The listener.
Speaker:Welcome again, this is the iron fist and the velvet glove podcast up to episode
Speaker:311, something a bit different for you this time, instead of the normal panel
Speaker:discussion I decided to, it was time to do a little talk on climate change, a
Speaker:bit of a one-on-one on climate change.
Speaker:So I don't have a normal panel, but Joe the tech guy was sitting at his
Speaker:computer twiddling his thumbs anyways.
Speaker:So he's joining in and say Joe is there he'll chip in as necessary.
Speaker:Thank you, Joe.
Speaker:And, and I'll do a bit of us solo spiel or with Joe's help and try and explain to
Speaker:you my understanding of climate change.
Speaker:And basically give you a bit of a 1 0 1 of what it's about and the typical
Speaker:arguments and the basic stuff that you need to understand about climate change.
Speaker:When you are sitting at a dinner party and somebody starts mouthing off as a climate
Speaker:change denier, and you want to have a few facts and figures and some argue.
Speaker:Ready for you.
Speaker:So, so that's what tonight is about it's climate change and some of the
Speaker:ins and outs, and I'm no, I'm no expert by any means, but I'll do my best
Speaker:to give you a bit of a run through.
Speaker:I mean, the important bits, if you're in the chat room, say hello and
Speaker:already, we've got what lead the wizard.
Speaker:Good.
Speaker:I Whatley good to see you there.
Speaker:So so yeah, climate change.
Speaker:So, okay.
Speaker:When thinking about, well, actually, you know, we really should apologize
Speaker:because we've reached 311 episodes of this podcast and really haven't
Speaker:discussed climate change until now.
Speaker:So it is one of the major, you know, Things that we should have spoken about.
Speaker:And it's quite an oversight to have not have spent some time on it.
Speaker:So apologies for that more makeup for a little bit tonight.
Speaker:And I think we need some safeness chaplains to help console us with the
Speaker:existential dread of climate change.
Speaker:That's it.
Speaker:And for some forgiveness, I need to go to confession and flagellate
Speaker:myself, something like that.
Speaker:So, so anyway and we'll definitely do a bit more on climate change
Speaker:than we have in the past.
Speaker:So once we've got this one under our belt, hello, to Daniel,
Speaker:he's in the chat room as well.
Speaker:So look, climate change.
Speaker:Okay.
Speaker:Let's face it.
Speaker:There are climate change deniers out there, and there's a lot of them and,
Speaker:and they seem to fall into the same sorts of people who would be anti-vaxxers
Speaker:and who would say lockdowns don't work.
Speaker:And who would say that five G is either dangerous or it's
Speaker:a plot to control our minds.
Speaker:People who are into conspiracies are into this sort of thing and, and sort of
Speaker:denying that climate change is manmade and is a problem, or, or at least made
Speaker:my is certainly a common thing out there.
Speaker:I'll tell you what though with the anti-vaxxers they
Speaker:are becoming same minds train.
Speaker:Like when I tune in and watch the premiers with their daily talks
Speaker:about the lightest COVID numbers.
Speaker:If you do that, ah, if you watch that on a Brisbane times, Facebook
Speaker:feed or heaven forbid a sky news, Facebook feed the comments section
Speaker:there by the anti-vaxxers it's insane.
Speaker:The level of people who are denying vaccinations and climbing
Speaker:all sorts of things about them.
Speaker:So they're not a fringe group anymore.
Speaker:They like becoming mainstream.
Speaker:But anyway, I digress.
Speaker:We're talking about climate change in this episode.
Speaker:So.
Speaker:One of the things with, with climate change vaccinations lockdowns, et cetera,
Speaker:is people feel that they can do their own research and figure it out for themselves.
Speaker:And as part of all this, I came across a website skeptical science.
Speaker:And it had a good little section about doing your own research, which I think is
Speaker:worth mentioning at the beginning here, before we get too far down the track.
Speaker:So the phrase do your own research seems ubiquitous these days often
Speaker:by those who don't accept mainstream science or news, conspiracy theories,
Speaker:and many who fashioned themselves as independent thinkers and on its face.
Speaker:It seems legit what could be wrong with wanting to seek out
Speaker:information and make up your own mind?
Speaker:And does this webs, excuse me, is this websites is the problem is.
Speaker:With doing your own research that's not what research is like.
Speaker:When scientists use the word research, they mean a systematic
Speaker:process of investigation.
Speaker:Evidence is collided evaluated in an unbiased objective manner.
Speaker:And those methods have to be available to other scientists
Speaker:for replication these days.
Speaker:When people say that they're doing their own research, I mean, they using a search
Speaker:engine to find information that conform confirms what they already think is true.
Speaker:So bear that in mind.
Speaker:Next time you hear somebody say, do your own research Googling away
Speaker:in your own bubble is not research.
Speaker:So science is a process.
Speaker:It's an attempt to understand reality and recognize how biased
Speaker:and flawed the human brain is.
Speaker:So real research is about trying to prove yourself wrong.
Speaker:Yeah, right.
Speaker:So the other thing, of course, in all of that is.
Speaker:You're not as smart as you think you are, unless you're an expert
Speaker:in a field you're researching.
Speaker:You're almost certainly not able to fully understand the nuance
Speaker:and complexity of the topic.
Speaker:So experts have advanced degrees.
Speaker:They've published research, they've got years of experience.
Speaker:They know the body of evidence and the methodologies, and they're
Speaker:aware of what they don't know.
Speaker:So experts can be wrong, but they're much less likely to be wrong than a non-expert.
Speaker:So thinking one can do their research on scientific topics, such as climate
Speaker:change or MRN vaccines is to fool oneself, to some extent, so the information's
Speaker:available, but it doesn't mean you've got the background knowledge to understand it.
Speaker:So you need to know your limit.
Speaker:So ultimately knowledge is a community effort.
Speaker:We don't think alone.
Speaker:And that what makes humans a successful species, we build off
Speaker:what other people are expert in.
Speaker:So that's why for anyone who isn't an expert in a particular field,
Speaker:our best chance at knowledge is to trust what the majority of
Speaker:experts in that area say is true.
Speaker:And then no research is involved.
Speaker:So unless you're an expert, there's a good argument for trusting what the majority
Speaker:of experts in an area say is true.
Speaker:If there's a clear and strong consensus, so in my little talk, the seeds evening,
Speaker:I'm not about to try and paint for you.
Speaker:The opposite picture of, of, of the of the mainstream view.
Speaker:I'm just going to give you the mainstream view.
Speaker:You want to find the try and waste your time on the opposite view.
Speaker:Go ahead.
Speaker:So really What is the consensus when it comes to climate change, what
Speaker:do our scientists, and again, from this sign website, skeptical science
Speaker:and I give a good explanation.
Speaker:When I say science achieves a consensus when scientists stop arguing.
Speaker:So initially when the question was asked, what would happen if we put a lot of
Speaker:carbon dykes dioxide in the atmosphere, there may have been many hypotheses about
Speaker:what's going to happen, but over a period of time, the ideas are tested and retested
Speaker:in the process of the scientific method.
Speaker:Because all scientists know that a big part.
Speaker:And so over a period of time, HIV is tested and retested.
