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£<br />

¤ ¤ ¢ ¤ ¤<br />

§<br />

¢ ¤<br />

¤ ¤ where is the bubble density and their geometric cross section.<br />

The probability for a pho<strong>to</strong>n of getting <strong>to</strong> the distance after steps is [53]:<br />

where<br />

£<br />

¦<br />

<br />

<br />

<br />

<br />

<br />

¤<br />

<br />

¤ <br />

<br />

<br />

¦<br />

§<br />

<br />

¤ ¤<br />

£<br />

¤ <br />

¦ ¡<br />

<br />

<br />

<br />

¡<br />

<br />

<br />

©¢¡¤£ <br />

¦¥ £ ¨§© © <br />

¡<br />

<br />

¡<br />

©<br />

<br />

¡ <br />

¦ <br />

<br />

¤ ¤<br />

£<br />

¤<br />

¦ is the average cosine of the scattering angle on a bubble, which has a value<br />

where<br />

of 0.75 under the assumption of spherical bubbles.<br />

Finally, the time distribution of an isotropic light source received at a distance £<br />

is obtained by<br />

expressing the path length as a function of time using <br />

¤<br />

<br />

§<br />

¦<br />

¤<br />

©<br />

and multiplying the expression<br />

given in Eq. 43 by an absorption fac<strong>to</strong>r in :<br />

<br />

£ <br />

<br />

<br />

¦<br />

£§<br />

<br />

where © <br />

<br />

, is the absorption ¤ ¤<br />

<br />

<br />

length and is the definition of<br />

the effective scattering length. For a more detailed discussion on the <strong>to</strong>pic, see [54, 55].<br />

¦<br />

<br />

© <br />

¦ © <br />

A first analysis was made on data taken during the 1993-1994 austral summer season, using<br />

a laser <strong>to</strong> send pulses of light with a wavelength of nm through optical fibers ending at<br />

a diffuser near OMs. By fitting time distributions between different such emitters and receivers<br />

(OMs) with the Green’s function of Eq. 45, the parameters © and could be extracted from<br />

the data. This procedure yielded an absorption length © <br />

m and a<br />

¦ <br />

depth dependent scattering length <br />

in the range 12.5-25 ¤ ¤ cm [54].<br />

A further analysis made in the following year [56] and using 10 different wavelengths in the<br />

range 410-610 nm, exhibited the strong wavelength dependence of the absorption length shown<br />

in Fig. 27(a).<br />

It also confirmed the depth behaviour of the scattering length (see Fig. 27(b)) observed in<br />

the previous analysis. An absorption length of 310 m at 380 nm could also be deduced using<br />

the Cherenkov light from atmospheric muons and comparing data time distributions with Monte<br />

Carlo simulation results [57]. The measured absorption lengths were longer than previous measurements<br />

made on ice in the labora<strong>to</strong>ry [58, 59], which can be explained by higher concentrations<br />

of impurities in the preparations.<br />

Eq. 45 is the Green’s function for the ideal case when at most one pho<strong>to</strong>n reaches the pho<strong>to</strong>cathode<br />

where it produces a pho<strong>to</strong>electron. In reality, a large number of pho<strong>to</strong>ns are emitted in a<br />

laser pulse, out of which several can reach the receiving OM. Each of these pho<strong>to</strong>ns is following<br />

the Green’s function, but the times recorded are those of the first leading edge of the first pho<strong>to</strong>n<br />

hitting the cathode. This biases the recorded time distributions <strong>to</strong>wards smaller time values. In<br />

order <strong>to</strong> select distributions where this effect is small, the zero:th class of the Poisson probability<br />

distribution for pho<strong>to</strong>electrons was computed as:<br />

¥<br />

¡ <br />

¦<br />

<br />

<br />

<br />

<br />

¦<br />

§ <br />

<br />

<br />

38<br />

(43)<br />

(44)<br />

(45)<br />

(46)

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