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PDF Ebook Missing Link: Volatility and the Debt Intolerance Paradox

It is a well documented empirical regularity that developing countries typically face an upward sloping supply schedule for international debt, and may be altogether excluded from international capital markets during bad states of the world (Diaz-Alejandro, 1984; and Sachs, 1989; Eichengreen and Lindert, 1989). In a recent paper, Reinhart, Rogoff, and Savastano (2003) take this evidence one step further. Combining macroeconomic data for the post-1970 period with information about sovereigns’ credit histories since the early nineteenth century, they argue that an important subgroup of middle-income countries or “emerging markets” have been systematically afflicted by what they call “debt intolerance.” That is, even though their external debt-to-GDP ratios are moderate by international standards and substantially lower than those of several high-income countries, these economies are perceived as riskier and unable to tolerate as much debt. Simply put, their sovereign riskiness appears to be out of proportion to the size of the respective debt burdens.

To explain this phenomenon, Reinhart, Rogoff, and Savastano (2003) invoke history. Virtually all these countries have tarnished credit histories, with several of them having defaulted a few times on their public debts. To the extent that those that have defaulted once or more in the past are likely to do so again in the future, the market threshold of what can be considered “safe” borrowing levels for these countries tends to be lower.2 As a theoretical story, however, this argument raises some important questions. For one, it touches on the contentious issue of what lenders take into account when evaluating sovereign risk.3 Also, it neither explains what causes serial defaulters to default in the first place, nor how most of today’s advanced economies—which have also defaulted several times in their history—managed to graduate out of the debt intolerant “club.”

Ebook Accounting Transparency and the Term Structure of Credit Default Swap Spreads

Traditional structural credit risk models originating with Black & Scholes (1973) and Merton (1974) define default as the first passage of a perfectly measured asset value to a default barrier. While later extensions that allow for endogenous default and debt renegotiations have increased predicted spread levels, it is well(known in the empirical literature that structural models underpredict corporate bond credit spreads, particularly in the short end. Reasons for the poor performance may lie in shortcomings in the models as well as factors other than default risk in the corporate bond credit spread.

As noted in Duq e & Lando (2001), it is typically diq cult for investors in the secondary credit markets to observe a firmos assets directly, either because of noisy or delayed accounting reports or other barriers to monitoring. Instead, investors must draw inference from the available accounting data and other publicly available information. As a consequence they build a model where credit investors are not kept fully informed on the status of the firm, but receive noisy unbiased estimates of the asset value at selected times. This intuitively simple framework has a significant implication for the term structure of credit spreads.

Ebook Diet and Health Changes at the End of the Chinese Neolithic: The Yangshao/Longshan Transition in Shaanxi Province

Considerable climate change following a pro-longed mid-Holocene climatic optimum (8,000–5,000 BP) is documented worldwide around 5,000 BP (Shi et al., 1993, 1994; Cohen, 1998; Thompson et al., 1995; Bond et al., 1997; Lamb, 1995; Sandweiss et al., 1996; Krishnamurthy et al. 1995; Sun and Chen, 1991; Jinqi, 1991). The signature of this change is not always clear and varies with the different methods used to track paleoclimate. Whether the change was rapid or slower and preceded by oscillations is not certain. DeMenocal et al. (2000) suggested that the onset of colder and drier climate worldwide was rapid and took place circa 5,000 BP. However, there is evidence for a prolonged period of climatic oscillations in China with very cold episodes during the fifth millennium BP (Shi et al., 1993).

In this paper we focus on subsistence adaptations of millet farmers from northern China that were established during the period of climatic optimum, as well as the adjustments made to the suggested period of oscillations and instability and subsequent onset of colder and more arid climate. The Yangshao culture (7,000–5,000 BP) developed during the time of the climatic optimum. For the two millennia of its existence, the Yangshao population remained sparse and static. Little evidence of social stratification is found for this time, and the Yangshao society is assumed to be egalitarian (Chang, 1986; Liu, 1996a). The later phase of this culture must have been affected by the weather oscillations that preceded Yangshao demise circa 5,000 BP. The period of colder and drier weather was accompanied by the rise of a new dominant culture in northern China, Longshan (5,000–4,000 BP), the predecessor of early dynasties.

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