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2.3. RADIATIVE TRANSFER 49<br />
2.3.2 Oxygen A-band measurements for solar photon path length distribution<br />
studies<br />
Participating scientists Scholl, T., and K. Pfeilsticker<br />
Abstract High resolution spectroscopy of the oxygen A-band (760-780 nm) in zenith scattered<br />
skylight is a powerful tool to infer path length distributions (PDF) of solar photons transmitted to<br />
the ground. The relation between the different moments of the PDF (〈L〉, 〈L 2 〉) and the rescaled<br />
cloud optical depth τ ∗ is a strong indicator for 3D-effects on the radiative transfer (RT).<br />
Height [m]<br />
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Figure 2.21: left panel: Measured radar reflectivities from KNMI 35 GHz Radar for May 22, 2003 UT 12:00-<br />
13:00, right panel: Mean cloud photon paths 〈Lc〉 as a function of effective cloud optical depth τ ∗ c . The black<br />
lines are predictions for different values of the Lévy exponent α ≤ 2. The 3 data clusters (color-coded blue,<br />
red and green) correspond to the 3 different probed cloud situations.<br />
Background Modelling RT in cloudy skies is<br />
one of the most challenging tasks in climate modelling.<br />
Photon PDF is commonly a hidden property<br />
of standard RT models, controlled by the<br />
spatial distribution of scattering and absorption.<br />
The distribution in the near infrared region is<br />
very representative for the shortwave region as<br />
a whole. The principle of equivalence allows to<br />
draw conclusions about radiative properties of<br />
the atmosphere from a photon PDF measured in<br />
one wavelength band, since the scattering properties<br />
of clouds and aerosols vary slowly and predictably<br />
with wavelength. Here the first two moments<br />
of the photon PDF of solar photons transmitted<br />
through cloudy skies to the ground are<br />
investigated. Combining the spectroscopic measurements<br />
with other cloud properties measured<br />
simultaneously by in-situ techniques during two<br />
campaigns allows to test the theory of anomalous<br />
photon diffusion through clouds.<br />
Methods and Results The multiple of different<br />
line strengths offered by the oxygen A-band<br />
implicitly provide direct information on the PDF<br />
of the photons transmitted to the ground. The<br />
spectral retrieval is solved by forward modelling<br />
the measured spectra with a prescribed photon<br />
PDF (usually a Γ function) at high spectral resolution.<br />
The free parameters of the PDF are<br />
then iteratively calculated by using a Nonlinear<br />
Least Square Fit leading to the searched quantities<br />
〈L〉 and 〈L 2 〉. Davis & Marshak [2002]<br />
inferred for the first moment of photon PDF:<br />
〈Lc〉/∆H = (1/2 · [1 + C(ɛ)] · τ ∗ ) α−1 . α is the so<br />
called Lévy index which ranges between 1 and 2.<br />
In particular, the value α = 2 is attained for a homogenous<br />
slab and for α < 2 for inhomogeneous<br />
slab. In Figure 2.21 the enhancement of the mean<br />
photon path length in the cloud (as a function of<br />
τ ∗ = τ · (1 − g)) and the received Lévy index is<br />
shown.<br />
The findings confirm the theory of anomalous<br />
photon diffusion through clouds and the predictions<br />
for the values in the path length to optical<br />
depth relations. It also provides further evidence<br />
that cloudy sky photon path length require consideration<br />
of non-classical photon transport theory.<br />
Funding comes through the AFO-2000 4D<br />
Clouds project (BMBF-07ATF24).<br />
Outlook Photon PDFs are a central concept of<br />
cloud RT modelling. For further improvements<br />
imaging DOAS spectroscopy at high temporal and<br />
spatial resolution is required.<br />
Main publication Scholl, T., Photon path<br />
length distributions for cloudy skies: Their first<br />
and second-order moments inferred from high resolution<br />
oxygen A-Band spectroscopy, PhD-Thesis,<br />
<strong>Universität</strong> Heidelberg, Heidelberg, in preparation.