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What Have We Learned From a Summer of Climate Reckoning?

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What Have We Learned From a Summer of Climate Reckoning?

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1630 segments

0:03

from New York Times opinion this is the

0:06

Ezra client show

0:10

[Music]

0:22

hey it is Ezra I am on book leave but

0:25

this week taking a turn at the mic is

0:27

David Wallace Wells he is a times

0:29

opinion writer he's the author of the

0:31

uninhabitable earth life after warming

0:34

and I just think that over the past

0:35

couple of years not just his work on on

0:37

climate change and biodiversity loss but

0:39

also has worked particularly on covid

0:41

has been absolutely fantastic so I asked

0:44

him to come on and do a couple shows

0:46

around these themes I hope you enjoy

0:52

from the perspective of the climate it's

0:54

been a hellish and disorienting summer

0:57

this June was the hottest June on record

1:01

July was the hottest July on record in

1:05

Phoenix all but one day in July crossed

1:08

110 degrees Fahrenheit

1:11

the city's burn units were filling up

1:13

with people who'd fainted on the street

1:14

and been burned by the asphalt which

1:17

measured as hot as 180 degrees

1:20

of course

1:22

is not all bad news there is genuinely a

1:24

Green Revolution underway and it's

1:26

moving much faster than what many

1:28

believe possible just a few years ago

1:30

emissions haven't yet begun to decline

1:32

but Renewables are being rolled out at

1:34

such a pace and at such a low cost

1:37

that many analysts believe will hit a

1:39

carbon Peak sometime this decade

1:42

conventional modeling suggests that in

1:43

just five years we may have cut our

1:46

expected warming for this Century almost

1:48

in half

1:49

but that doesn't mean we can declare

1:51

victory

1:52

over the last decade there's also been a

1:54

flurry of new science showing that

1:56

climate risks we once expected in some

1:58

worst case scenarios

2:00

May instead arrive with much less

2:02

warming and while all of those

2:04

projections come wrapped in uncertainty

2:07

one worrying possibility is that for all

2:09

that rapid decarbonization we may not

2:12

end up on net in a much better place

2:16

which is all to say that thinking

2:17

clearly about the state of climate

2:19

change requires now holding two pretty

2:21

contradictory seeming ideas in your head

2:23

at once we're finally taking action and

2:26

quite rapidly

2:27

but the planet is changing too perhaps

2:30

even more rapidly

2:32

to help talk me through where we are

2:34

today and where we're heading

2:36

there's no one I'd want to speak to more

2:37

than Dr Kate Marvel the senior climate

2:40

scientist at project drawdown she's just

2:42

about the best person I know at holding

2:44

those two different ideas in perspective

2:45

at once

2:47

as always you can email the show with

2:48

your thoughts and guest recommendations

2:49

at Ezra client show at nytimes.com

2:56

okay Marvel welcome to the podcast thank

2:58

you so much for having me so we're

3:00

talking in early August which means a

3:02

lot of the official July temperatures

3:04

have just sort of come in and it looks

3:07

like it was a really hot month and I

3:09

think the data I was looking at this

3:10

morning said that we broke the previous

3:12

record for the hottest month ever by

3:15

0.33 C which means

3:17

we didn't just nudge the record up we

3:19

broke it by like a quarter of all of the

3:21

warming we've ever done in human history

3:22

just this summer so I think in a certain

3:25

way it looks like a kind of a summer of

3:27

climate Reckoning or climate Awakening

3:30

on the other hand it seems like we sort

3:32

of do this every summer last year we had

3:33

extreme heat that killed 61 000

3:35

Europeans we had these dried riverbeds

3:37

and for all across Europe in the US too

3:39

in China but somehow this summer has

3:42

felt to me at least a little bit

3:43

different how has the summer look to you

3:46

I mean the first thing that comes to

3:48

mind when I think about this summer is

3:50

how unsurprised I am and how climate

3:54

scientists were at least mentally

3:55

prepared for extremely hot temperatures

3:58

this summer and that is because of two

4:01

things that's because of climate change

4:03

and that's because of the El Nino

4:05

conditions in the tropical Pacific El

4:08

Nino is a completely natural climate

4:11

phenomenon that after the seasonal cycle

4:13

is the primary source of variability in

4:16

the climate it's basically where you get

4:19

warmer than average temperatures off the

4:21

coast of Peru in the equatorial Pacific

4:24

and because the entire Earth system is

4:27

connected those have reverberations

4:29

across the globe so we've got this El

4:32

Nino condition but it's nowhere near as

4:36

strong as the strongest El ninos on

4:38

record in 1998 and 2016. which means we

4:42

think it's contributing less warming at

4:44

this point than previous ones yes and

4:46

the Really significant thing that it's

4:48

overlaid on top of is climate change

4:51

just to pull back for a minute I wanted

4:53

to ask you a really big picture question

4:55

which is

4:57

is warming speeding up this summer as

5:01

we've been going through all of these

5:02

sort of unusual events and trying to

5:04

make sense of them there have also been

5:05

a couple of Assessments suggesting that

5:07

over the last decade maybe the rate of

5:09

warming is moving up a little but then

5:10

there are other people looking at the

5:12

data and saying it's quite a linear

5:13

Trend how do you assess the state of

5:16

warming and what you think we might

5:18

expect over the next decade which is

5:21

likely to be defined not by dramatic

5:24

emissions increases not by dramatic

5:26

emissions decreases but probably

5:27

something like a plateau what are we

5:30

looking at you know are things getting

5:31

warmer faster or are we basically moving

5:34

forward at the same rate we were before

5:36

the short answer is I don't know

5:39

the longer answer is

5:42

probably 10 years ago you would probably

5:46

have been asking me is warming slowing

5:48

down and that's because following the

5:51

massive El Nino event of 1998 you could

5:54

if you kind of squinted draw a line

5:57

across global average temperatures that

5:59

didn't look like it was Rising very much

6:01

you can reassess the data and it looks

6:04

like it's rising a little bit but this

6:07

led to a lot of discourse about the

6:09

so-called Hiatus in warming you even had

6:12

people on the floor of the Senate saying

6:14

there hasn't been any global warming for

6:16

10 years where is your science now

6:18

and the reason for that is that there

6:22

was a small slowdown in the warming

6:25

these decades can happen we can have

6:27

Hiatus decades we can have surge decades

6:29

which is just a reminder that these

6:32

processes that we're talking about

6:34

tend to play out over very long periods

6:36

of time and because we are humans with

6:39

the lifespans that we have and because

6:40

the story of the emissions perturbation

6:42

is the story that we have which is

6:43

depending on how you want to count a

6:45

century and a half or maybe even just a

6:46

few decades old we want to tell stories

6:48

in really short time frames but the

6:50

climate system doesn't exactly cooperate

6:52

exactly and so there's the role of

6:55

internal variability where sometimes you

6:57

know in the Hiatus decades so following

7:00

you know the big El Nino of 1998 we seem

7:03

to have experienced cooler than average

7:05

conditions in the equatorial Pacific for

7:08

an extended period of time kind of a

7:10

protracted opposite of El Nino a la

7:12

nina-like state that gave rise to large

7:16

cloud cover over those regions and that

7:19

was a stabilizing feedback that

7:21

prevented lots of warming those

7:24

conditions are now gone and so there is

7:27

an explanation where that is just

7:29

internal variability sometimes this

7:31

happens sometimes the reverse happens

7:33

what for me is a much more interesting

7:36

question is the different things that

7:39

were we call it forcing the climate

7:41

system the different external influences

7:43

that are at play in the climate system

7:45

so there was a pronounced slowdown in

7:48

warming between about

7:50

1940 to about 1980. a large contributor

7:54

of that is what we call aerosols so

7:58

pollutants what sort of normal people

8:00

think of as pollution particulate matter

8:03

that comes off of burning coal plants

8:05

burning oil

8:06

that was a seriously huge problem in

8:11

North America and in Western Europe

8:13

and that not only showed up in Health

8:17

Data and the daily lives of people in

8:19

those regions I also showed up in the

8:22

global average temperature because

8:24

aerosols reflect sunlight which means

8:26

that when there are a lot of them out

8:27

there less sunlight is cutting to Earth

8:29

and therefore the warming effect is

8:31

limited not just reflecting sunlight so

8:33

aerosols are also extremely effective at

8:36

seeding clouds so there was that direct

8:38

effect of aerosols or gas and dust that

8:42

is blocking this on but they are also

8:43

making clouds which themselves block the

8:46

Sun and so we have pretty good reason to

8:48

believe that aerosol emissions were

8:51

masking the warming it would have been

8:53

warmer had those aerosol emissions not

8:56

been there now right now the world is

8:58

not emitting zero aerosols even though

9:01

after clean air legislation in the U.S

9:03

and Western Europe

9:04

the aerosol emissions from those regions

9:07

have substantially Fallen but they've

9:09

grown elsewhere

9:10

globally aerosol burden has declined but

9:14

the burden of aerosols has largely

9:15

shifted so we're looking at emissions

9:17

from South and East Asia right now

9:20

and we expect in the future that those

9:24

aerosols are going to be cleaned up we

9:27

have already seen Air Pollution Control

9:29

happening in China in particular but as

9:32

populations notice this they they do not

9:34

necessarily normalize it they demand

9:36

changes they demand action

9:38

and so in industrializing countries the

9:42

pattern tends to be that air pollution

9:44

gets really really really bad as the

9:46

country is industrialize and then people

9:48

get really really angry about it and

9:50

something is done about it

9:51

so it is an unalloyed good thing that

9:55

air pollution is projected to fall in

9:57

the future but in terms of the climate

10:00

impact we're going to see less of that

10:03

masking we're going to see less stuff in

10:06

the atmosphere that's reflecting the Sun

10:08

and so that is a really really important

10:12

problem in the future that even if we

10:16

got rid of all fossil fuel

10:17

infrastructure tomorrow

10:19

in the short term we would see a spike

10:21

in temperature because of that air

10:24

pollution which is killing us but also

10:26

blocking the Sun and the size of that

10:28

spike is there's a lot of uncertainty

10:30

around it even more than some of the

10:31

other forcings but my understanding is

10:34

that the sort of median estimate is that

10:35

it's offering about a half a degree

10:37

celsius of cooling and that some

10:39

estimates get quite close to a full

10:41

degree of Celsius of cooling which we're

10:44

not going to be cutting that pollution

10:45

tomorrow instantaneously but in a sort

10:48

of a imaginary model world where you did

10:50

do that you could be dealing with a

10:52

quite dramatic Spike not just the

10:53

equivalent of this July but something

10:55

like a much larger and more pronounced

10:58

effect and maybe even over the next few

11:00

decades seeing as much warming from

11:03

aerosol reduction is from additional

11:05

carbon emissions yeah I do want to be

11:07

very clear that that is not a reason not

11:09

to cut aerosol emissions but it is

11:11

something that we have to be aware of

11:13

there is a big difference though between

11:15

aerosols and greenhouse gases in how

11:18

they get into the atmosphere and what

11:20

they do once they're there so all of the

11:22

greenhouse gases we're talking about are

11:24

well mixed in the atmosphere so that

11:26

means it doesn't matter who emits them

11:28

somebody in America it's them somebody

11:30

in China miss them somebody in Australia

11:31

doesn't matter every molecule of

11:34

greenhouse gas put in the atmosphere has

11:36

the same warming effect no matter where

11:38

it comes from aerosols are far more

11:40

localized their impact depends on

11:43

prevailing winds their impact depends on

11:45

where they are emitted and they don't

11:47

live very long in the atmosphere after

11:48

they're put there

11:50

foreign

12:09

[Music]

