Increases in precipitation totals and intensity do not necessarily mean that additional water is available for agriculture. More intense rain leads to faster runoff, and higher temperatures increase evapotranspiration losses to the atmosphere, both of which result in less moisture retention in soils.
The entire United States is projected to warm substantially in the future. Even under a scenario of limited emissions increases and GHG concentrations (e.g., RCP 2.6), average temperatures are likely to increase by 1–2 °C over the next 40 years, which is substantially faster than the rate observed over the last 100 years
The changes in precipitation and temperature outlined above are extremely likely to have direct effects on U.S. agricultural production. Crops and livestock are sensitive to direct effects of climate changes, such as changing temperatures and
precipitation. Exceeding optimum temperatures for crops steadily reduces productivity up to a threshold, after which productivity decreases sharply, and increases animal stress, especially when coupled with high humidity. Precipitation decreases can make it difficult to store and deliver adequate water to crops at the right time, while increased overall
precipitation, and particularly increased intense precipitation, requires improved drainage to avoid
crop and soil damage.
Agriculture is also sensitive to indirect effects, such as increases in diseases and pests, and degradation of the natural-resource base, such as high quality soil and water, upon which agriculture depends. Climate change is projected to increase the growth and range of many weeds, insect pests, and pathogens harmful to agriculture, although the ranges of some invasive weeds could decrease.
Projected increases of intense precipitation coupled with increased drying of soils from higher temperatures increases
the risk of accelerated erosion of soils in many areas, which both degrades soil quality and increases the runoff of agricultural chemicals. Projected changes in precipitation are also likely to increase water-management challenges in agriculture. For
example, the combination of decreased snowfall and snowpack, increased rainfall (from less precipitation falling in frozen form and more in liquid form), earlier snowmelt, and decreased summer flows in streams and rivers could increase the need for water storage in many areas of the western United States.
Overall, the U.S. food system is expected to be fairly resilient in the near term due to its capacity to undertake adaptive actions such as increased irrigation, shifting of crop rotations and acreage devoted to specific crops in some regions, and alteration of nutrient inputs and other management practices. As climate change continues and temperature increases of 1–3 °C are coupled with changes in precipitation timing and intensity, yield and farm returns are projected to decline.
The continued changes expected between 2050 and 2100 under high-emissions scenarios are expected to have overall detrimental effects on most crops and livestock.
Finally, it should be recognized that there is a significant chance that current projections underestimate potential declines, because most analyses exclude production constraints arising from increased pest pressures, extreme events, and decreased ecosystems services (Walthall et al. 2012).