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J. Korshover and J. K. Angell

usual area in the Southeast (Fig. 2). Stagnationoccurred between 22 and 26 May, as a cool polar airmass settled over the southern and eastern part of thecountry, following the northeastward movement ofan East Coast low. Fog was common in the southeastern states during this period. The flow at 50 kPawas weak from the northwest, west and southwest,respectively.FIG. 3. As in Fig. 1, but for June. The one stagnation case in June was centered inAppalachia, slightly north of the usual location forthis

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