This passage is excerpted from material published in 1997.

Scientists have been puzzled by the seeming disparity between models of global warming based on greenhouse gas emissions and actual climatological data. In short, the world is not warming up as much as these models have predicted. In the early 1990s, Pat Michaels sought to explain this disparity, suggesting that sulfate emissions in industrial areas had a cooling effect, thus temporarily retarding global warming. Michaels later came to doubt this idea, however, pointing out that since most sulfate is emitted in the Northern Hemisphere, its cooling influence should be largely limited to that hemisphere. Yet, since 1987, warming in the Southern Hemisphere, which had been relatively intense, has virtually ceased, while warming in the north has accelerated. Thus, Michaels not only doubted the idea of sulfate cooling, but came to feel that global warming models themselves may be flawed.

Ben Santer disagrees. Santer contends that, in general, global warming occurs more slowly in the south because this hemisphere is dominated by oceans, which warm more slowly than the landmasses that dominate the Northern Hemisphere. But, according to Santer, the situation remains complicated by sulfate cooling, which peaked in the north in the mid-twentieth century. It drastically slowed warming in the Northern Hemisphere, and warming in the Southern Hemisphere raced ahead. Since 1987, Santer argues, the greenhouse effect has reasserted itself, and the north has taken the lead. Thus, Santer disputes Michaels’s claim that model predictions and observed data differ fundamentally.


The passage suggests that Santer and Michaels would be most likely to DISAGREE over which of the following issues?


Whether climatological data invalidates global warming models

Whether warming in the Northern Hemisphere has intensified since 1987

Whether disparities between global warming models and climatological data can be detected

Whether landmasses warm more rapidly than oceans

Whether oceans have a significant effect on global climate patterns

考题讲解

此讲解的内容由AI生成,还未经人工审阅,仅供参考。


正确答案是A。Santer 认为,由于硫酸盐的冷却作用,南半球的变暖跑在了前面,这样就延缓了全球变暖的进程,但他认为这个冷却作用已经开始减弱,全球变暖又开始回归,因此气候模型依然有效,而 Michaels 则认为,气候模型与观测数据本质上是不一致的,因此 Santer 与 Michaels 的看法完全不同,他们最可能不同意的问题就是气候模型是否被观测数据所驳斥,因此选择A 正确。

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