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Fourth Study Conference on BALTEX Scala Cinema Gudhjem

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3. Image Calibrati<strong>on</strong><br />

The images required very accurate navigati<strong>on</strong> data sets of<br />

both Helipod and Tornado. Beside the measurement of<br />

positi<strong>on</strong> and attitude it was necessary to make assumpti<strong>on</strong>s<br />

about the internal algorithms that c<strong>on</strong>trol the aperture stop of<br />

the Tornado IR camera. So after recalculati<strong>on</strong> of the images<br />

horiz<strong>on</strong>tal shift, deformati<strong>on</strong>, and n<strong>on</strong>-uniform exposure, a<br />

proper calibrati<strong>on</strong> of the image gray scale with the surface<br />

temperature (Helipod measurements) became feasible (Fig.<br />

5 and 6). A detailed descripti<strong>on</strong> of these algorithms will be<br />

published so<strong>on</strong>.<br />

Fig. 5: Tornado image c<strong>on</strong>taining two Helipod flights.<br />

Fig. 6: Same as Fig. 5, after the calibrati<strong>on</strong>. The color<br />

scale covers temperatures between 19° C (forest) and<br />

63° C (roofs).<br />

-40-<br />

4. Results and C<strong>on</strong>clusi<strong>on</strong>s<br />

Since the Tornado IR camera used analog technique<br />

(chemical films) the spatial resoluti<strong>on</strong> is in the order of a<br />

meter or (depending <strong>on</strong> aircraft's altitude) even better. The<br />

first impressive result of the analysis of these<br />

photographies is that the heterogeneity of the experimental<br />

site was much str<strong>on</strong>ger than assumed by the numerical<br />

models used so far. Especially the influence of the water<br />

c<strong>on</strong>tent of different soil types is clearly visible. But even<br />

in a uniformly planted field the temperature variati<strong>on</strong>s<br />

were large due to the varying water c<strong>on</strong>tent of the soil.<br />

The measurements at several ground stati<strong>on</strong>s give the<br />

opportunity for data quality c<strong>on</strong>trol and cross-validati<strong>on</strong>.<br />

The deviati<strong>on</strong> from ground-based measurements was<br />

always smaller than 2 K. The temperature accuracy of the<br />

calibrated images (in comparis<strong>on</strong> with the Helipod data)<br />

was better than 2 K in 95 % of all properly calibrated<br />

images. Some images (marked with an 'I' in Fig. 7) show<br />

systematic temperature bias due to a lack of absolute<br />

temperature measurements.<br />

Fig. 7: Calibrated temperature map of the LITFASS-<br />

2003 experimental site.<br />

Acknowledgments<br />

We are deeply grateful to the 51st rec<strong>on</strong>naissance<br />

squadr<strong>on</strong> (AG 51) 'Immelmann' of the German Air Force<br />

in Jagel. We are much obliged to the crew of the FJS<br />

Helicopter Service in Damme (Germany). The Helipod<br />

flights were funded by the German government (BMBF:<br />

EVA-GRIPS within DEKLIM, grant no. 01-LD-0301<br />

References<br />

Bange J. and Roth R.: Helicopter-Borne Flux Measurements<br />

in the Nocturnal Boundary Layer Over Land - a<br />

Case <str<strong>on</strong>g>Study</str<strong>on</strong>g>. Boundary-Layer Meteorol., 92, 295-325,<br />

1999.<br />

Bange J., Beyrich F., and Engelbart D.A.M.: Airborne<br />

Measurements of Turbulent Fluxes during LITFASS-<br />

98: A Case <str<strong>on</strong>g>Study</str<strong>on</strong>g> about Method and Significance.<br />

Theor. Appl. Climatol., 73, 35-51, 2002.

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