Working Group I – The Physical Science Basis

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SIXTH ASSESSMENT REPORT Working Group I – The Physical Science Basis Changing by Alisa Singer “As we witness our planet transforming around us we watch, listen, measure … respond”.

Transcript of Working Group I – The Physical Science Basis

Page 1: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Changing by Alisa Singer

“As we witness our planet transforming around us we watch, listen, measure … respond”.

Page 2: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

BY THE NUMBERS

Author Team

234 authors from 65 countries

28% women, 72% men

63% first-time IPCC authors

Review Process

78,000+ review comments

46 countries commented on Final

Government Distribution

14,000 scientific publications assessed

Page 3: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Page 4: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Page 5: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“Recent changes in the climate

are widespread, rapid, and

intensifying, and

unprecedented in thousands

of years.

[Credit: NASA]

Page 6: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Changes in global surface temperature relative to 1850-1900

Human influence has warmed the climate at a rate that is

unprecedented in at least the last 2000 years

Page 7: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Changes in global surface temperature relative to 1850-1900

Human influence has warmed the climate at a rate that is

unprecedented in at least the last 2000 years

1.1 C warmer

Page 8: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Changes in global surface temperature relative to 1850-1900

Human influence has warmed the climate at a rate that is

unprecedented in at least the last 2000 years

Page 9: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Highestin at least

2 million years

CO2concentration

Sea levelrise

Glaciersretreat

Arctic sea ice area

Fastest ratesin at least

3000 years

Lowest levelin at least

1000 years

Unprecedentedin at least

2000 years

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Extreme heat

More frequent

More intense

Heavy rainfall

More frequent

More intense

Drought

Increase in some regions

Fire weather

More frequent

Photo Credits from left: 1. Luiz Guimaraes 2. Jonathan Ford 3. Peter Burdon 4. Ben Kuo 5. NOAA

Ocean

Warming

Acidifying

Losing oxygen

Page 11: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“Unless there are immediate,

rapid, and large-scale

reductions in greenhouse gas

emissions, limiting warming to

1.5°C will be beyond reach.

[Credit: Peter John Maridable]

Page 12: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Future emissions cause future additional warming

Very high CO2 emissions

High CO2 emissions

Intermediate CO2 emissions

Low CO2 emissions

Very low CO2 emissions

Page 13: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Future emissions cause future additional warming

Very high CO2 emissions

High CO2 emissions

Intermediate CO2 emissions

Low CO2 emissions

Very low CO2 emissions

Near-term

1.5 C

Page 14: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Future emissions cause future additional warming

Very high CO2 emissions

High CO2 emissions

Intermediate CO2 emissions

Low CO2 emissions

Very low CO2 emissions 1.5 C

Near-term

Page 15: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Future emissions cause future additional warming

Very high CO2 emissions

High CO2 emissions

Intermediate CO2 emissions

Low CO2 emissions

Very low CO2 emissions

Mid-term

2 C

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

…at 2C …at 4C…at 1.5C

With every additional amount of global warming, changes

get larger.Simulated changes…

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Extreme rainfall intensifies by 7% for each additional 1C

at 1.5C

at 2C

With every additional amount of global warming, changes

get larger.

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“It is indisputable that human

activities are causing climate

change, making extreme climate

events, including heat waves,

heavy rainfall, and droughts,

more frequent and severe.

[Credit: Yoda Adaman | Unsplash]

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Observed warming

is driven by emissions

from human

activities, with

greenhouse gas

warming partly

masked by aerosol

cooling

warming

cooling

Page 20: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Observed warming

is driven by emissions

from human

activities, with

greenhouse gas

warming partly

masked by aerosol

cooling

warming

cooling

Observed warming Total human influence

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Greenhouse gases

warming

cooling

Observed warming

is driven by emissions

from human

activities, with

greenhouse gas

warming partly

masked by aerosol

cooling

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Pollution particles (aerosols)

warming

cooling

Observed warming

is driven by emissions

from human

activities, with

greenhouse gas

warming partly

masked by aerosol

cooling

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Natural factors

warming

cooling

Observed warming

is driven by emissions

from human

activities, with

greenhouse gas

warming partly

masked by aerosol

cooling

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Internal variability

warming

cooling

Observed warming

is driven by emissions

from human

activities, with

greenhouse gas

warming partly

masked by aerosol

cooling

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Human influence, main driver of…

• …Hot extremes, which have become more

frequent and more intense

Photo Credit: Chris JLPhoto Credit: Chris JL / flickr

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Human influence, main driver of…

• …Hot extremes, which have become more

frequent and more intense

• …ocean warming since the 1970s, and

ocean acidification.

