1. Ocean heat content from Argo (left scale: blue, original data; red, filtered) and ocean surface temperatures (right scale, green). Conversion of the OHC slope to W/m2 is made by multiplying by 0.62, yielding –0.161 W/m2.
Knox & Douglass’s findings about ocean heat content were based on empirical measurements and are consistent with studies by Willis, Loehle, and Pielke, and NOAA data [see Figure 3].
Knox & Douglass conclude that because “90% of the variable heat content resides in the upper ocean” the Fohc can accurately infer the Ftoa. Therefore if Fohc is negative then Ftoa is as well. A negative Ftoa is contrary to Trenberth’s claims of missing heat being stored most likely in the oceans. Without missing heat the models have greatly overestimated the effect of global warming.



4      Miskolczi – The optical depth of the atmosphere hasn’t changed

Figure 5 [from Miskolczi 2010]

Ferenc Miskolczi was a NASA atmospheric physicist whose 2 papers in 200720 and 201021were both peer reviewed and have never been refuted. These papers draw on data and calculations made by Miskolczi in a 2004 paper co-authored by NASA physicist Martin Mlynczak. Miskolczi 200422 shows that radiation leaving the Earth, outgoing long-wave radiation, is based on zonal and global averages of real atmospheric conditions as shown in the atmospheric optical thickness.
 Miskolczi 2007 and 2010 measure “the true greenhouse-gas optical thickness” [Abstract, Miskolczi 2010]. This is made up of two parts which are depicted in Figure 4.
a.     Ï„--  is defined as “the total IR flux optical depth” [page 5 Miskolczi 2007]. This is a measure of the total amount of infra-red or long-wave radiation which is absorbed between the surface and the top of the atmosphere.
b.     A -- is the flux absorbance [page 3 Miskolczi 2010] and is a measure of what wavelengths of long-wave radiation are being absorbed and transmitted in the atmosphere by 11 greenhouse gases [page 7, Miskolczi 2004].

Together Ï„A and A are the optical depth of the atmosphere The optical depth is a kind of proxy measure of the greenhouse effect. Global warming says that more COwill increase the optical depth. Miskolczi showed that available empirical measurements of the optical depth are consistent with no change in 61 years. This means that even though CO2 has increased over the 61 years of measurement and increased the optical depth slightly, “variations in water vapor column amounts” [Figure 11, Miskolczi 2010] have decreased the optical depth by a similar amount. Paltridge et al.23 have confirmed a decrease in water vapor for this period.
 If the optical depth has not increased overall, it suggests the slight warming of the 20th C has not been due to an increase in the greenhouse effect.
In addition Miskolczi also finds no positive feedback from water vapor on atmospheric long-wave radiation absorption, which negates what the models have predicted; this lack of positive feedback has been confirmed by the missing ‘Tropical hot spot’ [see section 6].