12:15

the way I read a lot of the sort of

12:17

real-time scientific analysis says that

12:19

a lot of these anomalies that we've seen

12:21

this year are within the range of what

12:24

was possible so in that sense as you say

12:26

it sort of confirms some of the

12:28

predictions and models that we've made

12:29

but they're also on the high end and I

12:32

wonder exactly how you think we should

12:34

think about that pair of facts that it's

12:38

not that these events are showing us

12:40

that our science is off but it is

12:42

showing us that we may be at least in

12:44

particular areas on particular points

12:46

skiing along the high end of what we

12:48

thought was possible at this level of

12:50

warming there are ways of interpreting

12:51

that as a comforting set of facts and

12:53

their ways of interpreting it as a

12:55

discomforting set of facts so how do you

12:56

think about it

12:57

from my perspective as a physical

13:00

scientist which I do not expect to be

13:01

the same perspective as you know a

13:04

normal person but for me when there is a

13:08

discontinuity or a disconnect between

13:10

what the models say and what is actually

13:12

happening my first question is why

13:16

is it just because while weird stuff

13:18

happens sometimes and you know this just

13:21

happens to be an event that is is

13:23

unusual or is it some fundamental

13:27

process that we're missing is there

13:29

something we don't understand about the

13:32

science

13:32

and in some cases we have identified

13:36

things that we don't understand about

13:38

the science and there are a whole bunch

13:40

of excited scientists trying to work on

13:43

those problems to try to figure out the

13:46

thing that we don't know

13:48

I think it is unnecessarily fatalistic

13:50

to say oh is the science right or is it

13:53

wrong I think for me the important

13:55

question is what do we understand and

13:58

what don't we understand and why I think

14:01

that kind of gets us into a broader

14:03

question about what climate models are

14:07

supposed to do

14:08

a climate model is supposed to be one

14:11

not in which the world as we know it

14:14

actually happens but it's something in

14:16

which the world we know it is possible

14:18

and what I mean by that is a climate

14:21

model is not designed to capture what we

14:24

call the internal variability of the

14:26

climate system the natural random slosh

14:29

back and forth of air and water that

14:33

kind of determines day-to-day weather

14:34

and even seasonal conditions like an El

14:37

Nino a climate model is not designed to

14:40

say in 1998 there was an El Nino and

14:43

this year there is an El Nino and in

14:45

three years there's going to be a la

14:47

nina a climate model instead you can run

14:50

it over and over and over again and

14:52

every time you run it the conditions are

14:55

going to be slightly different the slosh

14:57

of air and water are going to be in a

14:58

slightly different position and so a

15:01

climate model is not a weather model

15:03

it's not designed to sort of predict

15:05

short-term conditions or even

15:07

medium-term conditions what they should

15:09

do is they should reproduce the

15:11

statistics of these events they should

15:13

get the statistics correct and that

15:16

brings us into kind of a weird place

15:18

because when we're talking about the

15:21

statistics of extreme events

15:24

when we call them extreme events we're

15:26

kind of acknowledging that these things

15:27

are historically really rare it's really

15:30

hard to get those statistics and so we

15:34

are really reliant on the models to kind

15:37

of tell us like is this expected or not

15:39

how far out of the normal is this is

15:42

there going to be a normal anymore what

15:44

is that new normal going to look like

15:46

and I think the question of is it worse

15:50

than we expected that's often quite

15:52

oversold I think in the discussion like

15:55

my question to that is well did you

15:57

check because a lot of these you know

15:59

record-shattering events no climate

16:02

model was able to exactly predict in

16:05

2021 in the Pacific Northwest there is

16:08

going to be a devastating Heat Wave but

16:11

if you look at the emergence of these

16:13

record-shattering conditions climate

16:16

models pretty much say that they should

16:19

be happening you shouldn't just expect

16:21

records to be broken you should expect

16:23

them to be shattered

16:25

yeah I mean one thing that calls to my

16:28

mind and I'm reading this literature a

16:30

little bit more of a distance than you

16:31

are is just it's just striking to me

16:33

that we're talking about this summer

16:35

using all these variables which are much

16:38

more prominent in the discourse than

16:39

they were a few years ago and that's

16:40

just like we are still figuring things

16:42

out we are still learning and as a

16:44

result it makes me feel like as we're

16:46

entering into this time of real

16:48

transformation climate transformation

16:50

we're also being confronted with this

16:53

huge amount of uncertainty around

16:54

everything we know we have models that

16:56

they have confidence intervals but like

16:58

living that confidence interval means

17:00

actually living under a lot of

17:01

uncertainty because are you going to

17:02

land at the fifth percentile outcome

17:04

you're gonna land at the 95th percentile

17:05

outcome those are huge differences and

17:08

mentally we sort of calibrate our

17:10

expectations on the median projections

17:12

but like the world is telling us that

17:14

like climate and climate change is

17:16

actually quite a bit messier than taking

17:18

a median projection to the bank

17:19

absolutely for a long time I personally

17:23

have been really reluctant to talk about

17:25

on certainty because it is so easily

17:27

weaponized by bad faith actors so I want

17:30

to be really clear we don't know

17:32

everything but we don't know nothing

17:34

there are certain things that we are

17:36

very very very confident in carbon

17:38

dioxide methane nitrous oxide these are

17:41

greenhouse gases they make the Earth

17:43

warmer you put more of them in the

17:44

atmosphere you are going to see warming

17:46

that's not something that really any

17:49

serious scientist disputes that's just

17:51

very very basic physics then when it

17:54

comes to well what does that actually

17:56

mean what does it mean to live in a

17:59

world that's getting warmer again there

18:01

are some things that we are incredibly

18:03

confident in because they're just basic

18:05

physics warmer air is thirstier air you

18:08

are getting more evaporation from the

18:10

surface of the Earth

18:11

that water has to go somewhere and so on

18:14

average precipitation rates increase as

18:16

well at the same time we know that warm

18:20

air can hold more water vapor so the

18:23

carrying capacity of air for water vapor

18:25

increases by about seven percent for

18:28

every degree celsius we warm and what

18:30

that means is that when we do have these

18:32

heavy downpours there is more water to

18:35

dump on us that's something that we

18:38

understand really really well but then

18:41

what does that mean for rainfall in a

18:44

particular town a particular area that's

18:47

where we start really running into the

18:50

limitations of our knowledge the

18:51

limitations of of models in general

18:54

and that's because the Earth is an

18:56

incredibly complex interconnected system

18:58

and that complexity can make it really

19:01

really difficult to make solid firm

19:04

projections

19:06

a lot of times uncertainty is seized

19:08

upon because people think oh it's

19:09

uncertain well it could be terrible but

19:13

it could also be great and so it'll

