A Tuesday in October
1The weather club at Ridgeview Middle School, in the central United States, runs a small weather station on the roof. It records temperature, humidity, air pressure in hectopascals (hPa), and the direction the wind blows from. On Monday night, club members saw an alert on their forecast app: a cold front was moving east across the region and would reach the school on Tuesday.
2Large bodies of air called air masses take on the temperature and moisture of the places where they form. Air that sits over the warm Gulf of Mexico usually becomes warm and humid. Air that forms over central Canada in fall is usually cold and dry. Cold air is denser than warm air. When air is pushed upward, it cools, and when humid air cools, some of its water vapor can condense into clouds and rain. A front is the boundary where two air masses meet.
3On Tuesday, club member Keisha Morgan copied the station's readings every three hours. Around 4 p.m., a line of thunderstorms swept over the school with gusty wind and heavy rain for about 30 minutes. At lunch the air had felt warm and sticky, with a steady breeze from the south. By the time Keisha walked home that evening, the air felt crisp and she was glad she had brought a jacket.
4The club also checked two other weather stations on a straight east–west line through the school. Westfield is 90 km west of the school and Eastbrook is 60 km east. At each station, the club found the time when the wind suddenly turned to blow from the northwest.