Pearson eText for Exercises for Weather & Climate -- Instant Access (Pearson+)
9th Edition
ISBN: 9780137612949
Author: Greg Carbone
Publisher: PEARSON+
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Textbook Question
Chapter 6, Problem 3E
Use the temperature and mixing ratio data to plot the two air samples in Figure 6-1.
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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 6 Solutions
Pearson eText for Exercises for Weather & Climate -- Instant Access (Pearson+)
Ch. 6 - Use Table 6-1 to find the saturation mixing ratio...Ch. 6 - What are the mixing ratio (m) values of samples A...Ch. 6 - Use the temperature and mixing ratio data to plot...Ch. 6 - Plot the mixed air sample in Figure 6-1.Ch. 6 - What is the new temperature?Ch. 6 - Saturation mixing ratio?Ch. 6 - Mixing ratio?Ch. 6 - Prob. 8ECh. 6 - The nonlinear relationship between temperature and...Ch. 6 - Calculate the temperature of an unsaturated air...
Ch. 6 - Consider air parcel A, which is 28C at the...Ch. 6 - Now consider air parcel B with a surface...Ch. 6 - Why would the warmer parcel cool at a slower rate...Ch. 6 - Fill in Table 6-3 below to show the temperature...Ch. 6 - Calculate the lifting condensation level (LCL) for...Ch. 6 - What do the above calculations tell you about the...Ch. 6 - Prob. 18ECh. 6 - At what height would cloud bases form? ________...Ch. 6 - How do the sea-level temperature and dew point on...Ch. 6 - Which side of the mountain is more often cloudy...Ch. 6 - What is the lifting condensation level in this...Ch. 6 - Enter the correct parcel temperatures and parcel...Ch. 6 - Using the diagram on the next page and Figures 6-5...Ch. 6 - Would you forecast thunderstorms during these...Ch. 6 - How is saturation achieved to form most clouds?Ch. 6 - What is the difference between a stable and an...
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- 45) The roughness layer refers to A) the atmospheric layer where wind has the fastest velocities. B) the layer of active weather between the stratosphere and the surface. C) the shallow layer of nearly still air. D) the layer of the atmosphere where dust storms occur.arrow_forward47) Deflation is the process by which A) wind transports smaller particles leaving behind only larger pebbles and rocks. B) sands are deposited closer to the source area and silts are deposited farther. C) sand dunes migrate downwind as sand saltates up the windward face. D) rocks are worn away by bombardment of particles carried in Windstream.arrow_forward46) In Barchan dunes, the slip face is oriented A) on the convex side of the dunes. B) parallel to wind direction. C) on the concave side of the dunes. D) at varying angles.arrow_forward
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