19:15

probably be fine and I think it's really

19:17

important to be clear that we have ruled

19:20

out fine it's not going to be fine

19:22

warming is going to have consequences

19:24

and uncertainty is not our friend

19:27

because if we had that degree of

19:29

certainty if we knew sea levels will

19:31

rise exactly this amount and then they

19:33

will stop and warming will stabilize at

19:36

exactly this amount and it will stop we

19:38

would be able to make rational

19:40

adaptation decisions they would be

19:42

difficult they would be costly but we

19:44

would be able to make those decisions

19:46

because because there is that

19:48

fundamental uncertainty in the system

19:49

that's impeding our ability to make

19:52

decisions and to adapt to what's coming

19:55

and what's already here

19:57

one thing I think about is science

19:59

always has uncertainty built into it but

20:01

it's also just this crazy uncertainty

20:02

experiment that we're running by moving

20:05

the planet's climate into a new climate

20:07

system in which they're going to be a

20:09

lot of similarities and continuities but

20:10

they're going to be some things that are

20:11

really different and so there's beyond

20:14

the sort of basic scientific humility of

20:17

like acknowledging uncertainty there's

20:19

also just you know we're running this

20:21

experiment for the first time and we

20:23

have very good educated guesses about

20:25

where it will lead us but it's the risk

20:28

of running an experiment like this at

20:29

all is that they're going to be some

20:30

things that surprise us when you and I

20:32

last spoke it was about a year ago and

20:34

it was for a piece I was doing about

20:36

kind of the narrowing window of climate

20:38

future so a lot of apocalyptic things a

20:40

lot of apocalyptic future seemed you

20:42

know relatively speaking less likely

20:44

although we couldn't rule them out

20:45

entirely and as you just said a minute

20:47

ago a lot of the everything's going to

20:48

be fine soft Landing Futures where we're

20:50

also looking

20:52

pretty unlikely if not impossible one of

20:54

the other people I spoke to for that

20:56

piece was Catherine hayo and she said

20:58

something to me that I've been thinking

20:59

about a lot this summer which was you

21:01

know we've definitely done a lot in

21:03

decarbonization to reduce the upper

21:05

limit of our expected warming we're

21:07

thinking we're going to see less warming

21:08

than we thought was likely five years

21:10

ago that's great but we're also learning

21:12

a lot about when climate extremes arise

21:15

when really big impacts might hit us

21:18

hard and mostly we're learning that

21:21

those are happening sooner and faster

21:22

than we might have thought five or ten

21:24

years ago and you see a sort of similar

21:26

story unfolding in the Tipping points

21:29

discourse where the people who have been

21:31

most worried about tipping points used

21:34

to talk about them as risks at higher

21:37

levels of warming and are now talking

21:38

about them as risks at lower levels of

21:40

warming maybe even at levels of warming

21:41

like the one we're at right now and I

21:43

wonder if that is how you see the really

21:46

big picture here that even as we're

21:48

doing quite a lot to take control of

21:51

global temperature rise through

21:53

decarbonization not enough but a lot

21:55

we're also learning about how messy and

21:58

risky life at even lower temperatures

22:00

would be

22:02

I agree I think a lot of times people

22:04

are tempted to see a Paris agreement

22:06

warming Target like two degrees Celsius

22:09

or 1.5 degrees which is the high

22:11

ambition warming Target which a lot of

22:13

people are really focused on right now

22:15

those targets are not very meaningful

22:19

scientifically the Earth doesn't really

22:22

know the difference between 1.5 and 1.6

22:25

so a lot of times people think well

22:28

tipping points will definitely be

22:30

triggered if we cross a particular

22:33

threshold and that goes back to the

22:35

question of uncertainty I don't have

22:36

enough certainty I don't have enough

22:37

science nobody does to be able to say we

22:41

are safe if we limit warming to a

22:43

particular level

22:44

the flip side is also true we are not

22:46

doomed if we exceed 1.5 we are not

22:49

doomed if we exceed two if we blow past

22:51

a particular Target I think the UN

22:53

messaging is correct that it's every

22:55

tenth of a degree that matters

22:57

but going back to your question of when

23:01

might we expect these tipping points to

23:03

be breached that's something that keeps

23:06

a lot of scientists up at night so the

23:08

scientific definition of a Tipping Point

23:10

is

23:12

something that you cross that you can't

23:15

get back within time scales relevant to

23:19

human lives or human civilizations so

23:21

some of the Tipping points that we're

23:23

really worried about have to do with the

23:25

circulation of the atmosphere or the

23:27

ocean that's something that is very very

23:29

worrisome well talk us through a little

23:31

bit maybe about each of those and what

23:33

it would look like to cross those

23:34

thresholds and be on the other side of a

23:36

Tipping Point sure so let's talk a

23:38

little bit about what the ocean actually

23:40

does for us the ocean is incredibly

23:42

important in the climate system it's

23:45

obviously a near Infinite Source of

23:47

water that's where water gets evaporated

23:50

from that then gets turned into clouds

23:52

and rain and goes back

23:53

it also is really really effective at

23:57

taking up both carbon and heat so the

23:59

ocean's taking up about 25 percent of

24:02

anthropogenic carbon dioxide emissions

24:05

that's not for free a lot of that is

24:07

going into acidifying the ocean

24:10

the ocean is also very effective at

24:12

taking up heat it's absorbing the

24:14

equivalent of five nuclear bombs a

24:17

second of kind of anthropogenically

24:19

added heat heat that humans have put in

24:22

the atmosphere and another way of just

24:23

thinking about that first just to jump

24:25

in for a second is it's something like

24:26

90 of the extra heat the global warming

24:28

is produced goes into the ocean which

24:29

means they're getting nine times as much

24:31

of an impact as we're getting on lands

24:32

the oceans that's right the ocean does a

24:34

lot um the ocean also moves quite a lot

24:37

of heat around in the climate system the

24:40

currents that have names the currents

24:42

that we think about are generally

24:44

surface currents things like the Gulf

24:46

Stream those are driven by the winds and

24:49

the rotation of the earth and the Gulf

24:52

Stream and other surface currents will

24:54

exist no matter what we do they will

24:57

exist as long as the Earth is round and

24:59

rotating but those surface current

25:01

systems are superposed on a deeper

25:05

longer term circulation which we call

25:09

the thermohaliens circulation and that

25:11

is really driven by not wind but density

25:14

so what happens when water flows north

25:17

to the Arctic for example in the

25:19

Atlantic eventually a lot of it forms

25:22

sea ice the Left Behind water that

25:25

doesn't form the sea ice is saltier it's

25:28

cold it's dense and that makes it sink

25:30

so at the bottom of the ocean we have

25:33

this sort of river of failed ice that is

25:36

flowing and it's flowing Southward

25:38

eventually that water upwells it comes

25:41

to the surface again and it closes that

25:43

Loop so we have this density driven

25:46

ocean conveyor belt that moves over

25:49

hundreds of thousands of years water

25:52

around the Earth's oceans and when the

25:55

circulation of that gets messed up we

25:58

