Flat Earth Al calls Global Warming Skeptics “Racists”

However, it is Al Gore himself who seeks to reduce world population in underdeveloped countries by installing his carbon tax scam, which would not allow the developing world to achieve First World living standards.

By Caroline May
The Daily Caller
August 28, 2011

One day climate change skeptics will be seen in the same negative light as racists, or so says former Vice President Al Gore.

In an interview with former advertising executive and Climate Reality Project collaborator Alex Bogusky broadcast on UStream on Friday, Gore explained that in order for climate change alarmists to succeed, they must “win the conversation” against those who deny there is a crisis. (RELATED: Bill McKibben: Global warming to blame for Hurricane Irene).

“I remember, again going back to my early years in the South, when the Civil Rights revolution was unfolding, there were two things that really made an impression on me,” Gore said. “My generation watched Bull Connor turning the hose on civil rights demonstrators and we went, ‘Whoa! How gross and evil is that?’ My generation asked old people, ‘Explain to me again why it is okay to discriminate against people because their skin color is different?’ And when they couldn’t really answer that question with integrity, the change really started.”

The former vice president recalled how society succeeded in marginalizing racists and said climate change skeptics must be defeated in the same manner.

“Secondly, back to this phrase ‘win the conversation,’” he continued. “There came a time when friends or people you work with or people you were in clubs with — you’re much younger than me so you didn’t have to go through this personally — but there came a time when racist comments would come up in the course of the conversation and in years past they were just natural. Then there came a time when people would say, ‘Hey, man why do you talk that way, I mean that is wrong. I don’t go for that so don’t talk that way around me. I just don’t believe that.’ That happened in millions of conversations and slowly the conversation was won.”

“We have to win the conversation on climate,” Gore added.

When Bogusky questioned the analogy, asking if the scientific reasoning behind climate change skeptics might throw a wrench into the good and evil comparison with racism, Gore did not back down.

“I think it’s the same where the moral component is concerned and where the facts are concerned I think it is important to get that out there, absolutely,” Gore said.

Gore also took shots at Texas Gov. Rick Perry, who has lambasted climate change alarmists on the presidential campaign trail, and at other politicians who dare to question the veracity of global warming science.

“This is an organized effort to attack the reputation of the scientific community as a whole, to attack their integrity, and to slander them with the lie that they are making up the science in order to make money,” Gore said.

Ironically, back during Perry’s days as a Democrat, the Texas governor supported Gore in his 1988 presidential bid. Perry became a Republican in 1989.

Majority of Human Race Does Not See Global Warming as Serious Threat

CNSNews.com
April 26, 2011

Most of the human race does not see global warming as a serious threat, according to a Gallup poll released last week that surveyed individuals in 111 countries.

Respondents were asked: “How serious of a threat is global warming to you and your family?” They were given the options of answering: not at all serious, not very serious, somewhat serious or very serious.

Worldwide, only 42 percent told Gallup they believed global warming was either a “somewhat serious” or “very serious” threat. Gallup did not publish the separate percentages for each answer.

In the United States, 53 percent said they believed global warming was a “somewhat serious” or “very serious” threat to themselves and their families. That was down from 63 percent in polling that Gallup did on the question in the United States in 2007 and 2008.

Of the 111 countries that Gallup polled, Greece ranked as No.1 for popular fear of global warming. In that southern European country 87 percent said global warming was a “somewhat serious” or “very serious” threat.

That was a far higher percentage than across the Mediterranean in Egypt, a desert nation, where only 18 percent said they believed global warming was a somewhat serious or very serious threat.

Somaliland ranked dead last—with only 10 percent of local residents saying global warming was a somewhat serious or very serious threat.

Yemen ranked second to last with 13 percent.

China, the world’s largest greenhouse gas emitter, ranked 105th out of 111 among the countries polled by Gallup. Only 21 percent of Chinese said they believed global warming is a somewhat serious or very serious threat to themselves or their families.

Globalists, Climate Alarmists Move Forward with Deindustrialization Agenda

Reuters
April 8, 2011

Rich and poor nations overcame deep divisions on Friday to cut a deal that maps out U.N. climate negotiations for 2011, building on last December’s agreement in Mexico and hardening the focus on tougher issues.

