Emissions Concentrations Impacts Climate (GtC/yr) (ppmv) - - PowerPoint PPT Presentation

emissions concentrations impacts climate gtc yr ppmv
SMART_READER_LITE
LIVE PREVIEW

Emissions Concentrations Impacts Climate (GtC/yr) (ppmv) - - PowerPoint PPT Presentation

Emissions Concentrations Impacts Climate (GtC/yr) (ppmv) Sea-level rise ( ) Heat waves Drought Extremes etc. Emissions Concentrations Impacts Climate (GtC/yr) (ppmv) Sea-level rise ( ) Heat


slide-1
SLIDE 1

Emissions (GtC/yr) Concentrations (ppmv) Climate (℃) Impacts

  • Sea-level rise
  • Heat waves
  • Drought
  • Extremes
  • etc.
slide-2
SLIDE 2

Climate Sensitivity (℃/ppmv)

  • Cloud feedbacks
  • Non-linear
  • Depends on timescale!

Emissions (GtC/yr) Concentrations (ppmv) Climate (℃) Impacts

  • Sea-level rise
  • Heat waves
  • Drought
  • Extremes
  • etc.
slide-3
SLIDE 3

Carbon Cycle

  • Ocean uptake
  • Land uptake
  • Feedbacks etc.

Climate Sensitivity (℃/ppmv)

  • Cloud feedbacks
  • Non-linear
  • Depends on timescale!

Emissions (GtC/yr) Concentrations (ppmv) Climate (℃) Impacts

  • Sea-level rise
  • Heat waves
  • Drought
  • Extremes
  • etc.
slide-4
SLIDE 4

Carbon Cycle

  • Ocean uptake
  • Land uptake
  • Feedbacks etc.

Climate Sensitivity (℃/ppmv)

  • Cloud feedbacks
  • Non-linear
  • Depends on timescale!

Emissions (GtC/yr) Concentrations (ppmv) Climate (℃) Impacts

  • Sea-level rise
  • Heat waves
  • Drought
  • Extremes
  • etc.

Carbon-Climate Response (℃/GtC)

  • Function of cumulative emissions
  • Basis for carbon budget, Paris, etc.
slide-5
SLIDE 5

Solomon 2009, PNAS Year Atmospheric CO2concentration

slide-6
SLIDE 6

Solomon 2009, PNAS Year Atmospheric CO2concentration Ocean heat content/thermal expansion

slide-7
SLIDE 7

Solomon 2009, PNAS Year Atmospheric CO2concentration Ocean heat content/thermal expansion Year Temperature response

slide-8
SLIDE 8

Solomon 2009, PNAS

Ocean carbon uptake Ocean heat uptake Constant temp. response!

+ =

Year Atmospheric CO2concentration Ocean heat content/thermal expansion Year Temperature response

slide-9
SLIDE 9

Solomon 2009, PNAS

Ocean carbon uptake Ocean heat uptake Constant temp. response!

+ =

Year Atmospheric CO2concentration Ocean heat content/thermal expansion Year Temperature response

Ceasing emissions today will fix surface temperatures at today’s values, for hundreds of years.

slide-10
SLIDE 10

Solomon 2009, PNAS

Ocean carbon uptake Ocean heat uptake Constant temp. response!

+ =

Year Atmospheric CO2concentration Ocean heat content/thermal expansion Year Temperature response

Ceasing emissions today will fix surface temperatures at today’s values, for hundreds of years.

(sea level and deep ocean temps, however, will continue to rise)

slide-11
SLIDE 11

Value of CCR ?

Year

Williams 2017, Journal of Climate CCR for model ensemble under emissions consistent with 1%/yr CO2 increase

CCR (℃/1000 GtC)

slide-12
SLIDE 12

Carbon Cycle

  • Ocean uptake
  • Land uptake
  • Feedbacks etc.

Climate Sensitivity (℃/ppmv)

  • Cloud feedbacks
  • Non-linear
  • Depends on timescale
  • Ignores carbon cycle

Emissions (GtC/yr) Concentrations (ppmv) Climate (℃) Impacts

  • Sea-level rise
  • Heat waves
  • Drought
  • Extremes
  • etc.

Carbon-Climate Response (℃/GtC)

  • Function of cumulative emissions
  • Basis for carbon budget, Paris, etc.
  • Timescale-independent
  • Accounts for carbon cycle