could expect to see large disruptions to

26:01

things like precipitation patterns we

26:04

have really good evidence that in the

26:06

70s and 80s pollution particulate matter

26:09

what we call aerosols from Western

26:11

Europe and North America actually cooled

26:14

the North Atlantic and there is a lot of

26:16

evidence that links that to a migration

26:19

of the rain band especially over the

26:21

Sahel and Africa so that is just kind of

26:24

an example of how again interconnected

26:28

everything is other things scientists

26:30

are thinking about are disruptions to

26:32

the arrivals of the seasonal monsoons

26:34

much like the rainfall in the Sahel that

26:37

I discussed

26:38

the monsoons are are very seasonal and

26:42

enormous walls of the world population

26:45

is dependent on Monsoon rain fed

26:48

agriculture so any disruption we have to

26:51

the monsoon could have massive massive

26:54

humanitarian consequences and that's

26:57

only the circulation category of tipping

27:02

points we might see

27:04

and those are systems that if they move

27:06

into a new phase we would expect to not

27:08

recover on the time scale of of

27:11

centuries right it would take longer

27:12

than that yes so then how does that

27:14

change the way that you think about the

27:16

broader Story I mean one thing I've as

27:19

I've been Reckoning with a lot of this

27:21

material that's occurred to me is that

27:22

we have so much science and so much

27:24

science communication about climate

27:27

change impacts this Century but thinking

27:29

about tipping points really does sort of

27:31

pull your mind a little bit further into

27:33

the future and force you to think about

27:35

climate change as a millennial kind of

27:38

event how do you balance those two

27:41

perspectives in your mind like because

27:43

there are plenty of things that like

27:45

you know may result in relatively

27:48

manageable climate Futures over the

27:50

course of the next 50 years but over the

27:51

course of the next five centuries or 10

27:53

centuries we'll be much more disruptive

27:55

I mean sea level rise is probably the

27:57

most obvious of those but how do you

27:59

balance those two different time scale

28:00

perspectives living living in the

28:02

present where we're making decisions

28:03

living a little bit in the medium-term

28:05

future where we think about the sort of

28:07

consequences of those decisions for our

28:09

children and their grandchildren and

28:10

then in the much deeper future where

28:12

we're like thinking about a world that's

28:15

probably in ways totally independent of

28:17

climate very transformed from the one

28:19

that we know today

28:20

you can ask a question what is the

28:24

warming commitment that we've already

28:26

locked in even if we zeroed out

28:28

emissions tomorrow

28:31

if we zeroed out emissions tomorrow the

28:34

consensus among most of the models is

28:37

that warming would stop

28:39

you would have a balance between two

28:41

effects so the ocean would continue to

28:44

warm up but at the same time the natural

28:47

carbon cycle would start to slowly

28:50

remove some of that carbon that's

28:52

accumulated in the atmosphere and the

28:54

net effect of those is essentially no

28:57

more warming and this is one of the

28:59

reasons why getting to Net Zero is so

29:01

important it's not just because it

29:02

actually allows us to stop warming it

29:04

could over the course of a century or so

29:06

would allow us to undo some of it too in

29:07

theory net negative would probably undo

29:10

it because again at Net Zero you've got

29:12

this you know natural drawdown of some

29:15

of the CO2 in the atmosphere but at the

29:17

same time you've got the ocean still

29:19

responding and so the compensation of

29:21

those is not that warming decreases but

29:23

warming stops in order to get warming to

29:26

decrease you generally need to do

29:28

something extra to take CO2 out of the

29:30

air whether those are enhancing land or

29:33

ocean natural sinks or engineering a

29:36

sink so you know sucking CO2 out of the

29:38

air somehow

29:39

but then the question is okay well if

29:42

warming stops whenever we stop emitting

29:46

does that mean climate change stops and

29:48

the answer is no because we are still

29:51

not finished responding to the warming

29:54

that has already occurred so even if we

29:58

did zero out emissions tomorrow and even

30:00

if we froze the temperature at 1.2

30:03

degrees Celsius above pre-industrial

30:05

temperatures

30:06

the Earth system is not done responding

30:09

to that and so we expect to see some

30:12

amount of sea level rise into the Far

30:15

Far Future as a result of that

30:18

so that's kind of one way of answering

30:20

your question we are not committed to

30:23

further warming we can stop anytime we

30:25

want to but we are not yet done

30:27

responding to the warming that's

30:29

occurred already

30:30

I've seen estimates for the amount of

30:32

additional warming that would be

30:34

required to keep carbon concentration

30:37

stable which is to say to prevent the

30:40

carbon cycle to draw down that carbon

30:43

and keep warming going as opposed to

30:46

even stopping it at something like one

30:48

to two gigatons a year and maybe that's

30:51

not precisely right there's uncertainty

30:53

around that but you know it just is

30:55

really striking to me that the Canadian

30:57

wildfires we've seen this year have

30:59

already emitted more than a gigaton of

31:00

carbon and we're not expecting those to

31:02

happen every single year but the idea

31:04

that we can be sure that if we manage

31:07

our emissions as aggressively as we can

31:09

that there aren't going to be some

31:10

surprises like those Canadian fires that

31:12

are contributing additional carbon and

31:15

preventing us from drawing down what's

31:17

in the atmosphere already that seems

31:19

quite scary that brings up another

31:21

potentially scary thing which is the

31:23

idea of a carbon cycle feedback so as

31:26

you pointed out things that live on the

31:29

surface of the planet either in the

31:31

ocean or on the land take carbon dioxide

31:33

out of the atmosphere by photosynthesis

31:36

to make themselves grow

31:37

you know a forest takes carbon dioxide

31:40

out of the atmosphere not because it

31:42

loves us not because it wants to absolve

31:45

humans of what we do but because it

31:47

needs the carbon dioxide to grow like

31:49

trees exist to exist and when they are

31:51

done existing they are done sequestering

31:53

that carbon dioxide and if we Bank on

31:57

trees to take the carbon dioxide out of

32:00

the atmosphere for us what happens when

32:02

we make it too hot for certain types of

32:04

trees to survive

32:06

there's a lot of worry speaking of

32:08

tipping points that the Amazon

32:10

rainforest and other tropical

32:11

rainforests could switch from being a

32:14

net sink of carbon dioxide removing it

32:16

from the air to a net source of carbon

32:19

dioxide and so these carbon cycle

32:21

feedbacks how are living things on the

32:24

planet going to respond to increased

32:28

warming those are big wild cards the

32:31

uncertainties are large it's almost

32:34

never a good story none of the models

32:36

are projecting a significant uptick in

32:39

the ability of the biosphere to remove

32:40

carbon in the future

32:42

so that kind of gets back to should we

32:45

do that experiment and I think no I

32:48

don't want to know what the carbon cycle

32:50

feedbacks are I don't want to know how

32:52

sensitive the Earth is to doubled carbon

32:54

dioxide I don't want to know the answer

32:56

to any of these research questions that

32:59

I'm interested in I don't think we

33:01

should do that experiment

33:04

[Music]