Speaker:That's the processes of the scientific method and scientists trying to get
Speaker:it right and try to get it right because they get a reputation.
Speaker:So the ones that don't pan out will fall by the wayside, the ones that work out and
Speaker:make sense survive amongst the hypothesis.
Speaker:And so there's no consensus in science is different from a political one.
Speaker:There's no vote scientists just give up arguing because the sheer white of
Speaker:consistent evidence is too compelling.
Speaker:And that's what we've reached when it comes to climate and the consensus that
Speaker:our plant, our, our planet is warming and that warming is caused by humans.
Speaker:So there's a link here in the shiny Knights, which is They will
Speaker:authors of seven climate consensus studies and the knives rule.
Speaker:They and they each had done their own studies about what is the
Speaker:consensus amongst scientists.
Speaker:And they came out with a hundred percent.
Speaker:Three of them came out with naughty 7%, actually four of
Speaker:them said 97% once it 93%.
Speaker:And the other one said 91% individually, they came up with that as the, as
Speaker:the consensus view on climate change.
Speaker:And they then write a joint Piper.
Speaker:And the conclusions were that somewhere between 90 and a hundred percent of
Speaker:experts agree that humans are responsible for climate change with most of
Speaker:the studies finding 97% consensus.
Speaker:Interesting to note that when science is unsettled, the argument takes
Speaker:place in scientific forums, right?
Speaker:When, when one side has lost, it moves to the mainstream media because they've
Speaker:failed to convince their colleagues.
Speaker:The only people they convince are the lay people who have no knowledge.
Speaker:And so if the conversation is happening in the press or on social
Speaker:media, it means that the scientists already know what the answer is.
Speaker:And this person hasn't managed to convince his colleagues, his peers.
Speaker:That's true.
Speaker:That's, that's a good way of looking at it.
Speaker:So I've got on the screen, the listener, if you're listening to this podcast
Speaker:the audio version of this, and you sometimes watch the video version.
Speaker:This might be an episode where it's worth watching the video version, because there
Speaker:will be a few charts and graphs to put up.
Speaker:So One of the other things that they said in their joint report was that
Speaker:the greater, the climate expertise among those surveyed the higher, the
Speaker:consensus on human caused global warming.
Speaker:So there's a chart there that basically shows that the more expert
Speaker:people were amongst the experts than the more likely they were to agree
Speaker:on a human caused global warming.
Speaker:So that's, you know, realistically, when you look at COVID and the, and the
Speaker:disputes we've got amongst experts as to all sorts of things to do with COVID.
Speaker:If we look at these figures of 97%, that's a pretty high and strong
Speaker:figure in the scheme of things.
Speaker:And we've really reached the point in life haven't made, where it's
Speaker:almost impossible to expect a hundred percent agreement on things.
Speaker:97% is pretty strong consensus.
Speaker:So so, so yeah so basically my first argument was do your own
Speaker:research is really limited.
Speaker:If you're not an expert, you can fall for some pretty big traps.
Speaker:And for most people relying on a strong consensus of experts is
Speaker:the most sensible thing to do.
Speaker:And the strong consensus of experts is that we've got human
Speaker:caused global warming going on.
Speaker:So we'll get into what, you know, the, the reasons and the arguments
Speaker:and the facts and all the rest of it.
Speaker:But that's a good starting point as to As to kicking off this discussion.
Speaker:So, right.
Speaker:By the way so those who are opposed to taking action to curb climate change,
Speaker:having guised in a misinformation campaign to deny the existence of
Speaker:the expert consensus and they've been successful and the public badly
Speaker:underestimates the expert consensus.
Speaker:So apparently only 16% of Americans realize that the consensus is above 90%.
Speaker:So there we go.
Speaker:All right.
Speaker:So with all that changing what's that Joe that's changing limited
Speaker:news is changing their teen limited news is changing their chain.
Speaker:Yeah.
Speaker:The Murdoch press now, now going to spruik human induced climate change.
Speaker:Yes.
Speaker:Why are they doing that?
Speaker:I'm not fully across that story, but that's only come out in the
Speaker:last time or two as an, a jug.
Speaker:It has.
Speaker:Yay.
Speaker:Is it because of some government inquiry about them or something like that,
Speaker:they feel they're under threat in some way, or is it because there's a change?
Speaker:There's a handover from the old guard new guard.
Speaker:Ah, okay.
Speaker:So yeah, they've came out with some statement have in mind that sort of made
Speaker:that clear, which is a strength, strange thing to have to do carbon zero for 2050.
Speaker:I think there's supposed to be salty.
Speaker:Okay.
Speaker:Well with the Murdoch press on board, who knows what's possible, but at the moment
Speaker:only 16% of Americans realize that the consensus amongst experts is above 90%.
Speaker:Right.
Speaker:So I'm no expert.
Speaker:Of course you've gathered that.
Speaker:And I'm not going to try and prove climate change is wrong.
Speaker:I'm not going to waste my time on that.
Speaker:I'll just give my understanding of the consensus view and
Speaker:the reasoning behind it.
Speaker:And and really, I'm just sort of looking at, you know, if you're at a dinner
Speaker:party, people still have those things and the somebody mapping off phase a
Speaker:climate skeptic, you'll have a few bits of arguments and information up your
Speaker:sleeve that you can, that you can use.
Speaker:So, so, right.
Speaker:So one of the things that kicked me off is and I've got some information, I'll
Speaker:be drawing on two sources for a while.
Speaker:I'll be talking about in this episode.
Speaker:One is a book called climate change.
Speaker:What everyone needs to know second edition by Joseph Romm and book.
Speaker:His credentials are pretty good and it's on the back of his book where he's being
Speaker:involved in a lot of Stuff to do with climate change science and finishes off.
Speaker:He's a senior fellow at the center for American progress, and he
Speaker:holds a PhD in physics from MIT.
Speaker:Like he's a smart guy and seems knowledgeable on the topic.
Speaker:And a lot of his stuff is referenced.
Speaker:The other thing that I'll be drawing on of coolest is the IPC reports.
Speaker:So this is the intergovernmental panel on climate change, who just
Speaker:came out with, they had 20, 21 report.
Speaker:So that's really the sort of two sources that are, I'm going to be relying on.
Speaker:And oh, who we got in the chat room.
Speaker:What Lee, the wizard Harry and financial solvent.
Speaker:That's a quite nice I'll let you read all that stuff, Joe, I'll get too distracted.
Speaker:If I get into that singing out.
Speaker:If this stuff does that I should know about, okay.
Speaker:Please help Joe.
Speaker:Okay.
Speaker:Here's one of the things right from the get go that I didn't
Speaker:understand about climate change and this whole idea of a blanket.
Speaker:And I can remember Dr.
Speaker:Carl talking on a podcast and it was about how energy would bounce
Speaker:off the earth surface and would hit this sort of greenhouse gases and
Speaker:then bounce back to earth and warm us up more than we were before.
Speaker:And at the time I was thought to myself, well, if we've built up only
Speaker:these particles in the atmosphere that are blocking the heat from leaving the
Speaker:earth, surely those same particles would have blocked the heat arriving on the
Speaker:earth at the same time from the sun.
Speaker:So wouldn't may have been reflected.