The deal in Bangkok came after nearly four days of talks that some developing nations said were needed to “recalibrate” U.N. climate negotiations after last year’s Cancun agreements.

They wanted an agenda that tackled the fate of the Kyoto Protocol on fighting global warming and rich countries’ pledges to cut emissions, and clarified sources of cash for poorer nations rather than just building on what was agreed at Cancun.

But many rich nations said some developing nations were simply trying to row back on what was agreed in Cancun and this undermined negotiations this year that culminate in the South African city of Durban from late November.

Many nations were unhappy that much of the April 3-8 meeting was taken up arguing over the agenda, with the United States saying the delay dampened the mood, while some developing nations had misgivings about the end result. All expressed an urgency to press ahead with negotiations.

“It’s less rosy today than when we came in (at the start of the meeting),” senior U.S. negotiator Jonathan Pershing told reporters. In particular, he said some countries wanted to renegotiate the Cancun decisions.

“I don’t think that’s going to be constructive. What became evident is that we can expect more of that going forward,” he said.

Tosi Mpanu Mpanu, chair of the Africa Group, said he had mixed feelings. “Thank god we came up with an agenda. It’s a pity it took so long. What does it say for the rest of the year?”

FRAUGHT

Cancun is widely regarded as saving the often fraught negotiations from collapse.

Nations agreed curbs on the loss of tropical forests, schemes to transfer clean technology to poorer nations and help them adapt to climate change impacts, and a goal for rich countries to provide $100 billion a year in aid from 2020.

But it side-stepped tougher issues, such as whether to extend or replace the Kyoto Protocol, with concerns growing that a new pact or extension to Kyoto will not be agreed before the pact’s first phase ends next year.

Kyoto binds almost 40 industrialized nations to cut greenhouse gas emissions by an average of 5.2 percent below 1990 levels during the five-year period 2008-2012. A second phase is meant to increase those cuts for rich nations.

It is the only pact imposing legal obligations on emissions cuts and the U.N. talks have been hobbled by disagreement over how to extend that obligation to all major economies, such as China, the world’s top greenhouse gas emitter.

The United States is No. 2. It never ratified Kyoto.

In Bangkok, there was a fresh focus on trying to find a compromise, with the agreed agenda stating there should be a continued discussion of the legal options of a new agreement that captures emissions curbs by all major economies.

“This evening in Bangkok, parties agreed an agenda to work toward a comprehensive and balanced outcome at the U.N. Climate Change Conference in Durban,” said U.N. climate chief Christiana Figueres.

But disputes still loom over the size of rich nations’ pledges to cut emissions, with the United Nations saying they are not enough to avoid average global warming of less than 2 degrees Celsius.

Nations agreed in Cancun to work to keep the rise below this level to stave off ever greater extremes of droughts and floods, crop failures and rising sea levels.

Environmental groups were worried by the outcome of Bangkok.

“Once again, delegates could not reach agreement over key issues, including the future of the Kyoto Protocol, bringing the talks to a screeching halt almost from the beginning,” said Tasneem Essop of WWF.

Others pointed to the urgency to act to fight the impacts of climate change.

“There’s uncertainty about where the Cancun agreements take us, and can countries meet their commitments, and is it enough? And I think that was really at the heart of the agenda debate,” said Angela Anderson of the U.S. Climate Action Network.

Albedo and OLR Radiation with Variations of Precipitation – Implications for AGW

By William M. Gray & Barry Schwartz
March 3, 2011

INTRODUCTION

Global warming scenarios from CO2 increases are envisioned to bring about rainfall enhancement and resulting upper troposphere temperature and water vapor increases. The initial warming resulting from the blockage of infrared (IR or OLR) radiation due to CO2’s increases has been programmed in climate models to develop yet additional rainfall, temperature, and water vapor increases. This causes an additional blockage of IR energy to space which is substantially larger than the original CO2 blockage of IR by itself. This additional longwave IR blockage of energy to space (a positive feedback mechanism) is simulated in the models to be twice or more as strong as the original IR blockage from CO2 alone. We question the reality of this positive feedback mechanism. This study is directed towards determining the reality of such large positive feedback processes. This is a crucial question for determining the likely amount of global warming that will result from the anticipated doubling of CO2 by the end of the 21st century.