Photo Credit: Baptiste Azais

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Human influence, main driver of…

• …Hot extremes, which have become more

frequent and more intense

• …ocean warming since the 1970s, and

ocean acidification.

• …changes we see in the frozen areas of

the planet:

Photo Credit: Kenneth Mankoff

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Human influence, main driver of…

• …Hot extremes, which have become more

frequent and more intense

• …ocean warming since the 1970s, and

ocean acidification.

• …changes we see in the frozen areas of

the planet:

• global retreat of glaciers since the 1990

Photo Credit: Kenneth Mankoff

Page 29: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Human influence, main driver of…

• …Hot extremes, which have become more

frequent and more intense

• …ocean warming since the 1970s, and

ocean acidification.

• …changes we see in the frozen areas of

the planet:

• global retreat of glaciers since the 1990s

• 40% decrease in Arctic sea ice since 1979

Photo Credit: Andy Mahoney

Page 30: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Human influence, main driver of…

• …Hot extremes, which have become more

frequent and more intense

• …ocean warming since the 1970s, and

ocean acidification.

• …changes we see in the frozen areas of

the planet:

• global retreat of glaciers since the 1990s

• 40% decrease in Arctic sea ice since 1979

• decrease in spring snow cover since the 1950s.

Photo Credit: Andy Mahoney

Page 31: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“Climate change is already

affecting every region on Earth,

in multiple ways.

The changes we experience will

increase with further warming.

[Credit: Hong Nguyen | Unsplash]

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

New regional information

Inform decisions

related to risk

management and

adaptation

A third of our report is

dedicated to regional

climate information

Page 33: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

New regional information

Inform decisions

related to risk

management and

adaptation

A third of our report is

dedicated to regional

climate information

Page 34: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Climatic impact-drivers

Heat &

cold

Rain &

drought

Snow &

ice

Coastal &

oceanic

Wind Other Open

ocean

A climatic impact-driver could go over thresholds known to

lead to severe consequences for people, agriculture, or wildlife

Threshold

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Changes to the Water cycle

With warmer temperature

Atmosphere can hold more water

More and faster evaporation

Heavier precipitation

Atmosphere

Frozen regions

Land Ocean

Page 36: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Changes to the Water cycle

Heavier rainfall

Intensifying dry seasons and droughts

Atmosphere

Frozen regions

Land Ocean

More global warming

Page 37: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Rainfall and Monsoon

Annual Rainfall on Land

Increasing

Monsoons

Changing in complex ways

Photos: Left: Arek Socha, Pixabay: Right: James Martin Phelps

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Interactive atlas

https://interactive-atlas.ipcc.ch/

#IPCCData #IPCCAtlas

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“There’s no going back from some

changes in the climate system…

[Credit: Jenn Caselle | UCSB]

Page 40: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Ocean and ice sheets

Ocean temperature

Increasing

Greenland Ice Sheet

Melting

Sea level

Rising

Photo Credits from left: NOAA; Konrad Steffen; Allan Grinberg

Page 41: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“…However, some changes could

be slowed and others could be

stopped by limiting warming.

[Credit: Andy Mahoney | NSIDC]

Page 42: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“To limit global warming, strong, rapid, and sustained reductions in CO2, methane, and other greenhouse gases are necessary.

This would not only reduce the consequences of climate change but also improve air quality.

[Credit: evgeny-nelmin.]

Page 43: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Every tonne of CO2 emissions adds to global warming

Very high CO2 emissions

High CO2 emissions

Intermediate CO2 emissions

Low CO2 emissions

Very low CO2 emissions

Increasing CO2

Incre

asin

g t

em

pera

ture

s

Page 44: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Every tonne of CO2 emissions adds to global warming

Very high CO2 emissions

High CO2 emissions

Intermediate CO2 emissions

Low CO2 emissions

Very low CO2 emissions

Increasing CO2

Incre

asin

g t

em

pera

ture

s

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

LANDOCEAN

CO2Carbon dioxide

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SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

CO2Carbon dioxide

CH4Methane

Page 47: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

“The climate we experience in the future depends on our decisions now.

Page 48: Working Group I – The Physical Science Basis

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

9 August 2021

#ClimateReport #IPCC

SIXTH ASSESSMENT REPORTWorking Group I – The Physical Science Basis

Thank you.

@IPCC

@IPCC_CH

linkedin.com/company/ipcc

IPCC: www.ipcc.ch

Interactive Atlas: interactive-atlas.ipcc.ch

IPCC Working Group I TSU:

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