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Cloud Statistics from Calipso Lidar Data for the ... - espace-tum.de

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Chapter 5. <strong>Cloud</strong> free statistics 54<br />

(a)<br />

60°N<br />

30°N<br />

0°<br />

3600<br />

3200<br />

2800<br />

2400<br />

2000<br />

1600<br />

30°S<br />

60°S<br />

180° 135°W 90°W 45°W 0° 45°E 90°E 135°E<br />

180°<br />

(b)<br />

(c)<br />

1200<br />

800<br />

400<br />

0<br />

1000<br />

4000<br />

Mean cloud gap length [km]<br />

100<br />

10<br />

1<br />

Global mean cloudless fraction 40.5 %<br />

Global mean cloud gap length 7.41 km<br />

0.0 0.2 0.4 0.6 0.8 1.0<br />

Mean cloudless fraction<br />

(d)<br />

Total number of measurements<br />

1000<br />

100<br />

250 measurements 98.9 %<br />

500 measurements 82.2 %<br />

1000 measurements 34.2 %<br />

10<br />

0.0 0.2 0.4 0.6 0.8 1.0<br />

Mean cloudless fraction<br />

60°N<br />

30°N<br />

0°<br />

30°S<br />

60°S<br />

50<br />

45<br />

40<br />

35<br />

30<br />

25<br />

20<br />

15<br />

10<br />

5<br />

180° 135°W 90°W 45°W 0° 45°E 90°E 135°E<br />

180°<br />

Figure 23: Total number (a) and <strong>the</strong>ir respective mean length (b) of cloud gaps<br />

<strong>for</strong> <strong>the</strong> complete data set of 2007 on a 2 ◦ x 2 ◦ grid. As shown in (a) <strong>the</strong> amount<br />

of pure cloud gaps dominates over <strong>the</strong> tropic and subtropic ocean regions, while <strong>the</strong><br />

mean cloud gap length in km (d) has its maximum above <strong>the</strong> global <strong>de</strong>serts and high<br />

mountain ranges. To support this statement, (b), on <strong>the</strong> one hand shows that <strong>for</strong> a<br />

high cloudless fraction, <strong>the</strong> mean cloud gap length rises, but on <strong>the</strong> o<strong>the</strong>r hand very<br />

few measurements are available <strong>for</strong> regions with a high cloudless fraction (c).

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