Atmospheric Spectroscopy - The Budker Group

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Atmospheric Spectroscopy

A look at Absorption and Emission

Spectra of Greenhouse Gases

Our Atmosphere

Diagram taken from http://csep10.phys.utk/astr161/lect/earth/atmosphere.html

Composition of the Atmosphere

N

2

= 78.1%

O

2

= 20.9%

H

2

0 = 0-2%

Ar + other inert gases = 0.936%

CO

2

CH

4

= 370ppm (0.037%)

= 1.7 ppm

N

2

0 = 0.35 ppm

O

3

= 10^-8

+ other trace gases

Earth’s Radiation Budget

Electromagnetic Spectrum

Near Infrared

Thermal Infrared

• Over 99% of solar radiation is in the UV, visible, and near infrared bands

• Over 99% of radiation emitted by Earth and the atmosphere is in the thermal IR band (4 -50 µm)

Electromagnetic Spectrum

Near Infrared

Thermal Infrared

Diagram modified from www.spitzer.caltech.edu/Media/guides/ir.shtml

• Over 99% of solar radiation is in the UV, visible, and near infrared bands

• Over 99% of radiation emitted by Earth and the atmosphere is in the thermal IR band (4 -50 µm)

Blackbody Radiation Curves for Solar and

Terrestrial Temperatures

Diagram taken from Peixoto and Oort (1992)

• Without greenhouse gases the temperature of the Earth’s surface would be approximately 15 degrees Fahrenheit colder than it is today

• This is due to the fact that certain trace gases in the atmosphere absorb radiation in the infrared spectrum (wavelengths emitted by the Earth) and re-emit some of this radiation back down to Earth

What are the Major Greenhouse Gases?

N

2

= 78.1%

O

2

= 20.9%

H

2

0 = 0-2%

Ar + other inert gases = 0.936%

CO

2

CH

4

= 370ppm

= 1.7 ppm

N

2

0 = 0.35 ppm

O

3

= 10^-8

+ other trace gases

Molecular Absorption

• The total energy of a molecule can be seen as the sum of the kinetic, electronic, vibrational, and rotational energies of a molecule

• Electronic energy α

• Vibrational energy α

• Rotational energy α a

2 h

2 ma

2

2 mM

 2

Ma

2

=> visible/ultraviolet

=> thermal/near infrared

=> microwave/far infrared

• Vibrational transitions (higher energy) are usually followed by rotational transitions (lower energy) and we thus see groups of lines that comprise a vibration-rotation band

electronic rotational vibrational

Energy level diagram of CO

2 molecules showing relative energy spacing of electronic, vibrational, and rotational energy levels

Vibrational Transitions of a Diatomic

Molecule

• The molecular bond can be treated as a spring and thus a harmonic oscillator potential can be approximated for the molecule

• Evib = v(v+1/2) and v = (1/2π)(k/µ) 1/2

• However, polyatomic molecules are more complicated due to their more complex structure

• For polyatomic molecules, any allowed vibrational motion can be expressed as the superposition of a finite amount of vibrational normal modes, each which has its own set of energy levels

Vibrational Transitions of Polyatomic

Molecules

• Any molecule has 3N degrees of freedom, where N is the number of atoms in the molecule.

– Translational Degrees of Freedom: 3

Specifies center of mass of the molecule

– Rotational DOF: 2 (linear), 3(nonlinear)

Describes orientation of the molecule about its center of mass

– Vibrational DOF: 3N-5 (linear), 3N-6 (nonlinear)

Describes relative positions of the nuclei

• Vibrational DOF represent maximum number of vibrational modes of a molecule (due to degeneracies and selection rules)

Harmonic Oscillator Approximation for

Polyatomic Molecules

• E vib

= G(v

1

,v

2

,…) = ∑ v j where v v j j

(v j

’+1/2)

’= 0,1,2,… are the vibrational quantum numbers

= (1/2 π)(k/µ) 1/2 is the frequency of vibration and k is the bond force constant

• Selection rules: Δv j

= ±1

• This means that in the motion of a polyatomic molecule = motion of N harmonic oscillators, each with their own fundamental frequency v normal modes j vib

=>

• Vibrational state of triatomic molecule represented by (v

1 v

2

– v

1

= symmetric stretch mode, v stretch mode

2

= bending mode, v

3 v

3

)

= asymmetric

– Stretching modes of vibration occur at higher energy than bending modes

• If dipole moment doesn’t change during normal mode motion, that normal mode is infrared inactive.

• Number of IR active normal modes determines number of absorption bands in IR spectrum

• Higher order vibrational transitions lead to frequencies slightly displaced from the fundamental and of much less intensity due to smaller population at higher energy levels.

Rotational Transitions of Polyatomic

Molecules

Approximate as rigid network of N atoms (rigid rotator approximation)

Rotation of a rigid body is dependent on its principle moments of inertia

I xx

=

∑ m j

[(y j

-y cm

) 2 + (z-z cm

) 2 ]

• A set of coordinates can always be found where the products of inertia (I xy

, etc) vanish. The moments of inertia around these coordinates are the principle moments of inertia.