We have analyzed a wide variety of albedo and IR differences which are associated with rainfall variations on many different space and time scales. Our goal is to determine the extent to which we are able to accept or reject the reality of the Global Climate Model (GCM) simulations. The following analysis indicates that the GCM simulation of the influence of a doubling of CO2 give far too much global warming. We anticipate that a doubling of CO2 will act in a way to cause the global hydrologic cycle to increase in strength by approximately 3-4 percent. Our analysis indicates that there will be very little global temperature increase (~0.3oC) for a doubling of CO2, certainly not the 2-5oC projected by the GCMs.

DATA ANALYSIS

We have analyzed 21 years (1984-2004) of ISCCP (International Satellite Cloud Climatology Project) outgoing solar (albedo) and IR (OLR) on various distance (from local to global) and time scales (from daily to decadal). We have investigated how radiation measurements change with variations in precipitation as determined from NCEP-NCAR reanalysis data on a wide variety of space and time scales (Figure 1). We have stratified our radiation and rainfall data into three latitudinal sections and six longitudinal areas (Figure 2). We analyzed IR and albedo changes which were related to reanalysis-determined rainfall variations by month (January to December) and by yearly periods for the tropics (30oN-30oS; 0-360o) and for the globe, defined as 70oN-70oS; 0-360o for this study.

For each month and region we have categorized our 21 years of ISCCP radiation data into the 10 highest average monthly rainfall values and subtracted the 10 lowest average monthly rainfall values. We analyzed IR and albedo differences between these 10 highest versus 10 lowest precipitation months. These monthly rainfall differences were typically between 4-7 percent of the total rainfall. For the 10 highest minus 10 lowest yearly rainfall differences within the tropics (30oN-30oS; 0-360o) and for most of the globe (70oN-70oS; 0-360o), rainfall differences varied between 2-3 percent.
A second rainfall stratification involved comparing the rainfall and associated IR and albedo differences for variations in rainfall for the years of 1995-2004 versus the years of 1984-1994. The latter 10 years had approximately two percent more tropical and global rainfall than the earlier period. The individual monthly differences for the earlier and latter period were in the range of 3-4 percent of the mean rainfall values.

The third rainfall stratification involved daily mean rainfall and its association with IR and albedo at many individual stations. We also analyzed 3-hourly radiation information associated with daily average rainfall differences. Our individual 3-hour albedo analysis showed that albedos can be as high as 800-1000 Wm-2 over heavy rain and cloud regions near mid-day.

FINDINGS

a)  The albedo occurring over the top of strong precipitation and high cloud regions typically increases at a greater rate than does the usual decrease of IR within these same rain and cloud areas. Heavy rain and cloud areas are local places of strong enhanced net radiation to space (Figure 3 – left diagram). In almost all organized rain and cloud areas we find that albedo to space goes up in both magnitude (Wm-2) and in percentage more than the expected simultaneous magnitude and percentage reduction of IR flux to space.

In the adjacent subsidence areas of little or no cloudiness and rain there is typically a reduction of albedo that is one to two times greater than the enhancement of IR to space (right side of Figure 3). In scattered and broken cloud areas of little or no significant rain there is typically a close balance between the enhancement of IR to space and the reduction of albedo.

b)  IR and albedo usually change in opposite directions. They have a high negative correlation. There are places and times however, where IR and albedo change together to either enhance or to suppress outward radiation flux.

c)  The typical enhancement of rainfall and updraft motion in the cumulus and cumulonimbus clouds within heavy raining meso-scale disturbance areas acts to increase the return flow subsidence in the surrounding broader clear and partly cloudy regions (Figure 4). Global rainfall increases typically cause an overall reduction of specific humidity (q) and relative humidity (RH) in the upper and middle tropospheric levels of the broader scale surrounding subsidence regions. This leads to a net enhancement of IR to space, both over the tropics and the globe. Albedo is typically decreased as much or more than IR is increased in the broadscale clear and partly cloudy areas. But over the rainy and cloudy areas, the albedo is greatly enhanced. The albedo enhancement over the cloud-rain areas tends to increase the net (IR + albedo) energy to space more than the weak suppression of (IR + albedo) in the clear and partly cloudy areas.