Speaker:Y from us as much as reflecting hate back into us is what
Speaker:all of us sort of thinking.
Speaker:I just couldn't get my head around it.
Speaker:And I was talking to Joe in the chat room, Joe, what did he say beforehand?
Speaker:Jane?
Speaker:What were you saying about, yeah.
Speaker:If you go into a greenhouse or possibly a better example that we've all had
Speaker:is if you go and sit in the car, even on an overcast day you know, how much
Speaker:hotter it gets inside than outside.
Speaker:Yes.
Speaker:And you can feel the sun's energy heating up the car.
Speaker:Yes.
Speaker:And not escaping.
Speaker:Yeah.
Speaker:So the heat manages to come through the glass of the windscreen or the
Speaker:greenhouse inside, and then doesn't bounce out in the same level.
Speaker:Sam is trapped within.
Speaker:And so how does that work in terms of the greenhouse gases?
Speaker:So.
Speaker:The sun's Pake intensity is visible light of the solar energy
Speaker:hitting the top of the atmosphere.
Speaker:One third is reflected back into space by the atmosphere itself and
Speaker:by the Earth's surface, they lay in the ocean and it seems especially the
Speaker:ice being white and highly reflect.
Speaker:So visible light coming from the sun.
Speaker:One third of it bounces back into spice as the rough calculation.
Speaker:So the, as an aside, the amount of energy is equivalent to four Hiroshima,
Speaker:atomic bomb destinations per second, or 7.4 quadrillion kittens sneezes per se.
Speaker:You could too much, Tom and Haynes, Joe, as an aside.
Speaker:That's good.
Speaker:Okay.
Speaker:So one third bounces back.
Speaker:The wrist is absorbed mostly by the by the earth, especially our oceans
Speaker:and this price is hates up the planet, but the earth rewrites the energy,
Speaker:it has absorbed mostly as hate in the form of infrared radiation.
Speaker:So it rewrites the EITs, this infrared radiation outwards say some naturally
Speaker:occurring atmospheric gases, let the visible light Skype through to interspace
Speaker:while trapping certain types of infrared radiation, these greenhouse gases,
Speaker:including water methane and carbon dioxide trap, some of the rewriting highlighted.
Speaker:So they act as a partial blanket that keeps the planet as much
Speaker:as 60 degrees Fahrenheit warmer than it otherwise would be.
Speaker:Which of course is normally ideal for us.
Speaker:So visible light comes in, one-third bounces off two-thirds gets absorbed
Speaker:the earth, rewrite the EITs infrared radiation that hits the greenhouse
Speaker:gases, the gases, which allow the visible law to transfer through.
Speaker:Don't allow this infrared to transfer through as easily and
Speaker:then bounce it back to earth.
Speaker:That's how it works.
Speaker:So climate science predicts.
Speaker:So if you accept that theory the prediction is that if the warming is
Speaker:caused by an increase in greenhouse gases, we expect the lower atmosphere,
Speaker:the troposphere to warm up the upper atmosphere, the stratosphere
Speaker:to cool, and the boundary between them, the troppo pause to rise.
Speaker:And all of that has been observed.
Speaker:So for instance, recent warmings would you to increases in the intensity of
Speaker:radiation from the sun then in addition to the troposphere stratosphere should
Speaker:be warming too, which is not happening.
Speaker:So for people who are climate change deniers, you have to at your dinner
Speaker:party, talk to them about the, the lower atmosphere, the upper atmosphere and the
Speaker:middle atmosphere and say, well, whatever alternative theory you may have, if you
Speaker:simply say all the sun must be stronger at the moment that's, what's causing the
Speaker:planet to heat up, then you would say, well, can you explain to me why the upper
Speaker:atmosphere is actually cooler and cooler?
Speaker:If if what you're saying is true, that doesn't make sense.
Speaker:So the the sort of theory of this climate science neatly explains what's
Speaker:actually happening in these atmospheres.
Speaker:So I thought that was interesting, Joe, given your knowledge of cat sneezing
Speaker:and Hiroshima bomb, do you probably all buried it or you are rare of those
Speaker:levels in the atmosphere already?
Speaker:Where are you?
Speaker:I haven't yet.
Speaker:There is a really good U Q online course which goes into the science of
Speaker:climate change and how we know this.
Speaker:And that was one of the things it discussed.
Speaker:Along with carbon 14 isotopes or carbon isotopes.
Speaker:I don't know if you're touching on that.
Speaker:Th as a fossil carbon, rather than the forestation.
Speaker:Yes.
Speaker:I'll get to that.
Speaker:Okay.
Speaker:Alrighty.
Speaker:So satellites measure less heat escaping out to space at the particle
Speaker:wavelengths that carbon dioxide absorbs heat, thus finding direct experimental
Speaker:evidence for a significant increase in the Earth's greenhouse effect.
Speaker:So if less heat is escaping the space, where is it going?
Speaker:Well, it's going back to the earth surface and surface measurements, confirm
Speaker:this observing more downward infrared radiation, a closer look at the damage
Speaker:at radiation Fonz, more heat returning at carbon dioxide wavelengths leading
Speaker:to the conclusion that this experimental data should effectively in the argument
Speaker:by skeptics that no experimental evidence exists for the connection
Speaker:between greenhouse gas increases in the atmosphere and global warming.
Speaker:So again, If somebody wants to deny climate change, you need to say, well,
Speaker:here's what the evidence is explained to me how our hotter son be the
Speaker:explanation, given those challenges in those different atmospheres, right?
Speaker:A couple of other bits of information, carbon levels.
Speaker:So stuff with climate science is done, particularly with temperatures and things.
Speaker:It's kind of a comparison to our pre-industrial is so they
Speaker:look back 250 years quite often.
Speaker:So at the Dawn of the industrial revolution, industrial revolution,
Speaker:250 years ago, the carbon dioxide in the atmosphere was
Speaker:approximately 280 parts per mil.
Speaker:And it now exceeds 400 and That can specifically measure the type of carbon
Speaker:that's building up in the atmosphere.
Speaker:And I know it comes from the combustion of fossil fuels as opposed to other
Speaker:sources such as deforestation.
Speaker:And so so that's quite compelling as well that this increase in carbon
Speaker:dioxide is from fossil fuels and where the reason fossil fuel carbon
Speaker:is being released in the atmosphere.
Speaker:It's pretty clear.
Speaker:So so we've got us as the cause of the carbon entering the atmosphere and
Speaker:we've got this evidence of, of what's happening with temperatures in the
Speaker:atmosphere and we'll get onto evidence of temperatures happening on earth.
Speaker:Now, before all that, though a skeptic might side.
Speaker:Well, there might be other reasons why the planet is warming.
Speaker:That might not be the only reason it might explain some of it, but
Speaker:there could be other factors involved that are causing the warming.
Speaker:And so but according to the science, the other factors that might affect
Speaker:global temperature at this particular stage in the cycles should actually be
Speaker:cooling the earth rather than hating it.
Speaker:So one of those would be sun activity.
Speaker:So the sun doesn't stay at a constant energy level.
Speaker:It it goes up and down in the sort of approximately 11 years cycles.
Speaker:But in recent years we've actually seen the deepest soul,
Speaker:a minimum in nearly a century.