33:24

[Music]

33:28

one of the things that has always struck

33:30

me about your writing and you're

33:31

thinking that not just your scientific

33:32

work but in your sort of more essayistic

33:34

work is how much you do Center the sort

33:38

of the human elements there's these

33:39

climate dynamics that are going on some

33:41

of them we understand quite well others

33:43

a little bit less well but we have a

33:45

pretty good sense of you know the broad

33:46

trajectory of climate change we may even

33:48

have a relatively good sense of where

33:50

the energy transition is going but all

33:52

of that is like interacting and

33:53

interfacing with the world that we have

33:55

built socially politically economically

33:58

through culture through infrastructure

34:00

and in addition to the climate

34:02

experiment we're running we're also

34:03

running this other quite messy

34:04

experiment which is like how does a

34:06

planet warmed by say two degrees or two

34:09

and a half degrees interact with the

34:11

civilization that we built under

34:12

conditions of zero degrees of warming

34:14

and even putting aside like whether the

34:17

infrastructure works or doesn't how does

34:20

it interact with our politics and our

34:22

economics to be

34:24

responding to and adjusting to a world

34:26

that's as distorted or contorted as a

34:29

world of two or two and a half degrees

34:30

would be I wonder if you could talk a

34:32

little bit about that about the human

34:33

element how you think we're doing on

34:35

that front you know politically

34:37

culturally psychologically are we making

34:40

the right sense of the changes that

34:42

we're seeing out in the world are we

34:43

confused about it like are there things

34:45

that you think the public should better

34:47

understand or you wish the public would

34:49

better understand about

34:50

what is being asked of us as people in

34:53

addition to what we're doing to the

34:55

planet itself

34:57

I think I am probably the worst person

34:59

in the world to ask that question no

35:01

because I am a physicist right like it

35:04

is my job to understand how air and

35:08

water move around in the system and air

35:12

does exactly what physics tells it to do

35:15

it's really easy to understand it always

35:18

does the same thing it fits inside an

35:20

equation really well there are

35:22

uncertainties that come from the fact

35:24

that there's a lot of air there's a lot

35:25

of water there's a lot of land it's all

35:28

interacting but fundamentally those

35:31

things do what you tell them to do

35:33

because they are obeying the laws of

35:34

physics people do not do what you tell

35:37

them to do that's why I find them

35:39

fascinating but that's also why I don't

35:41

understand them and I don't make any

35:43

pretense to having any sort of special

35:46

Insight or moral superiority to tell

35:50

people what to do

35:51

I do find people very interesting though

35:53

and I do find past examples of how

35:56

people have reacted to past climate

35:59

change to be completely fascinating so

36:01

in between you know the 1300s 1400s to

36:05

about the 1700s in the northern

36:09

hemisphere we seem to have experienced

36:12

relatively cool conditions something

36:15

that's sometimes called the little Ice

36:16

Age the best attribution Science Now

36:20

sort of thinks that was due to a mixture

36:23

of some circulation changes in the North

36:25

Atlantic and primarily a series of

36:28

really powerful volcanic explosions

36:30

which blocked the sun cooled down the

36:33

planet at least partially

36:35

and if you look at the history

36:38

especially in Europe of the little Ice

36:40

Age things start getting real weird you

36:43

start seeing an increase in religious

36:46

conflict you also start seeing an

36:48

increase in witch burnings and a lot of

36:51

times the witches that are getting

36:52

burned are getting burned or hung or

36:54

executed or accused because of something

36:58

they have done to the weather they have

37:00

raised the storm they have killed the

37:03

crops they have made the winds blow they

37:07

have done something

37:08

and it's really fascinating to look at

37:12

the linkages between the weather getting

37:14

weird and these cultural impacts that

37:18

come out of it now do I think that

37:21

climate change is going to lead to an

37:23

increase in witch burning no but it does

37:25

show how climate change happens in the

37:29

world that we've built for it and that's

37:32

something that is impossible to fit in

37:34

an equation it's impossible to have a

37:38

model that's at all meaningful that says

37:40

that well as carbon dioxide

37:42

concentrations increase the number of

37:46

old women who are going to be accused of

37:49

Witchcraft is also going to increase

37:51

that's not something that makes any

37:52

sense but that really does show the

37:55

fundamental unpredictability of human

37:58

beings and human civilizations in the

38:01

face of adversity sometimes there is

38:03

conflict you know people fight each

38:05

other

38:06

sometimes there is collaboration which

38:10

one of those is more likely to happen

38:12

well I think both are going to happen in

38:13

the future and I think it's really

38:15

impossible to have a grand unified

38:18

theory of a species that's so deeply

38:23

weird as we are

38:25

yeah I want to talk a little bit in a

38:27

minute about the suitability of the

38:29

world as we have built it for the

38:31

climate that we are entering into but

38:33

before we get to that I just wanted to

38:34

pick up on a couple threads from that

38:37

last answer I was just reading an

38:38

article in The Economist about the heat

38:41

waves and in it they drew on this work

38:44

by Marshall Burke and Sal Shang and

38:46

Edward Miguel about the relationship

38:48

between climate and conflict which

38:50

suggested that as temperatures global

38:51

average temperatures got hotter we might

38:53

see some significant additional conflict

38:56

mostly at the interstate and Civil War

38:58

kind of level and The Economist was

39:00

saying just looking at the anomalous

39:01

temperatures in July we might see like

39:04

50 more conflict than we would see

39:06

otherwise without that warming and I

39:08

emailed Marshall and said well I know

39:09

your data was like based on long-term

39:11

average trends like is this a fair

39:14

leap to make and he said well we're

39:15

actually updating it for monthly

39:17

averages and the numbers aren't very

39:18

different so I wouldn't be surprised if

39:20

that was actually how it netted out and

39:22

that is absolutely astonishing to think

39:24

about even in the range of possibilities

39:25

here but it also brings to mind all of

39:28

these other questions about how we talk

39:30

about the attribution of really

39:33

complicated events and episodes to

39:36

climate change or not how do you think

39:38

about

39:39

how to talk about that complicated web

39:42

of causality and how do you think the

39:44

world as a whole is doing and

39:46

understanding just how complicated those

39:48

Dynamics really are I think we need to

39:51

acknowledge that we're not going to get

39:53

the comfort of this false binary we're

39:55

not going to be able to say climate was

39:58

the only Factor but that doesn't mean

40:00

it's not a factor take for example

40:02

wildfires wildfires are dependent on

40:06

many different things they're dependent

40:08

on the weather hot dry conditions

40:10

they're dependent on the amount of fuel

40:12

they're dependent on ignition so either

40:15

lightning or Human Action and they're

40:18

dependent on suppression the damage they

40:20

do really depends who's Living In Harm's

40:23

Way

40:24

and not all of those things are amenable

40:29

to description by physics I focus a lot

40:32

on the physical causes because that's my

40:35

job that's my expertise but when we talk

40:38

about wildfires let's take for example

40:41

even though we're here on the East Coast

40:42

we've had impacts from Eastern Canadian

40:45

wildfires let's talk about wildfires in

40:47

the west because the science is much

40:49

more robust when we talk about wildfires

40:51

in Western North America

40:52

we do know that the hot dry conditions

40:58

that are more conducive to fire fire

41:00

weather those are getting much more

41:02

likely we also have reason to believe

41:05

that we're going to see much like a

41:07

swingier precipitation really really wet

41:10

wet Seasons really really hot and dry

41:13

