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Fog, Rain and a Warm Front at the Ferry Dock
Grade 6 earth science: analyze a ferry dock weather log and air pressure data to explain how an arriving warm, humid air mass changed a coastal town's weather.
Grade 6ScienceInteractive · Printable
Aligned toMS-ESS2-5
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What’s included
- Single worksheet
- Auto-graded online
- 1 NGSS standard
- Printable answer key
- 11 questions
- Classroom-ready
Details
- Format
- Interactive · Printable
- Grade
- Grade 6
- Subject
- Science
- Question types
- Fill in the blank, Multiple choice, Circle the answer, Short answer
About this worksheet
What students practice
- Students use weather data to find when a warm air mass replaced a cool one.
- Students use pressure differences to predict which way air moves and where wind is stronger.
- Students interpret a weather forecast given as a probability.
How to use
Read the passage together and point out each column of the log. Students then work through the sections and use log data in their final explanation.
Curriculum
NGSS standard covered
Use data on moving air masses to explain how they cause changes in weather.
Preview
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Fog, Rain and a Warm Front at the Ferry Dock
Use a harbor weather log and pressure data to explain how a new air mass changed the weather.
The dock weather log
Read the passage and study the dock log. Then answer the questions.
A Foggy Thursday at Osprey Harbor
1Osprey Harbor is a fishing and ferry town on the Atlantic coast of the United States, with open ocean to its south and east. Each spring, the harbor master, Mr. Obi Mensah, lets members of the Bayside Middle School sailing club help read the weather instruments on the ferry dock. The ferry to Long Gull Island crosses only when the captain can see far enough ahead, so the dock crew watches the weather closely.
2Large bodies of air called air masses take on the temperature and moisture of the places where they form. Air that forms over cool land in spring is often cool and fairly dry. Air that forms over warm ocean water far to the south is usually warm and humid. Warm air is less dense than cool air. When air rises, it cools, and when humid air cools, some of its water vapor can condense into clouds, drizzle or rain. A front is the boundary where two air masses meet.
3On Wednesday night, a cool air mass sat over the harbor, and the forecast showed a warm, humid air mass over the ocean to the south, moving slowly north. On Thursday, club member Iris Lindqvist copied the dock readings every three hours. The morning felt chilly. By early afternoon, a gray, steady rain had been falling for hours and thick fog hid the island. In the evening the fog began to lift, and the air felt warm and sticky, even though the Sun had already set.
4Mr. Mensah also showed Iris how wind is linked to air pressure. Near the ground, air tends to flow from places with higher pressure toward places with lower pressure. When the pressure changes a lot over a short distance, the wind is usually stronger. At noon, he checked the pressure at a weather buoy out at sea and at an airport inland, both on a straight east–west line through the harbor.
| Time | Temp (°C) | Humidity (%) | Pressure (hPa) | Wind from | Weather |
|---|---|---|---|---|---|
| 6 a.m. | 8 | 65 | 1019 | East | High thin clouds |
| 9 a.m. | 9 | 78 | 1015 | East | Low gray clouds |
| Noon | 10 | 92 | 1010 | East | Steady rain |
| 3 p.m. | 11 | 97 | 1006 | Southeast | Drizzle, thick fog |
| 6 p.m. | 18 | 90 | 1005 | South | Cloudy, fog lifting |
| 9 p.m. | 19 | 88 | 1006 | South | Mostly cloudy |
- A. 6 p.m. and 9 p.m.
- B. 6 a.m. and 9 a.m.
- C. Noon and 3 p.m.
- D. 3 p.m. and 6 p.m.
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