Speaker:According to NASA, as I explained in 2009.
Speaker:So we've had unusually low levels of solar activity that would
Speaker:otherwise be cooling the earth.
Speaker:So so I will bring up a chart on for those were able to see it.
Speaker:And what you've got is a temperature 11 year average is the
Speaker:red line going up dramatically.
Speaker:And you've got solar energy, essentially the blue line down the bottom, which
Speaker:in the last since the 1960s leveled off and around 2000 actually decreased.
Speaker:So it's not possible to blame increased solar energy as the cause of our global
Speaker:warming scientists have measured it.
Speaker:And that's not what it is.
Speaker:What's some other reasons John has, when I talk solo, my voice
Speaker:actually dries out quicker.
Speaker:I've got a tank more water than went on with the other guys.
Speaker:You need some Robina?
Speaker:I do.
Speaker:Okay.
Speaker:One other reason volcanic activity is, is sometimes a cause, but in recent decades
Speaker:volcanic activity has released particles had partially blocked the sun and also
Speaker:serve to cool the planet slightly.
Speaker:So the voltage canning activity would not have contributed to the
Speaker:warming and the other possible influence last but not least is.
Speaker:Is the orbit of the earth around the sun and the why that the planet
Speaker:wobbles around its axis as well.
Speaker:During that orbit.
Speaker:So the orbit changes gets closer and further away from the sun and then
Speaker:the upline that sort of bubbles in different lies as it goes around as well.
Speaker:And there's a bit of a correlation between the, the orbit of the
Speaker:earth and ice ages over time.
Speaker:It's not the only cause of ice ages.
Speaker:There are other factors, particularly carbon buildups as well, but it is, it
Speaker:certainly has, seems to have perfect now.
Speaker:According to ice cores from Antarctica over the past 400,000 years it's
Speaker:being dominated, dominated buying glycine heels, so called periods,
Speaker:ice ages that Moneta normally last about a hundred thousand years.
Speaker:And it's been punctuated by, into glacial short, warm periods, which
Speaker:typically last about 11,500 years.
Speaker:So, so normally ice age of a hundred thousand years, and a nice warm
Speaker:period of about 11,500 years and, and our current nice warm period.
Speaker:Now current into glycine will hold the Hallows scene.
Speaker:It's already been going 12,000 years.
Speaker:So some people might say, well, if a new eyesight is imminent Mike, it's
Speaker:gotten to be warming the planet.
Speaker:And so let me just see here.
Speaker:Let me just see.
Speaker:So what are the conditions like?
Speaker:So at the moment the earth should be cooling slightly, but the current
Speaker:factors of orbit and tilt very weak and they're not acting within
Speaker:the same timescale and they're out of phase by about 10,000 years.
Speaker:So their combined effect would probably be too weak to trigger an ice age.
Speaker:So we've got quite an unusual combination of orbit and tilt at the moment.
Speaker:That would mean we're not normally was slightly cooling or we should be slightly
Speaker:cooling, but not entering an ice age and a similar sort of combination of orbit
Speaker:and tilt happened 430,000 years ago.
Speaker:That had a nice warm period lasting 30,000 years.
Speaker:So we're in that sort of range at the moment.
Speaker:So according to the orbit and tilt of the earth really we should be slightly
Speaker:cooling, but really not very much.
Speaker:And we should be really enjoying a a nice interglacial period of a 30,000
Speaker:years rather than the normal 11,500.
Speaker:So without him and interference, because of the orbit and tilt
Speaker:there should be a slight cooling.
Speaker:So essentially the sorts of things when people say, well, we don't know whether
Speaker:the warming is caused by humans or whether it's caused by other factors.
Speaker:When you look at the other factors, sun activity, volcanic action,
Speaker:and the orbit tilt of the earth.
Speaker:All those factors are actually pointing to a cooling rather than a heating.
Speaker:So yeah.
Speaker:You're anything to Joe to add to that that you're aware of in terms of factors?
Speaker:No.
Speaker:Are you going to cover off the amount of human released
Speaker:carbon E compared to natural?
Speaker:I don't know if I am, I have to get through my night.
Speaker:CJ, let me see.
Speaker:Let's see what happens is I go through them and see if it
Speaker:covers what you're talking about.
Speaker:Actually, maybe this next chart we'll, we'll do it.
Speaker:I think.
Speaker:Excellent.
Speaker:So let's look at amplifying effects.
Speaker:So I'm gonna to bring up a chart here.
Speaker:Let me just share that on the screen.
Speaker:And this is a temperature for the past.
Speaker:420,000 years.
Speaker:And it's basically showing peaks and troughs as temperature rises and
Speaker:falls for the last 450,000 years.
Speaker:Isn't it amazing that scientists can actually gather this DOD?
Speaker:It's quite incredible to think about in what you notice is that when the
Speaker:earth warms up, when temperatures increase, it really increases very
Speaker:quickly and quite dramatically like the really sharp, almost vertical
Speaker:line that just climbs up, hits a peak.
Speaker:And then the S the cooling is a much more gradual step ladder, a step down
Speaker:approach over a longer period of time.
Speaker:So, so over the last 450,000 years, as you look at the fluctuations in
Speaker:temperature, basically there are these really, really sharp, quick
Speaker:sparks of an increasing temperatures.
Speaker:And then a more gradual drop-off down to get to the lower temperature
Speaker:and then another big spike.
Speaker:So that also matches up with CO2 concentrations as measured at the
Speaker:time, as well as quite a strong correlation between carbon dioxide
Speaker:and temperatures, which is on the next chart that I've put up as well.
Speaker:But just going back to that first one, where you look at how quickly
Speaker:the temperatures rise and what that tends to indicate is that events happen
Speaker:really quickly when there's initial warming, that there is an amplification
Speaker:effect is possible with things, get a really quick raw lawn on accelerate.
Speaker:For some reason, there are other, there are factors that must come into
Speaker:apply that accelerate the warming the dimes sort of come into play sometimes.
Speaker:To accelerate the, the, the cooling, if you like.
Speaker:So let's get that all sake and look at me.
Speaker:So data reveals over time, last 450,000 years, that when an initial
Speaker:warming is triggered by an external force, such as orbital change,
Speaker:the planet can warm up fast.
Speaker:Then in turn implies that the climate system has strong amplifying feedbacks,
Speaker:which turn a small initial warming into a large hating fairly quickly.
Speaker:So what are these possible amplifying feedbacks?
Speaker:And this comes from the book I mentioned before climate change.
Speaker:Everyone needs to know by Joseph, Ron, and he said, One of the big ones is,
Speaker:has sea ice and land-based ice shrink.
Speaker:This causes a decrease in the Earth's overall reflectivity, which
Speaker:leads to more absorption of heat, especially in the polar agents.
Speaker:So that makes sense.
Speaker:Start to lose that ice.
Speaker:Get less reflection off the ice, more absorption.
Speaker:Another key rapidly acting amplifying feedback is driven by water vapor.
Speaker:As the planet starts to heat up evaporation increases, which puts
Speaker:more water vapor into the air.
Speaker:And guess what, what a Viper is a potent heat-trapping greenhouse gas.
Speaker:My carbon dioxide.