dry seasons that has implications for

41:16

fuel right if you have a really really

41:18

wet winter you could have a lot of

41:21

vegetation growing and that vegetation

41:22

is going to dry out in the summer and

41:25

burn so those things are kind of

41:28

amenable to description via equations we

41:32

can say this is our knowledge of physics

41:34

this is how it's changing but what does

41:38

that mean in terms of the ability or the

41:41

desire of humans to venture into forests

41:44

and build campfires or have gender

41:47

reveal parties or whatever you know you

41:49

are looking at the culmination of not

41:53

just current policy choices but a long

41:55

history of policy choices who gets to

41:57

live on that land who gets driven off

42:00

that land who gets to make these

42:01

decisions and again I can't put it in a

42:04

climate model but it doesn't mean that

42:06

it's not vitally crucially important

42:09

yeah I mean Wildfire I think is a really

42:11

powerful example for a number of reasons

42:13

but one of the things that I always find

42:15

myself thinking about is you know

42:17

hearing occasionally from people who say

42:19

we shouldn't worry all that much about

42:20

the trends in Wildfire because fires

42:22

used to be much more pervasive in the

42:24

American West 500 years ago 200 years

42:27

ago and that's true there was more

42:29

burning in those forests in the past but

42:31

also there were not 40 million people

42:33

living in California there were probably

42:34

less than one million and the way that

42:36

we think about those risks has a huge

42:38

amount to do with those 40 million

42:40

people not just the fires themselves and

42:43

whether 2020 was merely the worst season

42:46

in 130 years or whether it was the worst

42:49

season in 500 years

42:50

and

42:52

even in a relatively steady climate

42:55

trajectory where things are getting kind

42:56

of predictably worse our experience of

42:59

that climate may still involve quite a

43:01

lot of shock moments because the world

43:04

that we've built

43:06

out in you know the infrastructural

43:07

world but also our political systems our

43:10

emotional infrastructure all of that is

43:12

calibrated to climate conditions we've

43:15

already left behind and as a result

43:16

there's going to be some episodes in

43:19

which we can tolerate some amount of

43:21

additional warming and some higher

43:22

impacts and risks but then at a certain

43:25

point that gets broken you know if you

43:27

think about sea level rise and floods

43:29

and a small flood wall can protect some

43:32

high days of flooding then you've got to

43:34

really you know even just the last foot

43:35

can have a completely devastating impact

43:37

on the city I wonder how you think about

43:39

that set of questions like the degree to

43:42

which we are all of us living on

43:46

assumptions from an earlier climate era

43:50

how much we have to do to navigate the

43:54

new world full of more climate risks and

43:57

how far along in that process we are at

44:00

a policy level but also at a you know

44:02

emotional sort of intellectual level so

44:05

first of all no adaptation is not really

44:09

an option anymore we have no choice but

44:12

to adapt to the changing climate because

44:14

climate change is already here I was

44:17

watching a documentary the other day and

44:19

it was kind of old it was about 15 years

44:21

old and I was so struck by the fact that

44:23

they were using polar bears to

44:25

illustrate climate change and I was

44:26

thinking nobody really does that anymore

44:28

because it's so obvious that this is not

44:31

a problem that just affects polar bears

44:32

this is a problem that is affecting us

44:34

and it's something that we are going to

44:36

have to prepare for at the same time you

44:39

sometimes hear this very glib like oh

44:41

we're rich we'll just adapt especially

44:44

in wealthy countries and there is no

44:46

just to the adaptation because first of

44:49

all if you don't reach Net Zero if you

44:52

don't stop climate change it's a

44:55

constant moving Target adapt to what on

44:58

the other hand adaptation means

45:00

something really really drastic it means

45:03

relocation of communities it means maybe

45:05

abandoning really beloved areas

45:09

it is an extraordinary undertaking that

45:12

doesn't mean that it's not necessary

45:14

that doesn't mean that it's not possible

45:16

but I don't think we should be glib

45:18

about it at all

45:20

along the way there there's also the

45:22

risk I think that as we see more and

45:24

more intense impacts start to adapt to

45:27

some degree we also adapt by normalizing

45:30

and by acclimatizing to things that we

45:33

would have considered unworkable and

45:34

unlivable conditions not that long ago

45:37

and I think that you know our experience

45:38

with Wildfire smoke here is pretty

45:41

Illuminating which is to say like there

45:43

were people who worried about smoke

45:45

impacts from fires five years ago in

45:47

California but most people worried about

45:49

property damage and lives lost and towns

45:52

being destroyed then starting in 2020

45:54

when we had these really eerie images

45:56

from San Francisco really bad toxic air

45:59

days I think the public started to worry

46:01

a bit more about smoke and and public

46:03

health impacts but those of us living in

46:06

the east coast were like well that's

46:07

crazy Californians they're dealing with

46:09

that that's well beyond what I could

46:11

tolerate in my own life and then we had

46:14

a few days depending on how you want to

46:16

count a few days or a few weeks of

46:17

really bad air here and

46:20

almost like by the second or third day

46:23

the emotional calibration at least of

46:25

people I knew was like well I guess this

46:27

is going to be a thing now

46:28

it wasn't to treat this impact which

46:31

five years ago we would have thought of

46:33

as totally intolerable as still

46:35

intolerable it was to incorporate that

46:38

into our understanding of the next 10 or

46:40

15 years of our lives and there's a way

46:42

in which that's quite healthy because

46:44

probably it is going to be a feature of

46:47

at least our worries if not coming every

46:49

summer but it also tells us something

46:52

about how quickly we're redefining our

46:54

standards for a comfortable climate

46:57

capable of sustaining human flourishing

46:59

and how differently we're defining those

47:01

terms in order to allow ourselves some

47:04

safe operating space emotionally for

47:06

living in that world I'm actually going

47:08

to disagree with you because what what

47:10

is a podcast without a good fight so I

47:13

actually think we cannot normalize this

47:15

and we have to push back really really

47:17

hard when you say cannot you mean that

47:18

it's beyond our capacity or do you mean

47:20

that we have to resist it we have to

47:21

resist it yeah we have to resist it and

47:23

I think there has been a strain in

47:27

climate storytelling of fatalism and

47:30

sometimes that fatalism is coupled with

47:32

while humans are bad and terrible and

47:34

this is our divine judgment our

47:36

punishment sometimes it's scolding like

47:38

you are terrible and this is your

47:40

punishment I have to live within I hate

47:41

you and sometimes it's just very sort of

47:44

fatalistic there's nothing we can do

47:46

about climate change we're just going to

47:48

have to live like this for the rest of

47:50

our lives

47:51

when the Cuyahoga River caught on fire

47:53

the air quality was terrible in New York

47:56

but that would have been kind of a

47:58

moderately bad day not that much

48:00

different than normal you know in my

48:03

parents Lifetime and that was normalized

48:08

for a long time until it wasn't until it

48:11

became clear that there were Solutions

48:14

now I don't want to say that any

48:17

particular single piece of legislation

48:19

can ever solve all of the problems but

48:22

the Clean Air Act of 1970 which was not

48:26

passed by a wonderful loving Man Who

48:30

Loved Humanity in the environment that's

48:31

not how you described Richard Nixon no

48:33

it's not but you know there was a

48:37

Confluence of factors there was

48:39

increased scientific understanding of

48:41

where this problem was coming from and

48:43

what we could do about it there was

48:45

popular pressure the first Earth day was

48:47

1970 lots of people out on the streets

48:50

marching School groups Church groups and

48:53

there was a president who saw an opening

48:55

not because he was a lovely warm fuzzy

