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Snowed Out: Lake-Effect Snow and the Creek Cleanup
Grade 6 earth science: station readings across Lake Erie show how a cold, dry air mass picked up heat and moisture and caused lake-effect snow.
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
- 10 questions
- Classroom-ready
Details
- Format
- Interactive · Printable
- Grade
- Grade 6
- Subject
- Science
- Question types
- Fill in the blank, Multiple choice, Circle the answer, Sorting, Short answer
About this worksheet
What students practice
- Students analyze station data to describe how an air mass changed as it crossed a lake.
- Students explain how a cold air mass moving over warmer water caused heavy snow downwind.
- Students use an hourly weather log to explain why the snow stopped and predict a change.
How to use
Read paragraphs 1 and 2, then trace the wind's path across the station table from west to east before students answer. The hourly log is for Section 2.
Curriculum
NGSS standard covered
Use data on moving air masses to explain how they cause changes in weather.
Preview
OwlSheets.com
Snowed Out: Lake-Effect Snow and the Creek Cleanup
Use station data to explain how a lake changed a cold air mass.
Saturday morning across the lake
Read the passage and the station table. Then answer the questions.
A Cleanup on Hold
1The Cattail Creek Stewards, a volunteer group from Lakeview Middle School, planned to pick up trash along their creek on a Saturday in mid-November. Cattail Creek winds through a town on the eastern shore of Lake Erie and empties into the lake. The town and its weather stations are made up, but the weather they show is common there in late fall. On Friday evening, group leader Mr. Tomasz Brzezinski sent a message: the forecast called for "lake-effect snow" overnight.
2An air mass takes on the temperature and humidity of the place where it forms. Behind a cold front, a cold, dry air mass from central Canada had spread over the Great Lakes, and the wind was blowing from the west, along the length of Lake Erie. In November, the lake water still holds heat from the summer. On Saturday morning, the water near the lake buoy was 10 °C.
3Sixth grader Lena Kowalczyk woke up to deep snow. At 7 a.m. she looked up the readings from five stations that lie in a line from west to east, along the path of the wind. One reading shows how much water vapor the air held, in grams of water vapor in each kilogram of air (g/kg).
4Lake-effect snow usually falls in long, narrow bands, often 10 to 40 km wide, that line up with the wind. Under a band, snow can pile up quickly, while a town just outside it may see sunshine. Lena kept an hourly log at the creek for the rest of the day.
| Station | Where | Air temp (°C) | Water vapor (g/kg) | Snow, last 12 h (cm) |
|---|---|---|---|---|
| West end | West shore of the lake | −8 | 1.6 | 0 |
| Lake buoy | Middle of the lake | −5 | 2.4 | not measured |
| Cattail Creek | East shore | −4 | 3 | 28 |
| Hill town | 25 km inland, 400 m higher | −6 | 2.4 | 46 |
| Far inland | 110 km inland | −8 | 1.8 | 2 |
Compared with the air at the west end, each kilogram of air at Cattail Creek held g more water vapor and was °C warmer.
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