Patz Jonathan A, Vavrus Stephen J, Uejio Christopher K, McLellan Sandra L
Center for Sustainability and the Global Environment (SAGE), Department of Population Health Sciences, University of Wisconsin-Madison, Madison, Wisconsin 53726, USA.
Am J Prev Med. 2008 Nov;35(5):451-8. doi: 10.1016/j.amepre.2008.08.026.
Extremes of the hydrologic cycle will accompany global warming, causing precipitation intensity to increase, particularly in middle and high latitudes. During the twentieth century, the frequency of major storms has already increased, and the total precipitation increase over this time period has primarily come from the greater number of heavy events. The Great Lakes region is projected to experience a rise these extreme precipitation events. For southern Wisconsin, the precipitation rate of the 10 wettest days was simulated using a suite of seven global climate models from the UN Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report. For each ranking, the precipitation rate of these very heavy events increases in the future. Overall, the models project that extreme precipitation events will become 10% to 40% stronger in southern Wisconsin, resulting in greater potential for flooding, and for the waterborne diseases that often accompany high discharge into Lake Michigan. Using 6.4 cm (2.5 in) of daily precipitation as the threshold for initiating combined sewer overflow into Lake Michigan, the frequency of these events is expected to rise by 50% to 120% by the end of this century. The combination of future thermal and hydrologic changes may affect the usability of recreational beaches. Chicago beach closures are dependent on the magnitude of recent precipitation (within the past 24 hours), lake temperature, and lake stage. Projected increases in heavy rainfall, warmer lake waters, and lowered lake levels would all be expected to contribute to beach contamination in the future. The Great Lakes serve as a drinking water source for more than 40 million people. Ongoing studies and past events illustrate a strong connection between rain events and the amount of pollutants entering the Great Lakes. Extreme precipitation under global warming projections may overwhelm the combined sewer systems and lead to overflow events that can threaten both human health and recreation in the region.
水文循环的极端情况将伴随全球变暖出现,导致降水强度增加,特别是在中高纬度地区。在20世纪,主要风暴的频率已经增加,这一时期总降水量的增加主要来自更多的强降水事件。预计五大湖地区此类极端降水事件将会增加。对于美国威斯康星州南部,利用联合国政府间气候变化专门委员会(IPCC)第四次评估报告中的七个全球气候模型模拟了最潮湿的10天的降水率。对于每个排名,这些强降水事件的降水率在未来都会增加。总体而言,模型预测威斯康星州南部的极端降水事件强度将增强10%至40%,导致洪水发生的可能性更大,以及伴随大量水流排入密歇根湖而出现的水传播疾病发生的可能性更大。以每日6.4厘米(2.5英寸)的降水量作为启动合流污水溢流进入密歇根湖的阈值,预计到本世纪末,这些事件的频率将上升50%至120%。未来热力和水文变化的综合影响可能会影响休闲海滩的可用性。芝加哥海滩关闭取决于近期降水量(过去24小时内)、湖水温度和湖面水位。预计强降雨增加、湖水变暖以及湖面水位下降都将导致未来海滩污染。五大湖为超过4000万人提供饮用水源。正在进行的研究和过去的事件表明降雨事件与进入五大湖的污染物数量之间存在紧密联系。全球变暖预测下的极端降水可能使合流污水系统不堪重负,导致溢流事件,威胁该地区的人类健康和娱乐活动。