• Spacing between rotational lines described by rotational constants:

A = h / (8 π 2 c I

A

) B = h / (8 π 2 c I

B

) C = h / (8 π 2 c I

C

) where by convention I

A

> I

B

> I

C

• If I

A

• If I

A

• If I

A

If I

A

= 0, I

B

= I

B

= I

B

≠ I

B

= I

= I

C

≠ I

C

≠ I

C

C

=>

=>

=>

=> linear (CO

2

) spherical top (CH symmetric top

4

) asymmetric top (H

2

0, O

3

, N

2

0)

Due to the selection rule

ΔJ = 0, ±1, the rotational band is divided into P (ΔJ = -1), Q

(

ΔJ =0), and R (ΔJ = +1) branches

• A pure rotational transition ( Δv=0) can only occur if molecule has permanent dipole moment

Linear Molecules

• Ia = 0, Ib = Ic .

Erot = BJ ( J +1)

• Centrifugal Distortion Correction for polyatomic molecules (less rigid than diatomic molecules)

= D [ J ( J +1)] 2 + higher terms

Spherical Tops

• I

A

= I

B

= I

C

• Quantum mechanics can solve the energy of a spherical top exactly

• Result: E rot

(J,K) = F(J,K) = BJ(J+1) J = 0,1,2… degeneracy: g

J

= (2J+1)

• Selection rule: ΔJ = 0, ±1

2

• The symmetry of these molecules requires that they do not have permanent dipole moments. This means they have no pure rotational transitions.

• Centrifugal Distortion Correction: D [ J ( J +1)]2

Symmetric tops

• Quantum mechanics can also solve symmetric tops

• Ia = Ib < Ic => oblate symmetric top (pancake shaped)

• Ia < Ib = Ic => prolate symmetric top (cigar shaped)

• Oblate sym top:

E rot

(J,K) = F(J,K) = [BJ(J+1) + (C-B)K 2 ] degeneracy: g

JK

= 2J+1 J = 0,1,2… K = 0,±1,±2... ±J where J = total rotational angular momentum of molecule

K = component of rotational ang. momentum along the symmetry axis

Prolate sym top:

E rot

(J,K) = F(J,K) = [BJ(J+1) + (A-B)K 2 ]

For the sym. top molecules with permanent dipole moments, these dipole moments are usually directed along the axis of symmetry. The following selection rules are assigned for these molecules:

ΔJ = 0 ,±1 ΔK = 0 for K ≠ 0

ΔJ = ±1 ΔK = 0 for K = 0

Where ΔJ = +1 corresponds to absorption and ΔJ = -1 to emission

Asymmetric Tops

• I

A

≠ I

B

≠ I

C

• Schrodinger eqn has no general solution for asymmetric tops

• The complex structure of asymmetric does not allow for a simple expression of their energy levels. Because of this, the rotational spectra of asymmetric tops do not have a well-defined pattern.

Summary of Tuesday

• Atmosphere is composed primarily of N2 and O2 with concentrations in the ppm of greenhouse gases (aside from H20 which varies from 0-2%)

• These GHG (H20, CO2, CH4, O3, N20) have huge impact on the

Earth’s energy budget, effectively increasing temperature of Earth’s surface by ~15 degrees Fahrenheit.

• GHG absorb largely in the infrared region which indicates vibrational and rotational transitions of the molecules upon absorption of a photon

• Vibrational energy levels are greater than rotational by a factor of

√(m/M)

• Vibrational transitions described by fundamental (normal) modes which are determined by number of vibrational degrees of freedom of that molecule: 3N -5 for linear, 3N-6 for nonlinear. Superposition of these normal modes can describe any allowed vibrational state.

• Ex) for triatomic molecule, vibrational state represented by (v

1 where v

1

= symmetric stretch mode, v asymmetric stretch mode

2

= bending mode, v

3

= v

2 v

3

)

• Rotational energy levels determined by principle moments of inertiadivides molecules into four catagories (linear, spherical top, symmetric top, assymetric top). Each has own energy eigenvalues and selection rules.

