2012–14 North American drought
The 2012-2014 North American Drought, an expansion of the 2010–2012 Southern United States drought, originated in the midst of a record breaking heat wave. Low snowfall amounts in winter, coupled with the intense summer heat from La Nina, caused drought-like conditions to migrate northward from the southern United States, wreaking havoc on crops and water supply. The drought has inflicted, and is expected to continue to inflict, catastrophic economic ramifications for the affected states. It has exceeded, in most measures, the 1988-1989 North American drought, the most recent comparable drought, and is on track to exceed that drought as the costliest natural disaster in US history.
The drought includes most of the US, parts of Mexico, and central and Eastern Canada. At its peak on July 17, it covered approximately 81 percent of the contiguous United States with at least abnormally dry (D0) conditions. Out of that 81%, 64% was designated as at least moderate drought (D1) conditions. Its area was comparable to the droughts in the 1930s and 1950s but it has not yet been in place for as long. In March 2013, heavy winter rains broke a three-year pattern of drought in much of the Southeastern United States, while drought conditions still plague the Great Plains and other parts of the US, according to the U.S. Drought Monitor.
Drought is expected to continue in parts of North America through 2013. Beginning in March 2013, improved rainfall across the Midwest, southern Mississippi Valley, and Great Plains began gradually alleviating drought in these areas, while drought continued to intensify in the Western United States. Heavy rains across previously drought-stricken areas resulted in widespread flooding in portions of the Midwest, a phenomenon which was named "weather whiplash". By June 2013, approximately the eastern half of the United States was drought-free, while conditions continued to gradually improve across the Plains. Moderate to severe drought continues to impact and worsen throughout the western United States, with some portions of the United States being afflicted by the drought for over three years. Through the winter of 2013-2014, California continued to receive record low rainfall. For many locations, the calendar year of 2013 was the driest year in over 130 years. Some locations received less than half of their previous record low rainfall amounts. 
The drought was set in motion when strongly positive Arctic oscillation and North Atlantic oscillation conditions removed winter storms from the US. When spring arrived, very little snow existed to melt and moisten the ground, and thus very little water to evaporate and create rainfall. The effects of the lack of snow were immediate. Dry conditions could be noticed immediately, and contributed to a weak tornado season in the US. The strongest tornado outbreak of the year, March 2, occurred right as the snow was finishing melting. The drought continued to steadily intensify along with a decline in rainfall which is still ongoing. The Summer 2012 North American heat wave caused further evaporation of groundwater, lakes, reservoirs, and rivers and streams.
As moisture has continued to decline, the conditions are becoming self-sustaining (i.e. a lack of rainfall means that less moisture is available to promote additional rainfall, in a vicious cycle). In many areas, the only way for drought conditions to be significantly alleviated in the short-term would be for a discrete, long-lived, and large system (such as a tropical cyclone) to impact the area. Soil hardening due to the drought means that even if a large amount of rain falls in a short time, most of it will run off quickly causing flash floods rather than drought relief. The June 2012 North American derecho and other strong storms in late June and early July did not appear to ease drought conditions, as the rainwater ran off rapidly from the affected areas.
The drought is expected to continue and possibly intensify into the end of November for a large part of the country. Although drought/dry conditions are likely to drop at least one category level in the Southwest, Southeast, Northeast, and Northern Plains as well as portions of the Ohio River Valley, it is expected to have both short-term and long-term impacts across nearly the entire affected area.
Crops, particularly strains grown in the most heavily affected regions (such as corn and soybeans), have been noted to be failing or yielding very low this year due to the drought's presence in farming areas. This increase in cost will most likely move up the feeding chain and result in raised prices for meat, dairy, and processed food products.Food prices are expected to rise dramatically because the resulting supply shortfall. The price of farm equipment, on the other hand, is expected to decrease as farmers are forced to sell off their equipment and machinery to cope with decreased incomes.
1,692 counties across 36 states in the US have been legally declared primary natural disaster areas as of August 17 as the drought continues to cover 62% of the contiguous US. Hundreds of additional counties bordering the primary disaster areas are designated as "contiguous" disaster areas, and are also eligible for federal aid.
The drought affects Canada mainly in the east in Ontario, Quebec and the Atlantic provinces where there has been record setting heat and very little rainfall. Summer crops in these areas have been affected and the price of produce is expected to increase, particularly corn and soybean.
Concurrent and Related Weather Events
- March 2012 North American heat wave
- Summer 2012 North American heat wave
- June 2012 North American derecho
- 2012 Oklahoma wildfires
- 2012 Colorado wildfires
Other Widespread Severe Droughts
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