d)  We observe that upper level RH and moisture content (q) at 300 mb (~10 km) and 400 mb (~8 km – not shown) are typically reduced for increasing amounts of net tropical rainfall. This is a direct consequence of the slightly greater return flow mass subsidence coming from the smaller areas of strong and concentrated updrafts of the deep cumulonimbus (Cb) rainclouds. This lowering of upper-level water vapor over the broad subsidence areas slightly increases the optical depth (τ) and slightly lowers the radiation emission level to a warmer layer where more IR energy is able to be radiated to space.

The NCEP reanalysis data shows that there has been a steady decrease in upper tropospheric RH over the last 40 years (Figure 6). ISCCP data for the tropics show a small decrease in precipitable water (PW) since the mid 1980s (Figure 7). We do not find that net tropospheric water vapor content is necessarily related to rainfall rate. Increases in tropical and/or global rainfall typically lead to decreases in upper tropospheric water vapor content. This is in contrast with the general assumption of most climate scientists who believe that as global rainfall increases that tropospheric water vapor content will have to rise. This thinking fails to take into account the nature of the small-scale cumulus convective units. With the proper convective cloud model it is quite plausible that upper tropospheric moisture undergoes a decrease as tropical and/or global rainfall rates go upward. A long observational paper is presently being prepared to more fully document our many observations of the association of changes of rainfall with albedo and IR.

4. IMPLICATIONS OF THESE OBSERVATIONS

The above measurements are at odds with the GCM simulations of precipitation increase associated with rising CO2 amounts. Most GCMs show large upper tropospheric tropical temperature and water vapor increases to be associated with increased rates of precipitation. We do not observe such upper tropospheric temperature and moisture gains with rainfall enhancement. The GCM simulations assume that CO2’s blockage of IR stimulates an enhancement of extra rainfall which causes yet larger increases in upper level temperature-moisture and consequently causes stronger reductions in IR energy to space. These assumptions require the models to impose an increase in water vapor (to keep RH constant) as upper level temperature gains occur. We do not observe such upper-level temperature and moisture rises. We do not find that upper tropospheric temperature and RH are necessarily related to each other as the GCMs typically assume. We also do not find that upper and lower tropospheric water vapor amounts are strongly correlated with one another as the GCMs do.

It is possible for the troposphere to gain energy from increases in CO2 and to simultaneously enhance its radiation to space to largely balance out all or most of the CO2 energy gains. Such a compensation will allow CO2 to increase with very little or no gain in tropospheric temperature. Such energy compensation can occur by CO2 increases causing a lowering of the radiation emission level to a warmer temperature and thereby increasing the outward IR (σT4) flux to space. The energy compensation can also occur by assuming that the CO2-induced extra cloudiness-rainfall causes a compensating rise in albedo. Or, the CO2-induced blockage could be compensated for (as the GCMs have chosen to do) by having upper tropospheric temperature rise by amounts of 3-4oC or more. Our observations suggest that such an upper-level warming and consequent moistening process due to rising levels of CO2 does not occur.

Read Full Study…

Climate Sensitivity Reconsidered Part 1

A special report from Christopher Monckton of Brenchley for all Climate Alarmists, Consensus Theorists and Anthropogenic Global Warming Supporters

January 20, 2011

Abstract

The Intergovernmental Panel on Climate Change (IPCC, 2007) concluded that anthropogenic CO2 emissions probably
caused more than half of the “global warming” of the past 50 years and would cause further rapid warming. However,
global mean surface temperature TS has not risen since 1998 and may have fallen since late 2001. The present analysis
suggests that the failure of the IPCC’s models to predict this and many other climatic phenomena arises from defects in its
evaluation of the three factors whose product is climate sensitivity:

1) Radiative forcing ΔF;
2) The no-feedbacks climate sensitivity parameter κ; and
3) The feedback multiplier f.
Some reasons why the IPCC’s estimates may be excessive and unsafe are explained. More importantly, the conclusion is
that, perhaps, there is no “climate crisis”, and that currently-fashionable efforts by governments to reduce anthropogenic
CO2 emissions are pointless, may be ill-conceived, and could even be harmful.

