GEOG 102 Mod 6 Lab
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Oregon State University, Corvallis *
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102
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Geography
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Apr 3, 2024
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docx
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3
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Ruby McNamee
GEOG 102
GEOG 102 Module 6 Lab: Good to the Last Drop
How do planners use the water-budget concept to meet community needs?
Part A (40 pts)
Water-budget variables are presented in Table 1 and the relationship between these variables is shown in Figure 1 below:
Table 1: Water budget variables
PRECIP
Precipitation
How much water comes into the area from the atmosphere.
POTET
Potential evapotranspiration
How much water could be evapotranspired by the incoming solar radiation, if there were an unlimited supply of water.
ACTET
Actual evapotranspiration
Water which returns directly to the atmosphere through evaporation or transpiration by plants within the area.
STRGE
Soil moisture storage
Soil moisture water which is resident (stored) the soil.
Δ
STRGE
Change in soil water storage
Change in soil moisture storage is water which is added to or removed from the soil.
DEFIC
Soil moisture deficit
There is not enough water in the area to allow for maximum evapotranspiration (POTET). Therefore, there is a "deficit" ... the amount of incoming solar radiation that is "wasted" because there is not enough water (either PRECIP soil moisture (STRG)) in the area to be evapotranspired.
SURPL
Surplus
Water which runs off into streams/rivers and leaves the area.
Figure 1: Water-balance equation
or viewed another way
PRECIP
= ACTET +
SURPL ± ΔSTRGE
(POTET – DEFIC)
Calculations (20 pts)
1.
[20 pts]
Using the data presented in Table 2 below and the water balance equation, complete the remainder of the blanks in the water-balance table. Note that for Kingsport, the soil-moisture storage capacity is 100 mm. Use the numbers that are filled in already for Jan and Jun to help you complete the remaining calculations. You can type directly into the table.
Ruby McNamee
GEOG 102
IMPORTANT: DO NOT
use the hints in the textbook.
For whatever reason they are completely
misleading. Instead, use the hints below, refer to the Lab Guidance page, and post on the Q&A Discussion board if you need additional help.
Table 2 Kingsport Water Balance (numbers in millimeters)
Kingsport Water Balance
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Total
PRECIP
95
94
98
77
110
93
140
118
54
52
54
103
1,088
POTET
6
7
22
62
102
144
162
141
99
55
10
8
818
PRECIP – POTET
89
87
76
15
8
-51
-22
-23
-45
-3
44
95
---
STRGE
100
100
100
100
100
49
27
4
0
0
0
95
---
Δ
STRGE
0
0
0
0
0
-51
-22
-23
-4
0
0
95
---
ACTET
6
7
22
62
102
144
162
141
58
11
10
8
733
DEFIC
0
0
0
0
0
0
0
0
-41
-44
0
0
-85
SURPL
89
87
76
15
8
0
0
0
0
0
44
0
319
1.
Analysis (10 pts)
2.
[3 pts]
With respect to water supply, what occurs during the warm summer months (Jun-Jul-
Aug)? What about during the cooler winter months (Dec-Jan-Feb)?
-
In the warm summer months, water supply decreases heavily, but there is still some. In the cooler winter months, the water supply was full. 3.
[2 pts]
During what month(s) is flooding most likely? What about drought conditions?
-
Flooding is most likely during the cool months when the water supply is full. Drought is most likely in the warmer months when the water supply is low or empty.
4.
[3 pts]
What is the net demand for water in June? After this demand is satisfied in part by soil-moisture utilization, what is the remaining water in soil moisture to begin the month of July?
-
The net demand for water in June is precip-potet=-51. After this demand is satisfied by soil-
moisture utilization, there is a remaining 49 left in storage for the next month. 5.
[2 pts]
Based on the total PRECIP vs the total POTET and the monthly STRGE values, how would you describe the average soil-moisture conditions in Kingsport over the course of a year?
-
The Average soil-moisture conditions in Kingsport over a year tend to be good. 6/12 months the water storage is full. 3 of the remaining 6 months contain some storage, though not full. The final 3 months don’t have any water in storage. Only 5/12 months will there be more evaporation than precipitation, meaning less than half of the year it will dip into the water storage. On average, Kingsport has some soil-moisture if not full soil-moisture conditions. Conclude (10 pts)
6.
[3 pts]
What needs to happen for a water deficit to occur at a location?
-
For a water deficit to occur, the water storage must already be very low or zero, and PRECIP
- POTENT must be a negative value, meaning it is dipping into the already low storage.
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