5      McShane and Wyner24 – The Hockeystick is broken

Figure 6. McShane&Wyner, page 36

Blakeley McShane and Abraham Wyner attempted to replicate Michael Mann’s infamous hockeystick using Mann’s own data. The hockeystick first appeared in Mann’s 1998 paper and has been a centre-piece of global warming evidence ever since. The hockeystick is important because it supposedly shows recent warming is exceptional and “unprecedented”. The hockeystick is based on dendro-climatic proxies or tree-rings which supposedly provide evidence for past temperatures. Mann’s hockeystick shows basically flat temperature until the 20th C and then a sudden and rapid increase.
Mann’s data was highly problematic. Mann had used the wrong type of tree, and at times, hardly any samples. Some of the tree-ring records even show the opposite “temperature” trend to what thermometers show suggesting those trees don’t make a good or accurate alternative to thermometers.
McShane &Wyner tried to create the same graph from the same data, but, as Figure 5 above shows, could not. They conclude:
“Using our model, we calculate that there is a 36% posterior probability that 1998 was the warmest year over the past thousand. If we consider rolling decades, 1997-2006 is the warmest on record; our model gives an 80% chance that it was the warmest in the past thousand years. Finally, if we look at rolling thirty-year blocks, the posterior probability that the last thirty years (again, the warmest on record) were the warmest over the past thousand is 38%.”[page 37]
So, even using Mann’s dubious data and employing a variety of statistical methods, McShane & Wyner’s model suggests that there is only an 80% chance that one recent decade was the warmest of the last 1000 years, and 1998 is most likely not the warmest year [64% against] and the last 30 year period, is also unlikely to have been the warmest [62% against]. In other words, the type of weather we have now has all occurred before, and in the not too distant past when CO2 was supposedly low.
The paper correctly describes the importance of the hockeystick not only to global warming but also Green policies:
 “the effort of world governments to pass legislation to cut carbon to pre-industrial levels cannot proceed without the consent of the governed and historical reconstructions from paleoclimatological models [ie hockeysticks] have indeed proven persuasive and effective at winning the hearts and minds of the populace.” [page 2]
It would seem the hearts and minds have been won with false promises.
In recognition of the importance of McShane & Wyner’s paper it was published as an edition discussion piece in Annals of Applied Statistics25 As well as the original paper 15 discussion papers were included in the edition.
Two salient points emerge from this discussion. The first is noted in McIntyre and McKitrick’s comment where they say:
McShane & Wyner’s results are, in a sense, a best case as they assume that the quality of the data set is satisfactory [page 4]
In fact, as noted, the data was not satisfactory. The significance of this is that the ‘science’ of the hockeystick is the data; the data is the proxy for the climatic processes which are analysed in McShane & Wyner’s statistical overview.
This statistical analysis is the second point and it is in this respect that McShane & Wyner are unassailable because they have anticipated every complaint and objection to their critique of Mann’s statistical justification for the hockeystick. As this stage therefore their view on the hockeystick is definitive.

6      McKitrick, McIntyre, Herman26 - The hot spot is really missing

Figure 7. Based on Figures 2 and 3, page 13 of McKitrick et al.

If the IPCC models are right about the feedbacks, we would see a hot spot 10km above the tropics. Global warming theory says this should happen because more water will have been evaporated to this part of the atmosphere and would have caused rapid warming. Observations as shown in Figure 7 contradict this . Thus the main, most powerful factor in the climate models turns out to not match the real world.
Douglass et al 27 pointed out the glaring discrepancy of the missing hot spot in 2007. However Douglass et al did not adequately distinguish model variability in terms of single model or ensemble model outputs. Nor did Douglass et al adjust the data for autocorrelation which meant the data did not have satisfactory confidence levels or error bars.
As a result Santer et al [2008] 28 claimed Douglass got it wrong, and that the data and the models did agree. But Santer et al used a truncated set of data ending in 1999 to achieve the model and data correlation.
Christy et al [2010] 29 responded to Santer et al by developing a scaling ratio comparing the atmospheric trend to the surface trend. Christy et al showed the models predicted a scaling ratio of 1.4 ±0.8 [i.e. the atmosphere should warm 40% faster than the surface]. In reality the observations showed a scaling ratio of 0.8 ± 0.3 [i.e. the atmosphere was not warming as fast as the surface].
McKitrick et al [2010] also use the extended data and addressed the data adjustment issues but used a greater range of statistical analysis. They found that the model predictions are about 4 times higher and outside the error bars of the weather balloons and satellites measurements [see Figure 7].
McKitrick et al’s findings have been replicated by Fu et al 30 who also find a discrepancy between the models and observations about Troposphere warming, although not to the same extent as McKitrick et al do. However, in a follow-up paper, McKitrick 31 not only confirms that the predictions of warming by the models have been exaggerated but also shows the small amount of recent warming was due to a natural climate shift in 1977. This climate shift has been noted by many other researchers 32 and means global warming is playing an even smaller role then predicted by the models.
As noted in section 4, the absence of a tropical hot spot vindicates Miskolczi because either the optical depth is not changing or, if it is, it means that extra water vapor and CO2, which would change the optical depth, are not heating in the way predicted by AGW.
7 Anagnostopoulos, G. G., Koutsoyiannis, D., Christofides, A., Efstratiadis, A. & Mamassis, N.: The only thing certain is the models are wrong.
If McKitrick et al shows that the IPCC global computer models can’t model the present and therefore the future, Professor Demetrius Koutsoyiannis and his team show those models can’t even model the past
Koutsoyiannis is one of the world’s leading hydrologists and an expert on Hurst and stochastic effects. Hurst or Long Term Persistence refers to the uncertainty and random qualities present in all complex natural systems. Koutsoyiannis argues that global warming modeling does not take into account this uncertainty.
In his 2008 paper Koutsoyiannis33 compared the model predictions from 1990 to 2008 and whether those models could retrospectively match the actual temperature over the past 100 years. This test of retrospectivity is called hindcasting. If a model has valid assumptions about the climatic effect of variables such as greenhouse gases, particularly CO2, then the model should be able to match past known data.
Koutsoyiannis’s 2008 paper has not had a peer reviewed rebuttal but was subject to a critique at Real Climate by Gavin Schmidt.34 Schmidt’s criticism was 4-fold; that Koutsoyiannis uses a regional comparison, few models, real temperatures not anomalies and too short a time period.
Each of Schmidt’s criticisms was either wrong or anticipated by Koutsoyiannis. The period from 1990-2008 was the period in which IPCC modeling had occurred; the IPCC had argued that regional effects from global warming would occur; model ensembles were used by Koutsoyiannis; and since the full 100 year temperature and rainfall data was used in intra-annual and 30 year periods by Koutsoyiannis anomalies were irrelevant.
In 2008 Koutsoyiannis found that while the models had some success with the monthly data all the models were “irrelevant with reality” at the 30 year climate scale.
Koutsoyiannis’s 201035 paper “is a continuation and expansion of Koutsoyiannis 2008”. The differences are that (a) Koutsoyiannis 2008 had tested only eight points, whereas 2010 tests 55 points for each variable; (b) 2010 examines more variables in addition to mean temperature and precipitation; and (c) 2010 compares at a large scale in addition to point scale. The large, continental scale in this case is the contiguous US.
Again Koutsoyiannis 2010 found that the models did not hindcast successfully with real data from all the 55 world regions not matching what the models produced. The models were even worse in hindcasting against the real data for the US continent.
So that is 3 strikes for global warming models; they could not predict the future in 1990; they cannot predict the present and they could not replicate or match the past.

