4.4 Article

Projected climate change effects on subsurface drainage and the performance of controlled drainage in the Western Lake Erie Basin

期刊

JOURNAL OF SOIL AND WATER CONSERVATION
卷 72, 期 3, 页码 240-250

出版社

SOIL WATER CONSERVATION SOC
DOI: 10.2489/jswc.72.3.240

关键词

climate modeling; drainage water management; DRAINMOD; Ohio

资金

  1. USDA National Institute of Food and Agriculture (NIFA) [2011-68002-30190]
  2. USDA Natural Resources Conservation Service (NRCS) [GRT00022685]
  3. Ohio Sea Grant
  4. Overholt Drainage Education and Research Program
  5. Department of Food, Agricultural & Biological Engineering
  6. Ohio Agricultural Research and Development Center, Ohio State University Extension, the Ohio State University
  7. USDA ARS Soil Drainage Research Unit

向作者/读者索取更多资源

The US Midwest is expected to experience higher intensity rainfall events along with an increased chance of drought during the mid-and late 21st century under projected future climate scenarios. Development of strategies to mitigate the impact of these projected changes on agricultural production and environmental quality is important for ensuring agricultural resiliency to future climate. This study used the DRAINMOD hydrologic model to simulate subsurface drainage discharge at a field site in the headwaters of the Western Lake Erie Basin using future climate patterns projected by 20 general circulation models. Despite projected increases in rainfall, by the late twenty-first century, subsurface discharge was projected to decrease 7% and 11% under representative concentration pathway (RCP) 4.5 and RCP 8.5, respectively. Reductions in subsurface discharge were attributed to increased temperature and evapotranspiration. The performance of controlled drainage was not projected to change on an annual basis throughout the next century. The benefits of controlled drainage systems as an agricultural best management practice were still evident under the projected climate change of the next century. The role of controlled drainage as a means to potentially retain more crop available water in the soil profile could become critically important under future climate conditions.

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