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prevails farther downstream over the central and eastern Pacific. Over the western Atlantic, the shear distribution is almost symmetrical. Further downstream the shear is in general very weak and anticyclonic except over the eastern Mediterranean (contours not shown). At 320 K, the shear asymmetry over the western Pacific has changed in favor of anticyclonic shear. Over the western Atlantic, the shear distribution is almost symmetrical. At higher levels (330, 340 K), there is a general asymmetry of the
prevails farther downstream over the central and eastern Pacific. Over the western Atlantic, the shear distribution is almost symmetrical. Further downstream the shear is in general very weak and anticyclonic except over the eastern Mediterranean (contours not shown). At 320 K, the shear asymmetry over the western Pacific has changed in favor of anticyclonic shear. Over the western Atlantic, the shear distribution is almost symmetrical. At higher levels (330, 340 K), there is a general asymmetry of the
