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Ice supersaturation as seen from TOVS

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Figure

Fig. 1. Map of the frequency of occurrence of ice supersaturation in the TOVS UTHi product obtained from HIRS/2 channel 12 radiance which is sensitive to altitudes between about 300 and 500 hPa.
Fig. 2. Non-normalised statistical distribution of UTHi (solid) derived from HIRS/2 channel 12 data via the algorithm of Eqs
Fig. 3. Non-normalised statistical distribution of the inverse reference pressure 1/P H in ice supersaturated regions
Fig. 4. Non-normalised statistical distribution (solid line) of the brightness temperature in HIRS/2 channel 12, T 12 , for soundings indicating supersaturation (U i > 100%), and where the inverse reference pressure is between 0.52 and 0.67
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