Complete Project 3.2 – Localized Hazards

Question #2: Complete Project 3.2 – Localized Hazards – on pages 105-106 of your text.
Harris County, which covers 1,778 square miles (US Census Bureau), is situated on the upper Gulf Coast in Southeast Texas. It is limited by Waller County on the north and west, Montgomery County on the north, Liberty and Chambers Counties on the east, Galveston and Brazoria Counties on the south, and Fort Bend County on the west. Harris County’s southern half is level seaside prairie and the northern half touches the moving East Texas timberlands. Focal Harris County is 55 feet above ocean level. The area rises slowly to more than 200 feet on the northern outskirts, while the smallish feigns around upper Galveston Bay slide to ocean level. The dirt is substantial dark seaside earth in the south and sandy soil north of Buffalo Bayou. Local trees incorporate pine and such hardwoods as oak, fiery debris, and hickory. The normal yearly precipitation in Harris County is 48.19 inches, and the mean temperature is 69.6 degrees F. Harris County is truly subjected to a tropical storm sway by and large like clockwork, any of which can be calamitous because of its vicinity to the Gulf Coast. The province has the potential for other characteristic catastrophes too, especially flooding.
Flood
Flooding is the most regular and excessive normal risk in the United States, bringing about more than 10,000 passings since 1900. (U.S. Water News Online, 2000) Historically, almost 90 percent of presidential debacle presentations result from surge related occasions. (FEMA) Floods are by and large the consequence of unnecessary precipitation, and can be grouped in two general classifications: general and streak surges. General surges are characterized as precipitation over a given waterway bowl, while streak surges are the result of overwhelming confined precipitation falling in a brief span period. The seriousness of a surge occasion is dictated by the accompanying attributes: a blend of stream and waterway bowl geology and physiography; precipitation and climate designs; late soil dampness conditions; and the level of vegetative clearing. The intermittent flooding of terrains adjoining waterways, streams, and shorelines is a characteristic and inescapable event that can be required to happen based upon built up repeat interims. The repeat interim of a surge is characterized as the normal time interim, in years, expected between a surge occasion of a specific greatness and an equivalent or bigger surge. Surge greatness increments with expanding repeat interim.

Need Help Writing an Essay?

Tell us about your assignment and we will find the best writer for your paper.

Get Help Now!