• Aucun résultat trouvé

The North Atlantic variability structure, storm tracks, and precipitation depending on the polar vortex strength

N/A
N/A
Info
Télécharger
Protected

Academic year: 2021

Partager "The North Atlantic variability structure, storm tracks, and precipitation depending on the polar vortex strength"

Copied!
23
0
0

Chargement.... (Voir le texte intégral maintenant)

Texte intégral

Figure

Figure 1: Teleconnectivity of the 15-day low pass filtered geopotential height of the 300-hPa level in December to March from 1958 to 1998
Fig. 2. As in Fig. 1, but for 15-day low pass filtered data at the 1000 hPa level. The isoline interval is 0.05
Fig. 3. Composites of the positive (left) and negative (right) of the index of eastern NA-WVR pattern: (a), (b) monthly rms of bandpass filtered 500 hPa geopotential height, (c), (d) precip-itation rate (mm/d)
Fig. 4. As Fig. 3, but for western NA-WVR.

Références

Télécharger maintenant ( PDF - 23 Page - 1.18 MB )

Documents relatifs