51.   Onshore breezes will direct cool air with spotty showers into the western Washington.

52.   Onshore breezes will direct damp air inland across much of New England and parts of the Middle Atlantic States.

53.   Robust high pressure systems are crucial to a snowstorm because they direct cold air south from Canada.

54.   Slow-moving low pressure west of Oregon will continue to direct moist air toward northern California and southern Oregon.

55.   Strengthening breezes from the southwest will direct milder air into the Midwest and western Great Lakes.

56.   Sultry weather from the South will direct tropical air into the Middle Atlantic region.

57.   The clockwise circulation around this fair weather system will direct warmer air from the Plains toward the Middle West.

58.   The clockwise circulation of air around these highs directs air westward toward the California coast.

59.   The high pressure responsible for the chilly air mass will direct cold air with scattered showers into the central and Northern Plains.

60.   The unusual chill in the South is due to an active jet stream which has directed Canadian air to the Gulf Coast.