Tables give exact values, so errors come from picking the wrong cell: a total row read as an entry, a column in thousands mixed with one in lakhs, or a blank or 'NA' cell read as zero. Before reading, scan every heading for its unit and look for total rows and columns; a printed total is also a free check on your own addition.
Histograms show how many items fall in each class interval of a continuous variable, with the bars touching. Read the class boundaries from the horizontal axis first. When all the classes are equally wide, the height of each bar is its frequency. When the widths differ and the vertical axis is labelled frequency density (frequency per unit of class width), the AREA of a bar is its frequency.
Scatter plots show one point per item, with one variable on each axis. When both axes start at zero, the ratio xy for a point is the slope of the straight line from the origin to that point: points on one line through the origin share the same ratio, and a point above the line y=kx has a ratio greater than k (for x>0). A general upward drift of the points shows that the two quantities tend to rise together; it does not show that one causes the other.
FREQUENCY FROM A HISTOGRAM WITH UNEQUAL CLASSES
Frequency=Frequency density×Class width
A bar of height 6 per unit over the class 20 to 30 stands for 6×10=60 items. Comparing the heights of bars of different widths compares densities, not frequencies.
RATIO FROM A POINT OF A SCATTER PLOT
xy=slope of the line from (0,0) to (x,y)
Holds only when the plotted origin really is (0,0). If either axis is offset (starts above zero), compute xy from the values read off instead.
Two- and three-dimensional plots. A 2-D plot shows one quantity against another (a line graph or a scatter plot). A 3-D plot shows a quantity z that depends on two variables x and y: drawn in perspective as a surface, or flattened into a contour plot, a map of the (x,y) plane on which each contour line joins points with the same value of z. A heat map does the same with colours, each colour standing for a range of z.
Adjacent contour lines differ by a fixed contour interval. Where the lines crowd together z changes quickly (a steep slope); where they are far apart it changes slowly. Two contour lines of different values never meet or cross, because a point has only one value of z. A set of closed rings with values increasing inwards marks a peak; values decreasing inwards mark a hollow.
AVERAGE GRADIENT FROM A CONTOUR MAP
Average gradient=horizontal distancechange in z=horizontal distance(number of intervals crossed)×(contour interval)
Both in the same unit. The horizontal distance is the ground distance, so convert the map distance with the scale first. Often written as '1 in N', meaning a rise of 1 unit for every N units horizontally.
Maps. A map is a scaled drawing of an area. The scale may be a ratio (1:50,000 means 1 cm on the map is 50,000 cm, i.e. 0.5 km, on the ground), a statement ('1 cm to 2 km') or a scale bar. Unless a north arrow shows otherwise, north is at the top, east to the right, south at the bottom and west to the left; NE, SE, SW and NW lie 45∘ from their neighbouring cardinal directions. A data map shades regions by class intervals given in its legend, so two regions in the same shade may differ by up to the width of a class.
WORKED EXAMPLE · CONTOUR MAP AND SCALE
On a map drawn to a scale of 1:25,000, a straight path runs from point A on the 120 m contour line to point B on the 220 m contour line, and measures 8 cm on the map. The ground rises steadily from A to B, and the contour interval is 20 m. Find (a) the number of contour intervals the path crosses, (b) the ground distance from A to B, (c) the average gradient of the path, and (d) the ground area of a field that occupies 6 cm² on the same map.
▸ Solution
(a) Rise =220−120=100 m, so the path crosses 20100=5 contour intervals.
(b) Ground distance =8×25,000=2,00,000 cm =2 km =2,000 m.
(c) Average gradient =2,000100=201, i.e. 1 in 20, or 5%.
(d) 1 cm on the map is 25,000 cm =0.25 km, so 1 cm² is (0.25)2=0.0625 km², and the field is 6×0.0625=0.375 km². Using the linear scale only once would give the wrong 6×0.25=1.5.
Answer: (a) 5; (b) 2 km; (c) 1 in 20 (5%); (d) 0.375 km².