Conclusion

The global warming models amplify CO2’s effect by 3 – 7 fold, but no matter how you measure it [outgoing long wave radiation, cloud changes, optical depth, historical temperatures, vertical heating patterns in the atmosphere] the real measurements contradict the models and their assumptions about the feedbacks appear to be unconnected with real data. It follows that the global warming predictions about climate sensitivity to a doubling of COare exaggerated by at least 3C.
Figure 8 Climate Sensitivity Comparison

The Hansen36 point of 1.2C in Figure 8 is a non-feedback calculation for the temperature increase from a doubling of CO2. While that non-feedback figure is essentially meaningless in the real world it is a convenient half-way house between the climate sensitivity estimates of the IPCC and the models which assume positive feedback and the empirical measurements of the papers discussed in this article which consider the actual measured feedbacks to increases in CO2.
The climate sensitivity estimates of the discussed papers establish two points which are fundamentally opposite to global warming. The first is that a large portion of the temperature response to 2X CO2 has already occurred. COatmospheric concentrations have risen approximately 40% since 1900. Any temperature increase due to the increase in COduring this period would have already occurred.
The second point and as a corollary to the first is that there is no delay or lag in temperature response as a proxy for climate sensitivity. The IPCC makes a distinction between transient climate sensitivity and equilibrium climate sensitivity with transient climate sensitivity being less and on a shorter term than equilibrium sensitivity [see AR4, WG 1, TS.6.4.2]. These papers strongly suggest that there is no such distinction between transient and equilibrium sensitivity and that any COtemperature response is not delayed. This aspect of climate sensitivity has been independently confirmed in the Beenstock and Reingewertz analysis.37 Beenstock finds that any effect COincrease has on temperature is temporary and not related to the absolute level ofCO2.
The global warming predictions are contradicted by past, present and future data. Feynman’s maxim applies and the vast funding which is now being directed to ‘solving’ global warming should be redirected to hypothesis which are consistent with empirical data and confirmed by observable evidence.

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