Consider this scenario: As temperatures in high latitudes get colder, snow and ice accumulate As snow and ice accumulate, more solar radiation is reflected As more solar radiation is reflected, less energy is stored so temperature gets even colder Is this an example of positive feedback, negative feedback or lack of feedback?
Consider this scenario: As temperatures in high latitudes get colder, snow and ice accumulate As snow and ice accumulate, more solar radiation is reflected As more solar radiation is reflected, less energy is stored so temperature gets even colder Is this an example of positive feedback, negative feedback or lack of feedback?
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Consider this scenario:As temperatures in high latitudes get colder, snow and ice accumulateAs snow and ice accumulate, more solar radiation is reflectedAs more solar radiation is reflected, less energy is stored so temperature gets even colderIs this an example of positive feedback, negative feedback or lack of feedback?
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Step 1
This scenario is an example of ice-albedo feedback. As temperatures in high latitudes decreases, it increases the accumulation of snow and ice. This accumulation increases the reflection of solar radiation. It leads to more cooling.
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