The context

LOBALLY-AVERAGED land and sea surface absolute temperature TS has not risen since 1998 (Hadley Center; US National Climatic Data Center; University of Alabama at Huntsville; etc.). For almost seven years, TS may even have fallen (Figure 1). There may be no new peak until 2015 (Keenlyside et al., 2008).

The models heavily relied upon by the Intergovernmental Panel on Climate Change (IPCC) had not projected this multidecadal stasis in “global warming”; nor (until trained ex post facto) the fall in TS from 1940-1975; nor 50 years’ cooling in Antarctica (Doran et al., 2002) and the Arctic (Soon, 2005); nor the absence of ocean warming since 2003 (Lyman et al., 2006; Gouretski & Koltermann, 2007); nor the onset, duration, or intensity of the Madden-Julian intraseasonal oscillation, the Quasi-Biennial Oscillation in the tropical stratosphere, El Nino/La Nina oscillations, the Atlantic Multidecadal Oscillation, or the Pacific Decadal Oscillation that has recently transited from its warming to its cooling phase (oceanic oscillations which, on their own, may account for all of the observed warmings and coolings over the past half-century: Tsonis et al., 2007); nor the magnitude nor duration of multicentury events such as the Medieval Warm Period or the Little Ice Age; nor the cessation since 2000 of the previously-observed growth in atmospheric methane concentration (IPCC, 2007); nor the active 2004 hurricane season; nor the inactive subsequent seasons; nor the UK flooding of 2007 (the Met Office had forecast a summer of prolonged droughts only six weeks previously); nor the solar Grand Maximum of the past 70 years, during which the Sun was more active, for longer, than at almost any
similar period in the past 11,400 years (Hathaway, 2004; Solanki et al., 2005); nor the consequent surface “global warming” on Mars, Jupiter, Neptune’s largest moon, and even distant Pluto; nor the eerily- continuing 2006 solar minimum; nor the consequent, precipitate decline of ~0.8 °C in TS from January 2007 to May 2008 that has canceled out almost all of the observed warming of the 20th century.

Figure 1
Mean global surface temperature anomalies (°C), 2001-2008


An early projection of the trend in TS in response to “global warming” was that of Hansen (1988), amplifying Hansen (1984) on quantification of climate sensitivity. In 1988, Hansen showed Congress a graph projecting rapid increases in TS to 2020 through “global warming” (Fig. 2):

Figure 2
Global temperature projections and outturns, 1988-2020


To what extent, then, has humankind warmed the world, and how much warmer will the world become if the current rate of increase in anthropogenic CO2 emissions continues? Estimating “climate sensitivity” – the magnitude of the change in TS after doubling CO2 concentration from the pre-industrial 278 parts per million to ~550 ppm – is the central question in the scientific debate about the climate. The official answer is given in IPCC (2007):

“It is very likely that anthropogenic greenhouse gas increases caused most of the observed increase in [TS] since the mid-20th century. … The equilibrium global average warming expected if carbon dioxide concentrations were to be sustained at 550 ppm is likely to be in the range 2-4.5 °C above pre-industrial values, with a best estimate of about 3 °C.”

Here as elsewhere the IPCC assigns a 90% confidence interval to “very likely”, rather than the customary 95% (two standard deviations). There is no good statistical basis for any such quantification, for the object to which it is applied is, in the formal sense, chaotic. The climate is “a complex, nonlinear, chaotic object” that defies long-run prediction of its future states (IPCC, 2001), unless the initial state of its millions of variables is known to a precision that is in practice unattainable, as Lorenz (1963; and see Giorgi, 2005) concluded in the celebrated paper that founded chaos theory –
“Prediction of the sufficiently distant future is impossible by any method, unless the present conditions are known exactly. In view of the inevitable inaccuracy and incompleteness of weather observations, precise, very-long-range weather forecasting would seem to be nonexistent.”  The Summary for Policymakers in IPCC (2007) says –“The CO2 radiative forcing increased by 20% in the last 10 years (1995-2005).”

