By David; Swing, Ross Duxbury
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31). New Orleans grew rapidly in the nineteenth century as a result of its busy port and the success of steamboats in making swift upriver travel possible. The relatively high ground near the river soon filled up with structures, and the obvious direction to expand was northward into the swamps toward the lake. For that to happen, the landscape would have to change. Largely to be cleared were the majestic bald cypress trees; their wood was durable timber, so resistant to rot that it was called “the wood eternal” (Dennis 1988).
Approximately 200,000 of an original population of 440,000 now live in New Orleans, and the African-American proportion has dropped from 67 to 47%. Certainly the poor suffered more than the affluent. It took a week to evacuate all of the 122,000 people who were stranded in the Superdome and the Convention Center. Ari Kelman, my colleague who wrote a fine book on the earlier history of New Orleans entitled A River and Its City (Kelman 2006), said that the idea was to “Move the homeless, the elderly, the impoverished, the unlucky, all those poor souls who couldn’t get out of New Orleans in time to avoid Hurricane Katrina; move them into the city’s cavernous domed football stadium.
But one has to understand that there are scattered and indirect references to climate and rainfall, pattern of tropical monsoon and cyclonic depressions in many ancient and medieval texts like Mahabharata and Ramayana, Chinese accounts, writings of Mughal court historians. The ancient Greek sources relating to Alexander’s invasion may be of some help too. Cultural representations of natural calamities or climate as found in literature or various visual arts are also worth looking into. It is high time to embark on a project of constructing a comprehensive history of climate in South Asia.
Aircraft of the Royal New Zealand Air Force by David; Swing, Ross Duxbury