Speaker:Basic physics tells us that a warmer atmosphere is able to hold more
Speaker:moisture at a right of approximately 7% increase per degree Celsius.
Speaker:So we'll get into some figures lighter.
Speaker:Since the industrialized, the temperature has risen by about a degree.
Speaker:That means that our atmosphere is holding about 7% more moisture.
Speaker:As a result, another sort of amplifying feedback is clump.
Speaker:Tines leads to more forest fires and you get carbon dioxide
Speaker:released by burning trees.
Speaker:And a fourth one that he likes to emphasize in this book is the thawing
Speaker:of permafrost can also release additional carbon dioxide and methane.
Speaker:Say Meetha mine is an interesting one compared to carbon dioxide.
Speaker:As a heat-trapping capacity, it's 34 times stronger than carbon
Speaker:dioxide over a 100 year time scale.
Speaker:It's actually, it seems like it disappears from the atmosphere a lot quicker.
Speaker:Over 20 year timeframe, methane is 86 times stronger.
Speaker:A large part of the difference is that the atmospheric lifetime of
Speaker:methane is approximately 12 years.
Speaker:It was carbon dioxide.
Speaker:It's a lot longer, but they're much stronger in terms of trapping eight.
Speaker:And so is a big problem that we have to be concerned with.
Speaker:And this guy in this book talks about methane being released from the permafrost
Speaker:and he's a little bit he nights, apparently the IPC report, Joe, they
Speaker:don't really take into account the meth.
Speaker:Being released from the permafrost as an amplifying effect, as much as this guy
Speaker:likes to say, have you heard much about methionine permafrost, anything like that?
Speaker:Yeah, so I think lots of Siberia, they're saying the permafrost is
Speaker:thawing and there's big concerns that a large amount of medium
Speaker:will be released very, very soon.
Speaker:And also I think there are some big holes appearing in parts of Siberia.
Speaker:Mm.
Speaker:I think I read somewhere where the may time was escaping sight quickly
Speaker:that the, the a frost was not freezing either during winter because of
Speaker:just so much movement of methane.
Speaker:And I think also images of, of like a permafrost on fire not so long ago.
Speaker:So there's a lot of methane in the air to be released and it's dangerous
Speaker:in terms of its heat trapping.
Speaker:Okay.
Speaker:Other things to be aware of severe precipitation.
Speaker:So we seemed, it seems anecdotally as we look around that well actually
Speaker:it's a matter of fact, really the worst Deluges of Ryan have jumped,
Speaker:not merely be cool is warmer.
Speaker:Air holds more moisture that in turn gets sucked into my just storm systems.
Speaker:Climate scientists have explained that climate change is altering the jet
Speaker:stream and weather patterns in ways that can cause storms storm systems to slow
Speaker:down or get stuck, thereby giving them more time to dump heavy precipitation.
Speaker:So when it rains, it pools literally.
Speaker:So that's one of the things that scientists are looking at is that this
Speaker:climate change is causing a change in the in the Northern hemisphere in particular
Speaker:because of the jet stream changing, right.
Speaker:And these weather patterns getting stuck and hovering either areas much longer,
Speaker:whereas in the past they would move on.
Speaker:So causing more damage, greater Deluges of Ryan.
Speaker:That's what happened in America a few years back with a polar vortex.
Speaker:And so the weather systems, the jet streams moved and there was a
Speaker:large surge of Arctic care, the move down over central north America.
Speaker:And they had very, very cold temperatures because of that.
Speaker:Yes.
Speaker:So shifting that called air down because of the movement jet stream
Speaker:and the jet stream also changing such that these systems don't move on
Speaker:sometimes like they normally would.
Speaker:An interesting one is snow.
Speaker:So when it's cold enough to snow, snow storms, we field by more water
Speaker:vapor and thus be more intense.
Speaker:So you may have heard of the saying it's too cold to snow.
Speaker:If it's very, very cold, then there is too little water vapor in the
Speaker:air to support a heavy snow fall.
Speaker:So we've known for a long time that warmer than normal winters
Speaker:actually favor snow storms.
Speaker:So oh, it's secure.
Speaker:It's considered a desert because it is so cold that it doesn't snow.
Speaker:There you go.
Speaker:Yeah.
Speaker:So there's very little precipitation though.
Speaker:I called it.
Speaker:Can't hold the moisture.
Speaker:Yeah.
Speaker:So so according to this theory, what we will find is at the beginning
Speaker:and end of winter, it will be slightly warmer and you'll get
Speaker:rain will result instead of snow.
Speaker:However, during the middle of winter, the extra water vapor in the atmosphere
Speaker:that is now called enough to create snow will mean you'll have largest
Speaker:nudge storms will be developing.
Speaker:So.
Speaker:Here's a tip for you, dear listener.
Speaker:If you get nothing else, if you're booking ski holidays over the next
Speaker:century, I'm booked for the middle of the season, not for the shoulder
Speaker:beginnings or in periods and you'll be falling to be the skinning at least.
Speaker:So so where am I up to?
Speaker:That's what we know there.
Speaker:Now I'm going to move on to the so that's a lot of the, sort of
Speaker:the theory of climate science and in what we think happens.
Speaker:And the intergovernmental panel on climate change came out with a report.
Speaker:It was their sixth assessment report in a, provides a high level summary
Speaker:of the understanding of the current state of the climate, including how
Speaker:it is changing and the role of human influence in the state of knowledge
Speaker:about possible climate futures.
Speaker:So a bit of a summary of where we're at.
Speaker:That's what's the IPC report.
Speaker:So.
Speaker:What did it say about the current state of our climate?
Speaker:It said that each of the last four decades has been successfully warmer
Speaker:than any other decade that preceded it since 1850 and global surface temperature
Speaker:was 1.09 degrees higher in 2011 to 2020 than it was in 1850 to 1900.
Speaker:A lot of these comparisons, again with this sort of 1850 to 1900
Speaker:period, this pre-industrial period.
Speaker:So we're about a degree Celsius, a warmer in our global surface temperature.
Speaker:I've a land it's even more.
Speaker:So it's 1.59, as opposed to the ocean, which is 0.8, eight.
Speaker:I'm giving you these figures.
Speaker:There's actually a range.
Speaker:And I'm giving you the, sort of the main, what I'm giving you.
Speaker:Some of these figures.
Speaker:So, and they're saying that they think that basically all of that
Speaker:is to do with human induced causes.
Speaker:Let's see, one, one degree doesn't sound like much does it, but let's
Speaker:putting up another chart, which we'll try and put that into contexts
Speaker:on the screen is another chart.
Speaker:And this goes back 2000 years and basically see the changes in
Speaker:global service Jesus on the left is but yes, that's right, baby Jesus
Speaker:on the lift and 2020 on the far.
Speaker:Right.
Speaker:And you'll see that there's a band of of temperature variations, and.
Speaker:Essentially the temperature changes that we've had right at the end
Speaker:is this crazy, ridiculous spike.
Speaker:That's just come out of Norway in comparison with the trend
Speaker:line to the previous two.
Speaker:Can you turn that into present presentation mode instead?
Speaker:Yeah, I can make it the guy that's the best I can do as it sounds, or
Speaker:even Andrew was asking Ron, okay.
