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Snowed Out: Lake-Effect Snow and the Creek Cleanup worksheet preview

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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

MS-ESS2-5

Use data on moving air masses to explain how they cause changes in weather.

Preview

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Name Date

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.

7 a.m. Saturday, Wind From the West at All Stations
StationWhereAir temp (°C)Water vapor (g/kg)Snow, last 12 h (cm)
West endWest shore of the lake−81.60
Lake buoyMiddle of the lake−52.4not measured
Cattail CreekEast shore−4328
Hill town25 km inland, 400 m higher−62.446
Far inland110 km inland−81.82
1.

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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