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Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA [email protected]. edu http://envsci.rutgers.edu/~ robock Climate Dynamics 11:670:461 Lecture 2, 9/8/14
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Alan Robock Department of Environmental Sciences

Jan 02, 2016

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Lecture 2, 9/8/14. Climate Dynamics 11:670:461. Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA. [email protected]. http://envsci.rutgers.edu/~ robock. - PowerPoint PPT Presentation
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Page 1: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental Sciences

Rutgers University, New Brunswick, New Jersey USA

[email protected]

http://envsci.rutgers.edu/~robock

Climate Dynamics11:670:461

Lecture 2, 9/8/14

Page 2: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Nitrogen (N2), oxygen (O2), and argon (Ar) make up for 99% of the atmosphere, but are not greenhouse gases.

Water vapor (H2O), carbon dioxide (CO2), methane (CH4), ozone (O3), and nitrous oxide (N2O) are greenhouse gases.

A greenhouse gas absorbs infrared radiation, whichcreates molecular vibrationand bending.

Collisions transfer energy to heat the surrounding gas.

But, what is a “greenhouse gas” anyway?

Water vapor (H2O) vibration modes

http://www.lsbu.ac.uk/water/vibrat.html

Page 3: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

CCSM Climate “Forecasts”

(°C)

Produced by Gary Strand, NCAR

(°C)

Page 4: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

IPCC AR4, Chapter 1 Fig. 1.1

Page 5: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Fig. 1.2

Bretherton Diagram

Page 6: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Fig. 1.2

Bretherton Diagram

Page 7: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Page 8: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Page 9: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Page 10: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

http://data.giss.nasa.gov/gistemp/graphs_v3/Fig.A2.pdf

Recovery from volcanic eruptions

dominates

Tropospheric

aerosols mask warming(global

dimming)

Greenhouse gases

dominate

Page 11: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Desire for improved well-being Consumpt

ion of goods and services

Impacts on

humans and

ecosystems

Climate change

CO2 in the atmosphe

re

Consumption of

energy

CO2 emissions

CO

NSER

VATI

ON

EFFICIENCY

LOW

-CARBON

ENERG

Y

SUFFER

ING

SOLA

R RA

DIA

TION

MAN

AGEM

ENT

CA

RB

ON

DIO

XID

E

REM

OVA

L

ADAPTATION

After Ken Caldeira

Page 12: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Annual average surface air pressure. Interval 50 mb.

Fig. 2.1

Page 13: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Fig. 2.1

Annual average surface air pressure. Interval 50 mb.

Page 14: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Fig. 2.2

Page 15: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 2.3

Annual mean900 mb

geopotential height (m)

Annual mean200 mb

geopotential height (m)

Page 16: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

SciencesFig. 2.3

Annual mean900 mb

geopotential height (m)

Annual mean200 mb

geopotential height (m)

Page 17: Alan Robock Department of Environmental Sciences

Alan RobockDepartment of Environmental

Sciences

Seasonal900 mb

geopotential height (m)

Fig. 2.4