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CHAPTER 8 • Insolation Control of Monsoons  153


        way. Instead, it appears that plateau uplift sensitizes the  7. How do tectonic uplift and orbital variations
        monsoon system to insolation forcing in such a way      combine to affect the long-term intensity of
        that the combined monsoon response to uplift and inso-  monsoons?
        lation is stronger than a simple linear combination of the
        two effects.
                                                             Additional Resources
          Key Terms                                         Basic Reading

        orbital monsoon           anoxic (p. 143)           Companion Web site at www.whfreeman.com
          hypothesis (p. 139)     thermocline (p. 145)        /ruddiman2e, pp. 9–11, 15–18, 21–24, 32.
        nonlinear response        clipping (p. 148)         Kutzbach, J. E. 1981. “Monsoon Climate of the Early
                                                              Holocene: Climate Experiment with Earth’s Orbital
          (p. 140)                orbital tuning (p. 149)     Parameters for 9000 Years Ago.” Science 214: 59–61.
        threshold level (p. 141)
                                                            Ruddiman, W. F. 2005. Plows, Plagues and Petroleum,
        sapropels (p. 143)                                    Chapter 5. Princeton, NJ: Princeton University
                                                              Press.
          Review Questions                                  www.classzone.com/book/earth_science/terc/content
                                                              /visualization, Chapter 24: Monsoon Circulations.
         1. In what way is the orbital monsoon hypothesis an
            extension of processes driving modern monsoons?
                                                            Advanced Reading
         2. Why does the intensity of 23,000-year monsoon   Olsen, P. E. 1986. “A 40-Million-Year Lake Record of
            peaks vary at intervals of 100,000 and 413,000 years?  Early Mesozoic Orbital Climatic Forcing.” Science
                                                              234: 842–48.
         3. How did the Mediterranean Sea acquire a         Pokras, E. M., and A. C. Mix. 1987. “Earth’s
            freshwater lid during times when very little      Precession Cycle and Quaternary Climatic Changes
            precipitation was falling in that region?
                                                              in Tropical Africa.” Nature 326: 486–87.
         4. Explain how the opposed July/February timing    Rossignol-Strick, M., W. Nesteroff, P. Olive, and C.
            of past monsoon changes in China and Brazil       Vergnaud-Grazzini. 1982. “After the Deluge:
            lends strong support to the orbital monsoon       Mediterranean Stagnation and Sapropel
            hypothesis.                                       Formation.” Nature 295: 105–10.
                                                            Ruddiman, W. F., 2006. “Viewpoint: What Is the
         5. Does peak monsoon strength lag behind summer
            insolation forcing?                               Timing of the Orbital Monsoon?” Quaternary
                                                              Science Reviews 25: 657–58.
         6. What similarities exist between monsoon changes  Yuan, D., et al. 2004. “Timing, Duration, and
            in Pangaea 200 Myr ago and those in North Africa  Transitions of the Last Interglacial Monsoon.”
            during the last several hundred thousand years?   Science 304: 575–78.
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