McKnight's Physical Geography: A Landscape Appreciation (12th Edition)
McKnight's Physical Geography: A Landscape Appreciation (12th Edition)
12th Edition
ISBN: 9780134195421
Author: Darrel Hess, Dennis G. Tasa
Publisher: PEARSON
Question
Book Icon
Chapter 9, Problem 1LC
To determine

To explain: Whether the amount of precipitation and evapotranspiration over the continents the same or not.

Expert Solution & Answer
Check Mark

Answer to Problem 1LC

The amount of precipitation and evapotranspiration are not the same over the continents, rather the precipitation amount goes beyond the amount of evapotranspiration.

Explanation of Solution

Of the total precipitation falling on the Earth, only 22percent reaches the continents while the rest 78percent reaches the oceans. The precipitation falling on the continents undergoes complex series of processes. The water may runoff to the lakes, streams or rivers, infiltrate into the ground and rest goes to the atmosphere through evaporation and transpiration.

The water infiltrated may else be stored as soil moisture or penetrates to even more depth to become a part of the groundwater. The groundwater would appear again on the surface as springs and the soil moisture would ultimately transpire or evaporate into the atmosphere.

If taken on a global scale including both the oceans and land surface the rate of precipitation and evapotranspiration is in balance. But if the continents alone are considered, precipitation surpasses evapotranspiration and vice versa in the case of oceans. The advectional movement of moist marine air onto the land surfaces creates this imbalance between the precipitation and evapotranspiration on continents.

Want to see more full solutions like this?

Subscribe now to access step-by-step solutions to millions of textbook problems written by subject matter experts!
Students have asked these similar questions
SOUTH Judith River Eagle Warm Mowry Shak Kooter Thermope Jurassic Ellis Seyenite Porphry Metamorphic Rocks Gravity-Slide Faults Bearpaw Shale 3 Mississippian Mission Canyph Devonian Jefferson Limestone an Platheadbandstor Bakken/3 Forks Shale NORTH Ordovician Bighorn Dolomite Little Rocky Mountains No Scale - Drawing is approximate length of Reservation Hogeland Basin Creating a cross-section requires some subjective decisions on your part, but it needs to be geologically reasonable. For example, the thickness and dip of a planar layer should remain relatively constant unless the map data requires otherwise. Planar layers should also be laterally continuous unless there is evidence otherwise. Similarly, keep the structure as simple as you can. Steps to producing a cross section: I. Choose the location and direction of the profile on the geological map (usually a straight line) II. Draw or plot the topography of the profile on the cross-section III. Add the geological features from the…
second question plss
H D Figure 13.14 4 v C ax. G Figure 13.15 JV T R K 5 ७ हाकालयकाळात Oldest Younges! Oldest 10
Knowledge Booster
Background pattern image
Similar questions
SEE MORE QUESTIONS
Recommended textbooks for you
Text book image
Applications and Investigations in Earth Science ...
Earth Science
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:PEARSON
Text book image
Exercises for Weather & Climate (9th Edition)
Earth Science
ISBN:9780134041360
Author:Greg Carbone
Publisher:PEARSON
Text book image
Environmental Science
Earth Science
ISBN:9781260153125
Author:William P Cunningham Prof., Mary Ann Cunningham Professor
Publisher:McGraw-Hill Education
Text book image
Earth Science (15th Edition)
Earth Science
ISBN:9780134543536
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:PEARSON
Text book image
Environmental Science (MindTap Course List)
Earth Science
ISBN:9781337569613
Author:G. Tyler Miller, Scott Spoolman
Publisher:Cengage Learning
Text book image
Physical Geology
Earth Science
ISBN:9781259916823
Author:Plummer, Charles C., CARLSON, Diane H., Hammersley, Lisa
Publisher:Mcgraw-hill Education,