Weather Balloons and Atmospheric Processes

Weather Balloons and Atmospheric Processes

Assessment

Interactive Video

Geography

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video tutorial explores the mechanisms that lead to rain formation, focusing on the role of rising air masses, cooling, and condensation. It explains lapse rates and how they are measured using weather balloons. The tutorial also covers different lifting mechanisms, such as orographic lifting, and their impact on precipitation, including the rain shadow effect observed in mountainous regions.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary reason rising air masses lead to precipitation?

They increase in density.

They cool and reach dew point temperatures.

They absorb more sunlight.

They become warmer as they rise.

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which process is responsible for summer thunderstorms?

Radiative heating

Adiabatic cooling

Evaporative cooling

Orographic lifting

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How is the lapse rate defined?

Change in humidity with elevation

Change in temperature with elevation

Change in pressure with elevation

Change in wind speed with elevation

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the dry adiabatic lapse rate approximately?

1.5°C per 100 meters

0.5°C per 100 meters

2°C per 100 meters

1°C per 100 meters

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where can data for determining the local lapse rate be obtained?

Local weather stations

University of Wyoming's website

National Oceanic and Atmospheric Administration

Local meteorological offices

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to a weather balloon at its maximum elevation?

It remains stationary.

It bursts and falls back to Earth.

It continues to rise indefinitely.

It descends slowly without bursting.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the orographic effect?

The increase in humidity on the leeward side of a mountain

The cooling of air as it rises over a mountain

The warming of air as it descends a mountain

The decrease in wind speed over a mountain

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