ISOLINE MAPS

Geography 101 Lab

Writeup Instructions: For this lab, you will take a MULTIPLE CHOICE QUIZ. In the Submit Labs area, simply click the appropriate lab quiz, follow instructions, and answer the 20 multiple choice questions. The quiz questions are taken from the material below. I recommend that you answer the sample questions first and then do the quiz. All quizzes will be somewhat different because questions are randomly selected from a large data base. You can repeat the quiz if you wish, I will keep the highest grade. DO NOT submit the answers to the questions to me, simply take the quiz in the Submit Labs area.

Purpose: Introduce students to one of the most common and useful types of maps used in studying the natural environment. When completed, the student should understand the basic meaning of isolines maps, how to construct them, and how to derive information from them.

Many surfaces in nature are represented with isolines. They provide a method of representing 3-Dimensional surfaces on 2-Dimensional maps. An isoline is simply a generic term for any line on a map that connects points of equal value. Some examples of isolines are:

Name Connects Equal Values of
Contour Elevation
Isohyet Rainfall
Isobar Air Pressure
Isotach Wind Speed
Isohaline Salinity
Isoseismal Earthquake Intensity
Isoflor Number of Plant Species

Part 1: Basic Rules

Some basic rules regarding isoline (and isopleth) maps are:

The map below is an isoline map showing isobars (in millibars) for the area Hawaiian Islands area. Isobar maps are useful in weather forecasts.  After reading the information above, answer the following sample questions regarding the isobaric map:

Sample Questions:

  1. Isobars show equal values of what?
  2. Do any isobars touch or overlap?
  3. What is the pressure interval in millibars between isobars on this map?
  4. What is the pressure at point A?
  5. What is the difference in pressure between B and A?
  6. Where is the highest pressure located?
  7. Estimate the pressure at point C.
  8. Estimate the pressure at point D.
  9. What direction will air flow, from B to A or from A to B?
  10. Name three other environmental variables not mentioned in this lab exercise or listed above that could be mapped using isolines.

Figure 1: Isobar Map

Part 2: Drawing and Interpreting Isolines

Isoline maps show patterns in an easily recognizable way. Usually they are constructed from scattered observations that are difficult to interpret. The mapmaker (or the computer) must convert these isolated observations into a complete isoline map by interpolating between observed values and then connecting points of equal value. The resulting isoline map gives a much clearer view of the pattern.

Consider the map to the right showing isohyets of annual rainfall over East Maui in millimeters (2000, 3000, etc.). The numbers beside the black dots are observed rainfall amounts measured at various stations. The BLUE isohyets have been interpolated based on the rainfall station values and are all correct. The RED isohyets may or may not be correct.

Notice how the BLUE isohyets pass between observations of higher and lower value. The 2000 mm isohyet, for example, passes between the 2345 mm and 1799 mm stations just north of Hana and the 6000 mm isohyet passes between the 5920 mm and 6231 mm stations further inland. For points that are between isohyets or point values, you can estimate rainfall amounts. A point halfway between the 4000 and 5000 mm isohyets, for example, would receive about 4500 mm rainfall per year on average. A point halfway between the 2200 and 2840 mm stations would receive about 2520 mm rainfall per year.

Sample Questions:

Using Figure 2: Intrepreting Isolines at the right:

11. What is the approximate rainfall value at A based on the BLUE isohyets?
12. What is the approximate rainfall value at B based on the BLUE isohyets?
13. What is the approximate rainfall value at C based on the BLUE isohyets?
14. What is the approximate rainfall value at D based on nearby station values?
15. What is the approximate rainfall value at E based on nearby station values?

Use Figure 2 and the Basic Rules from Part 1 above to answer the following questions:

16. Is there anything wrong with line F? If so, what?
17. Is there anything wrong with line G? If so, what?
18. Is there anything wrong with line H? If so, what?
19. Is there anything wrong with line I? If so, what?
20. Is there anything wrong with line J? If so, what?

main rain

Figure 2: Interpreting Isolines

Figure 3: Drawing Isolines

 

 

In Figure 2 above, some of the RED isohyets are wrong. Try to draw the isohyets for the bottom half of the map correctly. Remember, each isoline must pass between observations with higher and lower values, never between two lower values or between two higher values. For example, the 5000 mm isohyet will pass between the stations with 5439 and 4013 mm of rainfall. The 2000 mm isohyet with pass between the stations with 1622 and 2469 mm rainfall. And so on. Your completed map should look like a thumbprint.