Speaker:Andrew Fullscreen at Trevor and that's the best I can do.
Speaker:I think so.
Speaker:So you can see that the band of global surface temperature changes fairly
Speaker:consistent, actually going down a bit.
Speaker:And then this crazy spike at the end is where we currently are.
Speaker:So one degree is a lot.
Speaker:So.
Speaker:By the way, show notes on the website, iron fist, velvet, glove.com, dyer.com.
Speaker:You'll see a PDF will appear where all this stuff can be accessed.
Speaker:So, so yeah, so that's one degree since 1850.
Speaker:So till now, and most of that is attributed to carbon monoxide,
Speaker:but a fair proportion of that is attributed to methane.
Speaker:On the positive side, we did quite well with sulfur dioxide where we
Speaker:reduced that, and we would have had some cooling as a result.
Speaker:So that's in relation to aerosols and things like that.
Speaker:So we have actually done some things, right.
Speaker:In fact, Joel mentioned we also get changes in ocean currents.
Speaker:Yes.
Speaker:Concern about the there's a global ocean circulation, which takes heat
Speaker:away from the equatorial regions and moves it up towards the polar
Speaker:regions the most well known, obviously being the Gulf stream, right?
Speaker:And with a melting sea ice, you get a desalination or a watering down of the
Speaker:saltiness of the ocean, which interferes with the flow of the water currents.
Speaker:And that will actually make the equator warmer on the poles colder.
Speaker:Okay.
Speaker:But it seems to be that there's an amplifying effect that the Arctic
Speaker:in particular is warming up faster than anywhere else on the planet.
Speaker:It seems.
Speaker:And that's because the ice is melting there and a few other factors.
Speaker:So there's a range of things happening.
Speaker:Isn't there all into applying amongst themselves.
Speaker:There is.
Speaker:And the concern is that any one of these could suddenly tip us over as he
Speaker:showed with the warming, the forcing to tip us over a catastrophic edge.
Speaker:So there's a whole bunch of complicated things that interplay
Speaker:and one could accelerate and cause all sorts of amplifying factors.
Speaker:So didn't read that one about the sea counts, but I hadn't finished
Speaker:the book yet, but I might get, I might find something there.
Speaker:So anyway, carbon dioxide and methane that responsible for a fair bit of
Speaker:the a fair bit of the global warming.
Speaker:And we did quite well in terms of reducing nitrogen oxides and sulfur dioxide.
Speaker:So we've done some good things.
Speaker:Okay.
Speaker:Also just in terms of carbon levels, So in 2019, the atmospheric
Speaker:carbon dioxide concentrations were higher than at any time.
Speaker:In at least 2 million years.
Speaker:We can say that with statistically high confidence and concentrations
Speaker:of methane and into what's that nitrous oxide into that would be
Speaker:nitric oxide, I think into, oh, sorry.
Speaker:Nitrogen dioxide.
Speaker:Would it be, I don't know, a noxious oxide.
Speaker:They were higher than at any time in at least 800,000 years.
Speaker:So CO2.
Speaker:Currently higher than any time in the last 2 million years, hand methane
Speaker:and nitrous oxide higher than at any time, at least the last 800,000 years.
Speaker:So it makes you what, sorry.
Speaker:Giant makes you laugh.
Speaker:Doesn't it?
Speaker:Cause pause for concern.
Speaker:So so one degree may not seem like much, but we're also seeing
Speaker:some big F but we're seeing some already big effects on our planet.
Speaker:So the Arctic sea ice last summer Arctic sea ice area was smaller than at any time.
Speaker:In the past a thousand years, we can say that with medium confidence
Speaker:almost all of the world's glaciers are retreating synchronously, synchronously,
Speaker:synchronously, synchronously complicated.
Speaker:Yes.
Speaker:Since the 1950s, that's unprecedented at UN in at least the last 2000 years.
Speaker:Sea levels.
Speaker:You know, the scene level globally increased by about 20
Speaker:centimeters between 99 0 1 and 2018.
Speaker:And it's currently increasing by 3.7 millimeters per year.
Speaker:That's sort of right of increase is going up.
Speaker:So the main sea level has risen faster since 1900 than either any preceding
Speaker:century in at least the last 3000 years.
Speaker:So that's going up very quickly.
Speaker:Hate extremes have become more frequent and more intense.
Speaker:Well called extremes have become less frequent and less severe.
Speaker:And Ryan extremes, the frequency and intensity of heavy precipitation events
Speaker:has increased in Sonata in fifties.
Speaker:So looking towards the future, according to the IPC report, and
Speaker:they've done some modeling and delis.
Speaker:Now, if you listened last week to what we talking about, the Delta Strine
Speaker:and modeling of hospitalizations and deaths in your mind, you should be
Speaker:saying models, models, because it's a difficult thing, creating models and
Speaker:having any confidence in what they, what they say, but we've got to do it
Speaker:as the, I think we've got isn't it.
Speaker:So what they've done a bit like with the Delta striding, where there
Speaker:were sort of like good, medium and bad sort of scenarios, that's what
Speaker:they've done in this report in terms of our carbon emissions they
Speaker:basically had five different scenarios.
Speaker:Sort of too bad two good and one in between and looking at what
Speaker:might happen to our climate, depending on which of the scenarios.
Speaker:So in terms of these scenarios, the, the best of them assume that we would
Speaker:get to net zero emissions shortly after 2050, and that we would actually enter
Speaker:negative territory slightly in sort of negative over the next 50 years.
Speaker:And actually I should put this one up on the screen.
Speaker:Let me do that.
Speaker:So put that up on the screen.
Speaker:So that's the best I can I explain it and I'll put that on
Speaker:for let's see, you can see that.
Speaker:Okay.
Speaker:That's the best I can do.
Speaker:So if you're looking at the screen the bottom line, Aqua blue net emissions
Speaker:shortly after 2050, and go into negative emissions for the rest of the century.
Speaker:Second best scenario, we're going to zero emissions by about 2075.
Speaker:And they negative after that.
Speaker:The middle scenario, which is the one we'll probably concentrate on
Speaker:a fair bit, is where nothing much changes in terms of our emissions.
Speaker:Till about 2050, where it slowly goes down, but we're still emitting
Speaker:carbon more than we are absorbing it by the end of the century.
Speaker:And then the two worst scenarios, which are probably the way our
Speaker:politics is wrong, operating, becoming even more likely where we
Speaker:increase the carbon that we emit.
Speaker:At different levels.
Speaker:So that's the five different scenarios that the IPC looked at the RPCC looked at.
Speaker:And, and let me just get out of that screen and get that one out of the Y
Speaker:and let's see what they had decided.
Speaker:So, yeah, I remember we've already had a one degree increase in temperature
Speaker:since that 1850 to 1900 period.
Speaker:And let's look at what they say will be that long consequences.
Speaker:Okay.
Speaker:It's up on the screen and at the top of the screen is the best case
Speaker:scenario and the bottom of the screen is the worst case scenario.
Speaker:So In the near term under all of these scenarios, they reckon we're
Speaker:going to look at at least another half a degree Celsius increase.
Speaker:I have the next 20 years in terms of, by the end of the century, 2100,
Speaker:under the best nice scenario, we're still going to look at another sort
Speaker:of half a degree of increase in temperature from what we've already had.
