The Mississippi River: A Comprehensive Analysis

Categories: America Flood Geography Mexico Natural resources River Water

Analysis, Pages 5 (1250 words)

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Introduction

The Mississippi River, a prominent geographical feature of North America, has captivated the attention of scientists, engineers, and geographers for centuries. Stretching from its source in Lake Itasca, Minnesota, to its majestic culmination in the Gulf of Mexico, Louisiana, this mighty river boasts a rich history and an extensive geographical footprint. This essay delves into the geography, hydrology, and historical context of the Mississippi River, aiming to provide a comprehensive understanding of this iconic waterway.

Geography of the Mississippi River

The Mississippi River is one of the longest rivers globally, with varying estimates placing its length between 2,320 to 2,550 miles.

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Its width fluctuates dramatically, ranging from a mere 20-30 feet at Lake Itasca to over four miles at Lake Onalaska. The river's depth is equally diverse, measuring less than three feet deep at its source but exceeding 200 feet at a specific point in New Orleans. Covering an extensive watershed boundary, the Mississippi River's drainage basin is delineated by the Rocky Mountains in the West, the Appalachian Mountains in the East, and numerous lakes in the northeast.

Hydrology and Watershed Area

The hydrology of the Mississippi River is intricate, encompassing a drainage area that spans 1.2 to 1.8 million square miles, encompassing 41% of North America.

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Its watershed area begins over 1,475 feet above sea level at Lake Itasca and descends to sea level at its mouth. Tributaries, such as the Missouri River in the dry mid-west and the Ohio River in the wet highlands, significantly contribute to the river's flow.

Flooding Along the Mississippi

The Mississippi River has a complex history of flooding, categorized into three distinct levels of severity: minor, major, and extreme.

Minor Flooding

Historically, the Mississippi River would annually surpass its bankfull discharge, causing minor flooding events that resulted in minimal or no property damage but occasional public inconvenience.

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These minor floods primarily occurred in late spring due to snowmelt increasing the river's volume and heavy rainfall in the Appalachian Mountains. Engineers working on the river aimed to prevent even these minor floods, ultimately curbing their frequency through flood prevention measures.

Major Flooding

Major floods, predicted to transpire every five to ten years, stem from exceptionally heavy rainfall events, typically with a recurrence interval of once every ten years. Seasonal rainfall, in conjunction with saturated ground, contributes to the heightened risk of major floods. This level of flooding can cause extensive inundation, property damage, road closures, and necessitate the evacuation of people and livestock.

Extreme Flooding

The most devastating category, extreme flooding, is forecasted to occur approximately once every 40 years. These events may result from an exceptionally intense period of heavy rainfall, overwhelming the Mississippi's flood prevention techniques such as levees, dams, and channel straightening. The unprecedented 1993 flood, lasting over 144 days from April 1st to September 30th, exemplified the catastrophic consequences of an extreme flood.

Weather Conditions Before the 1993 Flood

Leading up to the 1993 flood, atypical weather conditions prevailed across the Mississippi River basin. Excessive rainfall, approximately 200-250% above normal levels, persisted for extended periods, often exceeding 20 days instead of the average 8 to 9 days. These prolonged heavy rains saturated the soil and swelled the river. The uncharacteristic weather patterns were attributed to warm, moist air streams from the Gulf of Mexico converging with cold, dry air from the Midwest and Canada. Condensation resulting from the collision of these air masses led to extraordinary precipitation levels.

Furthermore, a high-pressure system situated over the southeast United States obstructed the normal distribution of precipitation over the northeastern states, concentrating rainfall disproportionately over the Midwest. This unusual meteorological phenomenon exacerbated the already heightened rainfall levels in specific areas, setting the stage for the catastrophic 1993 floods.