Natural or anthropogenic CO2 in the atmosphere induces a “radiative forcing” ΔF, defined by IPCC (2001: ch.6.1) as a change in net (down minus up) radiant-energy flux at the tropopause in response to a perturbation. Aggregate forcing is natural (pre-1750) plus anthropogenic-era (post-1750) forcing. At 1990, aggregate forcing from CO2 concentration was ~27 W m–2 (Kiehl & Trenberth, 1997). From 1995-2005, CO2 concentration rose 5%, from 360 to 378 W m–2, with a consequent increase in aggregate forcing (from Eqn. 3 below) of ~0.26 W m–2, or <1%. That is one-twentieth of the value
stated by the IPCC. The absence of any definition of “radiative forcing” in the 2007 Summary led many to believe that the aggregate (as opposed to anthropogenic) effect of CO2 on TS had increased by 20% in 10 years. The IPCC – despite requests for correction – retained this confusing statement in its report.  Such solecisms throughout the IPCC’s assessment reports (including the insertion, after the scientists had completed their final draft, of a table in which four decimal points had been right-shifted so as to multiply tenfold the observed contribution of ice-sheets and glaciers to sea-level rise), combined with a heavy reliance upon computer models unskilled even in short-term projection, with initial values of key
variables unmeasurable and unknown, with advancement of multiple, untestable, non-Popperfalsifiable theories, with a quantitative assignment of unduly high statistical confidence levels to nonquantitative statements that are ineluctably subject to very large uncertainties, and, above all, with the now-prolonged failure of TS to rise as predicted (Figures 1, 2), raise questions about the reliability and hence policy-relevance of the IPCC’s central projections.

Dr. Rajendra Pachauri, chairman of the UN Intergovernmental Panel on Climate Change (IPCC), has recently said that the IPCC’s evaluation of climate sensitivity must now be revisited. This paper is a respectful contribution to that re-examination.

The IPCC’s method of evaluating climate sensitivity

We begin with an outline of the IPCC’s method of evaluating climate sensitivity. For clarity we will concentrate on central estimates. The IPCC defines climate sensitivity as equilibrium temperature change ΔTλ in response to all anthropogenic-era radiative forcings and consequent “temperature feedbacks” – further changes in TS that occur because TS has already changed in response to a forcing – arising in response to the doubling of pre-industrial CO2 concentration (expected later this century).  ΔTλ is, at its simplest, the product of three factors: the sum ΔF2x of all anthropogenic-era radiative forcings at CO2 doubling; the base or “no-feedbacks” climate sensitivity parameter κ; and the feedback
multiplier f, such that the final or “with-feedbacks” climate sensitivity parameter λ = κ f. Thus –

ΔTλ = ΔF2x κ f = ΔF2x λ, (1)
where f = (1 – bκ)–1, (2)

such that b is the sum of all climate-relevant temperature feedbacks. The definition of f in Eqn. (2) will be explained later. We now describe seriatim each of the three factors in ΔTλ: namely, ΔF2x, κ, and f.

1. Radiative forcing ΔFCO2, where (C/C0) is a proportionate increase in CO2 concentration, is given by several formulae in IPCC (2001, 2007). The simplest, following Myrhe (1998), is Eqn. (3) –

ΔFCO2 ≈ 5.35 ln(C/C0) ==> ΔF2xCO2 ≈ 5.35 ln 2 ≈ 3.708 W m–2. (3)

To ΔF2xCO2 is added the slightly net-negative sum of all other anthropogenic-era radiative forcings, calculated from IPCC values (Table 1), to obtain total anthropogenic-era radiative forcing ΔF2x at CO2 doubling (Eqn. 3). Note that forcings occurring in the anthropogenic era may not be anthropogenic.

Table 1
Evaluation of ΔF2x from the IPCC’s anthropogenic-era forcings


From the anthropogenic-era forcings summarized in Table 1, we obtain the first of the three factors –
ΔF2x ≈ 3.405 Wm–2. (4)

Continue to Part 2

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