Speaker:And under the worst case scenario, another three and a half degrees.
Speaker:In other words, middle scenario, another degree, 1.7 on average, these
Speaker:are all guesstimates, the statistical ranges, but even on the best estimate,
Speaker:we're looking at by the end of the century, another half a degree.
Speaker:Possibly another and on the worst case, another three and a half degrees.
Speaker:And so that's their estimate of what's likely to happen in terms of temperatures,
Speaker:best case best case was the top one.
Speaker:Yes.
Speaker:Another one, but best case of our worst emissions 4.4, it could be
Speaker:as bad as that was best estimate.
Speaker:The best estimate.
Speaker:Sorry.
Speaker:Yeah.
Speaker:So it's halfway between 5.7, correct?
Speaker:Between 3.3 to 5.7.
Speaker:Yeah.
Speaker:So yeah.
Speaker:That's what the IP cc's saying that we're looking at and you'd have to think based
Speaker:on current policies around the world, we're looking at at least the medium to
Speaker:worst case scenarios, at least another one or two degrees or at least another
Speaker:two to three degrees is on the card.
Speaker:Isn't it?
Speaker:So let me get rid of Put that off there and come back to it.
Speaker:Okay.
Speaker:So so really what are we looking at?
Speaker:It's virtually certain that the land surface will continue to
Speaker:warm more than the ocean surface, likely 1.4 to 1.7 times more.
Speaker:It's virtually certain that the article continue to warm more
Speaker:than global surface temperature.
Speaker:Very likely heavy precipitation events will intensify and become more frequent.
Speaker:And there's a channel shop.
Speaker:It'll be in the nights, basically sighing the sorts of things that are normally
Speaker:10 year events in terms of precipitation will become five-year events and even
Speaker:more intense and 50 year events and others will just become more commonplace.
Speaker:So these major Storm systems, particularly in the Northern hemisphere, it seems
Speaker:J they just, the way there's that with that the way the climate is operating
Speaker:and seems particularly to affecting the Northern hemisphere, just anecdotally
Speaker:in my view, compared to the rest of the Southern hemisphere, what I'm hearing is
Speaker:I'll probably retire back to the UK then.
Speaker:Yeah.
Speaker:You'll probably retire back to them.
Speaker:Yeah.
Speaker:Why is that?
Speaker:Cause then because then it'll have an Australian light climb.
Speaker:My wife visited her niece in Ireland and had trouble because
Speaker:there was a hurricane there.
Speaker:Like you never have hurricanes in Ireland, are you?
Speaker:But that's the other thing you get, Joe is if you want Australian climate, you'll
Speaker:get Bush fires and hurricanes as well.
Speaker:Do you want that?
Speaker:Okay.
Speaker:One interests me as well is sealer.
Speaker:So let me put the sea level one up.
Speaker:So under the, under the medium case scenario we're looking at, by the
Speaker:end of the century, I an increase in sea level of about 0.7, five meter
Speaker:that's under the medium case scenario.
Speaker:Under the best case scenario, we're looking at half a meter
Speaker:and under the worst case, we're looking at nearly nearly a meter.
Speaker:I believe we had one night, five that's increasing sea level by 2100.
Speaker:I live in Queensland.
Speaker:Well, we all live on the coast, nearly all of us in Australia.
Speaker:Aren't we?
Speaker:And how many places can you think of that would be in deep trouble?
Speaker:If there's a 0.7, five of a meter increase in the sea level, like by
Speaker:the end of the century, that is going to cause a lot of problems, not only
Speaker:in Australia, but around the world.
Speaker:That's one of the biggest impacts I think, besides the storms that
Speaker:will ravage places, the sea level one is going to be a real kick out.
Speaker:Yeah.
Speaker:Well of course, if you're Peter Dutton, you joke about that, right?
Speaker:To your mates in front of a microphone, don't you, that's what he's been doing.
Speaker:Yeah.
Speaker:And if this continues, the sorts of things that could happen in the centuries
Speaker:later are too scary to contemplate.
Speaker:Yeah.
Speaker:I'm in this concern about a lot of the Pacific islands
Speaker:that are built on Carla tolls.
Speaker:Because even now the slightest storm, the storm surge is going across the islands.
Speaker:The islands are getting inundated.
Speaker:If they get another half meter a lot of the islands are
Speaker:literally just above sea level.
Speaker:Yes.
Speaker:And we've got those areas like Louisiana in America, and that, that had just
Speaker:built on swamps and reclined land.
Speaker:So they're enormous trouble if sea temperatures rise.
Speaker:So, so that's the kind of nutshell breakdown that I wanted to give on
Speaker:climate change was where we stand.
Speaker:So let's go through some of the Joe, do you want to add anything before I
Speaker:thought might get through some of the comments and see what people are saying,
Speaker:unless you want to add anything of your knowledge of climate change, including
Speaker:cat sneezing to the mix before we do that I can't think of anything off hand.
Speaker:Okay.
Speaker:So I'll just start at the most recent Tom, the warehouse guy, China is responsible
Speaker:for around 25 to 28% of all emissions.
Speaker:Let me pull it up on the screen actually.
Speaker:The next highs is the U S at 11%.
Speaker:Climate change is another failure of international law.
Speaker:Now, enforceability, there's an interesting debate because the bricks
Speaker:countries, so Brazil, Russia, India, China they didn't go through the industrial
Speaker:revolution and they argue that the first world, so Europe and the states
Speaker:went through the industrial revolution.
Speaker:Created a lot of pollution at that time.
Speaker:So we've had our chance to pull it with greenhouse gases and they need their
Speaker:chance to leap forward their industry to build up their economy to the same
Speaker:level as Europe and the states have.
Speaker:And therefore the west should be reducing their emissions first, allowing India and
Speaker:China, a bit of leeway on their pollution.
Speaker:Before we start becoming heavy handed and emissions trading, it
Speaker:sounds a fair enough argument.
Speaker:Plus we've just outsourced our carbon emissions to a developing country
Speaker:because they're making all this stuff.
Speaker:So that's what happens when you, when you make stuff, isn't it, to some
Speaker:extent is some of that manufacturing would be part of the problem, but,
Speaker:but in terms of, you know, they're building, I mean, cement causes is a
Speaker:big factor in terms of global warming.
Speaker:Well, when you've had dirt roads and mud hearts and you start
Speaker:creating skyscrapers and freeways, you end up using lots of cement.
Speaker:And I think it's a strong argument to say, well, you guys have
Speaker:the chance to industrialize.
Speaker:What, what do you, we just don't get the chance now or how come you
Speaker:got a free ride caused the problem.
Speaker:And now we're all in the same boat together.
Speaker:Like I think it's actually a legitimate argument, Tom, the way high sky.
Speaker:Do you have any sympathy for developing countries?
Speaker:Do you think perhaps the developed countries having done their fair share
Speaker:of polluting and moved on maybe should have harsh of restrictions on them now
Speaker:as a result, what do you think, Tom?
Speaker:The warehouse guy.
Speaker:What else we got here?
Speaker:Dire straits is an upside I'll get ocean views in my house.
Speaker:Getting in will be fine.