The 1993 Floods: An Unprecedented Disaster

The 1993 floods along the Mississippi River were of unparalleled magnitude, causing widespread devastation across nine states and affecting the lives of over 930,000 people. Key statistics of the 1993 floods include:

An inundated area of 500 miles along the river channel, spanning 200 miles in width and covering 27,000 square miles of land.
Approximately 3 billion cubic meters of water overflowed the river channel onto the floodplain.
Crop destruction on 12,000 square miles of farmland, rendering some areas unusable due to the deposition of thick layers of sand, resulting in total costs of $6.4 billion.
At least 75 towns were completely submerged under water.
Flooding endured for almost 200 days in certain regions, such as the 144 days experienced in St. Louis, Missouri.
Total damage estimates ranged from $15 to $20 billion.

Human impacts were equally devastating:

52 fatalities were attributed to the floods.
74,000 individuals were forced to evacuate their homes.
330,000 people had to be rescued from roofs, trees, or high ground.

Infrastructure and economic losses were substantial:

Approximately 50,000 houses sustained damage or were destroyed.
Roads were closed down, resulting in $500 million in losses due to damage.
Barge traffic ceased for two months.
All railroad traffic halted in the Midwest.
Ten airports were flooded and subsequently closed.
Of the 1,300 levees, 1,000 failed to hold back floodwaters.
Sewage and water treatment plants were destroyed, contaminating water pipes with sewage and agricultural chemicals.

Causes of the 1993 Floods

The catastrophic 1993 floods were the result of a combination of physical and human factors, contributing to the unprecedented scale of the disaster.

Physical Causes

The vast drainage basin of the Mississippi River, covering nearly half of the United States, ensured that a substantial amount of rainwater from across the country would eventually flow into the river, increasing the risk of flooding.
The presence of significant tributaries, notably the Missouri River from the dry Midwest and the Ohio River from the wet Appalachians, brought additional water into the Mississippi, amplifying its flow during heavy rainfall events.
The extraordinary precipitation in 1993, approximately double the average, elevated the river's volume and escalated the risk of flooding.
Snowmelt from the Appalachian Mountains added to the river's flow.
Excessive rainfall led to saturated ground conditions, causing rainwater to run off rapidly into the river rather than infiltrating the soil.
Short, intense storms, characteristic of the 1993 weather patterns, generated high runoff rates, resulting in a sudden surge of water into the river.

Human Causes

The straightening of the river course, achieved by cutting through meanders to expedite discharge, increased the potential for flash floods, where sudden downpours in specific areas could cause rapid, severe flooding.
Levees, while constructed to prevent flooding, sometimes exacerbated the situation by isolating natural flood buffers like wetlands and floodplains. Levees also hindered the flow of water from outside the river channel back into the river.
The collapse of levees could lead to disastrous flooding as the sudden release of pressure within the channel allowed water to spread into the floodplain. Moreover, levee debris could accumulate in the riverbed, elevating its level over time.
Deforestation to accommodate urban growth reduced transpiration and increased the risk of erosion.
Farmland, with its organized rows of crops, proved less effective at retaining water compared to natural vegetation with random root growth patterns, contributing to rapid runoff to the river.
Urban development, featuring impermeable asphalt surfaces on roads, accelerated surface runoff, causing water to reach the river quickly, especially during storms.

Summary

The catastrophic 1993 floods along the Mississippi River, despite its rarity, exposed the intricate interplay between natural and human factors in shaping the river's hydrology and flood dynamics. While the Mississippi River has been tamed to a certain extent through engineering and flood prevention measures, the 1993 floods demonstrated the unpredictability and potential consequences of extreme weather events and human interventions. The ongoing debate continues over whether the benefits of controlling the river outweigh the risks, with the Mississippi remaining a formidable force of nature that refuses to be completely tamed.

The Mississippi River: A Comprehensive Analysis. (2021, Jun 02). Retrieved from https://studymoose.com/mississippi-river-located-north-america-begins-lake-itasca-minnesota-flows-south-ending-gulf-mexico-louisiana-new-essay