Exercises for Weather & Climate (9th Edition)
9th Edition
ISBN: 9780134041360
Author: Greg Carbone
Publisher: PEARSON
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Chapter 3, Problem 10E
To determine
The explanation accounting the general pattern is observed by an individual each day, and the factors that cause the difference in the magnitude of peak long-wave radiation emitted by the Earth’s surface between February 1–3 and August 1–3 in the Hourly radiation fluxes—Maun, Botswana.
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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 3 Solutions
Exercises for Weather & Climate (9th Edition)
Ch. 3 - a. The Sun has an average surface temperature of...Ch. 3 - a. In question 1, how many times warmer is the Sun...Ch. 3 - Calculate the wavelength of maximum emission for...Ch. 3 - In what portion of the electromagnetic spectrum...Ch. 3 - Why is incoming short-wave radiation higher in...Ch. 3 - The solar noon solar radiation values at the top...Ch. 3 - Based on the incoming shortwave radiation curves,...Ch. 3 - At 12:30 p.m. on August 2, the surface receives...Ch. 3 - Thinking about the radiation laws, why does...Ch. 3 - Prob. 10E
Ch. 3 - Table 3-2 shows the four radiation fluxes at 7:00...Ch. 3 - Using the surface net radiation data, explain why...Ch. 3 - Explain changes in afternoon air temperature with...Ch. 3 - Why is the peak net radiation approximately the...Ch. 3 - How does the net surface radiation pattern differ...Ch. 3 - In Figure 3-7, draw the stacked bar graph showing...Ch. 3 - How do the proportions of sensible, latent, and...Ch. 3 - The proportion of each of these fluxes depends, in...Ch. 3 - a. Figure 3-9 shows the diurnal air temperature...Ch. 3 - Peak radiation occurs at Maun from mid-November to...Ch. 3 - Water vapor is a very effective greenhouse gas,...Ch. 3 - Prob. 22ECh. 3 - Prob. 25ECh. 3 - Prob. 28ECh. 3 - Prob. 29ECh. 3 - Prob. 30ECh. 3 - Prob. 31ECh. 3 - Prob. 32ECh. 3 - Prob. 33ECh. 3 - Prob. 1RQCh. 3 - Prob. 2RQ
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