la T s Crocus et la T s ERA-i sont préalablement filtrées selon la présence des données MODIS. L'amplitude MODIS, l'amplitude Crocus et l'amplitude ERA-i s'appuient donc sur les mêmes instants horaires. La figure 5.8 compare l'amplitude Crocus médiane et l'amplitude ERA-i médiane à l'amplitude MODIS médiane sur l'ensemble de la période, ), pendant l'hiver (juin, juillet et août), 2000. ,
ERA-i est en grande partie la conséquence d'une mauvaise reproduction de la variabilité de la T s en hiver avec la T s ERA-i qui présente un biais chaud dû à une surestimation du flux de chaleur sensible lors de conditions atmosphériques stables (Figure 3.10) Crocus étant forcé en entrée par la vitesse du vent à 10 m d'ERA-Interim, la sous-estimation de l'amplitude Crocus en hiver peut s'expliquer par la sous-estimation, 2013. ,
amplitude diurne entre Crocus et ERA-Interim se retrouvent sur l'ensemble du domaine, alors que Crocus est forcé en entrée par les données ERA-Interim. A titre d'exemple, en été, l'amplitude maximale simulée par ,
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Description schématique des différents types de métamorphoses conduisant à la formation des principaux types de neige saisonnière, identifiés selon l'ancienne classification internationale de la neige, p.13, 1990. ,
(gauche) mesure de la densité d'échantillons de neige prélevés en surface ; (droite) mesure d'un profil de densité, p.29, 2014. ,
(e) Pole of inaccessibility (AWS13), (f) Princess Elisabeth station (AWS16), (g) Dome C in 2009 and (h) Dome C in 2012. « Pole of I.» means Pole of Inaccessibility and « Pr Elisabeth » means Princess Elisabeth. The number N of simultaneous MODIS T s and in situ T s used in the evaluation primarily depends upon satellite overpasses and cloudiness, AWS stations, N also depends upon the filter used to, p.48 ,
South Pole, (e) Plateau Station B and (g) Pole of Inaccessibility. Same comparisons but only when MODIS T s are available at the same time : (b) Dome C,(d) South Pole, (f) Plateau Station B and (h) Pole of Inaccessibility. The green line represents the 1 :1 line, p.52 ,
T s MODIS (ligne bleue), T s L2 IASI (point rouge), T s retsituée IASI (point vert) et (bas) du rayonnement thermique infrarouge LW down BSRN à Dôme C pour les mois de (a) novembre 2009, (b) décembre 2009 et (c) janvier 2010. La figure (d) est un zoom sur la période, p.75, 2009. ,
T s MODIS (ligne bleue), T s L2 IASI (point rouge), T s retsituée IASI (point vert) et (bas) du rayonnement thermique infrarouge LW down BSRN à Pôle Sud pour les mois de (a) novembre La figure (d) est un zoom sur la période 22 au 29 décembre, p.76, 2009. ,
calculées à partir de la T s MODIS sur la période du 3 juillet au 31 août 2013 : (a)(d) T s ARPEGE, (b)(e) T s IFS et (c)(f) T s, p.79 ,
10 janvier (transect n°1) et (b) le 13 janvier 2015 (transect n°2) La moyenne glissante de la T s est calculée sur différent intervalles : 200 m, 400 m, 1000 m et, p.91, 2000. ,
La T s MODIS pluri-annuelle est calculée en moyennant sur la période 2000-2013 la T s MODIS de chaque heure de chacun des jours d'une année. La moyenne journalière pluriannuelle de la T s MODIS est calculée en moyennant sur la période 2000-2013 la T s MODIS de chaque jour d'une année, p.96, 2000. ,
du SW down BSRN (jaune) et du LW down BSRN rouge à Dôme C entre le 11 décembre, p.97, 2009. ,
L'été regroupe les mois de novembre, décembre, janvier et février, p.102 ,
Série temporelle de la T s in situ mesurée sur une surface de densité faible (? = 149 kg m ?3 ) (rouge) et de la T s in situ sur une surface de densité forte (? > 500 kg m ?3 ) (noir), p.107 ,
Série temporelle de la T s in situ mesurée sur une surface de densité faible (? = 149 kg m ?3 ) (rouge) et de la T s in situ sur une surface de densité forte (? > 500 kg m ?3 ) (noir) ,
Série temporelle de la T s Crocus simulée à partir de différentes valeurs de forçage ERA-Interim du SW down entre le 1 er et le 4 novembre, p.109, 2009. ,
149 kg m ?3 ) (pointillé rouge), de la T s in situ mesurée sur une surface de densité forte (? > 500 kg m ?3 ) (pointillé noir) et de la T s Crocus à densité fixée entre 50, situ mesurée sur une surface de densité faible, p.115 ,
700 kg m ?3 calculé à partir (a) de la T s in situ mesurée sur une surface de densité ? > 500 kg m ?3 et (b) à partir de la T s in situ mesurée sur une surface de densité ? = 149 kg m ?3, p.116 ,
149 kg m ?3 ) (pointillé rouge), de la T s in situ mesurée sur une surface de densité forte (? > 500 kg m ?3 ) (pointillé noir) et de la T s Crocus à densité fixée entre 50, situ mesurée sur une surface de densité faible, p.117 ,
700 kg m ?3 calculé à partir (a) de la T s in situ mesurée sur une surface de densité ? > 500 kg m ?3 et (b) à partir de la T s in situ mesurée sur une surface de densité ? = 149 kg m ?3, p.118 ,
Rayonnement thermique descendant BSRN et (b) vitesse du vent BSRN entre le 17 novembre, p.124, 2009. ,
Biais de l'amplitude médiane Crocus en fonction de la densité pour différents forçages (a) de la vitesse du vent, (b) du flux radiatif SW down et (c) de la vitesse du vent et du flux radiatif SW down à, p.128 ,
(g) Pole of inacessibility et (i) Princess Elisabeth en Même comparaisons en été (NDJF) : (b) Pôle Sud, (d) Kohnen, (f) Plateau Station B, (h) Pole of inacessibility et (j) Princess Elisabeth . Ces comparaisons s'effectuent sur l'ensemble des valeurs quotidiennes d'amplitude diurne en, p.139, 2009. ,
ligne bleue) et de l'amplitude médiane mensuelle MODIS (pointillé bleu) en 2009 à (a) Pôle Sud, c) Plateau Station B, (d) Pole of Inacessibility et (e) Princess Elisabeth. . . . . . . . . . . . 141 ,
hiver (JJA) et en été (NDJF) calculée sur la période 2000-2012. (d)(e)(f) Idem pour les amplitudes Crocus. (g)(h)(i) Idem pour les amplitudes, p.148 ,
La sensibilité est déterminé à partir de l'amplitude Crocus médiane estivale (NDJF) sur la période, p.152, 2000. ,
550 kg m ?3 et (g) 700 kg m ?3, p.153 ,
NDJF) en fonction de la densité sur la période novembre-février entre 2000 et 2012 selon différentes stations : Dôme C, Pôle Sud, Biais de l'amplitude Crocus médiane estivale, p.154 ,