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| The 2003 national drought affected different regions at different times. The year started with a very dry January in the southwestern and southeastern quarters of the nation. Persistently below-average precipitation in the Upper Mississippi Valley and Great Lakes region during the winter resulted in record (Minnesota) or near-record dry November-March ranks for several states. The West region (California-Nevada) experienced subnormal precipitation during the last half (January-March) of their wet season. | ![]() |
| Spring was very dry in the southern Plains, with Texas experiencing the driest March-May in the 109-year record during 2003. |
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| Unusually dry and warm conditions during the early summer to early autumn months exacerbated drought in the West and central to northern Plains, resulting in the expansion of the national drought area. The Northwest, Southwest, West North Central, and East North Central regions were especially affected. Several states had precipitation ranks in the top ten driest category for May-September, July-October, and August-October. The drought severely impacted pasture and rangeland, streamflow, and soil moisture in several states. A meager winter snowpack and below-average precipitation across much of the western mountains failed to recharge depleted reservoirs and set the stage for an active wildfire season in the West. But for the year, the number of acres burned across the US was near average. | ![]() |
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| At year's end, moderate to extreme drought covered approximately 56 percent of the western states from the Rockies to the Pacific coast. During the peak of the 2003 drought, about 80 percent of this region was affected, which rivals the extensive drought area of the worst 20th century droughts. A major late winter storm dumped near-record snowfall on parts of the central Rockies, bringing snow water content to near or slightly above average, and a series of winter storms late in the year brought above-average rain and snow to parts of the West. Short-term relief resulted from these systems, but the moisture deficits in the West were so great from three to five years of drought that many more months of above-average precipitation are needed to end the drought in much of the region. |
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| More detailed information on drought during 2003 can be found on NCDC's monthly climate summary pages. |
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 branchs during 2003:
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For all climate questions other than questions concerning this report, please contact the National Climatic Data Center's Climate Services Division:
Climate Services DivisionFor further information on the historical climate perspective presented in this report, contact:
NOAA/National Climatic Data Center
151 Patton Avenue
Asheville, NC 28801-5001
fax: 828-271-4876
phone: 828-271-4800
email: ncdc.info@noaa.gov
Richard Heim-or-
NOAA/National Climatic Data Center
151 Patton Avenue
Asheville, NC 28801-5001
fax: 828-271-4328
email: Richard.Heim@noaa.gov
Jay Lawrimore
NOAA/National Climatic Data Center
151 Patton Avenue
Asheville, NC 28801-5001
fax: 828-271-4328
email: Jay.Lawrimore@noaa.gov
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