The Physical Environment
                                                       
Contents | Glossary | Atlas |  Index | TPE Today | Blog | Podcast | Google Earth | Search

Chapter Review Questions

Assess your understanding of concepts related to this chapter by answering the questions below. Click the question to reveal the correct answer.
Insolation: highest amount in the tropical/subtropical deserts; minimum at the poles. Net radiation: maximum in the tropical/subtropical oceans; minimum at the poles.
Albedo is the proportion of light reflected from the surface. It is mostly determined by the color of the surface though sun angle influences albedo for some surfaces like water.
The amount of radiation emitted by a body depends on the temperature of the emitting body.
Sun angle is a largely determined by the tilt of Earth's axis. The sun angle varies by latitude, time of day. time of year, and slope of the surface.
A gas that is a selective absorber is one that absorbs only particular wavelengths of light. The gasses of Earth's atmosphere are considered selective absorbers as they tend to allow shortwave solar radiation through but absorbs longwave radiation emitted by the surface. 
Conduction is the heat transfer via molecular collisions. Convection is heat transfer by circulation. Radiation is heat transfer via electromagnetic radiation.
The maximum wavelength of emission depends on the temperature of the emitting body, the hotter the body the shorter the maximum wavelength of emission. The Sun being much warmer than the Earth emits most of its energy in the shortwave end of the electromagnetic spectrum while the Earth emits its energy in the longwave end of the electromagnetic spectrum.
  • March 21 and Sept 23: 0o latitude 
  • June 22: 23.5o North latitude
  • Dec 22: 23.5o degrees South latitude
They block incoming solar radiation reflecting it of their top and back out to space. They diffuse incoming solar radiation as well.
Net radiation is an accounting of incoming and outgoing components of radiation. It also is the amount of energy used to do work in the earth system.
There is a net gain of radiation between about 38o North and South latitude. Poleward of these latitudes there is a net loss of radiation.
There is more latent heat flux in a humid region because there is more water available than in a desert region.

Previous | Continue


Contents |Glossary | Atlas Index  |  Blog | Podcast | Google Earth | Search Updates | Top of page

About TPE | Who's Used TPE |  Earth Online Media

Please contact the author for inquiries, permissions, corrections or other feedback.
Michael Ritter (tpeauthor@mac.com)

For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography.
Date visited.  ../title_page.html

Help keep this site available by donating through PayPal.

paypal

Creative Commons License
Unless otherwise stated, this work is licensed under a
Creative Commons Attribution-ShareAlike 4.0 International License