presentation slides; els 2013

11
Scattering of Palagonite, Mars analog dust, Modeled with Ellipsoids ELS XIV, 17 21 June, 2013, Lille, France Sini Merikallio a , T. Nousiainen a,b , M. Kahnert c,d , A.-M. Harri a a Finnish Meteorological Institute, P.O. Box 503, 00101 Finland, [email protected] B Helsinki University, Finland c Swedish Meteorological and Hydrological Institute, Folkborgsvägen 17, 60176 Norrköping, Sweden d Chalmers University of Technology, 41296 Gothenburg

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Scattering of Palagonite,

Mars analog dust,

Modeled with Ellipsoids

ELS XIV, 17 – 21 June, 2013, Lille, France

Sini Merikallioa, T. Nousiainena,b, M. Kahnertc,d, A.-M. Harria

aFinnish Meteorological Institute, P.O. Box 503, 00101

Finland, [email protected] BHelsinki University, Finland cSwedish Meteorological and Hydrological Institute,

Folkborgsvägen 17, 60176 Norrköping, Sweden dChalmers University of Technology, 41296

Gothenburg

Objectives

1. Testing suitability of ellipsoids to model

mars analog dust particle single scattering

properties. Achieved by comparing to

measured laboratory data.

2. Testing relative

impacts of refractive

index, size and shape distribution.

Measurements by Laan et. al., Icarus 199, 2009

Mars dust

Reff = 1.6 um,

m = 1.5 + 0.002 (1000 nm)

upto 1.5 + 0.015 (320 nm).

@ lambda = 320, 500, 1000 nm

Palagonite

Reff = 4.5 um – 11.1 um,

m = 1.6 + 0.0001i

@ lambda = 632.8 nm

Values from Wolff et. al., JGR 114, 2009

and Wolff et. al. Icarus 208, 2010

Tool: Theory The scattering of an ensemble of randomly oriented

particles can be described by a scattering matrix:

(For spheres: F11 = F22 and F33 = F44)

Stokes vector scattering matrix

in

in

in

in

4434

3433

2212

1211

sc

sc

sc

sc

V

U

Q

I

FF00

FF00

00FF

00FF

V

U

Q

I

Stokes vector

Ellipsoids

• Database of Meng et. al. J. Aerosol. Sci. 41, 2010.

Bi et. Al., Applied Optics 48, 2008

– Same database used for

Earth atmospheric dust.

• How well does it work?

• With what kind of shape distribution?

Shape

distribution

best for each element.

X best for the whole matrix

scattering angle θ scattering angle θ

spheroid best fit, sphere, x Measurements,

individual ellipsoids, ellipsoid best fit

Osa 2 –> move to Mars

Single scattering

albedo ω

Asymmetry

parameter g

Mie Best-Fit Equiprobable n3 n3 spheroids

Mie Best-Fit Equiprobable n3 n3 spheroids

Conclusions

Ellipsoids, even more then spheroids, improve greatly on Mie-models.

Good fits, but different optimal shape distributions for different scattering matrix elements makes it hard to suggest a universally optimal shape distribution.

Study submitted to Optics Express.

Other planets, here we come!

Thank you! [email protected]