 |
U.S. Drought
|
The data presented in this
drought report are preliminary. Ranks, anomalies, and percent areas
may change as more complete data are received and
processed.
National Drought Overview
The year began
drier than average across a broad swath of the country from the
Southwest to the Great Plains, across much of the Gulf
Coast, and into the coastal Southeast. Above average
precipitation continued to erode the drought areas in the
Pacific Northwest. This pattern continued throughout the spring and
into the summer. By
fall,
drought was concentrated in the Plains, especially in Texas and
Oklahoma. By the end of the
year, drought subsided in much of the Southeast, but was
prominent across parts of the Plains. The U.S. Drought
Monitor depicts conditions at the end of the year.
Several short-lived dry episodes occurred in other regions
throughout the year, notably in the mid-Atlantic in February and
March, the Northeast coast in March, the
Pacific Northwest in July and
August, and Florida
for
much of the year. The percent area* of the contiguous U.S.
experiencing moderate to extreme drought grew steadily from 20
percent in January to a peak of about 52 percent by July, then
declined during the second half of the year. |

 |
|
*This drought statistic is based on the Palmer Drought Index, a
widely used measure of drought. The Palmer Drought Index uses
numerical values derived from weather and climate data to classify
moisture conditions throughout the contiguous United States and
includes drought categories on a scale from mild to moderate,
severe and extreme. |
| The most extensive
national drought coverage during the past 100 years (the period of
widespread reliable instrumental records) occurred in July 1934
when
80 percent of the contiguous U.S. was in moderate to extreme
drought. Although the current drought and others of the 20th
century have been widespread and of lengthy duration, tree ring
records indicate that the severity of these droughts was likely
surpassed by other droughts including that of the 1570s and 1580s
over much of the western U.S. and northern Mexico. |
Regional Drought Overview
| Impacts from this
year's drought were felt especially hard by the agricultural and
hydrological communities. Low
streams, reservoirs, and stock ponds and
depleted soil moisture ravaged
pastures and
rangeland throughout the Plains, and
numerous wildfires prompted governors and the USDA to declare
drought disasters in parts or all of several states in the middle
of the country. The South Platte River was nearly dry during the
summer, low water levels in the Mississippi and Missouri Rivers
forced an early end to barge transportation, several municipalities
imposed water use restrictions, livestock was prematurely sold,
crops died before harvest. In many areas, such as in South Dakota
and Nebraska, recovery of grazing lands from drought is not
expected for at least two years. |

 |
| In the Southeast
summer drought impacted agriculture and water supplies. The pecan
crop was small, but of higher quality, corn and soybean yields
dropped by about 10 percent from 2005, shallow rooted ornamental
trees such as dogwoods suffered, forage decreased, hydropower
production was reduced, and water use restrictions were imposed. By
the end of the year,
Florida had experienced the second driest December-November in
the 111-year record. |
 |
| The western Great
Lakes region experienced low grass seed production because of
drought and high temperatures, dying fish in the Minnesota lakes,
decreased forage production, dying of Christmas tree saplings and
wildfire hazards. Minnesota had the fifth driest May-July in the
112-year record. A positive impact of the drought was increased
business by repair facilities caused by boats that sustained damage
while in lakes with low water levels. |
 |
| The year ended with
back-to-back major winter storms across the Great Plains. Heavy
December snow and rain brought drought relief to the central High
Plains and adjacent Colorado Rockies. Dry conditions prevailed
during the month across the central Appalachians and parts of the
Southwest. By the end of the year, mountain
snowpack was below normal across much of the Southwest and
central Rockies. |
 |
Pre-instrumental Drought Perspective
Tree ring records
provide a useful paleoclimatic index that extends our historical
perspective of droughts centuries beyond the approximately 100-year
instrumental record. Several paleoclimatic studies have shown that
droughts as severe or worse, both in magnitude and duration, than
the major 20th century droughts have occurred in the U.S. during
the last thousand years. The following paleodrought reports have
been prepared by the NOAA/NCDC Paleoclimatology
and Climate
Monitoring branches during 2006:
|
Citing This Report
NOAA National Centers for Environmental Information, State of the Climate: Drought for Annual 2006, published online January 2007, retrieved on May 26, 2021 from https://www.ncdc.noaa.gov/sotc/drought/200613.