Excerpts from:
Precipitation in the Upper Mississippi River Basin,
January 1 Through July 31, 1993

K.L. Wahl, K.C. Vining, and G.J. Wiche.
U.S. Geological Survey Circular 1120-B

Abstract

Excessive precipitation produced severe flooding in a nine-State area in the upper Mississippi River Basin during spring and summer 1993. Following a spring that was wetter than average, weather patterns that persisted from early June through July caused the Upper Midwest to be deluged with an unusually large amount of rainfall. Monthly precicitation data were examined at 10 weather-station locations in the flood-affected region to illustrate precipitation patterns and amounts in the flood-affected area. In 1993, all 10 of the selected locations received greater than the normal rainfall for January through June 1961-90, 8 of the 10 locations receiced more than 200 percent of the normal rainfall for July 1961-90, and 3 received more than 400 percent of the normal rainfall for July. (The average rainfall for any given 30-year period is termed the "normal" rainfall for the given period.) May through July 1993 was the wettest or nearly the wettest such period on record at many locations in the flooded area. Of the 10 locations, 6 received more rainfall in the first 7 months of 1993 than generally is received in a year.


INTRODUCTION

This report, one of a series that documents the effects of the 1993 flooding in the upper Mississippi River Basin, covers precipitation in the upper Mississippi River Basin from January 1 through July 31, 1993. As of August 1993, large storms continued to pass through the affected area; however, weather conditions indicate that the widespread flooding might be coming to an end. The floodwaters in the Mississippi river crested at St. Louis, Missouri, on August 1, while the river stages along the mainstem and on the principal tributary streams upstream from St. Louis were receding.

This report provides a general overview of the usually excessive precipitation that produced severe flooding in a nine-State area in the upper Mississippi river Basin (fig. 1) during spring and summer 1993. A general overview of precipitation during the first 7 months of 1993 is presented.

Preparation of this report required cooperation among many persons in many organizations. The authors are particularly appreciative of the cooperations of State Climatologists and of persons in various State agencies and in the offices of the National Weather Service, National Oceanic and Atmospheric Administration, for making provisional data and maps available on a near real-time basis.


PRECIPITATION, JANUARY 1-JULY 31, 1993

General precipitation conditions throughout the nine-State area of the upper Midwest for the 7-month period ending in July are best summarized by the following news item from the Associated Press, July 17, 1993:

The rain, of course, was the problem. Although much of the spring downpour fell on vast undammed tracts and could not be contained, the real culprit was the volume dumped by stalled weather systems. With the ground already saturated by spring rainfall, June was the wettest month in the regions since record keeping began. July was just as soggy.

The Associated Press statement was accurate when written in mid-July but proved to be conservative. July ended up being much soggier than June.


Monthly Precipitation

Annual precipitation over the nine-State area affected by the flooding (fig. 1) generally averages more than 30 inches but ranges from about 16 inches in south-central North Dakota to about 40 inches in southern Missouri. Although precipitation is about evenly divided between the first and last halves of the year. Normally, 45 percent of the annual precipitation falls between April 1 and July 31; June precipitation represents about 15 percent (2-5 inches) of the average annual precipitation total.

Figure 1: The Mississippi River Basin and general area of flood streams, June to August 1993.

Precipitation amounts recorded throughout the upper Mississippi River Basin during the first 7 months of 1993 generally were substantially greater than normal (January-July 1961-90). Although April-through-July precipitation was much greater than normal. little evidence early in the year indicated that precipitation amounts in 1993 would be above normal. January-through-March precipitation in the States of the upper Mississippi was near normal to slightly above normal. Because precipitation for those 3 months is often in the form of snow and generally total less than 6 inches of moisture, potential flooding caused little concern. However, that situation began to change in April.

Precipitation in April and May over the area ranged from near normal to much greater than normal, but the areas of greatest precipitation differed for the 2 months. April rainfall was nearly twice the normal amounts in parts of Wisconsin and in Missouri but was only moderately above normal in much of the remainder of the flood-affected area. By contrast, May rainfall was more than twice the normal amounts for the month over an area that extended from southeastern South Dakota across Iowa to eastern Kansas. The largest storms, though, were still to come.

In early June, a weather pattern (fig. 2) developed that was characterized by a strong low-pressure system over the Western United States and a corresponding large high-pressure system positioned over the Southeastern United States. The jetstream dipped south over the Western United States and flowed northeasterly across the upper Midwest. A southeastern high blocked the eastward movement of storms, thus creating a convergence zone between the warm, moist flow from the Gulf of Mexico and the much cooler nd drier air from Canada, which resulted in thunderstorms. This pattern persisted through most of June and July (National Weather Service, 1993). As a result, the upper Midwest with this convergence zone was deluged with rain while the Southeastern and the Eastern United States from Alabama to Vermont, under the influence of the high-pressure system, was very hot and dry. Slight movements in the atmospheric pattern determined the timing and location of the excessive rainfall throughout the upper Midwest.

Figure 2: Dominant weather patterns over the United States for June through July 1993.

The persistence of this weather pattern caused unusually large amounts of rain to fall over the upper Midwest. These large amounts and the wetter-than-normal spring produced flooding throughout the upper Mississippi River Basin, including the lower Mississippi River Basin. The rains were extraordinary in the areal extent and in the amounts accumulated in the first 7 months of the year. Precipitation for the first 7 months totaled more than 20 inches over most of the flood-affected area and was more than 40 inches in areas of northeast Kansas and east-central Iowa (fig. 3a). Most of the area received from 150 to 200 percent of the 1961-91 normal amounts for January through July (fig. 3b).

Figure 3. Areal distribution of total precipitation in the area of flooding in the upper Mississippi River Basin, January to July 1993.
(Left) A: In inches (Right) B: In percentage of 30-year normal for January through July 1961-90.