Absorption and Radiation by Land and Water The purpose of this lab report is to investigate the differences in absorption and radiation properties between land and water. The experiment involved measu

Absorption and Radiation by Land and Water

The purpose of this lab report is to investigate the differences in absorption and radiation properties between land and water. The experiment involved measuring the absorption and radiation of heat by land and water samples exposed to a light source. The results demonstrated distinct variations in the absorption and radiation characteristics of land and water due to their differing physical properties. These findings contribute to a better understanding of the Earth's energy balance and the role of land and water in influencing climate patterns.

Methods:

Experimental Setup:

Two identical containers were filled with equal amounts of water.

A heat source, such as an incandescent lamp, was placed equidistant from both containers.

Thermometers were inserted into the water and the surrounding air to measure temperature changes.

Data Collection:

The initial temperature of the water and the surrounding air was recorded.

The heat source was turned on, and the experiment was conducted for a specified duration.

Temperature measurements of the water and air were recorded at regular intervals.

The experiment was repeated using land samples, such as soil or sand, instead of water.

Calculation:

The change in temperature for each sample was calculated by subtracting the initial temperature from the final temperature.

The absorbed heat was determined by subtracting the temperature change of the surrounding air from that of the sample.

The radiation properties were compared by analyzing the rate of temperature increase and decrease.

Results:

The water sample showed a slower rate of temperature increase compared to the land sample.

The water sample also displayed a slower rate of temperature decrease after the heat source was turned off.

The land sample exhibited a higher rate of temperature increase and decrease compared to the water sample.

The temperature change of the air surrounding the water sample was lower than that surrounding the land sample.