48:58

wonderful person but because the

49:00

conditions made this possible and I

49:03

think there are a lot of stories of

49:05

environmental success in the record none

49:08

of them are perfect analogies for where

49:10

we are that's what it means to be living

49:13

in the future we are not living in a

49:15

story that has ever happened before I'm

49:17

sorry that's just what it means to be

49:19

alive but I think we cannot normalize

49:21

this we cannot say the climate is just

49:24

going to change and we're going to blow

49:25

past all of these targets and it's just

49:27

going to get worse and worse and worse

49:29

like I think we have to demand this is

49:31

we don't like this we don't

49:34

want to live like this instead of

49:36

accepting it well I think as a sort of

49:38

political goal and value said that's

49:39

totally admirable but when I think about

49:41

for instance the way that people in

49:43

Florida or California are responding to

49:45

the end of insurance for their homes

49:48

we're not seeing a mass Exodus in fact

49:50

we're still seeing to some degree in

49:51

some parts of those States real

49:53

population growth we're seeing tons of

49:55

people flooding to the parts of the US

49:57

where climate impacts are expected to be

49:59

most intense and maybe that's a sign of

50:01

optimism about our ability to redesign

50:03

our future to allow us to live in those

50:05

conditions but it also seems like not

50:07

necessarily the most rational response

50:10

to a climate we know is changing and

50:13

suggests that on the whole at a

50:15

population level even as we're

50:16

endeavoring to limit warming and

50:19

endeavoring to make a future that's more

50:20

livable we're also coming to accept

50:23

climate outcomes that a decade or a

50:26

generation ago would have seemed quite

50:27

horrifying to many of us I mean I think

50:29

we have no choice but you know you say

50:31

accept I say continue to live through

50:34

yeah you know like I don't know

50:36

precisely what the boundary between

50:38

acceptance and and merely continuing to

50:41

exist is yes these are conditions that

50:44

are happening the skies in New York were

50:46

orange earlier this summer in Phoenix

50:49

it's been over 100 degrees for however

50:51

long these are conditions that are

50:54

happening I think that it is completely

50:57

appropriate to demand that they not

51:00

happen you know we can't demand no

51:02

global warming we're already at 1.11.2

51:06

degrees above pre-industrial

51:07

temperatures we can't put that cap back

51:10

in the back we can't say we want no

51:11

global warming but we can say we want to

51:14

limit global warming and we want

51:17

sensible adaptation measures and both of

51:20

those things are incredibly tall orders

51:23

but that's what politics is for right

51:26

like we want to live in a society we

51:29

want there to be buildings built we want

51:30

there to be roads we want there to be

51:32

Subways and all of those things are way

51:35

way bigger than any one person can

51:37

deliver but we want them so we have them

51:41

and I think we need to say this is not

51:43

acceptable this is not normal and things

51:46

have to change

51:47

and when you take off your physicist hat

51:49

and put on like your politics hat like

51:52

how do you assess the state of climate

51:54

politics in the U.S and more generally

51:57

around the world I mean obviously

51:59

we're moving faster than used to be the

52:02

case there's more General consensus

52:05

about the fact of the problem the

52:07

necessity of taking some action in

52:08

response to it than even just five years

52:10

ago you know across the world but we're

52:13

still falling short of the goals and

52:17

targets that we sort of collectively set

52:18

for ourselves even as some of those

52:21

targets start to seem less safe than

52:23

they might have seen five or ten years

52:24

ago so how do you think about the state

52:27

of Politics as it relates to this

52:29

challenge like how do you calibrate your

52:30

own sense of of where we are and where

52:32

we're headed I have scrupulously avoided

52:35

having a politics hat I don't want one

52:37

what I can say from my personal

52:40

experience is I have noticed a sea

52:44

change

52:45

5 10 15 years ago there was only one

52:48

story that ever got told about climate

52:50

change and it was is it happening let's

52:52

get all of these scientists who say it

52:54

is and like this one guy says it's not

52:56

all right let's have them fight and I

52:58

understand where that came from the urge

53:02

to sort of inject conflict and drama

53:04

into what's fundamentally a really

53:06

really difficult thing to wrap your mind

53:07

around

53:08

sometimes it would be scientists

53:10

fighting with guy in a suit sometimes it

53:12

would be like look at this sad polar

53:14

bear it's gonna die and it's all your

53:15

fault because you're a bad person but

53:17

those were really the only stories that

53:19

ever got told and in I want to say 2018

53:23

because that was the release of the un's

53:26

1.5 degree Special Report which Maya

53:30

culpa I was grouchy about I thought it

53:32

was fan fiction I thought well there's

53:35

no way we're going to limit warming to

53:36

1.5 degrees why are you doing this and

53:39

you know like oh boy what the world

53:40

needs is another report great let's do

53:43

that again and for reasons that I don't

53:45

understand I was so wrong I was so wrong

53:48

about how that was going to be received

53:50

I was so wrong about how that would land

53:53

and it started something

53:56

um now the same year that Greta started

53:58

striking the foundation of XR yeah the

54:01

the synonym of uh Sunrise Sunrise talk

54:04

about tipping points that's not

54:05

something that I was able to anticipate

54:08

and now I almost never get asked is it

54:12

real I almost never get asked well what

54:15

does climate change mean and why should

54:16

I care instead I get asked the really

54:19

good questions about uncertainty about

54:22

what's happening about how we can

54:24

prepare about what we can do

54:26

and for me personally the fact that we

54:30

are talking about what we can do is

54:33

really exciting because all I ever

54:35

wanted to be in the climate debate and

54:38

climate politics was irrelevant

54:40

and I am really really rapidly as a

54:44

scientist approaching that point where I

54:47

am not the first point of contact if

54:49

you're writing a climate story you don't

54:51

necessarily go and talk to a scientist

54:53

and say oh hey is this real is this

54:55

really happening you're gonna go and

54:57

you're going to talk to somebody who

54:58

works in renewable energy you're going

55:00

to talk to an electrician you're going

55:01

to talk to somebody trying to craft

55:04

climate policy

55:06

you're going to talk to an entrepreneur

55:07

and now there are so many more stories

55:10

to be told about climate and that's

55:13

something that is a massive massive sea

55:16

change for me yeah I mean I I think

55:18

you're being too modest about being

55:19

irrelevant even speaking on behalf of

55:21

climate science because I do think that

55:23

there are these really important

55:25

questions about exactly what it means

55:27

the difference between two and two and a

55:29

half degrees particular impacts in local

55:30

plan like there's a huge amount for

55:32

science to tell us I do think we're

55:34

living in a different world now where we

55:36

do see the Machinery of decarbonization

55:38

actually finally getting going we're

55:41

starting to see that show up in our

55:43

understanding of and our projections for

55:44

the future all of that's extremely

55:46

exciting but I worry a little bit that

55:48

the story of progress and

55:49

decarbonization is crowding out some of

55:52

these other challenges and these other

55:53

difficulties that we are excited to be

55:55

on the march to net zero even if it's

55:57

going to be in 2070 as opposed to 2050

55:59

and we're excited to be you know making

56:02

impossible the scariest climate Futures

56:04

that some of us worried a lot about a

56:05

few years ago but that doesn't mean that

56:08

the challenges aren't real and real

56:10

right in front of us and may even prove

56:12

quite catastrophic when all is said and

56:14

done and I wonder how you think about

56:16

those questions as a sort of

56:18

Storytelling level which is we obviously

56:21

need to be talking about both of these

56:22

things at once the things that the

56:24