Speaker:You just need a tinny.
Speaker:Yeah.
Speaker:Okay.
Speaker:This working my way back through time here that was Andrew talking
Speaker:about fresh water is lighter than salt water, but I don't know how it
Speaker:affects ocean currents, blah blah.
Speaker:Let me see Harry and financially soul and says, this is great.
Speaker:Now we can swim any day in September.
Speaker:Actually I wonder if this is going to do with the stingers coming down normally
Speaker:in Queensland, the stingers were just a, sort of a north Queensland phenomenon in
Speaker:terms of you can't swim in the summer, in the summer in north Queensland.
Speaker:Cause there's just too many stingers and they're finding that era Kanji was found
Speaker:or Fraser island last summer, I think.
Speaker:And I thought it was a couple of years ago, but yes.
Speaker:So that is one of the problems hearing and financially solvent is maybe I
Speaker:won't be able to swim on the gold coast in Salma because of goddamn stingers.
Speaker:So that is another problem.
Speaker:Let me see what else we got here.
Speaker:Andrew says the science around the cause of climate change might change some minds.
Speaker:What about just planning for the consequences?
Speaker:Agee increased climate refugees or water wars, et cetera.
Speaker:So, well honest government ads have alleged that the liberals have
Speaker:put people in both CSI row and.
Speaker:The bureau of meteorology who have refused the higher levels of
Speaker:refused to allow the words, climate change in some of the reports.
Speaker:And I believe Trump banned any planning for sea level rise rod.
Speaker:Yep.
Speaker:So, so there has actually been a pushback against planning for climate
Speaker:change from science denying governments.
Speaker:Yeah.
Speaker:Should we bag religion while we're right?
Speaker:I mean, one of the problems is that, you know, oh, it's the end times
Speaker:Jesus is going to come and save us.
Speaker:It doesn't matter.
Speaker:That's right.
Speaker:That's one of the things, if he believe that the rapture is eminent,
Speaker:that the end times are near, then it's like, well, why would I
Speaker:bother with all this sort of stuff?
Speaker:Like why put ourselves through pain now?
Speaker:Because we're all outta here.
Speaker:In the next 10 or 20 years when the ratchet comes, this is one of the problems
Speaker:that with, with this sort of religious belief, like we're not joking here.
Speaker:This actually has an effect on public policy, if you leaders
Speaker:believe in these sorts of things.
Speaker:So yeah, I don't know if if you can't change minds, it makes it harder to get
Speaker:the right people in power to make the policies so pushing it against the flow
Speaker:polo, if the biggest, if the biggest, most vocal opponents to climate change
Speaker:acceptance has changed their minds.
Speaker:It will be interesting to see what impact that has.
Speaker:Yes.
Speaker:And Murdoch newspapers is sort of what you're thinking
Speaker:of when you're saying that.
Speaker:Well all of the Murdoch press, so Fox news, particularly in the state.
Speaker:Yep.
Speaker:Andrew said in the chat room is the number of people accepting climate change
Speaker:increases, even Murdoch must realize deny views will cause people to turn him off.
Speaker:Maybe, maybe that's why he's done it.
Speaker:Certainly a lot of that, maybe not the nationals themselves, but
Speaker:a lot of their electorate, the farmers have seen the change and
Speaker:are becoming less and less enamored.
Speaker:And I believe who's the doctor in, in uh, Sydney, the female
Speaker:doctor who won a seat yeah.
Speaker:Former president of the AMA.
Speaker:Is that the one you're thinking of?
Speaker:Yes, I think so.
Speaker:Yeah.
Speaker:I can't remember.
Speaker:She, she was a former liberal member and she jumped ship because of climate change.
Speaker:Yeah.
Speaker:So, so there were a lot of conservatives who said, you know I'm very much a liberal
Speaker:through and through, but your policy on climate change just, I cannot support.
Speaker:Yeah.
Speaker:Yeah.
Speaker:Earlier on Tom said evening all, it would be good to hear your thoughts
Speaker:on Al gore and his work early on with global warming and an inconvenient truth.
Speaker:A lot of people get global warming and climate change confused.
Speaker:I guess one of the problems with this is that these sorts of issues have
Speaker:become so tribal, whether it climate change, vaccinations, whatever, putting
Speaker:a politician as the front man for this is probably not a good idea because
Speaker:people will just immediately reject him because they know what tribe
Speaker:he is and they won't even listen.
Speaker:You might be somebody who's more neutral would be a better front man for this.
Speaker:It certainly did contribute to the polarization.
Speaker:The other thing, according to the UK course the, the furry much led to, it was
Speaker:initially there was talk about a tax on the right wing and politics is anti-tax.
Speaker:Yes.
Speaker:And that politicized, the whole push back of we don't want yes.
Speaker:And other tax interfering with our business led to the
Speaker:rejection of the science.
Speaker:That was the reason for the tax.
Speaker:So rather than just arguing about a price on carbon is
Speaker:actually a very right-wing way.
Speaker:Yeah.
Speaker:Let the markets decide.
Speaker:And yet it was turned into a cudgel.
Speaker:Yep.
Speaker:It was turned into a tax and it wasn't, it was a price on carbon that we have.
Speaker:Yeah.
Speaker:I think one of the topics we'll do over the next next time we get onto this will
Speaker:be What policies have been proposed and how these carbon taxes and other things
Speaker:have what was proposed and how they would work and, and what, what is a good system?
Speaker:So can't get into that.
Speaker:The system is basically everybody bidding on how much carbon they'll
Speaker:save, if you pay the money and then paying money and not checking
Speaker:how much carbon they've actually.
Speaker:Yeah, yeah.
Speaker:Well, what could go wrong with that?
Speaker:Yeah.
Speaker:Surely that couldn't happen.
Speaker:Paying people money like that.
Speaker:Surely.
Speaker:Yeah.
Speaker:Yeah.
Speaker:I don't know enough about it.
Speaker:I guess what you're saying is that's what we've done and
Speaker:yeah, it is what we've done.
Speaker:Yeah, no surprise.
Speaker:Is it all right in the chat room?
Speaker:I think I've covered most of the ones that were they you had your own
Speaker:little private jokes going in there at different points, which I can't go into.
Speaker:If you've got anything else be quick, because we're about to Finish
Speaker:up with this one as our little introductory one on climate change.
Speaker:And if you've got any other ideas that you'd like to explore on this topic,
Speaker:give us a buzz, send some message.
Speaker:Let me know.
Speaker:Joe, you're not around next week.
Speaker:You've got something on yeah, it looks like I'm going for a
Speaker:little trip up to the beach again.
Speaker:Right?
Speaker:They don't have internet driving around central Queensland.
Speaker:I can probably jump in from the cabin.
Speaker:I have no idea what the quality will be like.
Speaker:Okay.
Speaker:It might be just shy and myself.
Speaker:We've got lots to talk about.
Speaker:It has been a lot of things have happened over the last week.
Speaker:So lots of good stuff to talk about next week with the panel
Speaker:might be just myself and Shea.
Speaker:And yeah.
Speaker:So hope you enjoyed this episode on climate change, short and sweet,
Speaker:but a good little intro and we'll be back next week with something else.
Speaker:Bye.
Speaker:For now.