Click for a printable map.

Sample Questions:

Look at your completed map.

21. Does rainfall tend to increase or decrease as you move inland (west) from Hana?
22. Starting from the bottom of the map at the rainfall value of 1622, does rainfall increase or decrease as you move directly northward?
23. The mountain name label "Haleakala" is located at the highest point in this map. On your completed map, where are the highest rainfall amounts located? The highest elevation? Lowest elevation? Intermediate elevation? North, south, or east of the highest point?
24. Where are the lowest rainfall amounts, near the coast or inland?

 

Part 3: Gradient and Profile

Isolines show surfaces whose values differ with location. Is there is no change, there would be no isolines. Therefore, there is always a gradient on an isoline map; for example from high to low pressure, high to low elevation, high to low concentration of a pollutant, high to low density of termites, and so on. The distance between isolines shows the amount of the gradient. Very close together means a steep gradient, and far apart means a gradual gradient. This can be quite meaningful. In hurricanes, the isobars are very close together and so the air pressure gradient is said to be high, or steep. This drives strong winds. We will look at gradient and profile using the example of contour maps, also called topographic maps, which are isoline maps showing surface elevation.

Figure 4: Reading Contour Maps

The image to the left shows a perspective view of a river mouth at the head of a valley between a steep cliff (to the left) and a smoother slope (to the right). The rendition of this topography as an isoline (contour) map from an overhead perspective is shown directly below.

Notice that the contours (isolines) are very close together where they represent the steep cliff and further apart in the flatter river valley. This property of isolines maps is referred to as the gradient, or the amount change over distance. In the case of contour maps, the gradient refers to the change in elevation over distance, which is very high for the cliff area and very low for the river valley. In practical terms, a high elevation gradient on a contour map refers to steep slopes and a low elevation gradient refers to flatter terrain. Gradient on other types of isoline maps can be interpreted similarly. A high pressure gradient on an isobar map indicates a high pressure gradient force and strong winds, while a low pressure gradient suggests light winds.

Profile refers to a cross-section, or horizontal view, of some part of the isoline map. For example, if I walked from A to B on the map, my path would look like the drawing at the bottom. First I walk up a gradual slope, then down a cliff, then across a flat river valley, then up slope that becomes increasingly steep..

Below is a topographic map of the area above Makawao, Maui, showing isolines of elevation called contour lines. Using the information given in the explanation above, try to answer the sample questions. If you get confused, I recommend doing an internet search with keywords "how to use topographic maps." You should come up with a list of several useful sites.

interpreting contours
Figure 5: Interpreting Contour Maps

Sample Questions:

25. The height interval between contour lines is 40 feet. Explain how to calculate this value using information given on the map.
26. What (in feet) is the highest elevation point on the map and what is its name?
27. What is the elevation at point D?
28. What is the elevation at point C?
29. What is the elevation at point E?
30. From point C, which direction is downhill (NE, NW,S E, or SW)?
31. Which point lies on the highest elevation gradient, C, D, or E?
32. In your own words, what is physically meant by "highest elevation gradient?"
33. Which point lies on the lowest elevation gradient, C, D, or E?
34. In your own words, what is physically meant by "lowest elevation gradient?"
35. If you walk from A to B, what is the lowest elevation you would reach?
36. If you walk from A to B, what is the highest elevation you would reach?

37. On a piece of paper, draw an approximate profile of your journey from point A to point B. Show where you go uphill and downhill and cross relatively flat areas.

38. Topographic maps show many features besides just elevation contour lines. Look at the map of the Makawao area and name four other features it shows the location of.

A perspective image of the path from A to B taken from Google Earth is shown below in Figure 6 (courtesy of Prof. Toshi Ikagawa). Compare this image to Figure 5 above. If you walked from A to B:

39. Do you cross through any developed areas with housing?
40. Primarily what type of land use would you walk through?
41. How many times would you cross a road? (compare with Figure 5)
42. How many small stream valleys would you cross through? (shown as the dark sinuous patches in the image, compare with Figure 5)
43. What direction would you be walking? (N, S, E, or W)

3d
Figure 6: Perspective Image of Path A - B