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<br /> <br />418 <br /> <br />ROGER A. PIELKE. JR. <br /> <br />NINE FALLACIES OF FLOODS <br /> <br />419 <br /> <br />perature variability. and a more active hydrological cycle, including the possibility <br />of more floods (see IPee, 1996a,b, on the science and impacts associated with <br />~Iimate change). <br />One result of scientific and political concern about the possibility of global <br />warming is a frequent association by the media and the public of almost every <br />extreme weather event with global warming. For instance, the cover of Newsweek <br />from 22 January 1996 carried the following title: 'THE HOT ZONE: Blizzards. <br />Floods. and Hurricanes: Blame Global Warming'. This article, and others like <br />il. carry the implication thaI global warming is responsible for recent climatic <br />extremes. In fUl.:t. it is essenlially impossible lo attribute ally particular weather <br />event to global warming. At the regional level scientists have documented various <br />increasing and decreasing trends in the frequency or magnitude of extreme events, <br />but are not able to associate those changes to global warming. Globally it is diffi. <br />cult for scientists to discern recent trends in extreme events. As the IPCC (1996a, <br />p, 173) notes: <br />Overall, there is no evidence that extreme weather events, or climate vari- <br />ability, has increased, in a global sense, through the 20th century, although <br />data and analyses are poor and not comprehensive. On regional scales there is <br />clear evidence of changes in some extremes and climate variability indicators. <br />Some of these changes have been toward greater variability; some h~ve been <br />toward lower variability. <br />Does the lack of a linkage between extreme weather events and global warming <br />mean that the public and policy makers need not concern themselves with climate <br />change? On the contrary; there are many reasons for the public and policymakers to <br />have an increasing concern about the impacts of extreme events. And this concern <br />is largely independent of the global warming hypothesis, for the following reasons. <br />Current knowledge is limited as to the potential impacts of a changing climate <br />on the number and intensity of hydrologic flood events (lPCC, 1996a; OTA, 1993; <br />Dracup and Kendall, 1990). It is certain that for particular regions and communities <br />the climate will change in some way or another. There will likely be some regions <br />thaI experience more flood events and others thaI experience less. It will almost <br />certainly be more straightforward to document these changes than to attribute them <br />to specific: causes such as human-caused global warming. For example, several <br />regions in the Upper Mississippi River Basin have seen trends (at 80% and 90% <br />confidence for different regions) of increasing precipitation since 1965 (Bhowmik <br />et aI., 1994). Meanwhile, the Colorado river basin has seen a decrease in streamflow <br />over the latter two thirds of the twentieth century (Frederick and Kneese, 1990). <br />Such 'winners and losers' have been documented in regions and nations around <br />the world (e,g.. Rao. 1995; Karl et aI., 1995), In the United States (about 6% of <br />the Earth's land surface), recent decades have seen an increasing trend (at vario~s <br />levels of confidence) in precipitation in certain regions and also streamflow (Kunkel <br />et aI., 1997; Karl et aI., 1996; Lins and Michaels, 1994). But it is not clear that more <br />precipitation (or changed frequencies of precipitation events) in the United States <br /> <br />are the cause of the documented increase in losses in recent decades; other factors <br />(such as human occupancy of flood plains, land use change, channel engineering, <br />nonstructural mitigation policies, etc.) must also be taken into account to arrive at <br />a final detennination of the relation of climate and impacts. <br />There are at least three implications of the uncertain climate future for societal <br />responses to floods. First, there is a continued need to document how climate has <br />changed in the past. So much atternion is focused on developing better predictions <br />of the future that we often neglect the wealth of data about the past. Second, there <br />is a need to systematically evaluate successes and failures in responding to past <br />climatic extremes. While we do not know exactly what the fUlUre will bring, we do <br />in many cases know that our responses to past events has been less than optimal. <br />Thus, at a minimum we should take care to ensure that we are at least prepared to <br />deal with the variability and extremes that have already occurred and been docu- <br />mented (Glantz, 1988). Finally, the uncertainty in the climate future underscores <br />the need to better understand the societal dimensions of the climate threat and to <br />take those adaptive measures that make sense based on our imperfect knowledge of <br />the certain past and uncertain future. A first step in that effort is to better understand <br />societal exposure to variability and extreme events. <br />No matter what the climate future holds, flood impacts on society may continue <br />to get worse. A study conducted by the U.S. Congressional Office of Technology <br />Assessment concluded that 'despite recent efforts, vulnerability to flood damages <br />is likely to continue to grow' (OTA, 1993, p. 253). The study based this conclusion <br />on the following factors, which have very little to do with climate: <br /> <br />I. Populations in and adjacent to flood-prone areas, especially in coastal areas, <br />continue to increase, putting more property and greater numbers of people at <br />risk, <br /> <br />2. flood-moderating wetlands continue to be destroyed, <br /> <br />3. little has been done to control or contain increased runoff from upstream <br />development (e.g., runoff caused by paving over land), <br /> <br />4. many undeveloped areas have not yet been mapped (mapping has been con- <br />centrated in alre'ady-developed areas), and people are moving into-such areas <br />without adequate information concerning risk, <br /> <br />5. many dams and levees are beginning to deteriorate with age, leaving property <br />owners with a false sense of security about how well they are protected, <br /> <br />6. some policies (e.g., provision of subsidies for building roads and bridges) tend <br />to encourage development in flood plains. <br /> <br />At a minimum, when people blame climate change for damaging flood events, they <br />direct attention away from the fact that decision makers already have the means at <br />their disposal to significantly address the documented U.S. flood problem. <br />