climate is telling us about how

56:26

different and likely how how much harder

56:28

life will be because of climate changes

56:30

but also

56:32

everything we're doing to take control

56:34

of those challenges both for limiting

56:36

warming and through adapting but finding

56:38

that balance feels to me like pretty

56:40

hard and maybe it feels hard to me

56:42

because I'm just on a roller coaster

56:44

about it in one month I feel one way and

56:45

one month I feel the next way about it

56:47

how do you think about it yeah again as

56:49

a kind of a storytelling level I think

56:52

all I can do is answer from myself so I

56:55

don't feel one particular way about

56:57

climate change I feel many different

56:59

ways about climate change some days I'm

57:01

very excited I'm very kind of Joyful by

57:04

looking at all of the work that's being

57:06

done sometimes I'm really afraid

57:08

sometimes I'm really really angry and I

57:11

think that's completely appropriate and

57:13

normal and natural to hold all of these

57:15

things in my head going back to your

57:18

question before about the time scales I

57:22

want to kind of invert that question

57:23

because that's the way that I think

57:25

about this a lot so there's a really

57:27

negative story you could tell where even

57:30

if we get everything right even if if we

57:32

reached Net Zero and 2050 like we're

57:35

supposed to and all of these amazing

57:37

Technologies come online and we rebuild

57:40

our entire Energy System our

57:42

transportation system we really

57:45

transform our farm system we do

57:48

everything right

57:49

we're not really going to be able to

57:51

tell climate wise for decades the best

57:55

case scenario from a climate perspective

57:58

is just less bad than it would be

58:01

otherwise and that's because it takes a

58:04

really really long time for these

58:05

changes to kind of percolate through the

58:07

system for you to distinguish the signal

58:09

from the noise so it's going to take

58:11

decades to say oh we're in the good

58:13

place as opposed to the bad place or not

58:15

the good place the less bad place

58:18

but if you

58:20

if he got the near-term benefits you get

58:24

rid of a coal-fired power plant and

58:27

immediately the next time it rains that

58:31

washes out all of the gross particulate

58:33

matter pollution the black coal plant

58:35

put in the atmosphere so you get cleaner

58:37

air almost immediately

58:39

that starts to show up in mortality

58:43

morbidity statistics really really

58:45

really quickly and just to put a pin on

58:47

it for the listeners like those numbers

58:49

are horrifyingly large you know some

58:51

estimates in the millions annually dying

58:55

from the pollution from fossil fuel

58:56

burning the estimates that I've seen say

58:58

air pollution is a factor in 11 of

59:02

deaths worldwide we're talking millions

59:04

and millions and millions of preventable

59:06

deaths so air pollution is a killer air

59:09

pollution is disgusting and air

59:12

pollution is not something that we have

59:14

to live with you know if I wanted to use

59:16

the linga I'd say that is a co-benefit

59:18

of climate Solutions but that is a

59:20

massive near-term benefit and there is a

59:23

large research literature that says that

59:25

we're going to see less infant mortality

59:28

we're going to see if we do this we're

59:30

going to see less mortality morbidity

59:32

we're going to see people living longer

59:34

healthier lives we're also going to see

59:36

increases in things like labor

59:38

productivity

59:39

now if we adopt various other climate

59:42

Solutions we get co-benefits in terms of

59:45

better biodiversity not cutting down

59:48

forests is a climate solution and that's

59:52

going to have co-benefits that show up

59:54

much much much quicker than any climate

59:56

benefit and so if you invert that and I

60:00

think about this a lot so in the ipcc

60:02

report there is a a figure of a child

60:06

born in various years and the climate

60:08

that they will experience as they grow

60:10

older I want to take that figure and I

60:13

want to kind of invert it and think

60:15

about if we take these climate actions

60:18

what are the positive benefits that can

60:21

accrue and when do they start accruing

60:22

so if we limit warming to 1.5 C our

60:27

great-grandchildren are going to thank

60:28

us for avoiding more catastrophic sea

60:32

level rise but if we do that we

60:35

ourselves not our children not even

60:37

ourselves in 10 years we are going to

60:39

experience those benefits of cleaner air

60:42

immediately there's going to be more

60:44

people alive now and I think that's

60:46

something that's really worth doing

60:48

personally

60:49

well I think that's a really great place

60:51

to end and you know since you've a

60:53

repeat guest you would know that as you

60:54

come on the show you're supposed to come

60:56

with three book recommendations um for

60:58

the audience what what are your books

61:00

my first book recommendation is actually

61:03

not a book it is a short story in fact

61:06

it's such a short story that it's about

61:07

a paragraph long and it's called on

61:10

exactitude in science by Jorge Luis

61:13

Borges and it is the perfect

61:15

distillation of the process of modeling

61:18

of trying to represent Nature by

61:21

something smaller and more tractable my

61:23

second book recommendation is kind of a

61:27

off the wall one we talked about the

61:30

little ice age and we talked about witch

61:32

burning in the little ice age

61:34

turns out that British monarch James the

61:38

first published a paper on how to

61:40

identify and deal with witches because

61:43

he was really obsessed with witches

61:46

being the king in the middle of the

61:48

little ice age

61:49

and he was previously the King of

61:53

Scotland he was brought down when

61:54

Elizabeth the first died and so if you

61:57

are a playwright and you want to appeal

62:00

to this kind of Scottish weirdo who's in

62:03

charge who's really obsessed with

62:05

witches what are you going to write and

62:07

so that's where Macbeth comes from and

62:09

I've been re-reading that in preparation

62:12

for some things that I'm writing about

62:14

the little ice age and I'm just really

62:15

struck by these themes of guilt and also

62:19

really struck by the extent to which the

62:21

witches and Macbeth are manipulating the

62:24

weather and so I think that is a really

62:26

interesting view into a world in a

62:30

different climate than the one we are in

62:31

right now

62:32

and my third book is not out yet but

62:35

it's available for pre-order in order to

62:38

preface this I have a lot of problems

62:40

with climate fiction I find a lot of it

62:42

to be kind of unnecessarily apocalyptic

62:45

or very preachy and it's just not

62:48

something that I like to consume off

62:50

hours and so there's a book which I've

62:53

been fortunate enough to read a

62:55

preliminary draft of it's called

62:57

Troubled Waters it's a novel by Mary

63:00

Anna is hegler and it's just a warm and

63:03

beautiful and complex story about a

63:06

southern black family wrestling with the

63:09

climate crisis

63:10

kid Marvel thanks for coming on the

63:11

program thank you so much for having me

63:14

[Music]

63:24

this episode of the Ezra Klein show was

63:27

produced by Roland who

63:29

fact checking by Michelle Harris with

63:31

Mary Marge locker and Kate Sinclair

63:34

senior engineer is Jeff gold

63:36

our senior editor is Roger Karma

63:39

the show's production team also includes

63:40

emefa agawu and Kristen Linton

63:43

original music by Isaac Jones audience

63:46

strategy by Christina samuelski and

63:49

Shannon Busta

63:50

the executive producer of New York Times

63:52

opinion audio is Annie Rose dresser and

63:54

special thanks to Sonia Herrero

63:58

please

63:59

[Music]

Interactive Summary

In this episode, David Wallace-Wells and climate scientist Dr. Kate Marvel discuss the complex state of global warming, examining the record-breaking heat of the summer, the role of natural climate variability like El Niño, and the interplay between human action and climate change. They emphasize the need to resist normalizing these extreme conditions while acknowledging the importance of both rapid decarbonization and urgent adaptation efforts. The conversation also explores climate 'tipping points,' the uncertainty inherent in climate models, and the immediate health co-benefits of shifting away from fossil fuels.

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