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many of the problems of the Germans during the 1930s and early 1940s were blamed on the Jews. During the 1980s, many (including several U.S. senators) suggested that AIDS was a plague from God for immoral homosexual behavior. Today, many blame illegal immigration as a critical factor in many societal ills, including problems such as economic woes, violence, and youth crime. Not everyone during the Middle Ages believed that good and evil, spirits and demons, sorcery and witchcraft contributed to mental illness (Kemp, 1990; Maher & Maher, 1985a). Some, such as Saint Thomas Aquinas (1225 1274), felt that there was both theological truth and scientific truth. For example, Aquinas reasoned that the soul was unable to become sick and, therefore, mental illness must have a physical cause or be due to problems in reason or passion (Aglioni, 1982). The late fourteenth-century French bishop Nicholas Oresme felt that abnormal behavior and mental illness were due to diseases such as melancholy (today s depression). Furthermore, the insane were sometimes humanely and compassionately cared for by people living in rural villages. Another model to explain abnormal behavior, which became especially popular during the sixteenth century, was the influence of the moon, stars, and alignment of the planets. A Swiss physician, Paracelsus (1490 1541), popularized the notion that various movements of the stars, moon, and planets influenced mood and behavior. Paracelsus also focused on the biological foundations of mental illness and developed humane treatments. Juan Luis Vives (1492 1540) and Johann Weyer (1515 1588) helped to shift theories of mental illness from a focus on the soul to an emphasis on behavior and promoted humane treatments of the mentally ill. During the Middle Ages, the biological, psychological, social, astrological, and supernatural influences on behavior were believed to be responsible for mental illness and abnormal

length (e.g., Pincus & Gurtman, 1995) or each item may be weighted equally (unit weighting) as in Gurtman, 1997. Breadth of coverage concerns how narrowly or broadly the measure samples from that particular circumplex domain. Narrow coverage suggests a cohesive test with delity of measurement, whereas broad coverage suggests a test that is less cohesive but that has greater bandwidth. (Cronbach, 1990). Breadth of coverage is indexed by the dispersion of the items around the mean that is, by its circular variance. Finally, factorial saturation indicates the amount of variance that the measure shares with that particular circumplex domain for example, how interpersonal it is when referenced to an interpersonal circumplex (e.g., Gurtman, 1991). It is calculated as the average vector length (VL) of the measure s items. Figure 16.10, reproduced from Pincus and Gurtman (1995), shows the results of this kind of analysis conducted on eight popular measures of interpersonal dependency. As can be seen, the measures circular means vary considerably, although most are in the lower right quadrant of the interpersonal circumplex, indicating that the measures generally tap friendly forms of submissiveness. The iconic representations, which are based on the circular variances, suggest that measures also differ in their breadth of coverage. (The circular variances, though not given directly, are related to the values listed in the last two columns.) Finally, each measure s factorial saturation, shown by the mean item vector length,

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Fig. 5.8 Base ow index values for ten major river catchments representative of a wide range of climatic regions within the contiguous United States of America. The gures shown are those proportions of total runoff (= 1) accounted for by base ow. Key to rivers shown: A, Dismal River, Nebraska; B, Forest River, North Dakota; C, Sturgeon River, Michigan; D, Ammonoosuc River, New Hampshire; E, Brushy Creek, Georgia; F, Homochitto River, Mississippi; G, Dry Frio River, Texas; H, Santa Cruz River, Arizona; I, Orestimba Creek, California; J, Duckabush River, Washington. The heavy black lines delineate 24 regions within which stream aquifer interaction processes at the catchment scale display relatively consistent patterns. (Adapted from data presented by Winter et al. 1998.)