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L. Médiane, La médiane M est la valeur pour laquelle 50 % des valeurs testées sont en dessous de ce seuil et 50 % au dessus. Elle peut aussi s'appeler percentile 50. C'est la valeur centrale par excellence. Pour la calculer il faut savoir si l'échantillon est pair ou impair

@. Un, angle zénithal proche de 55°, cinq pixels présentant l'anomalie thermique à une température de 295°K et température de l'arrière plan à 279°K

@. Un and . Fort, angle zénithal de inférieur à 1°, cinq pixels présentant l'anomalie thermique à une température de 500°K et température de l'arrière plan à 279°K

@. Un and . Fort, angle zénithal proche de 55°, cinq pixels présentant l'anomalie thermique à une température de 500°K et température de l'arrière plan à 279°K

. Wh and . Vh, mass", omega["air"]); field fh (Vh, 0.); field one (Vh, 1.); branch event

F. L_over_h and =. Omega, xmax()[0]; cerr << "# n tau_moy tau_int << endl; for (size_t n = 1; n <= n_max; n++) { field tau_air = gamma_air*tau_h

E. Du-sommet-la-de-la-topographie-du-cratère-dolomieu, Les différents MNE créés ne permettent pas tous d'obtenir des profils fiables, car nombre d'entre eux présentent de forts artéfacts en raison du relief et des faibles réflectances. Il a été possible d'obtenir trois profils avec les MNT qui ont servi de base de référence (Figure 5-3): ? Un ante effondrement de, ANNEXE, vol.8, 2007.

. Michon, b) Les modèles créés ne permettent pas seulement de suivre l'évolution de la topographie récente, Ces études viennent en complément de celles qui ont été réalisées par Villeneuve, 2000.