As we traveled through the tortured landscape of the Great Basin on our way to and from Utah, I was reminded of the long history of climatic change in this region. Millions of years ago, it was seabed. Thousands of years ago, it was largely filled with lakes and rivers fed by melting glaciers. Even after the glaciers began their abrupt but long retreat, the region remained wet and lush long enough for ancient humans to survive and prosper.
That prosperity didn’t last. The climate continued to change. Lakes and rivers shrank, and some disappeared altogether. Rainfall also declined. The Great Basin dried out. Crops failed. People died. The first inhabitants had all but vanished by the time more adaptable tribes arrived from the east to dig wells, divert rivers, and build cities.
Despite all the recent concern over climatic change, it is simply not a new phenomenon. In the broadest sense, human history has been defined by our response to this ongoing process. Legendary civilizations arose and thrived on the low-lying temperate plains, only to be washed away by the rising seas that heralded the beginning of a warmer, interglacial period. As the ice retreated, the survivors of the great floods migrated into the new lands, where they planted the seeds that grew into the nations we know today.
Humans have always adapted to such change or paid the price for failing to do so. Now, though, we talk of controlling the climate by our own hand and of spending the wealth of nations to do so. Assuming this ability is within our grasp and not another fiction of our own arrogance, how will we select the ideal global climate?
That is the question that still remains unanswered and, for that matter, largely unasked. Why should the predominant climate of the 20th century
A.D. be our ideal? It was but one point on the climatic spectrum—and perhaps an unstable one at that. Should we forgo adaptation in our pursuit of control? Our civilization will pay a high price if our quest for control fails—or perhaps even if it succeeds.