Rovibrational Energy

• Vibrational and rotational transitions usually occur simultaneously splitting up vibrational absorption lines into a family of closely spaced lines

• Rotational energy also dependent on direction of oscillation of dipole moment relative to axis of symmetry

– When oscillates parallel, ΔJ = 0 transition is forbidden and only P and R branches are seen

– When oscillates perpendicular, P, Q and R branches are all seen

• The rotational constant is not the same in different vibrational states due to a slight change in bond-length, and so rotational lines are not evenly spaced in a vibrational band

Rovibrational transitions in a CO

2 molecule

Diagram taken from Patel (1968)

The Primary Greenhouse

Gases

H

2

0

• Most important IR absorber

• Asymmetric top → Nonlinear, triatomic molecule has complex line structure, no simple pattern

• 3 Vibrational fundamental modes o

H H o symmetric stretch bend v

2

= 6.25

μm asymmetric stretch v

1

= 2.74

μm v

3

= 2.66

μm

• Higher order vibrational transitions (Δv >1) give weak absorption bands at shorter wavelengths in the shortwave bands

• 2 H isotope (0.03% in atm) and 18 O (0.2%) adds new (weak) lines to vibrational spectrum

• 3 rotational modes (J

1

, J

2

, J

3

)

• Overtones and combinations of rotational and vibrational transitions lead to several more weak absorption bands in the NIR

Absorption Spectrum of H

2

O

v

3

=2.66 μm v

1

=2.74 μm v

2

=6.25 μm

CO

2

• Linear → no permanent dipole moment, no pure rotational spectrum

• Fundamental modes: o c o symmetric stretch v

1

= 7.5

μm =>

IR inactive asymmetric stretch v

3

= 4.3 μm bend v

2

= 15 μm bend v

2

• v

• v

2

3 vibration is a parallel band (dipole moment oscillates parallel to symmetric axis), transition ΔJ = 0 is forbidden, no Q branch, greater total intensity than v

2 fundamental vibration is perpendicular band, has P, Q, and R branch

• v

3 fundamental strongest vibrational band but v terrestrial Planck emission functions

2 fundamental most effective due to “matching” of vibrational frequencies with solar and

• 13 C isotope (1% of C in atm) and 17/18 O isotope (0.2%) cause a weak splitting of rotational and vibrational lines in the CO

2 spectrum

IR Absorption Spectrum of CO

2 v

3 v

2

Diagram modified from Peixoto and Oort (1992)

O3

• Ozone is primarily present in the stratosphere aside from anthropogenic ozone pollution which exists in the troposphere

• Asymmetric top → similar absorption spectrum to H

2 configuration (nonlinear, triatomic)

0 due to similar

• Strong rotational spectrum of random spaced lines

• Fundamental vibrational modes o o o symmetric stretch v

1

= 9.01 μm bend v

2

= 14.3

μm o asymmetric stretch v

3

= 9.6

μm

– 14.3 μm band masked by CO2 15 μm band

– Strong v3 band and moderately strong v1 band are close in frequency, often seen as one band at 9.6 μm

– 9.6 μm band sits in middle of 8-12 μm H20 window and near peak of terrestrial Planck function

– Strong 4.7 μm band but near edge of Planck functions

IR Absorption Spectrum of O

3 v1/v3 v2

Diagram taken from Peixoto and Oort (1992)

CH

4

• Spherical top

• 5 atoms, 3(5) – 6 = 9 fundamental modes of vibration

• Due to symmetry of molecule, 5 modes are degenerate, only v

3 fundamentals are IR active

• No permanent dipole moment => No pure rotational spectrum and v

4

• Fundamental modes

H

H

C v

1

H

H

C v

2

C v

3

= 3.3

µm

C v

4

= 7.7

µm

IR Absorption Spectrum of CH

4 v

3 v

4

Diagram taken from Peixoto and Oort (1992)

N

2

O

• Linear, asymmetric molecule (has permanent dipole moment)

• Has rotational spectrum and 3 fundamentals

• Absorption band at 7.8 μm broadens and strengthens methane’s 7.6

μm band.

• 4.5 μm band less significant b/c at edge of Planck function.

• Fundamental modes:

O N N symmetric stretch v

1

= 7.8 μm asymmetric stretch v

3

= 4.5 μm bend v

2 bend v

2

= 17.0

μm

IR Absorption Spectrum of N

2

O

v

3

=4.5 µm v

1

=7.8 µm v

2

=17 µm

Diagram taken from Peixoto and Oort (1992)

Total IR Absorption Spectrum for the

Atmosphere

l b e i s i

V

Diagram taken from Peixoto and Oort (1992)

References

• Bukowinski, Mark. University of California, Berkeley. 21 April 2005.

• Lenoble, Jacqueline. Atmospheric Radiative Transfer. Hampton,

Virginia: A. DEEPAK Publishing, 1993. 73-91, 286-299.

• McQuarrie, Donald A., and John Simon. Physical Chemistry.

Sausalito, California: University Science Books, 1997. 504-527.

• Patel, C.K.N. “High Power Carbon Dioxide Lasers.” Scientific

American. 1968. 26-30.

• Peraiah, Annamaneni. An Introduction to Radiative Transfer.

Cambridge, United Kingdom: Cambridge University Press, 2002. 9-

15.

• Petty, Grant W. A First Course in Atmospheric Radiation. Madison,

Wisconsin: Sundog Publishing, 2004. 62-66, 168-272.

• Thomas, Gary E., and Knut Stamnes. Radiative Transfer in the

Atmosphere and Oceans. Cambridge, United Kingdom: Cambridge

University Press, 1999. 110-120.

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