Essentials of Meteorology: An Invitation to the Atmosphere (MindTap Course List)
8th Edition
ISBN: 9781305628458
Author: C. Donald Ahrens, Robert Henson
Publisher: Cengage Learning
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Question
Chapter 4, Problem 1QFR
To determine
The explanation of the movement of the water in the hydrologic cycle.
Expert Solution & Answer
Answer to Problem 1QFR
The movement of the water takes place in the five stages in the hydrologic cycle.
* Evaporation
* Condensation
* Precipitation
* Transpiration
* Sublimation
Explanation of Solution
Figure-(1)
The figure above represents the Hydrological cycle.
The stages of the movement of the water in the hydrologic cycle are as follows:
* Evaporation: Evaporation is the process in which the liquid particles turns into the vapor form.
* Condensation: Condensation is the process in which the vapor form gets converted into the liquid form.
* Precipitation: Precipitation is the process in which the water droplets formed in the atmosphere falls to the surface of the Earth under the action of gravity.
* Transpiration: The process of the removal of the water in the form of the vapors is known as transpiration.
* Sublimation: Sublimation is the process in which the conversion of the solid form to the gaseous form takes place.
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Students have asked these similar questions
44) In periglacial environments, the layer of ground that thaws every summer and freezes every winter is called
A) frost layer
B) permafrost
C) active layer
D) discontinuous permafrost
Use the attached piezometer map to make your own, clean version of the map, and indicate the elevation of the water table at all piezometer locations.
Draw equipotential lines (lines of equal water table elevation) using regular intervals – creating a contoured map of the water table.
Determine the direction of groundwater flow based on the horizontal gradient. Label the areas of recharge and discharge directly on your map.
Flow lines: Draw flow lines on your water table map. The lines should be at right angles to the equipotential lines and extend from the recharge area to the discharge area.
Hydraulic Gradient, Specific Discharge (Darcy Flux), Average Linear Velocity:
Using your water table map, estimate an average hydraulic gradient between two locations, call them locations A and B, one at the eastern-most and a second at the western-most extent of your dataset (note the north arrow on the map).
Calculate the specific discharge, q, between the two locations. For this calculation…
Calculate all the values of table 1:
Q in (L/day)
Q out (L/day)
Residence time (days)
Please show all steps
Chapter 4 Solutions
Essentials of Meteorology: An Invitation to the Atmosphere (MindTap Course List)
Ch. 4 - Prob. 1QFRCh. 4 - Prob. 2QFRCh. 4 - Prob. 3QFRCh. 4 - Prob. 4QFRCh. 4 - Prob. 5QFRCh. 4 - Prob. 6QFRCh. 4 - Prob. 7QFRCh. 4 - Prob. 8QFRCh. 4 - Prob. 9QFRCh. 4 - Prob. 10QFR
Ch. 4 - Prob. 11QFRCh. 4 - Prob. 12QFRCh. 4 - Prob. 13QFRCh. 4 - Prob. 14QFRCh. 4 - Prob. 15QFRCh. 4 - Prob. 16QFRCh. 4 - Prob. 17QFRCh. 4 - Prob. 18QFRCh. 4 - Prob. 19QFRCh. 4 - Prob. 20QFRCh. 4 - Prob. 21QFRCh. 4 - Prob. 22QFRCh. 4 - Prob. 1QFTAECh. 4 - Prob. 2QFTAECh. 4 - Prob. 3QFTAECh. 4 - Prob. 4QFTAECh. 4 - Prob. 5QFTAECh. 4 - Prob. 6QFTAECh. 4 - Prob. 7QFTAECh. 4 - Prob. 8QFTAECh. 4 - Prob. 9QFTAECh. 4 - Prob. 10QFTAECh. 4 - Prob. 11QFTAECh. 4 - Prob. 12QFTAECh. 4 - Prob. 13QFTAECh. 4 - Prob. 14QFTAECh. 4 - Prob. 15QFTAE
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